PROGESS RPTS FEBRUARY 1971 TO MAY 1973 - Geology ...

JVL JJ.NPORCUPINE A 42A i4SWee26 63.4827 CRAWFORD

INTER OFFICE CORRESPONDENCE

Attention: W.P.Hammond Date: February 15,19?1

Re: Exploration Program, Abitibi Option* Crawford Township, Ontario.

l have attached several plan dealing with Crawford Township most of the land In whloh Is Included in our Abitibi Option agreement* George's compilation (Figure 1) shows the general geology of the area the most striking feature of whioh is the body of ultrabasic rook located in the east central part of the township* Aeromagnetic contours in the ultrabasic area have been pencilled onto George's nap and some leeway is apparent as to how one might Interprete the extent of this intrusive body* Books to the south and west are largely felsic in character. This plan shows all of the known holes drilled in Crawford Township* Most of them were put down by INCO and scattered low values in Elno, copper and nickel are reported* The more interesting base metal intersections are tabled below, corresponding to the numbered locations circled in red on both of the accompanying maps*

1. Hole 2701? intersected 20.0 feet whioh assayed 0.41 percent zinc and 0.20 ounces silver per ton. Material conelets of graphitic tuff interbedded with andesite and tuffite*

2. Hole 25049 intersected andesite, tuff, chert and rhyolite whioh showed the following separate Elno sections*

it

5.0 0.355.7 0.308.3 0.46

3* Bole 25029 was drilled here and intersected 2*7 foot whioh assayed 0.44 percent copper*

4. Bole 25037 encountered interbanded andesite and graphitic schist whloh assays up to 0*43 percent copper across 4.5 feet.

5. Hole 27023 intersected andesite, peridotite, rhyolite flow breccia and dacite. The volcanic material assays from 0*05 to 0.20 percent Elno. One section of rhyolite flow breccia assayed 0*40 percent zinc across 15*5 feet.

POROUPINK MINES LIMITED


Attention: Date:

Re: Page tWO '

6* Bole 27005 collared Into peridotite which averages 0.20 percent nickel and bottomed in a pyrrhotite rich rhyolite.

7. Boles 25050 and 27095 intersected peridotite which assays from 0.25 to 0.40 percent nickel. Bole 27095 striking to the south averages 0*3** percent nickel over 775.0 feet* The sulphide content is very low.

The foregoing indicates that there are several areas in Crawford Township where further exploration can be considered.

A second map (Figure 2) shows the land (unooloured) in Crawford Township which is included in the Abitibi Option. Other patented land is shown coloured pink while Crown Land is coloured green. Bart of the Crown Land is presently staked. Several sections are narked out on the plan where useful exploration can be carried out.

ie A INCO traced out a strong non magnetic conductor here which Ls closed off at the east end. The eone is open towards the power line, the presence of which may account for the lack of an Input response in this area.

Zone B The INCO airborne and ground work shows a continuous conductive zone crossing the entire township. This eone was tested by 4 diamond drill holes 3 of which intersected some base metal value as listed. The section coloured blue was surveyed last aumuor as covered by a Shield report dated July 23,1970 and my memorandum dated August 4,197ft. The southeast corner of the block straddles the north contact of a body of ultrabasic rook.

Zone C The ultrabasic intrusive in this area is zoned with serpentinite predominating to the south and gabbro to the north. The serpentinite is rich In nickel, this being a constituent metal in the rook itself. The felsic rock flanking the body to the south was tested by one drill hole which shows abundant pyrrhotite (log for Bole 27005 appended).

MPINTYREPORCUPINE MINES UMITED


Attention: Date:

Re! page three

Exploration Program

Further work Is warranted In the sectors described above* This is based on the base metal values present and on the apparent cursory nature of previous exploration in the area* A high resolution GSC aeromagnetic survey of this area IB expected to be released shortly and it Is hoped that this information will define the picture with respect to magnetic bodies lying within or near Zones A and fi* An exploration program in Zone C is outlined below.

Zone C

This area can be considered to have BOBS potential for important nickel mineralization* This metal is a prominent constituent of the south part of the ultrabasic intrusive present here and there is evidence that the host rook to the south is rich in sulphur* A concentration of nickel sulphide near the ultrabasic contact is a reasonable possibility according to certain authors on this matter (Naldrett et al)* XNCO plans show an airborne conductor they have identified as 4-149 (Figure 2). The available information indicates that this particular conductor was not searched for or explored on the ground* An untested Input anomaly is also shown on Figure 2* No Input was recorded in the INCO 4*149 area and this is possibly due to power line interference.

A ground surveyvis recommended to grid the area straddling the south contact of the ultrabasic body* This area is blocked out and shaded yellow on the accompanying plan (Figure 2).

AS/ A.Skreoky

INTER-OFFICE CORRESPONDENCE

ATTRITION55 YONGE STREET. TORONTO. ONT.

O.E.HicksDATE May 10,1971

SUBJECT Exploration Program,Abitibi Option,Crawford Township, Ontario,

An accompanying plan shows the results of a magnetometer survey recently completed in Crawford Township, The main anomaly is due to serpentinized peridotite which was tested by several INCO drill holes.

Bradshaw shows a magnetic tongue protruding to the south west. There is an unusual pattern on the south part of line 1200 East. There is rwason to question the anomaly pattern shown in the area blocked out on the accompanying plan. Bradshaw points out that the survey was tied to the baseline which lies in a highly magnetic zone.

Would you arrange for a helicopter trip to the area to check out the magnetics, l particularly wish to confirm the tongue like feature indicated as well as the local highs on line 1200 East. Please note any topographical features as the magnetic pattern suggests that shallow overburden is present.

-^^AS/ A.Skrecky

MCINTYREPORCUPINE MINES LIMITED


Attention: W. P. Hammond Date; May 12,1971

Re: Exploration Program, Abitibi Option, . Crawford TOwnship, Ontario*

l have attached a copy of Bradshaw'B report on the magnetometer and electromagnetio surveys recently completed in Crawford Township. Nine separate conductors were picked up in this work. These hay* been plotted on the ooloured Magnetometer survey plan accompanying the report*

INCO drilled 4 holes in the north part of the survey area. Three of these holes are shown on an appended section. Gabbro and serpentinlEed peridotite were intersected with a progressive increase southward in the nickel content of the rook. HfCO plans note "no explanation 11 for the conductivity that they Measured. It seems likely that the effects obtained in the main magnetic anomaly area are due to a serpentinization of the rook. A drill hole on the west side of the survey area bottomed in a pyrrhotite rioh rhyolite.

Conductor A corresponds to an untested isolated Input anomaly (Anomaly 365W). Thsraxia displays a marked shift On the ground, depending on the transmitter location and this feature remains unexplained at present. There is an unusal magnetlo pattern in this area with a prominent unexpected north east trending anomaly present. Local highs in the south part of the survey area suggests shallow overburden.

There is reason for us to run a ground check to oonfIra the magnetic pattern indicated by the Bradshaw survey. This work has now been scheduled* Additional survey work may be necessary in the south part of the sheet*

AS/ A.Skreoky


ATTMKTION OF O.E.Hicks

55 YONGE STREET. TORONTO. ONT.

FEWOnDATE May 18,19?1

SUBJECT Geophysical Surveys

Field notes are often needed for reference purposes and in any event should be kept on file with the particular Job involved.

Would you establish a practice to leave this material with the summary sketches that you prepare. Notes should be complete as to the job, location, date and type of survey carried out. They should include any observations made during the traversing with respect to the type of terrain that is present as well as any topographical features.

AB/ A.Skrecky

TERINTER-OFFICE CORRESPONDENCE55 YONGE STREET. TORONTO. ONT.

DATE May 19, 1971

ATTENTION OF ,. ~ ,,W.P.Hammond

SUBJECT Progress Heport, SUBJECT Exploration Program,

Abitibi Option, Crawford Township, Ontario.

An attached overlay shows the results of reoent magnetometer work which was carried out to check on the results of a survey previously reported on by Shield Geophysics, Limited.

The isolated magnetic highs on line 1200 Batt were not picked up in the check survey and some ohange is apparent with respect to the shape of the magnetic anomaly on line 400 Bast* This feature now appears as a concentration of magnetic minerals which is separate from the serpentinite known to occur to the north.

Some conductivity has been measured in this area with the conductor axis as plotted. Technical problems are apparent with respect to the MoPhar V.E.M. survey work that has been carried out so far. Conductor C, as an example, cane through as a definite cone in the reconnaissance V.E.M. work and faded considerably when the detail work was carried out. The axis for Conductor A shifts a considerable distance when measured from different transmitter locations. Some of the effects can be credited to a ghosting through a localized conductive mass.

These features along with the presence of a power line just to the west, lessens the usefullness of V.E.M. equipment for detailing the Eones present in the area. There is a reasonably good chance that isolated magnetic anomalies lying south of the serpentinite sill would be due to concentrations of pyrrhotite. This mineral is common in the rholite intersected by an XNCO drill hole at the west end of the survey area, l propose to continue a magnetometer reconnaissance in the area marked on the appended overlay* A formal survey will be considered if other isolated magnetic anomalies are picked up* Our minimum follow up, at this stage, will consist of an IP traverse along line 400 Bast.

AS/ A.Skreoky

iINTER-OFFICE CORRESPONDENCE55 YONGE STREET, TORONTO. ONT.

DATE Kay 26, 1971

ATTENTION OF W.P.Hammond

Exploration Program, Abitibi Option, Crawford Township, Ontario t

A reconnaissance magnetometer survey has been completed Over an area west of the Isolated magnetic anomaly reoently outlined just south of a prominent ultrabasic mass in Crawford Township* An appended field sketch shows the results of this work. Only one satellite magnetic anomaly la indicated in the survey area, on line 400 Bast as shown* The tongue like feature on line 1600 West can be looked Into further if the main anomaly proves to be important*

The reconnaissance work was undertaken by Shield Geophysics Limited who were in the area to check out previously reported magnetic highs on line 1200 East. Bradshaw feels that a loose cable connection accounts dor the original survey results on that line.

The appended field plan also shows the results of the MoPhar V.E.M.survey over lines O to 1600 Bast inclusive. A shift in the axis of Conductor A can be explained by a southerly dip and an easterly rake for the conductive zone. Evidence at hand indicates that the conductor is related to the satellite magnetic body and that it is a valid drill target. A drill hole is recommended as shown.

Additional field work is being considered in the Conductor B area (see Shield Geophysics Limited report). This moderate strength conductor was picked up from two separate transmitter set ups and its persistence is In marked contrast to the survey results obtained for Conductor C. Conductor C was drilled by XnCO and while niokeliferous material was intersected, no explanation was obtained for the measured conductivity. A traverse with IP equipment is recommended. This should establish if significant sulphides are present.

AS/ A.Skreoky

PER-INTER-OFFICE CORRESPONDENCE55 YONGE STREET. TORONTO. ONT.

DATE

ATTENTION OF

SUBJECT pagft two

Technical Details and Estimated Cost for Tfre Proposed Diamond

Drilling Program

Drill Hole No. 90^71-1 (Crawford) location line 400 East

3100 South

dip - 60 o length 650 feet

gat ittft ted Cost f or, TDianondT IDrillJinft Fyograa

mobilization of equipment ( k miles ) | 1,500.00easing overburden 100 feet f 1,000.00AQ wireline 500 feet d 15.25 / foot S 2,900.00geology and sampling s 700.00transportation E 300.00oontingenoies f 600.00

total estimated eost | 7,000*00

AS/ A.Skreoky

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INTER-OFFICE CORRESPONDENCE55 YONGE STREET. TORONTO, ONT.

DATE July l, 1971

ATTENTION OFW.P.Hammond

Exploration Program,SUBJECT jnput 355 y ^^

Abitibi Option, Crawford Township, Ontario*

l have attached a log for the drill hole recently completed in Crawford Township* This hole tested Input anomaly 365* which had been earlier detailed by a ground survey. The Moderate BM anomaly outlined here lies at the south edge of a small isolated magnetic anomaly* These features in turn lie about 1500 feet south of a large body of niokeliferous serpentinite*

The BM anomaly was found to be caused by graphite* Core recovery was particularly bad in the anomaly area - no important mineralization however, was noted in the recovered material* There are no magnetic minerals present in the rook types intersected by the drill hole and the magnetic anomaly remains unexplained.

AS/ A.Skreoky

October 17.1972

W. P. Hammond

Exploration Program, Ultrabasic Bock Complex* Mcintyre and Abitibi Option land. Bast Central Crawford Township, Tlamins Area* Ontario*

The east central part of Crawford Township Is marked by a major centre of basic Intrusive activity. This is expressed on aeromagnetic maps by a cluster of strong magnetic anomalies. There ara five principal concentrations of magnetic minerals In this area. These are numbered on an attached 1320 seal* plan of Crawford Township and ara covered by the following comments*'

P The main part of this magnetic anomaly Hep on Crown land,

rilled one hole here years ago and found Interbanded gabbroand peridotite*

Zone 2 This eone Iles mostly on Abitibi land.1 It has not been explored in any way to our knowledge*

Zone 3 This east-west striking magnetic anomaly lies wholly on Abitibi land. IKCO drilled a 1*978*0 foot long hole into the oast end of the zone* This hole collared into felsic volcanics, intersected serpentinlEed peridotite and bottomed In gabbroic material. The peridotite assays about O .'30 percent nickel and the gabbro shows trace amounts of this metal**

Most of this zone lies on Abitibi land and has been Explored with 4 diamond drill holes* This drilling shows that the

anomaly consists of a basic intrusive having a northerly gabbroic phase and a southerly section of serpentiniced peridotite. Books Immediately south consist of rhyolite showing fair barron pyrrhotite* The gabbro contains a trace of nickel mineralieation while the peridotite averages 0*35 percent nickel (see accompanying drill section). Only a small part of this nickel is In the form of a nickel sulphide*

Zone S This eone lies on Mcintyre and Abitibi land and has not boon explored on the ground to date** The cone ehowe a general north-south trend and in this way Is distinctly different froa other embers of the ultrabasic complex described above* There is evidence that this magnetic body truncates against generally east-west striking volcanic rooks lying Just to the west. The west margin of the basic intrusive seems a likely area for major fracture tones where ore concentrations might be expected. LlneouttIng will be scheduled here at an early date following which geophysical surveying will be carried out.

AS/ A.Skreoky

INTER-OFFICE CORRESPONDENCE55 YONGE STREET, TORONTO. ONT.

DATE February 13, )V

ATTENTION OF Wayne R. 7wickey

SUBJECT Magnetometer Survey andInduced Polarization "lest work,Mining Claims P. 353544 - 47 and Abitibi Opfion,Lot 6, Concessions 3 and 4,Crawford 'J own ship, Ontario.

We have completed a magnetometer survey along with test induced polarization traversing over pans of .Lot 6, Concessions 3 and 4, Crawford 'township. The northerly part of the survey area covers 4 mining claims staked by Mcintyre last spring. Part of the survey grid lies on patented Abitibi Option land.

The survey area straddles a prominent r orth-south trending magnetic anomaly believed to be due to se rpentinized peridotite. There are no rock outcrops in the area where the overburden is believed lobe ir. excess of 120 feet deep.

I have plotted and coloured chargeability data on a Magnetometer Survey map of the area (Figure 1). The following is an outline of the results of the geophysical survey vork carried out here to date.

1. Line O was traversed with IP equipment to check out the following features.

(a) The Input survey flown over the Township early in 1972 indicated a north-south striking conductor at about 1700 West on Line 0. No response was obtained here by the IP work.

(b) Ground V. E. M. work a number of years ago detailed at 200 foot wide north-south striking conductor at 700 feet east on line 0. Diamond drilling had been recommended here at that time by a geophysical consultant. The V. E. M. feature may be related to a weak resistivity low centred at 350 East. There is no associated chargeability and our IP work tends to discount the value of this conductor.

(c) Induced polarization traversing was continued e.ast on line O to explore the north part of an interpreted sill of serpent] nixed peridotite. Moderate chargeability was measured here together with somewhat lower resistivity. The chargeability is probably due to minerals within the peridotite sill. Peak chargeability lies east of the magnetic high indicating that the peridotite sill dips to the cast.

INTER-OFFICE CORRESPONDENCE55 YONGE STREET. TORONTO. ONT.

DATE

ATTENTION OF

SUBJECT Page two

2. The induced polarization work carried out. on the north-southbase line traversed two Input anomalies which are expressed by weak chargeability centred at 2500 South and 3800 South. Both features correspond to resistivity lows indicating conductive material. INCO drilled a number of holes in 1966, one and a quarter miles to the west where graphite pyrite zones were intersected. The most northerly /.one, centred at 2500 South on the base line strikes fair east where it intersected and underlies the peridotite sill.

3. The induced polarization traverse on line 2400 South shows achargeability centre just east of a magnetic high, supporting an interpreted easterly dip to the peridotite sill. The resistivity low (R-l) outlined in this area is likely associated with conductive material underlying or at the base of the sill.

4. A number of I\odwell holes were drilled in the southerly part of the survey area last summer. These holes tested the Till and Bedrock along a section which was to include set ups on the interpreted sill of serpentinized peridotite. Bog like conditions were encountered at the north end of the traverse where we were forced to abandon the sampling program. Hole G-4 has been tied to our picket line grid and we are continuing a search for the other drill sites. The appended map . (Figure 1) shows hole locations, depth of overburden and bedrock geology. The geochemistry of till and bedrock material in this area shows mainly background values. A 32 foot section of Muddy Till in hole G-5 shows abundant particles of pyrite. The nearby chargeable zone is believed to be the source point for this material. A study of the till fraction in hole G-5 does not show any rock fragments that can be related to the nearby strong magnetic anomaly. This indicates an east of South glacial movement.

ConclusionsAn area at the base of the interpreted peridotite sill, near

line 2400 South, remains of interest to us as a possible centre for a concentration of economically important minerals. Further geophysical work is being considered at this particular location.

A. Skrecky. AS/rr

X/-/-/

EXPLORATION AORBEMBNT WITH AMAX SMOOTH ROCK FALLS FREEHOLD LESS CARNEGIE,

LUCAS AND CRAWFORD TOWNSHIPS HELD BY CROMARTY UNTIL DECEMBER 31/73^^^

AHAX arc definitely interested in Smooth Rock freehold, especially the Southern portion now held by Cromarty, and will enter lato an agreement roughly as follows only if they obtain at least one-half in 1974 of Townships now held by Cromarty and a first refusal on the balance.

We therefore have to decide now what our policy will be with Cromarty, i.e. do we give then another extension (already on a two-year extension to end of December 31/73)1 For all or half or a few square miles? Our Cromarty deal is a 491 share for Abitibi with no contribution by Abitibi for exploration expense, but we can be watered down to 9.8X if we do not put in Capital. AMAX have an office with four geologists in Timmins and could be a better bet in the long run.

AMAX prepared to apend #100,000 in three years from l January/ 73 on land now open, and assuming they get one* half of ground now held by Cromarty on l January/74 they will spend 550,000 more on exploration in two years. If they get the last half of ground now held by Cromarty will spend S 75, 000 on it in the year they get it (want option on it) - total S225, 000.

3. By the end of the exploration period (or at any time in it) AMAX could possibly designate one or more four square mile areas on which they would agree to apend a minimum of S^SO.OOO/year for three years or total of ^500, 000 on each area. (Includes what was originally spent on each area on exploration.) If $500,000 not spent they have no further interest in that specific four square mile area if they do they want a 12 VX interest in the land.

Their percent interest to be built up to 51X at a rate of 17. for each 517,500 spent their contribution 31,173,730 (AMAX said $ l, 200, 000) at that point and Abitibi to contribute funds on 49 X basis from that point. Orebody might or night not be outlined at this ttae or it might be outlined but not economical to develop until metal prices or technology change . AMAX insistent that they must have SIX interest in the piece of land involved (4 sq. m.) without a production commitment.

- 2 -

AMAX have dropped request for rights to 517. of land forever and will agree to a 20-year terra if we agree they could take up to the- full 20-year term to bring unit into production, i.e. spend balance over $500,000 at any time up to say year 18 (two year* to get into production).

4. Abitibi asking for 257. minimum retained interest if we do not elect to contribute 49fc of funds over 31,173,750, as it could be a marginal operation requiring Abitibi guaranteeon loan.

5. Hither party might want to hold their retained interest and let the other party go ahead with exploration (if any) over $1,1?3,750, plus cost to put into production. In our case the minimum retained interest we want is 25Z and theirs is 12tff if they have only spent $500,000 and proportionally more depending on what they have spent. Party that wants to go ahead would be responsible for raising capital and would be repaid after debt retired for expenditures beyond ?1,200,000 for AMAX and zero for Abitibi.

6. Bill James unable to say at this time which is better deal for Abitibi, Cronarty for three Townships or AMAX for whola area including the three Townships (assuming they end up with all). Canex were interested in the northern portion alone but we held out for 307. retained interest if we did not put money into exploration after $12,000. Canex offered 257. only.

Croraarty have another year to go but do not appear to be very active--probably due to lack of funds. AMEX could bring in funds plus a new approach and l would favour a deal with them on land now free, plus one-half of land now held by Cromany when available l January 1974. Cromarty could then retain balance for year or two if they would remain active and spend money.

7. AMAX insistent on Joint venture arrangement and Denver have not yet approved above deal in detail.

B. Decision required on what we do re Cromarty and are weprepared to spend money on exploration after $1 I 200,000 has been spent? The minimum retained Interest of 25X providesan out.

KEECostello/sw

cc; T. J. Bell W.S. Rothwell vb. Nay smith C.H. Rosier J.E. Maire W. James

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PATERSON, GRANT S WATSON LIMITEDr ***-

i \ formerly: an Paterson & Associates Limited / Consulting Geophysicists

i . ' Suite 2306, The Simpson Tower, 401 Bay Street, Toronto 103, Ontario, Canada. (416) 363-4261. Cables: Norquest. i

Norman R. Paterson, Ph.D., P.Eng.Roger K. Watson, R.A.Se., P.Eng. Fraser S. Grant, Ph.D., P.Eng.

March 21, 1973.

Mr. Alec Skrecky,Mcintyre Porcupine Mines Ltd.,Schumacher,Ontario.

RE: GROUND GEOPHYSICAL SURVEYS, TIMMINS AREA

Dear Alec:

This is further to our telephone conversation concerning several of the anomalies currently being followed up in Crawford, Carnegie and Lucas Townships.

Anomaly 5

I received your data on this anomaly today. As mentioned in our earlier letter, your present coverage is confined to the northwestern portion of this conductor, whereas we feel that the southeastern portion is more favourable. Nevertheless, there are one or two points that emerge from the data you supplied that are worth mentioning. The important thing, I think, is that two separate conductors were drilled by Inco, corresponding to two distinct INPUT anomalies and two sets of ground- EM anomalies. (Incidentally, it is noteworthy that the Mcintyre Survey in July, 1972, failed to detect the northern conductor, owing to the choice of transmitter locations. Weak inflections are seen in the profiles at the northern conductor location, which should have been recognized and detailed with a separate transmitter set-up.) The ^northern conductor is broader and weaker, and is apparently "caused by graphite. The southern conductor, which is the extension of the conductor we are interested in having tested further east, is of higher conductivity, and apparently caused by massive pyrite. The I.P. anomaly over this conductor is relatively weak, but strengthens towards the southeast, suggesting a broadening of the sulphide zone or the addition of graphitic material. Minor gold values are associated with the pyrite.

2

fvnomaly 38

As mentioned by telephone, the transmitter was located so as to emphasize Anomaly ,44, rather than Anomaly 38, though 44 appears to us to be of much lower interest. The transmitter should have been located some 600 feet further north, at about 14N of the base line. An additional line 600 feet west of Line 600W should be surveyed at the same time. Neither conductor is appreciably magnetic, so I would not attribute the cause to iron formation, though certainly there appears to be iron formation further north.

Anomaly 3

As with Anomaly 38, the transmitter postions on this grid were such as to provide the least possible chance of locating the conductor should it be in the position shown on the INPUT maps. In fact, the EM profiles to the north and to the south, join at just about the position shown for the conductor. I realize that what your operator is trying to do is to divide the 2600 foot long profile into two sections, while maintaining a more or less east-west transmitter-receiver orientation. However, when the conductor of interest is in the center of the 2600 foot long profile, the overriding requirement is to have the transmitter as closely as possible on strike. I would not object under the circumstances to having the transmitter set up 600 feet east of the eastern line, and running the receiver 1300 feet north and south of the inferred conductor location. Again, one and preferably two additional lines should be surveyed west of the present grid, as the airborne anomaly improves in this direction.

Anomaly 9

Here again, as with Anomalies 38 and 3, the EM transmitter has been positioned so as to provide minimum detectability to the conductor of interest. The inferred conductor position is at approximately 15S of the base line, just below the junction of the two sets of profiles. In fact, there is a small inflection at that point on both Lines 8E and 12E, suggesting that we have in fact got a conductor at this location. This should have been detailed with a transmitter set up at approximately 14S on Line 0. I would agree that there may be a conductor to the west of Line O, possibly swinging in a northerly direction, though this is not evident from the INPUT data, One or two east-west profiles from the last-mentioned transmitter set-up might be justified. The soil sampling

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south of Anomaly 9 produced apparently negative results, definitely down-grading this anomaly. Nevertheless, we still feel it should be detailed and possibly drilled.

Anomaly 24

The I.P. survey performed on this anomaly early this year covered the eastern portion only, though one line (Line 84W) did cross a portion of the conductor. This line also produced a good I.P. response, though south of the inferred conductor position. I shall be interested in seeing the EM and mag results on this grid, particularly over the western portion.

Anomalies 13 and 50

No data have yet been received on these two anomalies,

Anomalies 7 and 8

We did not pick these anomalies as being ofparticular interest, though they certainly are not explained. The ground results are consistent with the airborne, and our feeling is that they are probably due to graphite, with some overburden effect contributing.

Anomaly 3OA

Our comments on this anomaly were made in our letter dated March 19th.

Anomaly 94

Having examined the more recent data on your ground to the west of this anomaly, and discussed previous results in the area with you, we still feel that some potential remains in Lots 5 and 6, Concession I. Apparently the area was surveyed in an east-west direction by Inco, though I do not have their data. Not all the conductors were apparently drilled. I would like to see a portion of that area surveyed by Turam, particularly the eastern portion (Lot 5). As you pointed out, there are still unexplained I.P. anomalies along the boundary of Concessions I and II, in both Lots 4 and 5. These could be covered by Turam at the same time. Proximity to the Kidd Creek Mine and the presence of sulphides in virtually all the drilling, gives this area a very high priority.

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Thank you for sending in the data so promptly,

Yours sincerely, PATERSON, GRANT S WATSON LIMITED

ll

Norman R. PatersonNRP:kncc: Mr. Wayne Zwickey

f'L - s z 41* -* or- 9~ 73iii-. ^ ^*\ *? s- vPaterson, Grant &L Watson Limited 7 Consul ting Geophysicists. - — : v-

7May 31, 1973.

Suite 2306, The Simpson Tower, 401 Bay Street, Toronto, Ontario, Canada M51Telephone: (416) 868-0888 Cables: Ne rqufcst

Mr. Alec Skrecky,Mcintyre Porcupine I linos Ltd.,Schunuicher, Ontario,

Dear Mr. Skrecky:

I enclose the text of the interpretation section of our report on the Turam survey work done for you inCrawford and Carnegie townships. This is in its final form except for any additions or comments Dr. Paterson may v;ish to make on his return. It will be of value to have some discussion betvreen ourselves regarding some of the conclusions reached, particularly in the case of Anomaly 24M, and I would be glad to have a meet ing for that purpose at your convenience.

Yours ve ri' truly, PATERSON, GRANT 5. WATSON LIMITED

/vRKWtsm Roger K. Watsoncc, Mr. W. Zwickey

Dr. N. R. Paterson

INTERPRETATION

Area #3

This anomaly was detected by a vertical loop EM survey

and was confirmed by the Turam survey. The Turam data also

revealed a second anomaly 600 feet to the south which is

labelled 3S, while the main one is labelled 3N.

Anomaly 3N has a conductivity-width of 20 mhos. It

has no direct magnetic expression itself but lies about 200

feet south of a strong magnetic anomaly probably caused by

serpentinized ultra mafics and is considered attractive on

both geological and geophysical grounds. Analysis of the

strong magnetic^anomaly to the north provides a depth to

bedrock of y^ feet^v^hich is judged too deep for useful test

ing of this anomaly by gravity measurements.

It is concluded that the anomaly represents sulphides

or graphite or a mixture of both. It is recommended for

drilling on the priority B. The optimum drill-hole is recom

mended on Line 2W at 10 + 6ON dipping 50 degrees to the north

and extending 350 feet.

Anomaly 3S is a 600 foot long Turam anomaly with a

conductivity-width of 40 mhos. There is no magnetic expression

of this anomaly but its short length and high conductivity-

width suggest sulphides as the cause and it is recommended

for drilling on priority B. The drill-hole should be collared

on Line 2E at 4 4- 8ON, dipping 50 degrees north for a length

of 350 feet.

Anomaly #8

This conductor was detected by the VEM and shows it

dipping to the south. The Turam survey confirms this conductor

and shows a second weaker conductor to the south of the first and gradually angling away from it toward the west. A broad

magnetic anomaly underlies the eastern part of the conductor

but appears to be a basic intrusive through which the conductor

passes rather than a'magnetic sulphide forming part of the conductor. It is concluded that the anomaly represents

graphite with possible sulphides. The depth to bedrock is

calculated from magnetics at between 20 and 50 feet and a

gravity survey is recommended as a means of distinguishing

sulphides from graphite. This should be done on Lines O,

3W, and 6W. If it should be decided to drill without the

benefit of gravity surveying the optimum drill-holes would

be (a) Line 3W at 27 * OOS, dipping 45 degrees north for a

length of 300 feet and (b) Line O at 28 -J- 20S f dipping 45

degrees north for an extent of 400 feet.

Anomaly ft9

Anomaly 9 was detected by the vertical EM survey and confirmed by the Turam survey. The Turam work detected a

number of other parallel conductors of which two are judged

the most important and are labelled 9N and 9S. A third one

to the south of #9S was drilled in the past and was found to

be caused by graphitic slate with minor sulphides. The

thickness of overburden of this area from the drilling and analysis of magnetic anomalies is 50 feet. Conductivity-

width of the short northern anomaly averages out at 40 mhos.

The conductivity-width for Anomaly 9S is 20 mhos or less.

The banded character of the conductors in this area

suggests that the anomalies are caused by graphite and this is

confirmed to some extent by the drill-hole to the south.

However, economic sulphides could form part of the conductor

and it is recommended that a gravity survey be carried out in

an attempt to distinguish between graphite and sulphides.

This work should be done on Lines 4E to 12E between stations

10S and 26S. In addition, it is recommended that the 1-gamma

magnetic readings be completed on Lines 6E and 10E. Drilling

would be based on the results of these extra surveys.

Anomaly 9A is a north-south trending INPUT conductor.

It was detected on three lines with the Turam, and was found

to have a conductivity-width of less than 10 mhos and a general

shape of a flat-lying conductor. It is interpreted as a

clay anomaly and no further work is recommended.

Anomaly #24

This anomaly was detected by the VEM which indicated

a tabular conductor dipping toward the north. The Turam survey

confirmed the anomaly, which is labelled 24N on the Turam

diagram, and also detected several other anomalies to the south,

the most important of which are labelled 24M and 24S.

Anomaly 24N has a conductivity-width ranging from 17

to 28 mhos which is normally considered within the range of

graphite or sulphides. However, it has no magnetic response

and on Line 52W where an earlier I.P. survey was conducted,

there is no chargeability response. In fact, if anything,

the I.P. response is slightly below background. This combined

geophysical signature is one of highly conductive overburden

rather than sulphides or graphite and so this anomaly is down

graded. There is a remote possibility that the absence of

chargeability is merely due to the fact that the conductive material is continuous enough in thin sheets to provide an

EM conductor but occupies too small a volume to provide an

I.P. response. In any case, this would probably indicate too small a volume to be of economic interest. Anomaly 24N then

is believed caused either by highly conductive clay or very thin bands of graphite and at present is not believed worthy of additional development work.

* ,

Anomaly 24S has a relatively low conductivity-width {maximum 14 mhos). It correlates with some magnetic trends but does not exhibit a positive magnetic expression itself.

It is the typical response of a clay layer which is bounded by bedrock structure. No further work is recommended on this anomaly.

s

Anomaly 24M has conductivity-widths ranging from 22 to 31 mhos. It coincides with a resistivity anomaly found in the earlier I.P. survey and lies on strike with a weak I.P. anomaly. It has no positive magnetic response. This anomaly would appear to be caused by graphite or sulphides and it is re commended that additional I.P. work be considered and that the drilling results of the I.P. anomalies Zone A and Zone B further to the east be taken into consideration. The depth to bedrock based on analysis of the magnetic anomaly to the north lies between 110 and 130 feet below ground surface which is judged too deep for an adequate test by gravity methods,

Anomaly #29

A VEM survey detected at least one conductor and in dicated the general dip to the south. The Turam survey con firmed this conductor and revealed two adjacent parallel con

ductors. The central conductor has the highest conductivity- width, being 50 mhos on Lines 3 and 6E. The adjacent con ductors range from 9 to 33 mhos. Fluxgate magnetic surveys were done on two of the three lines and virtually no magnetic

^Pexpression of these conductors is seen. The exception to this is a 50-gamma anomaly on Line O which is approximately 100 feet away from the southernmost conductor and is on-strike with the central conductor. It would be useful to cover these con

ductors with 1-gamma magnetic surveying on all three lines. It

is concluded that the conductors represent graphite, possibly with some sulphides.

The depth of overburden is ambiguous. The regional depth contours and the results of the VEM survey indicate a depth between 150 and 175 feet. Analysis of the small magnetic

anomalies to the north of the conductors indicate the sources are less than 50 feet deep but they may be caused by boulders within the overburden. If the shallow depth were valid then a gravity survey would be of use in distinguishing between

graphite and sulphides. To resolve this ambiguity it would be of considerable value to survey all three Turam lines with a

1-gamma magnetometer. This new data might enable a more accurate depth to be calculated and would provide a better judgment on the cause of the conductors.

In any case, it is judged that the deeper depth is probably the most valid and because of the high conductivity width, the anomaly is recommended for drilling on a priority B. Lacking any additional information, the drill collars are re

commended as follows: (a) Line 6E at 20 4- 70S dip 60 degreesnorth, 450 feet

(b) Line 3E at 19 + SOS, dip 60 degrees

north, 450 feet.

Anomaly #30A

This anomaly is an attractively positioned short

anomaly lying off to one side of a long formational INPUT

conductor. The anomaly was detected on the ground by the

vertical loop EM and confirmed by the Turam survey. There

is an indefinite indication that it splits into two parallel

bands on Lines 3 and 6E. The main anomaly has a conductivity

width which is a consistent 17 or 18 mhos along its length.

This compares with the conductivity-width of 37 mhos which is

measured over the drill section of Anomaly 30 600 feet to

the south, and which was caused by a graphitic tuff containing

about 25% sulphides. The main anomaly has a 30-gamma magnetic

response on one line but no other response at the other survey

line. Its general character is one of graphite schists which

may or may not contain sulphides. From the nearby drill-holes,

the depth of overburden is believed to be greater than 100

feet and it is judged impractical to use the gravity method to

distinguish between graphite and sulphides. It is recommended

that this anomaly be drilled on a priority B from a drill set

up on Line 6E at O 4- SON, dipping 50 degrees to the northeast

and extending 530 feet.

Anomaly #38/44 Area

These two anomalies are parallel and about 700 feet

apart on the INPUT map. The vertical loop EM survey provided

a stronger response over Anomaly 44 than 38 and so the Turam

survey was designed to cover Anomaly 44. The profiles seemed

to have stopped just at the edge or the centre of Anomaly 38.

Anomaly 44 appears to be a series of banded conductors with

almost no magnetic correlation, except for a 15-gamma anomaly on

Line 6W at 9S. The conductivity-width varies from 13 to 21

mhos which is in the range covering both highly conductive over

burden and sulphides or graphite in bedrock. One exception is

on Line O where an in-phase anomaly shows a conductivity-width

of 100 mhos. The validity of this anomaly is in some doubt

owing to the complete lack of out-of-phase response.

The depth of bedrock is'estimated at 125 feet from analysis of the VEM profile and the regional overburden contours show it to be approximately 175 feet and so it is judged that the gravity method would not be of use in distinguishing be tween -graphite and sulphides. Based on the reasonably high conductivity-width and the weak magnetic correlation, it is recommended that this anomaly be drilled in a priority B in

two locations. The first is on Line 6W at 11 -f 40S dipping 50 degrees to the north for a length of 400 feet and the second is positioned to test the high conductivity-width anomaly on Line OW at 14 4- 25S dipping 50 degrees to the north and

extending 400 feet.

s

Anomaly t50

The VEM survey located this anomaly and shows a broad asymmetric cross-over which is indicative of a flat conductor. The Turam survey confirmed the anomaly is an east-west direction and the conductivity width ranged from 4 to 10 mhos. The Turam survey that was done on east-west lines revealed a

rather broad indefinite area of weak conductivity on the western side of the grid that did not really tie in with an INPUT conductor and is likely overburden. The east-west con

ductor lies in a generally low magnetic area and no discrete magnetic response is seen at any conductor. It is concluded that this anomaly represents an overburden conductor and no recommendations for further work are made.

Anomaly #61

The VEM survey detected this conductor and its profile

suggested either a vertical dip or a northward dip. The Turam

survey confirmed the conductor and shows a second one parallel4

to the first lying about 200 feet to the north. The Turam

was done using the field from a 60-cycle power line which

lies to the west of the conductor and actually cross an ex

tension of the conductor at an angle of 60 degrees or so. The

readings were made by tuning into the third and seventh

harmonic of 60 cycles which are 180 and 420 cycles respectively.

The response is stronger than what might be expected from this

rather poor coupling angle and this indicates a relatively

shallow dip, perhaps 60 degrees or less. The conductivity-

width of the anomalies was not calculated owing to the peculiar

geometry but, based on the relatively high ratios of in-phase

to out of phase response, it is believed that the conductivity-

width is high enough to be out of the range of clay anomalies

and into the range of graphite or sulphide deposits in bedrock.

The magnetic response of these conductors is zero, but only two

of the five lines were surveyed and it is recommended that 1-gamma

magnetic surveying be completed on the other three lines. A

depth calculation on one magnetic anomaly provides a depth to bedrock of 40 feet and is recommended that these anomalies be

investigated by gravity surveying in order to distinguish

between graphite and sulphide minerals. The most useful lines

to do this work would be Line O, 3, and 6E.

42A14SW0026 63.4827 CRAWFORD 020

REPORT OK

INDUCED POLARIZATION SURVEY

DRIFTWOOD GRIDLIFTWO ~ev*v TOWNSHIP. ONTARIO

on behalf ofMCINTYRE PORCUPINE MINES LTD.

Bale d'Urfe, Quebec

September 5th, 1973 Karl Glackmeyer, Eng.

KARL GLACKMEYER A ASSOCIATES LIMITED, Geophysical Consultants and Contractors

716 Cornwall Drive Bale D'Urfe 850, Quebec (514) 453-1982

REPORT ON

'INDUCED POLARIZATION SURVEY

DRIFTWOOD GRID

CARNEGIE TOWNSHIP, ONTARIO

on behalf of

MCINTYRE PORCUPINE MINES LTD.

INTRODUCTION

During July and August 1973, a geophysical

party, under the direction of the author, carried out

an induced polarization survey on a portion of the

Driftwood Grid, Carnegie Township, Ontario, on

behalf of Mcintyre Porcupine Mines Ltd.

The induced polarization survey was carried

out using a Scintrex Mark VII pulse type unit of high

sei^sitivity , with remote receiver of the Newmont type.

The current-on time was 2.0 seconds and the measuring

time was 0.5 seconds. Measurements are made from which

are derived two (2) physical properties, namely, the

chargeability (that is the I.P. factor), which is express-

l...

KARL GLACKMEYER 4 ASSOCIATES LIMITED

INDUCED POLARIZATION SURVEY RE: DRIFTWOOD GRID .2

ed in units of milliseconds and the D.C. resistivity

which is expressed in units of ohm-meters. The three-

array electrode configuration was employed with an

electrode separation of a s 100', 200' and 4.00 1 for

the survey carried out over L-10E; and the pole-

dipole electrode configuration was employed over L-24E

and L-26E with a B 200' for n ~ l, 2 and 3.

The purpose of the present survey was to map

the distribution within the underlying rocks of disse

minated metallic conductive minerals; such as pyrite,

pyrrhotite, chalcopyrite (but not sphalerite) and

graphite. Magnetite and serpentine are known to have

moderate polarization response. It is rarely possible

from I.P. data alone to differentiate between these

various potential sources of polarization response.

DISCUSSION OF RESULTS

Drawing 1301-1-A IP l R shows the charge

ability and resistivity profiles on a scale of 200* to

the inch for L-10E. The chargeability is plotted on a

scale of l" - 10 milliseconds while the resistivity

has been plotted logarithmically. Drawings 1301-1-B 4

C IP Si R show the chargeability and corresponding resist

ivity in contoured section on a scale of 200' to the

inch for L-24E and L-26E effectively. The chargeability


[NBUCED POLARIZATION SURVEY RE: DRIFTWOOD GRID .3

has been contoured at a 2.5 millisecond interval while

the resistivity has been contoured logarithmically t

L-10E

The chargeability values range from - 1.6

milliseconds to a maximum of 7.9 milliseconds observed

with the a e 400' electrode separation. The resistivity

data ranges from 135 ohm-meters observed with the a -

100' electrode separation to a maximum of 1,280 ohm-

meters observed with the a a 400' electrode separation.

The a s 100' electrode separation shows three separate,

moderate zones of polarization; each peak corresponding

with resistivity lows. The 200' and 400' electrode

separations show a broad moderate zone of polarization

accompanied by a broad zone of resistivity low values.

L-24E and L-26E

The chargeability data varies from - 0.6

millisecond to a maximum of 4.7 milliseconds. The

corresponding resistivity data varies from 90 ohm-

meters to a maximum of 444 ohm-meters. The overall

survey indicate a weak zone extending from 24S to 28S on

L-26E and a similar zone extending from 22S to 26S on

L-24E. In both cases, the chargeability data corresponds

with an increase in resistivity.

KARL GLACKMEYER A ASSOCIATES LIMITED

INDUCED POLARIZATION SURVEY RZ : DRIFTWOOD GRID

CONCLUSION AND RECOMMENDATIONS

The present induced polarization survey has

outlined three parallel zones of moderately high polar

ization on L-10E which enclose between 5% to 10SS

disseminated metallic conductive minerals by volume.

Since these metallic conductive minerals could be

either sulphide or graphite, it is not possible, from

the present data, to differentiate between the potential

sources of polarization response. These three parallel

zones have potential in depth as the polarization

response increases proportionally with electrode

separations.

The zone of polarization outlined on L-24E

and L-26E can be considered a weak zone of polarization

accompanied by a corresponding increase in resistivity

values. The most probable explanation for the observed

effects is a chargeability built-up due to shallow over

burden; or disseminated magnetite within the underlying

rocks.

Without knowledge of previous work, the

author considers the zone of polarization on L-10E to be

more important. Should previous work not have explained

this source of polarization, then additional work should

be carried in the vicinity of L-10E in order to further

delineate this zone.

I..

KARL GLACKMEYER b ASSOCIATES LIMITED

irDUCiiD POLARIZATION SURVZY O: DRIFTWOOD GRID .5

The present induced polarization data does

not justify further investigation of L-24E and 26E; however,

other geotechnical data could show positive signs.

Respectfully submitted,

Karl Glackmeyer, Eng.

KG/gc


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KARL GLACKMEYER ft ASSOCIATES LTD.Geophysical Consultants and Contractors

(514) 453-1982

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KARL GLACKMEYER

MCINTYRE PORCUPINE MINES LTD.Drift weed Grief

Carnegie


KARL GLACKMEYER * ASSOCIATES LTD.Coowfrantt mtf Corrtffctors

716 CoffMMfl Driv* d UT* 850 Otw

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MCINTYRE PORCUPINE MINES LTDDriftwood Grid

Ontario

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KARL GLACKMEYER * ASSOCIATES LTD.Geophysical Consultants and Contractors

716 Cornwall Drive Baie d Urfe 850, One (514) 453-1982SURVEYED BY

K. G.

/JO/ - t -A — /P* X

030

ELECTROMAGNETIC-MAGNETIC SURVEY

on the property of

MCINTYRE PORCUPINE MINES LIMITED

Crawford Township, Porcupine Mining Division, Ontario

by

SHIELD GEOPHYSICS LIMITtD

Timmins, Ontario,

July 23, 1970.

R. J, Bradahaui, P.Eng.,

Consulting Geologist.

INTRODUCTION

Magnetic end electromagnetic surveys have bean completed

on the property of Mclntyre Porcupine Mines Limited in Crawford

Township. The surveys wero completed in early July subsequent to

the establishment of picket lines in late June, 197Q.

The surveys sre part of a project to investigate the

property for base metal mineralization.

TY LOCATION AND ACCESS

The property forms the north half of patented Lota 5 and

6, Concession IV in Crawford Township approximately 25 miles north

of Timmins, Ontario.

A gravel road from Highway 11 naur Cochrane about 20 miles

long provides easy access to the property.

s UIORH

A conductive zone on the property has been investigated by

one hole drilled by Inco. In the west portion of the property, this

hole intersected a pyrite-hearing graphite zone in contact with green-

stone tind dunite.

GLUUGV ' - , : \ ; .

The conductive zone drilled by Inco is indicated to be

several thousand feet long striking in an east west direction.

George (April, 1970) indicates a northwest trending fault in the

east half of the property which terminates the conductive zone. The

conductive zone, presumably graphitic is indicated to be in contact

with felsic tc intermediate volcanic rocks and dunite.

A large airborne magnetic anomaly in the southeast portion

of the property probably represents an ultramafic intrusive.

- 2 -

C SURVEY RESULTS AND INTERPRETATION

The magnetic survey data le plotted and contoured on B

plan st EI scale of one inch to four hundred feat accompanying this

report. The raethod of survey utilizing a Scintrax M. F. -1-100

fluxgate magnetometer is described in the Appendix to this report*

The magnetic background of the property ia in the order of

i*00 to 500 gammas uith the isomagnetics trending in a very general

east-west direction.

The most prominent magnetic feature is a magnetic high in

thfi southeast sector of the property uith a peak magnetic susceptibility

of about 3,500 gammas. This magnetic high is likely caused by an

ultramafic intrusive uith the contact marked by the BOO gamma contour.

The strong magnetic gradient along the west contact suggests a steep

plunge of the intrusive to the southeast. ,

The only other magnetic feature of possible significance

consists of a magnetic high on Line 32E, Station 23, and magnetic

lou on Line 24E, Station 2+50 S. This feature strikes eaat ueet for

a length of about 1,200 feet and may, in port, represent a deeply

buried ultramafic intrusive.

SUKVEV RESULTS AND INTERPRETATION

The survey una conducted using a McPhar 1000 - 5000 vertical

loop unit which is described uith the survey method in the Appendix

to this report. The survey data is plotted on maps at a scale of

one inch to four hundred feet accompanying thia report*

Lines ****E, (*BE and SHE mere surveyed using the Ronka EM 16

because of power line interference of the McPhar unit.

A number of conductors ware outlined which are described

as follows:

~ 3 o

CONDUCTOR A

This conductor appears to cross the entire property in an

east-west direction although it uins not detected by the EM 16 unit

on Linao A^E, ^BC, and 52E.

The Inco drill hole on Line 12E indicates H*9 feet of over

burden. This deep overburden is confirmed by the dip angle profiles

which also indicates cnnductlve overburden. The lack of penetration

by the EM 16 unit is due to the deep conductive overburden in the aria.

Excellent conductivity is indicated by the low frequency

dip angle profiles from a source which dips ni-ar vertically.

In the area of Line 12E the conductivity is caused by pyrite-

bearing graphite nccording to the Inco drill hole.

CONDUCTOR 8

This conductor crosses Lines 20S, 2*4S, and 26B in the south

west sector of the property. It strikes north-south for a length of

at least 600 fruit.

uieak to moderate conductivity from H source which dips west

below deep overburden in inclicat&d by the dip angle profiles. With

differing transmitter locations, the conductor changes location

suggesting that the source may be fairly wide up to 200 feet.

The conductor follows generally a magnetic low and the

ieomagnBtlcs to the north on strike tend to strike north.

The conductor may bs caused by a mineralized fault zone.

CnNDUCTflK C

Dn Line 20B this weak one-line crossover has no magnetic

correlation.

..l,.CONDUCTOR D

This conductor is marked by inflections of dip angles on

Lines 32E, 36E, and iiQE, It strikes east-uest and ia quite weak.

This possible zone of conductivity le located riaar the volcanic-

ultramaf'ic intrusive contact and may be caused by shearing within

the ultramafic intrusive,

CONCLUSICNS

In tho north half of the property a strong conductor has

been traced across the property in an east-went direction. On Line

12E an Inco drill hole indicates the conductivity is cauand by pyrite-

bearing jraphitu. The only othur conductor of significance, termed

O on the accompanying maps, strikes north-south. Although of weak

to roodnrate strength this conductor appears to be valid* perhaps

by mineralization associated with a north-south fault*

RL'CDMMEftOATlUNS

H is proposed that consideration be given to an additional

drill test of Conductor A near the contact of tho inferred ultramafic

intrusive betweon Lines 32E and 3GE. Because of the proximity of iha

ultramafic intrusive in this area there may be a change in the character

of the mineralization of the conductor in this area.

It is recommended thnt Conductor B be investigated by drilling

on Line 2QS, Station 5* SOL. Thft hole should be drilled east at 55",

to a depth of about 550 feet, to investigate the conductive zone whichappears to dip ueat. .


SHILLD UF.DPHYBICS LIMITED,

\~~^\l~^*i-\:,.^~^---'

Timmins, Ontario, R* J. Bradshau, P.Eng.,

23, 1970. Consulting Geologist.

APPENDI.2!

SURUEV HETHLig AND INSTRUMENT DATA

ELECTRDHWSNETIC SURVEY

Any alternating magnetic field will induce an electrical

eddy current in the medium through which the magnetic field peases.

IT a source of an alternating magnetic field is located nuar a

conductive body anomalously strung eddy currents will be induced

in the deposit due to its high electrical conductivity* Electrical

currents induced in the conductive bndy will produce a secondary

m ignatic field proportional to the intensity of current flow.

A receiver coil tuned to the frequency of the transmit

ting device will pick up both the directly transmitted signs! and

the eddy current signal.

The electromagnetic unit used in this survey is a McPhar

unit and consists of a vertically mounted, motor-generator powered

transmitting cull operating at frequencies of 5000 and 1000 cps.

and a recsiving coil, tuned to the transmitting frequencies, an

inclinometer, an amplifier and a headset.

Throughout the survey, the transmitter and receiver ware

separated by distances of **QQ, 600 and 1200 fast. The plans of

the transmitter coil wsia oriented so that the transmitter uas

vertical and pointed towards the receiver. Orientation wits obtained

using s plate on which predetermined receiver positions warn plotted*

Stations were road at one hundred foot intervals. At all times, the

receiver "faced" the transmitter. The results obtained ara dip

angles, moauuraci in degrees. The dip angles are obtsined by first

orienting the receiver coil in the plane of the magnetic field by

rotating the coil about a vertical axis until a null or minimum

- li -

signal la obtained, and than rotating the coil about a horizontal

axis until a null or minimum signal is obtained. The angle which

the magnetic field makea with the horizontal is recorded as a "dip"

or "tilt" angle. In the abaence of a conductor the dip angle will

be zero since no secondary field le present. In the presence pf

a conductor, the axle of the receiver coil points toumrds the

conductor and the plane of the coll auay from the conductor* In

the presence of ti conductor, the secondary magnetic field is usually

displaced from the primary in-phaae aa well as direction so that

the total field la 'lliptlcally polarized. The receiver cannot

then be nulled completely but a minimum signal can be obtained,

the width of thu minimum being an indication of the phase displacement.

The tilt angles are plotted as profiles, the zero or

"croso-over" point indicating the focus.of the conductor axis.

Once e conductor axis has bison eatablinhed, the trans

mitter is.net up over the conductor and Unas are read on both

aiden of thu transmitter tind the conductor axis is traced out by

"leap frogging" f mm "cross-over" to "cross* over".

SPKCiriCATIKNS

Operating FrBquBnciBa; 1UQO and 5000 cycles par second

Range;, 2QOO foot separation betwerm transmitter and recuiver for a i 10 degree null width.

Pep t h of E xplor a t ion; Roughly half the distance between trans mitter and receiver.

Transmitter Hquer Supply; 500 watt alternator driven by a 1JCH.IVgasoline engine.

idel.ah.ts: Packboard-mounted engine generator 46 Iba.Transmitter coil on packboard l*'J Ibs.Coil mounting pole and spreader bar 22 Iba.Receiver 7 Ibe.

- lil -MAGNETOMETER SURVEY

A Sharpe M.F.-1 fluxgate magnetometer uas used in the

magnetic survey. This instrument measures the vertical component

of the earth's magnetic field in gammas. Base stations for de-j\ ,. ; : ' - .

l termining the magnetic diurnal variations were established along

the main base line at 10U foot intervals. Magnetic readings were

taken at 50 foot intervals, along the cross lines.

IN3KR-OFFICE CORRESPONDENCE55 YONGE STREET. TORONTO, ONT.

DATE August **. 1970

ATTENTION OF w.P.Hammond

SUBJECTAbitibi Option,Crawford Township, Ontario

Geophysical survey work has been completed on the north half of Lots 5 And 6, Concession 4, Crawford Township (Abitibi Option) as covered by the accompanying Shield Geophysics Limited Report*

Four conductors were picked up, one of which was previously known and drilled by Inoo as shown on the accompanying magnetometer plan* Conductor A can be traced across most of Crawford Township* Other Inco holes were drilled on this Eone one mile to the west of the map area and two and a half miles to the east* All holes showed weak zinc or copper values* The following is a summary of the log for the drill hole shown on the Magnetometer plan.

O - 182.0 - casing182.0 * 306.3 - andesite306*3 - 373*0 - rhyodacite - locally graphitic mineralized

with small amounts of pyrite and chalcopyrite* 336.0 - 338*7 -2*7 feet assayed 0.44 # copper

373.0 - - end of hole

The core from this hole is sheared at asmall angle to the hole direction. There is other evidence of this type of disturbance and the survey was directed to search for conductive zones trending in this direction. The following is an assessment of the conductors that have been outlined by the survey.

Conductor A - A strong conductor due mainly to graphite. Bradshaw recommends a drill test between lines 32 E and 36 E where changes in the content of the conductive zone might be expected due to its proximity to a body of ultra basic rock. I am in agreement that additional work is warranted in this particular area. This is a Nickel Offsets type probability.

Conductor B - This weak to moderate north south conductor may be up to 200 feet wide and like the others is covered by deep overburden. A north south disturbance in this area is supported by the Inco drill hole. Moderate conductivity likens the chance that sulphide mineralization is present. I agree that additional work is warranted

55 YONGE STREET, TORONTO. ONT.

DATE

ATTENTION OF

SUBJECT PAGE TWO

here and have staked one claim to oover the southerly extentIon of this zone.

Conductor C - A weak crossover of no interest at present

Conductor D - A weak conductor likely related to the ultra basic contact*

Recommendations

Additional work Is warranted on the property, at the following locations.

1. Anomaly A in the vicinity of line 3^00 East2. The central part of Anomaly B

Value at these sites is presently based on conductivity and on an indicated favourable geological environment* An upgrading of these features is necessary and the following work program is recommended.

1. A gravity profile over each anomaly to establish if a significant mass of material is present.2. A geochemical test at bedrock at each anomaly, using the Bondar - Clegg equipment to determine if economically important metals are present* 3* Formal diamond drilling if favourable results are obtained from the above work*

I am presently collecting promising sites for gravity work and for deep overburden drilling.

AS/sa A.Skreoky

June 15, 1970.

Mclntyre Porcupine Mines Limited, P,D, Box 970, Timmina, Ontario.

Attentions Mr. Ale* SkreckyExploration Department

Dear Sir:

Ret ElBctromaanetic-HBonetic Survqv CfBtffofd Township

The following are the terms under which Shield Geophysics Limited (hereinafter called the CONT.HACTOR) yill undertake to perform magnetic and electromagnetic surveys on the property of Mclntyro Porcupine Minee Limited (herelnaftfr called the COMPANY) in Crawford Townahip,

PROPERTV

The property le designated on a linacutting sketch provided by the COMPANY.

MAGNETIC SURVEY

A fluxgate magnetometer shall be uaed for the magnetic survey with readings to be taken at 100 foot atationa. Where the magnetic gradient is greater than 200 gammas per 100 feat, readings shall he taken at 50 foot intervale* ,

Coat of the survey thall be &55.QO per line mile.

ELECTROMAGNETIC SURVEY ,

A McPhar 1000/5000 electromagnetic unit shall be used for the electromagnetic survey. Y

- 2 -

Cost of the survey shall be S125.QQ per Una mile for general coverage and S150.QO par day for detailed coverage aadirected by the COMPANY,

TRANSPORTATION. ROOM AND BOARP

The CONTRACTOR ehall be responsible for the coat of transportation, room and board.'

REPORT AND MAPS

The CONTRACTOR shall prepare the report and maps to satisfy the requirements of the Ontario Department of Mines.

WORKMEN'S COMPENSATION ste,

The CONTRACTOR is responsible for Workman's Compen sation in compliance with the laws of Ontario.

The CONTRACTOR is also responsible for all uiagas, assessments, and deductions with respect to its employees and shall keep the property free of all liens in respect of its work.

IN WITNESS bJHEREDF ths parties hsreto have sat their hands end aeela.

COMPANY MCINTYRE PORCUPINE MINES LIMITED

CONTRACTOR SHIELD GEOPHYSICS LIMITED

42A14SW0026 63.4827 CRAWFORD 040

Keroh 17, 1171.

Mcintyre Porcupine Minus Liwited, 12? Third Avanue, Timmins, Ontario*

Attention i Mr f Alex Skrecky

Otter Mr. Sk rack y i

Rut Reconnaissance McPhsr Vertical LOOP

Three airborne conductive lonee in the eoutheeet sector of Crawford Township hove been investigated tiffing the McPher vertical loop electrouBgnfttlo unit. This work wen carried out on February 23, 24, 25 and Meroh 5, 1971.

^ocation l

In the eouth half of Lot 3, Conoeeelon III, aa in* diceted on the Bccompunyina plan, thle conductor correepond* very closely with a prominent airborne *iegnati6 antmely.

The preeenoe of a Moderately atrong conductive tone, striking northwest, and over 1200 feet long la confimed by the vertical loop survey.

location Z

In the north half of Lot 3, Concession II, QB in* dicated on the accompanying plan, this conductor appeera to be located along the aouth flank of the ognttlo anomaly as sociated with location 1.

. 2 .

The McPhar verticil loop survey indioataa a conduc tive zone at the bend in tho Driftwood River. Rather poorly defined, only the ysfit portion of the conductive ion* oppeere to have been located. The dip angle profilea indicate the presence of two parallel weak to moderate atrength eonductora etrikiny slightly north of weet. The aource of conductivity may be quite deeply buried, perhaps up to ZOO feet.

Location 3

In the north half of Lot 6, Conoeaelon III, thla conductor appears to be looated et the flank of an airborne magnetic high.

A week to moderately atrong conductive zone wae lo cated by the vertical loop aurvay. The axis of the conductor atrikea north 3D0 ueet and ia at leaat 1000 faet long. Vary deep overburden is indicated by the dip angle profiles.

Conclusions

For locations 1 and 2, it ia proposed that a grid be aBtabliahed ae indicated on the accompanying plan. The base line ie oriented north SO0 went and eight miles of picket are required. Magnetic and electromagnetic eurveye are recommended to determine the relatlonehip of the conductive zones to the magnetic susceptibilities and aet prioritlea on poaaible drill targata.

A grid of about 3.5 miles ia propoeed for location 3. Here the baaa line should be oriented north 30* ueet and magnetic and electromagnetic aurvaya carried but.

Respectfully eubwitted,

SHIELD GEOPHYSICS LIMITED,

R. J. Bradehaw, P. Eng., RJB:pd Conaulting Qeologiet.

8 7 6 5 4 3 2

Carnegie Twp.

LOCATIONPLAN

LEGEND

Meosurement stotion olong picket line

North dip angles to left of line South dip angles to right of line

West dip angles below the line

East dip angles above the tine

1000 cps

5000 cps

Transmitter location

•9 ' Conductor axis - 1000 cps

O— — - 5000 cps

INSTRUMENT McPhor (000/5000 E M

Profile scale l" ' 200

st O C

MAR VERTICAL LOOP SURVEY

LOCATION lSCALE l" - 400'

v\I'V*

McPHAR VERTICAL LOOP SURVEY

V, A \/ \\

Hifin

f). VI'J M

l " t

\

fi-

V 4

LOCATION 2.SCALE l" - 400' tr-


LOCATION 3

SCALE

I-


ROAD

CREEK

LOCATION 3SCALE l"-400'

r


DATE March 24, 1971

ATTENTION OF w.P.Hammon*T.Skinning

SUBJECT EM Reconnaissance, Abitibi Option, Crawford Township, Ontario.

l have attached a report prepared by Shield Geophysics covering their EM reconnaissance on Abitibi ground in Crawford Township. Please note the following with respect to eaoh location.

Location l

Ve have made several attempts to confirm this conductor location andaare still uncertain on this matter. Landmarks in the area are not very useful. The anomaly, as we flee it, is located midway between INCO 4-149 and ZNCO 4-89* This corresponds closely to Input 364A. No drill sites have been identified in the area as yet. We plan a grid here based on a 2800 foot long base line anchored on the known conductor with cross lines expending 3000 feet to the southwest. Mag and BM surveys will follow (see Figures l and 2).

Location 2

This survey work failed to account for Input anomaly 365W. The conductors that were located lie close to a property boundary line and l d* not propose to follow up this indication at present* An INCO drill hole 2000 feet to the south east intersected mainly rhyolite and the general environment connected with Location 2 is classed as favourable. Our proposed work at Location l may further upgrade Location 2 at which time the matter can be re considered.

Location 3

The conductor indicated at this location is very weak and l do not propose any follow up work.

AS/ A.Skreeky

MCINTYRE PORCUPINE MINES, LIMITED

tion Department 970, Ontario

March 29, 1971

Mr* B.J.Bradshaw, Shield Geophysics, Limited, 26 Pine Street, South, Timmins, Ontario

Dear Boni

This will confirm arrangement e made with you recedntly to carry out a program of lineouttlng, nagnetoaeter and electromagnetic surveys over a 4000 foot by *K)00 foot block to bc located on Lots 3 and U, Concession 3, Crawford Township, Lines will be cut at ^00 foot intervals in a southwest direction within this block which is anchored to a ground conductor you recently located in a reconnaissance survey of this area. The general picture le shown on an appended sketch.

We have attached a signed lineoutting contract which you are asked to complete and return to us. Would you also supply wfc with a letter which outlines terns covering the proposed geophysical surveys.

Tours very truly,

MoINTTRB PORCUPINE MINES LIMITED

AS/ A.Skreoky

42A14SW0026 63.1827 CRAWFORD 0B0

ELECTROMAGNETICS-MAGNETIC SURV/EY

on the property of

MCINTYRE PORCUPINE MINES LIMITED

Crawford Township, Ontario

vi.';

Timmins, Ontario,

May i*, 1971.

R. J. flradshauj, P. Eng.,


INTRODUCTION

Magnetic and electromagnetic surveys have been completed

on a small area in the southeast sector of Crawford Township for

Mcintyre Porcupine Mines Limited, ; , .

The object of the survey work was to more effectively

outline anomalous zones, indicated by airborne surveys, in the

search for base metal mineralization, primarily nickel,

The work was completed in March and April 1971.

f3RDPERTY LOCATION AND ACCESS

The area surveyed is part of a much larger area optioned

by Mcintyre from Abitibi. The picket line grid is mainly located

in Concession 111, Lots 3 and **, Crawford Township, 25 miles north

of Timmins, Ontario.

A timber road, built and maintained by Abitibi, from

Highway 11, provides access to the working area, a round trip

distance of 21** miles from Timmins, Alternatively, a helicopter

from the Timmins airport may be used for access to the area,

PREVIOUS iJDRK

The only previous work undertaken in the area, to the

writer's knowledge, is by Inco, According to the compilation

map by Shield Geophysics, for Mcintyre, three holes were drilled

by Inco within the area of the grid. In part, these holes ware

drilled to investigate an electromagnetic anomaly^ It is suggested

that the drilling did not account for the conductive zone although

- 2 - ' ,. -i "-- ' - , . ' '

asbestos and pyrrhotite were encountered in aha hole,

Mafic to ultramafic rocks, variably setpentinized,

aplite were encountered by the drilling. A,magnetic high in this

area represents the mafic and ultramafic intrusives, ,

Two drill locations were noted by the field operators,

during the survey, along Line 8UI. Presumably these are the tiuo

northernmost holes of the three hole section indicated on the

compilation map in the centre of Lot 3, Concession 111.

GEOLOGY

The compilation map by Shield, for Mclntyi-e, of Crawford

Township indicates that the northern half of the grid is underlain

by a mafic to ultramafic intrusive, variably serpentinized, with

some pyrrhotite and asbestos mineralization, covered by 90 to 150

feet of overburden. Based on less data the south half of the grid

is postulated to be underlain by generally east-west striking felsic

to intermediate flows and pyroclastic rocks,

Northwest striking faults are postulated in the immediate

area of the grid.

The geological environment is favourable to base metals,

particularly nickel, and asbestos mineralization.

MAGNETIC SURVEY RESULTS AND INTERPRETATION

The magnetic survey data is plotted and contoured oh the

accompanying plan at a scale of one infch to four hundred feet.

- 3 -

The isomagnetics trend In a southeast to easterly direction

uiith the exception of an area adjacent to Line 1*E, where the

isomagnetics, in part, trend northeast. As indicated on the

magnetic plan this anomalous feature is thought to be caused by

a fault zone with essentially vertical movement which strikes about

northeast.

The magnetic susceptibilities vary from over 8000 to

-3000 gammas* The area above the 1500 gamma contour is thought

to represent the mafic to ultramafic intrusive striking near east-

west. If the 1500 gamma isomagnetic represents the intrusive

contact, the body is at least 2300 feet wide. Serpentinization,

with the development of magnetite and perhaps asbestos, probably

accounts for the magnetic highs in the central area of the intrusive.

The small lenticular magnetic highs and lows in the

south area Of the grid are typical of mafic to intermediate volcanic

rocks.

ELECTROMAGNETIC SURVEY RESULTS AMD INTERPRETATION

The electromagnetic survey data is plotted and profiled

on two accompanying plans at a scale of one inch to four hundred

feet. A description of the instrument and survey method is provided

in the Appendix to this report.

Of numerous indications of conductivity, there appears

to be three main zones. These are designated A, B and C on the

accompanying plans.

Conductor A - This conductor, situated in the south portion of

the grid, strikes near east-west for a distance of at least 1600

feet. Depending upon the transmitter location the conductor axis

differs in location from the general coverage to tie detailed

plan, thereby suggesting a fairly wide zone of conductivity. The

axis location on the general plan is thought to represent the

strike of the zone most adequately, and perhaps the north edge of

the zone. A fault, postulated by George on the Shield compilation

plan, coincides in general with this conductor axis. The

conductivity may be classified as weak to moderate in strength*

Conductor B - In the east portion of the grid, this conductor is in

an area of very high magnetic susceptibilities, ranging from 5600

to 6600 gammas. It strikes east-uiest for a length of at least

1800 feet. Various transmitter locations indicate that the

conductive zone is approximately 150 feet wide. The weak to

moderate strength conductivity, appears to dp near vertically, and

may be caused by serpentinization with associated sulphide or asbestos

mineralization.

Conductor C - Striking northwesterly! this zone of conductivity

is situated in the northwest sector of the grid* It is very

poorly defined by the present survey work and is plotted from the

reconnaissance survey carried out in March, 1971, referrred to

as Location 1 on maps already submitted. This conductor may in

fact be the northwest extension of Conductor B which has been

- - . - interrupted by a northwest trending fault, mainly postulated from

the magnetic survey. Moreover this fault may account for the

difficulty in locating the conductor utilizing transmitter stations

on or east of the fault ibne in the present surveys. This weak

to moderate strength conductive zone appears to have been in

vestigated by the southernmost hole in the three hole section

drilled by Inco (See Previous Work), Pyrrhotite and asbestos

mineralization were reported in this hole*

Other Conductors - Each of the remaining conductive zones are of

limited length, having been indicated only on one line, or are

very weak. The northernmost two holes of the Inco drilling

would have intersected two very weak one line conductors.

CDIMCLUSIDIMS

The magnetic survey has outlined a mafic to ultramafic

intrusive, at least 230D feet wide, which strikes near east-west.

In the extreme north and south of the grid area, the magnetic

susceptibilities indicate the presence of northwest striking mafic

to intermediate volcanic rocks. This rock assemblage appears to be

cut by a north-east striking fault zone along Lines O to **E,

Three main conductive zones, termed A, B and C, and a

number of minor conductors are present within the survey area*

Conductor A may coincide or be associated with a northeast trending

fault postulated by George. More detailed magnetic work in this

area may indicate that certain magnetic features also correlate

with the conductor. Conductor 8, apparently 150 feet wide, follows

the axis of a magnetic high in an east-west direction* To the

west the conductor appears to be disrupted by a fault zone and

- 6 -

to east is open beyond the grid area. Serpentinization perhaps

associated with sulphides or asbestos is thought to be the cause

of this feature, Very poorly defined in this present survey,

conductor C may be the westward extension of conductor 8, west of

the postulated northeast trending fault. Serpentinization or

pyrrhotite mineralization encountered in an Inco hole may account

for this conductive zone.

The remaining conductors of limited length, and generally

quite weak, are not considered significant at this time.

RECOMMENDATIONS

Conductors A and B merit additional work. To assist

in locating possible drill sites it is proposed that some additional

geophysical work be considered for these two conductors. It is

proposed that conductors A and B be traced to the east to determine

whether or not the conductivity varies in strength. Also additional

magnetic work is proposed for the east extensiqns. More detailed

magnetic survey work on Conductor A, at 200 or 100 foot line

intervals, may show a correlation which merits drilling at a

particular location*


SHIELD GEOPHYSICS LIMITED,

\ - '~1\ Vi .- x*. * ^'(--i*———^-\

Timmins, Ontario, R. J. Bradshaw, P, Eng,,

May t*, 1971. Consulting Geologist,

C E R T I F I C A T E

I, Ronald 3. Bradshaw, residing at **8D Howard Street, Timmins,

Ontario, a consulting geologist with office ei 26 Pine Street

South, Timmins, Ontario, do hereby certify that:

I attended Queen's University, Kingston, Ontario, and graduated

with an Honours B.A, degree in Geological Sciences in 1958,

I am a Felloui of the Geological Association of Canada, and a Member

of the Canadian Institute of Mining and Metallurgy and of the

Association of Professional Engineers of the Province of Ontario.

I have no interest either directly or indirectly in the shares or

securities of Mcintyre Porcupine Mines Limited.

Timmins, Ontario,

May k, 1971,

R. J. Bradshaw, P, Eng.,


APPENDIX

INSTRUMENT DATA SURVEY METHOD

ELECTROMAGNETIC SURVEY

Any alternating magnetic field will induce an electrical

eddy current in the medium through which the magnetic field passes.

If a source of an alternating magnetic field is located near a con

ductive body anomalously strong eddy currents will be induced in

the deposit due to its high electrical conductivity. Electrical

currents induced in the conductive body will produce a secondary

magnetic field proportional to the intensity of current flow*

A receiver coil tuned to the frequency of the transmitting

device will pick up both the directly transmitted signal and the ;

eddy current signal.

The electromagnetic unit used in this survey is a McPhar

unit and consists of a vertically mounted, motor-generator powered

transmitting coil operating at frequencies of 5000 and 1000 ops,

and a receiving coil, tuned to the transmitting frequencies, and

inclinometer, an amplifier and a headset.

Throughout the survey, the transmitter and receiver were

separated by distances of **QO, 800 and 1200 feet. The plane of

the transmitter coil was oriented so that the transmitter was

vertical and pointed towards the receiver. Orientation was obtained

using a plete on which predetermined receiver positions were plotted.

Stations were read at one hundred foot intervals. At all times,

the receiver "faced" the transmitter. The results obtained are

dip angles, measured in degrees. The dip angles are obtained by

first orienting the receiver coil in the plane of the magnetic

- 2 -

field by rotating the coil about a vertical axis until a null

or minimum signal is obtained, and then rotating the coil about

a horizontal axis until a null or minimum signal is obtained*

The angle which the magnetic field makes with the horizontal is

recorded as a "dip" or "tilt" angle. In the absence of a conductor

the dip angle mill be zero since no secondary field is present.

In the presence of a conductor, the axis of the receiver coil

points towards the conductor and the plane of the coil auay from

the conductor. In the presence of a conductor, the secondary

magnetic field is usually displaced from the primary in-phase as

well as direction so that the total field is elliptically polarized.

The receiver cannot then be nulled completely but a minimem signal

can be obtained, the width of the minimum being an indication of the

phase displacement.

The tilt angles are plotted as profiles, the zero or .

"cross-over" point indicating the focus of the conductor axis.

Once a conductor axis has been established, the trans

mitter is set up over the conductor and lines are read on both

sides of the transmitter and the conductor axis is traced out by

"leap frogging" from "cross-over" to "cross-over".

SPECIFICATIONS

Operating Frequencies! 1DOO and 5000 cycles per second

Range: 20DD foot separation between transmitter and receiver for

a 10 degree null width.

Depth of Exploration; Roughly half the distance between trans

mitter and receiver.

Transmitter Power Supply: 500 watt alternator driven by a 1# H,P*

gasoline engine*

Weights:

Packboard-mounted engine generator UB Ibs,Transmitter coil on packboard 1*9 Ibs.Coil mounting pole and spreader bar 22 Ibs.Receiver 7 Ibs.

MAGNETOMETER SURVEY

A Sharpe M.F.-1 fluxgate magnetometer was used in the

magnetic survey. This instrument measures the vertical component

of the earth's magnetic field in gammas. Base stations for de

termining the magnetic diurnal variations were established along

the main base line at 100 foot intervals. Magnetic readings were

taken at 50 foot intervals, along the cross lines.

CRAWFORD 060

March 16,1973

Paterson Grant and Watson Limited

Technical Data,Anosmly 3 onfl Anomaly 9.Abitibi Option,Lot 6, Concession 6,Crawford Township, Ontario.

Mr.B.Guenther ha o forwarded the* following maps to you from our Toronto office, covering Anomaly 3 and Anomaly 9 located on Lot 6, Concession o, Crawford Township, Ontario.

1. MoPhar V.E.M. Survey oap2. Magnetometer Survey Plan (OP 70) 3* Magnetometer Survey Plan (HP l ) 4. Surface Plan

The Surface Plan shows the location of plugger holes which wore drilled last May by Bock Cormler of Bondar Clegg and Company Limited. Lower till material was recovered and analysed from 10 holes. Technical details on this work are attached.

The south halt of Lot 6, Concession 6, crawford Township was surveyed years ago and tested by one diamond drill hole, l have attached a plan showing the location of the drill hole and a section showing the drilling results.

deference was made In my memorandum to you dated March 8, to an Indicated north*south trending conductor lying just north west of Anomaly 9* This particular area remains to be checked out.

AS/ A.Rkreoky

Wajme R.ZwlokeyMarch 24/1973

Anomaly 3 and Anomaly 9 Areas, Lots 6 and 7, Conoesalon 6,* Crawford Township*, Ontario.

l have attached 200 ecale nap showing the results of detailed MoPhar V.B.M. surrey work In the Anomaly 3 and Anomaly 9 areas looated in Crawford Township*

This work has turned up a, northwest trending conductor whioh l have designated Anomaly 9A as shown** There is an Input anomaly at this particular location Hhioh we searohed for last summer using Sheridan Kelk equipment with negative results. Anomalies 3 and 9A would converge in the map area at a location which must be considered to be of eome interest to Us* The area lies in dense bush and formal lineoutting will be needed before further geophysical survey work is undertaken*

AS/ A.Skreoky

Paterson Grant and Watson Limltod March 24,1973

Anomaly 3 and Anomaly 9 Areas*Lots 6 and 7,Concession 6,Crawford Township, Ontario.

l have attached a 200 scale plan showing the results of McPhar V.E.M. detail work in the Anomaly 3 and Anomaly 9 areas in Crawford Township*

AS/ A.Skreoky

Bud! GeAntherMarch 24,1973

MoPhar V.B.M. Detail Survey Work, Anomaly 3 and Anomaly 9 areas. Lots 6 and ?, Concession 6, Crawford Township*

l have attached a 200 scale plan showing the MoPhar V.E.M.survey work recently completed In the Anomaly 3 and Anomaly9 areas located In the north part of Crawford Township. l

Would you add this Information to the V.B.M. Survey Plan already prepared for this area*"

Would you prepare a separate V.B.M. Survey Plan which would show the V.B.M. survey work on the south half of Lot 6, Con* 6, Crawford Township, excluding Information off of these staked claims." This V.E.M. survey map along with MP1 and GP 70 mag plans will be used for assessment work due soon on these claims*

AS/ A.Skreoky

oi man Pa

PATERSON, GRANT 6 WATSON LTD.

r\ersoijf 1k Associates Limited l Consulting Geophysicists

Suite 2306, The Simpson Tower, 401 Bay Street, Toronto 103, Ontario, Canada. (416) 363-4261. Cablet: Norquett.

Norman R. Paterson, Ph.D., P.Eng. Roger K. Watson, B.A.Sc., P.Eng. Fraser S. Grant, Ph.D., P.Eng.

March 28, 1973.


RE; ANOMALIES 3, 9, 8, CRAWFORD TWP.

Dear Alec:

We would judge that the above anomalies are now sufficiently well located to justify detailing before drilling. Accordingly we submit proposed line grids and transmitting loop locations for Turam surveys.

Each grid consists of 5 to 7 lines 2000 feet long, commencing 200 feet from the loop edge and extending roughly 1000 feet either side of the VEM conductor.

We have contacted Scintrex and one of their field men will be in touch with you by telephone very shortly.

Sincerely, PATERSON, GRANT 6c WATSON LTD.

Norman R. Paterson NRP:knEncl: i cc: Mr. Wayne Zwickey

April 4,1973

W.Laughlln

Sharpe MPI and MoPhar OP?0 Magnetometer Surveys, Lot o. Concession 6, Crawford Township, Ontario*

l have attached Sharpe MPI and MoPhar OP?0 Magnetometer Survey plans covering Lot 6, Concession 6, Crawford Township* Ontario* l feel that results can be favourable compared and that you con sider the fallowing notes*

1*1 have Inked In 50 gamma contours on the MPI survey plan*

2, Field work was not done with any ooapetlon In mind and It Is likely that greater care was taken with the GP70 survey which followed the MPI survey work*

3* The relatively low MPI response on line 2000 East may be spurious*

4. There is an unexplained contradiction in the extreme southwest corner of the survey area*

AS/ A.Skreoky

Paterson, Grant &L Watson Limited f Consulting Geophysicist sSuite 2306, The Simpson Tower, 401 Bay Street, Toronto, Ontario, Canada M5H 2Y4

Telephone: (416) 868-0888 Cables: Norquest

May 9, 1973.


Dear Mr. Skrecky:

I enclose copies of maps showing Dr. Paterson's

interpreted positions of Turam conductors and recommended drill-holes on anomalies 3, 9 and 14.

Yours truly,

PATERSON, GRANT 6 WATSON LIMITED

R.K. Watson RKW:kn Encl: cc: Mr. Wayne Zwickey

Anomaly 3

As with Anomaly 38, the transmitter postions on this grid were such as to provide the least possible chance of locating the conductor should it be in the position shown on the INPUT maps. In fact, the EM profiles to the north and to the south, join at just about the position shown for the conductor. I realize that what your operator is trying to do is to divide the 2600 foot long profile into two sections, while maintaining a more or less east-west transmitter-receiver orientation. However, when the conductor of interest is in the center of the 2600 foot long profile, the overriding requirement is to have the transmitter as closely as possible on strike. I would not object under the circumstances to having the transmitter set up 600 feet east of the eastern line, and running the receiver 1300 feet north and south of the inferred conductor location. Again, one and preferably two additional lines should be surveyed west of the present grid, as the airborne anomaly improves in this direction.

ANOMALY #3, CRAWFORD TWP.

2o v O.

BASS" LINE"

• — C)

- o

___-C)—————O

40 ir

X),

•O--72-A'

— 10 hi

-C)'

60- wi

*4l

sj

3^9

-X—

,- id graph, po py tfcpy)i ia,d,jiopri. po tpy

H io groph po ly.^,^*

e\

*eV

2*'-

FORM 168A SM-12-7i-NPC

MCINTYREPORCUPINE MINKS

DEPARTMENT CORRESPONDENCE September 10, 1973 .Attention:Mr.....................A...Skrecky...........................................l*: Flotation Test

File: (2) Drill Core Material ..........................................................,.,....,...... Anomaly 3N

Abitibi OptionCrawford Township, Ont.

^Conclusions -

The result of three separate sulphide flotation tests performed on your drill core material from Crawford Township showed approximately 60y(, recovery of Nickel. Although copper recoveries varied from 30 to 50^o, this is inconclusive because of the very low copper grade to begin with.

It is possible that a slightly higher nickel recovery can be obtained by varying flotation reagent addition, using soda ash instead of lime for pll control, and, adding sodium silicate to lower the insoluble fraction in the concentrate.

JTest Procedure -

From the 15-pound sample of drill core received, we have evil 4 samples for assay and three 1500-gm samples for flotation test work. Each sample was treated the same. The particulars of flotation were as follows:

Flotation pH: 10. O adjusted with lime Frother: MIBC as required Xanthate: Sodium Isopropyl 0. 10 Ib/ton Promoter: Copper Sulphate 0. 5 Ib/ton Conditioning Time: 3 minutes Flotation Time: 6 minutes

J?f ilj Core aJL*lcLS5iv!:l Qu^o Ni 7o Fe "/o Inspire .™

B C D

Average

/l

0. 020. 050. 050. 040. 04

0.410. 370.490.480. 44

7.47. 17.47. 07. 2

FORM 168A. SM-I2-72-NPC

PORCUPINE MINKB L.IMITKD

DEPARTMENT CORRESPONDENCEAttention: Mr. B*: Page 2.

A

B

C

ConcentratesTailingsConcentratesTailingsConcentratesTailings

0. 370. 030. 180. 020. 17

2.470. 22

l l, 030. 20a. 10

0. 02 0. 22

10. 6

7. 7 7. 4

50. 8

Recoveries based on nickel assays were 54. 81 0fo, 67. 66^0 and 62. 5 07o respectively, for the three tests. Although the concentrate and tailing fractions were not weighed, the weights of concentrate was calculated to be 150 gms. , 430 gms. and 370 grns. , respectively, for the three tests.

'swPeter Kresin,Mill Superintendent.

H. ZwloKe,

Drill Hole Sections,Anomaly 3 and 9 Areas,Crawford Township, Ontario, "*,

I have attached sections for the Anomaly 3 *nd 9 Areas located on Lots 6 and 7, Concession 6, Crawford Township.

AS/sa A.Bkreoky

Wayne fi. ZwiokeyJune 19, 1973.

Drill Hole No. 904-73-3.Anomaly 38,Abitibi Option,Lot 6, Concession 6,Crawford Township, Ontario*

I have attached a copy of the oore log for drill hole No. 904*73*3 completed yesterday In Crawford Township* I have also attached 2 prints of a section showing this particular drill hole.

AS/sfl A.Skreoky

Wayne R. ZwiokeyJune 28, 1973.

Hole No. 90^73-**.Anomaly 3N,Abitibi Option,Lot 7 t Concession 6,Crawford Township, Ontario,

X have attached a copy of the oore log for Hole , 904*73-** completed recently in the Anomaly 3N area in Crawford Township. This hole is shown on A drill section a copy of which is appended.

AS/sa AtSkreoky

INTER-OFFICE CORRESPONDENCEfl| P.O. BOX St. COMMERCE COURT WEST •^* TORONTO. ONTARIO MSL 1C1

DATE July 20, 1973 ATTENTION OF Mr. A. Skrecky

SUBJECT Nickel Assays - DDK 904-73-4 (Anomaly 3N)

Regarding the question you raise in your July 19 memo; in my opinion the nickel assays obtained fall within the "normal" range for peridotites with nickel contained in the silicate lattice. Throw in a little nickelferous pyrrhotite and I definitely feel we do not have anything out of the ordinary. Your statement that the peridotite mass may elsewhere contain important nickel-copper mineralization certainly cannot be disproved on the basis of what we know about it. The question is where, in or at the edge of the mass, do we begin looking for the sulphide rich plum?

WRZ:sl

c. c. File

Wayne R.ZwlokeyJuly 19.1973

Drill Core Assay Results,Hole No. 904-73-**,Anomaly 3N,Abitibi Option,Crawford Township, Ontario.

l have attached page 4 of the core log for hole 904-73*4 showing the sample record for sample sections from this holv* l

f believe that the assay office has switched samples 12o?l and and l am having the latter sample assayed again.

The peridotite at the bottom of Hole 904*73*4 shows a relatively high nickel, copper and sulphur content near the contact that was tested. There is reason to wonder about the possibilities of important nickel-copper mineralization at other parts of this

l particular peridotite mass and near other inferred bodies in north- - era Crawford Township. Can we get an opinion on this from specialists

on this matter possibly with the Itoloonbridge organleatlon.

AS/ A.Skreeky

c' t"

P.Kresin

Flotation Test,Drill Core MaterialtAnomaly 3N,Abitibi Option,Crawford Township, Ontario*

July 24,1973

We have crushed about 15 pounds of drill core Material from Crawford Township and would Ilka to find out the amount of metal bearing sulphides that are present In the rook*' Can thin be done In the alne laboratory? Some notes on this Matter are tabled below*

1. Rook consists of serpentiniged peridotite with about 5 percent sftlphide mineralisation. The rook assays about 0.30 percent nickel and 0*06 percent copper*

2. We would like nickel and oopper analysis on any sulphide fraction that can be floated off*

AS/ A.Skreoky

September 20,1973l .'- "

Wayne R. Zw l ok oy

Niokeliferous peridotite,Anomaly 3N Area,Abitibi Option,Lots 6 and 7 1 Concession 6, ,Crawford Township, Ontario*

l have attached two copies of a Hill report covering a flotation test on drill core from the bottom part of Hole No. 904-73-*** The test material was obtained by nixing rejects from the following samples*

' ,

Sample No. from Footage to feet! '

12673 396.5 to 401*5 5.012674 424.0 to 426*5 2*512675 436.0 to 441.0 5.0

The mill test shows that the hanglngwall area of the peridotite has a significant sulphur, nickel sulphide and .copper content* This particular mafic body would then have potential for nickel ore concentrations according to Cameron et al (se'e attached abstract).

Consideration should be given to testing the footwall area of the peridotite for a nickel sulphide concentration* An attached work sheet shows additional information with respect to the magnetic picture in the Anomaly 3N area*

AS/ A.Skreeky


ATTENTION OF

SUBJECT

P.O. BOX 51. COMMERCE COURT WEST TORONTO. ONTARIO MSL 1 CI

Mr. A. Skrecky

Anomaly 3, Abitibi Option, Crawford Township^^^^^

DATE September 28, 1973

Enclosed are four copies of the magnetometer

check survey for the above area showing the location of

drill holes drilled in 1973.

The field map of that area is attached.

R. Guenther

RG: sic. c. File

Encs.

December 4,1973

Wayne H.Zwlokey

proposed Drill Test, Anomaly 3N Area, Abitibi Option, Lot ?, Concession 6, Crawford Township, Ontario.

An attached section shows geophysical and geological information In the Anomaly 3N area located in the northerly part of Crawford Township. The section shows the rook formations intersected by Hole 904-73-4 drilled here last June. This hole bottomed In a sulphur rich peridotite. A flotation test was carried out on a 15 pound sample of crushed core which assayed 0*44 percent nickel* 61*7 percent of the contained nickel was floated off in a sulphide concentrate which assayed 1.80 percent nickel and 0.24 percent copper*

The presence of a sulphur rich peridotite showing an appreciable nickel sulphide content is considered to be an important feature from an economic standpoint. Several authors (Naldrett et al) suggest that nickel orebodies can occur In the footwall area of such peridotite masses* ; * 1 ,

Little is diectly known about the geological history of the northerly part of Crawford Township, The accompanying section Indicates that our drill test expored the hangingwall areaion of the peridotite and that anomalous features are present in the footwall area*

A diamond drill test of the footwall section is proposed on line O where a sharp magnetic .gradient Is present*

AS/ A.8kreeky

ANOMALIES CRAWFORD TWP.

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4aAMSW00a6 63.4827 CRAWFORD 070

REPORT ON TEST INDUCED POLARIZATION SURVEY

ABITIBI OPTION CRAWFORD TOWNSHIP. ONTARIO

ON BEHALF OF MCINTYRE PORCUPINE MINES LTD.

Bale D'Urfe, QuS. July 12th, 1971 KARL GLACKMEYER, Eng.

KARL GLACKMEYER fi ASSOCIATES LIMITED

l l l l l SUMMARY

l The present induced polarization survey

has been successful in penetrating 100' to 200' of

i clay type overburden, as well as outlining a very

B broad strong zone of above normal polarization res

ponse. A weak zone has been outlined and is considered

l to be due to a very deep zone of a lateral effect of

an adjacent zone. The strongest zone displays a peak

l chargeability zone of 50.0 milliseconds over a back-

m ground of 3.0 to 4.0 milliseconds. The most probable

explanation for the bulk of this zone is 15% to 208

l disseminated metallic conductive minerals within a

zone of basic to ultra-basic rocks. Although graphite

l could be the source for various reasons explained

m within this report, the author feels the source is

probably finely disseminated magnetite and/or sulphides

l and magnetic sulphides.

l

l

lKARL GLACKMEYER a ASSOCIATES LIMITED

l l l l l l l l l

l l l l

REPORT ON

TEST INDUCED POLARIZATION SURVEY

ABITIBI OPTION

CRAWFORD TOWNSHIP. ONTARIO

ON BEHALF OF


INTRODUCTION

j During June 1971, a geophysical party,

under the direction of the author, carried out a test

l induced polarization survey on a portion of the Abitibi

Option, Crawford Township, Ontario, on behalf of

" Mcintyre Porcupine Mines Ltd.

The induced polarization survey was carried

l out using a Scintrex Mark VII pulse type unit of high

sensitivity, with a remote receiver of the Newmont

type. The current on-time was 2.0 seconds and the

measuring time was 0.5 seconds. Measurements are made

from which are derived two (2) physical properties,

namely, the chargeability (that is the I.P. factor),

which is expressed in units of milliseconds and the

KARL GLACKMEYER * ASSOCIATES LIMITED

l l

REPORT ON TEST I.P. SURVEY RE ABITIBI OPTION______-2-

lD. C. resistivity which is expressed in units of ohm-

l

l

meters.

The purpose of the present survey was to map

l the distribution of disseminated metallic conductive

minerals within the underlying rocks; as well as to

l determine the effectiveness of this geophysical method

M in areas where overburden measures 100' to 200' or

more and is principally-composed of clay.

lThis type of survey is capable of mapping

most disseminated sulphides, such as pyrite, pyrrhotite,

chalcopyrite (but not sphalerite) and graphite. Magne

tite and serpentine are known to have moderate polari-

I zation response. It is rarely possible from I. P. data

alone to differentiate between these various potential

l sources of polarization response.

B


This induced polarization traverse was carried

M out along Line 8E extending from stations 36S to ION

using a three-array electrode configuration with an

lKARL GLACKMEYER l ASSOCIATES LIMITED

11 t 1111111111111111i

REPORT ON TEST I. P. SURVEY RE ABITIBI OPTION -3-

electrode spacing of 400'. The two hundred and one

hundred foot electrode configurations were used over

certain zones of interest.

The background in this area is considered

to be 3.0 to 4.0 milliseconds; values in excess of 6.0

milliseconds are considered to be anomalous. Two zones

have been outlined, one weak response at 26S and a very

strong response in the northern segment of the line.

The profile for the 400 1 electrode spacing is characte

rized by a weak double peak anomaly, the maximum res

ponse being 6.3 milliseconds, a slight depression in

the corresponding resistivity is noted. The profile

for the 200' electrode spacing indicated no response.

The most probable explanation for the obser

ved effect is a source at depths exceeding 300' or a

lateral effect from an adjacent source. In order to

ascertain which of the two possibilities are most

plausible, additional induced polarization surveying

would be required. Information from near-by drilling

may be helpful in interpretating this data.

———————————— KARL GLACKMEYER S, ASSOCIATES LIMITED

REPORT ON TEST I.E. SURVEY RE ABITIBI OPTION

l l l l

A large zone of very strong polarization

™ response has been outlined between stations 8S and ION.

B The 100', 200' and 400' electrode spacings were employed

over this zone and peak chargeabilities increased with

l electrode spacings. A maximum of 50.0 milliseconds

— was observed on the 400' electrode spacing between

" stations 5N and 6N. The corresponding resistivity data

U show a broad but distinct depression coinciding with

peak chargeability values.

lA previous magnetic survey has outlined a

B zone of high magnetic Intensity representative of a

M mass of ultra-basic rocks; drilling to the west has

confirmed the presence of ultra-basic rocks under 100

B feet to 120 feet of clay overburden.

B The most probable explanation for the bulk

M of the observed effects would be 15% to 20% dissemi

nated metallic conductive minerals within the under-

I lying lithologies. Whereas either graphite, sulphides

or magnetite could be responsible for the observed

B polarization effects, considering the intensity of the

ll ——————————————————— KARL GLACKMEYER 4 ASSOCIATES LIMITED ————————————————

l l l

REPORT ON TEST I.P. SURVEY RE ABITIBI OPTION -5-

lM response and rather heavy clay overburden, the author

* feels that the observed response must be attributed to

l a combination of finely disseminated magnetite and

sulphide mineralization. Graphite could be a factor;

g however, this possibility is secondary as graphite

— would not usually be disseminated over such widths.

™ It would be of interest to further evaluate this zone

l with additional induced polarization surveying before

drilling is considered.

Respectfully^ubmitted,

y -^-———— ^^

I Baie D'UrfS, Que. July 12th, 1971. KARL GLACKMEYER, Eng,

l

l

l

l

l

ll ——————————————————— KARL GLACKMEYER i ASSOCIATES LIMITED —————————

43AHSWeea6 63.4827 CRAWFORD 080

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42AMSW0026 63.4827 CRAWFORD 12)30

r

Geophysical Surreys, Abitibi Option, Anomaly 7 ana Anon*!? 8, Lot 8, Cono9011onB 5 and 6, Crawford Township, Ontario*

l have attached 200 soale plan* showing th* V.X.K. and magnetometer nurrey results oyer Anomaly 7 and Anomaly 8 located on Lot 8, Conoeesiona 5 *nd 6* Crawford Township, Ontario*

AS/ A.Skreoky

Anomalies 7 and 8~

We did not pick these anomalies as being ofparticular interest, though they certainly are not explained, The ground results are consistent with the airborne, and our feeling is that they are probably due to graphite, with some overburden effect contributing.

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PATERSON, GRANT 6 WATSON LTD.

i formerly; t Paterson fc Associates Limited f Consulting Ceophystci'stsi.--''' Suite 2306, The Simpson Tower, 401 Bay Street,Toronto 103, Ontario, Canada. (416) 363•4261. Cat

W. H. T.

m 9 MAR 1973esfNorquest.

Norman R. Paterson, Ph.D., P.Eng. Roger K. Watson, B.A.Se., P.Eng. Fraser S. Grant, Ph.D., P.Eng.

March 28, 197S.


RE; ANOMALIES 3, 9, 8, CRAWFORD TWP.

Dear Alec:

We would judge that the above anomalies are now sufficiently well located to justify detailing before drilling. Accordingly we submit proposed line grids and transmitting loop locations for Turam surveys.

Each grid consists of 5 to 7 lines 2000 feet long, commencing 200 feet from the loop edge and extending roughly 1000 feet either side of the VEM conductor.

We have contacted Scintrex and one of their field men will be in touch with you by telephone very shortly.

Sincerely, PATERSON, GRANT S WATSON LTD.

LANorman R. Paterson

NRP:knEnd: ycc: Mr. Wayne Zwickey \/

f: ''i .

.Me /NT/RIi: pOKCOpjNE: MINT'S LTD ABlTlfti OPTION ANOMALY 4 '6

t ' Lot 8 C OVA C f S S i c*\ l S" -4 (c Cre^-Ajit-.-f/ Ivof . f*\f.

S E 7) TURAM TYPE SOKVEY

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MEMO

TO: Alec Skrecky

FROM: R.K. Watson May 14th, 1973,

SUBJECT; ANOMALY #8, CRAWFORD TOWNSHIP

The anomaly resolves into two conductors which start together at Line 3E and gradually separate toward the west. The northernmost conductor, which was also detected by the vertical loop EM survey, has the highest conductivity- width, has some coincidence with a 150-gamma magnetic anomaly and is recommended for drilling. The vertical loop EM work suggested a vertical dip; the airborne study indicated a dip to the south and so we recommend drilling from south to north. The #1 priority drill-hole is recom^ mended collared at 27 '-f JLOSLjon,JLine. 3W dipping 50 freete'to the north and if this should be encouraging we recommSfid a second hole at 28 * 20S, dipping 50 degrees to the north which will also intersect the top of the second weak conductor.

(A/.

Roger K. Watson

MEMO

TO: Alec Skrecky

FROM: R.K. Watson May 14th, 1973,

SUBJECT; ANOMALY #8, CRAWFORD TOWNSHIP

The anomaly resolves into two conductors which start together at Line 3E and gradually separate toward the west. The northernmost conductor, which was also detected by the vertical loop EM survey, has the highest conductivity- width, has some coincidence with a 150-gamma magnetic anomaly and is recommended for drilling. The vertical loop EM work suggested a vertical dip; the airborne study indicated a dip to the south and so we recommend drilling from south to north. The #1 priority drill-hole is recom mended collared at 27 + IDS on Line 3W dipping 50 feet to the north and if this should be encouraging we recommend a second hole at 28 * 20S, dipping 50 degrees to the north which will also intersect the top of the second weak conductor.

Roger K. Watson

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MAGNETOMETER a EM. 16 TRAVERSESOUTH UZ LOT7 CONCESSION VI CRAWFORD TOWNSHIP

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DATE July 16,1973

ATTENTION OF Way ne H.Zwickey

r-nm^-r l? Test Work, SUBJECT Anomaly 8 Area,

Abitibi Option,Lot 8, Concession 5tCrawford. Township. Ontario.

Glo.clrr.oyer hns conpleted a fast IP traverse along the wh!.eh cronies the east end of Anomaly 8. An attached raap

shows the location of this work.

Field reports indicate that the anomaly area corresponds to weak chargeability (5*3 milliseconds) having no narked resistivity pattern.

^The IP response over this part of the zone is not iraressiveand we will proceed with the recommendations Paterson tabled in his June,1973 report.

AS/ A.Skrecky

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Input Intercej*:

Wayne B. ZwiekeyAUgUSt

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Diamond Drill Test, Anomaly 8, Abitibi Option, Lot 8, ConeosBIon 5, Crawford Township* Ontario,

I have examined the core for hole no. ^.73*7 recently tested anomaly 8 in Crawford Township*

•.-t'f.-'fs.f:~' "' frv* V* .-•'^•itf' ^i*-

oortsections hay* been sent out for gold assay* X taMpl* record ghe* t will be sent to you when theassay results are received* ^- ' - ' - . '-'i1 ..'-" i :*itv'.fi' *''V' / : 'f"'y-'; ' ?'v-'

There is no conductive material in the hole to aooount f or the anomaly present at this location* The Minor pyrrhotite* ' chalcopyrite mineralisation present in the lower part of the hole is not associated with any marked magnetic feature (see attached survey plan)* . . : ; : ;^.-*-..;- ! '/.r ,/ ;.-.-; v -1 ;' ^''^;-v^'^f.;*v •:'-.

- ; " "' -" - ," T -: r- ' -f .1' -i-^ '. ^'.' '- .'- * : -:' --

The magnetic anomalies elsewhere In the *ap however represent concentrations of pyrrhotite min and should be further inreatlga ted* ' ' '*.. \--^'

satipn'*

Additional surrey work Is scheduled east of the map area during 'the coming week*' ...'.-" . ,, '' ;f ,,: .. .v- vi-'-;-:;'.: '" ; -" ".r-"''-!^'"

AS/sa A.SkreckyA'*'

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Paterson, Grant and Watson LimitedSeptember 6, 1973*

Anomaly 8,Abitibi Option,Lot 8, Concession 5*Crawford Township, Ontario,

We have attached preliminary magnetometer and V.E.M. survey data covering the easterly part of Anomaly 8*

AS/sa A.Skreoky

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Paterson, Grant ^Watson Limited/Consulting GeophysicistsSuite 2306, The Simpson Tower, 401 Bay Street, Toronto, Ontario, Canada M5H 2Y4

Telephone: (416) 868-0888 Cables: Norquest

Mr. Alec SkreckyMcintyre Porcupine Mines LimitedSchumacherOntario

Dear Alec:

Re: Anomaly 8, Crawford Township

I have received the HEM results on this anomaly. Two conductors are obvious, both of them further north than the vertical loop EM conductor traced from the west. Both conductors are of very low conductivity and are probably related to overburden.

In my opinion, although the drilling of this anomaly was not completely conclusive, there is no doubt that you intersected the best part of the conductor and the magnetic body. I can see no justification for further drilling on this grid.

Sincerely,

PATERSON, GRANT S, WATSON LIMITE0

NRP:u Norman R. Paterson

c.c. Wayne Zwickey

B*

REPORT ON


CAMP 40 ROAD TRAVERSE

OARNEGI-E TOWNSHIP. ONTARIO

on behalf of


Bale d'Urfe, Qugbec September 5th, 1973 Karl Glackmeyer, Eng.

KARL GLACKMEYER ft ASSOCIATES LIMITED, Geophysical Consultants and Contractors 716 Cornwall Drive Bale D'Urfe 850, Quebec (514) 453-1982

REPORT ON


CAMP 40 ROAD TRAVERSE

CARNEGIE TOWNSHIP. ONTARIO

on behalf of


INTRODUCTION

During July 1973, a geophysical party, under the direction of the author, carried out an

induced polarization traverse on a portion of the Camp 40 Road, Carnegie Township, Ontario, on behalf of Mcintyre Porcupine Mines Ltd. The traverse

extended 4,400 north of mileage 21 along the Camp

40 Road.

The induced polarization survey was

carried out using a Scintrex Mark VII pulse type unit of high sensitivity, with remote receiver of

the Newmont type. The current-on time was 2.0 seconds

and the measuring time was 0.5 seconds. Measurements

are made from which are derived two (2) physical properties,


INDUCED POLARIZATION SURVEY RE: CAMP 40 ROAD TRAVERSE .2

namely, the chargeability (that is the I.P. factor), which is expressed in units of milliseconds and the D.C. resist

ivity which is expressed in units of ohm-meters. The pole-dipole electrode configuration was employed using

a 400* n - l electrode separation for maximum resolution and depth penetration. Additional investigation was

carried out between 16S to 32S employing the a - 400'

n m 2 electrode separation for greater penetration.

The purpose of the present survey was to

map the distribution within the underlying rocks, of disseminated metallic conductive minerals; such as

pyrite, pyrrhotite, chalcopyrite (but not sphalerite) and graphite. Magnetite and serpentine are known to have moderate polarization response. It is rarely possible from I.P. data alone to differentiate between these


Drawing 1301-31?;' S R shows in profile the chargeability and resistivity data on a 200' scale. The chargeability data has been plotted on a scale of l" a 10 milliseconds; whereas, the resistivity has

been plotted on a scale of l" s 200 ohm-meters. The chargeability values range from 2.7 milliseconds to a maximum of 5.1 milliseconds for the n m l separation and a maximum of 5.3 milliseconds for the n m 2 separation.

The corresponding resistivity data varies from 195 ohm- meters to a maximum of 599 ohm-meters.


INDUCED POLARIZATION SURVEY RE: CAMP 40 ROAD TRAVERSE .3


The present induced polarization profile hasoutlined one zone of moderately high chargeability response.

The corresponding resistivity data does not show any characteristic pattern; however, the zone of polarization is located immediately south of a contact between a zone

of higher resistivity values.

The most probable explanation for the observed effects is a zone enclosing a maximum of 5% disseminated

metallic conductive minerals within the underlying rocks. The resistivity data indicates the zone to lie at the contact of different geologic units. Magnetite or an ultra basic mass could give rise to similar effects.

Should the source of polarization not yet be

known, it is recommended that additional work be carried

out in order to further delineate this zone.


Karl Glackmeyer, Eng

KG/gc


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March 12,1973 x

Paterson Grant Mid Watson Malted

Anomaly Abitibi Option, Lot 3, Concession *tv Crawford Township, Ontario.

l have enclosed a copy of a report covering an IP survey over parts of Lots l to 4 inclusive, Concession 5, Crawford Township. Survey work was oarried out on line 5200 West which covers the easterly end of input Anomaly 24."

Other geophysical infornation la now being plotted at our Toronto office where Eudl Oaenther our draftsman has been asked to forward the following maps to you*

Magnetometer survey map (Sharpe MF 1)Magnetometer survey map (McPhar QP 70]V. B. M. Survey map (Mofhar 88 15]An assessment of the easterly part of the survey area has

been prepared and is on file at our Toronto offloe.

AS/ A.Skreoky

I.

R.Gu witherllaroh 12,1973

Geophysical BurrayB, Anonaly 24, Lot 3* Concession 4, Crawford Township, Ontario. (Abitibi Option)

Please plot the following Information on the plate that was earlier prepared covering Lots l to 4, Concession 4-, Crawford Twp.1. OP 70 magnetometer readings on Lines 5200 West, 56,60 and 6400 West2. MoPhsr V.B.K. profiles on the above picket lines.

Would you then send one print of eaoh along with a print of the HP l oagnetoaeter survey on Lots 2 to 4 inclusive to the following address.'

Paterson Grant and Ha teon Limited, Suite 2306, The Simpson Tower* 401 Bay Street,

f Toronto 103, Ontario.l aa today sending these people other notes on the above area

and will mention that the above prints will be forwarded to them from our Toronto offloe, it would be of soae help If your aaps refered to Anomaly 24 which lies on Lot 3* Concession 4, Crawford Township.

Many thanks Budi.

AS/ A.8k**oky

Anomaly 24Atofc. .A i h*

The I.P. survey performed on this anomaly early this year covered the eastern portion only, though one line (Line 84W) did cross a portion of the conductor. This line also produced a good I.P. response, though south of the inferred conductor position. I shall be interested in seeing the EM and mag results on this grid, particularly over the western portion.

PATERSON, GRANT S WATSON LIMITED

\ formerly: man Pa erson & Associates Limited t Consulting Geophysicists

^^ Suite 2306, The Simpson Tower, 401 Bay Street, Toronto 103, Ontario, Canada. (416) 363-4261. Cables: Norquest.

Norman R. Paterson, Ph.D., P.Eng. Roger K. Watson, B.A.Sc., P.Eng. Fraser S. Grant, Ph.D., P.Eng.

March 21, 1973.

Mr. A. Skrecky,Mcintyre Porcupine Mines Ltd.,Schumacher,Ontario.

RE; ANOMALY 24, CRAWFORD TOWNSHIP

Dear Alec:

We have just received the EM and mag data over Anomaly 24. We note that the magnetometer work adequately covers the inferred position of the conductor, but that the EM work, which was done last December, actually covers Anomaly 26, some 1000 to 1200 feet further south. Possibly you did additional EM work that we are not aware of?

If not, we would suggest that you locate a transmitter roughly at the base line on Line 52W, and run profiles on Lines 56, 60 and 64W, then run Line 52W with the transmitter on Line 64W.

Anomaly 26 appears to have been drilled and explained as graphite.

Yours sincerely, PATERSON, GRANT 6 WATSON LIMITED

Norman R. PatersonNRP:kncc: Mr. Wayne Zwickey

Paterson Grant and Wataon LimitedMarch 30,1973

Data, Anomaly 2,4, Abitibi Option, Lot 3, Concession k, Crawford Township, Ontario*

l frave attached a revioed V.B.M. Survey plan covering Anomaly 24 located on Lot 3, concession 4, Crawford TownBhlp,

A.Skreoky

Itodi GuunthorHarch 33,1973

Oeophyyical Data* Anorjaly 24, Abitibi Option, Lot 3, Concession Crawford Township*

l have attache:! a HcPhar V.E.H. Survey plan ohowln^ addition*]. EH work carried out In thu Anpualy 24 aroa. Ploaeo add thio Information to the survey plan prepared oarllor for this area* Would you cent Paterson Grant and Watson one oopy of the revised nap.

AS/ A.Skreeky

Pa


formerly: :ersoi)' fe Associates Limited l Consulting Geophysicists

Suite 2306, The Simpson Tower, 401 Bay Street, Toronto 103, Ontario, Canada. (416) 363-4261. Cables: Norquest.


April 5, 1973.


RE: ANOMALY 24, CRAWFORD TOWNSHIP

Dear Alec:

I enclose a print of your recent VEM survey map for the above anomaly, showing what I regard to be an appropriate Turam program.

As with the other Turam grids, I understand that a single frequency will be used for the grid as a whole, but that one profile (the one that shows the best anomaly on the initial coverage) will be re-surveyed with a second frequency. My preference would be to use the intermediate frequency for the initial coverage and the low frequency for the detail profile.

Yours sincerely, PATERSON, GRANT S WATSON LTD,

'(X-^'VWv

Norman R. Paterson NRP:kn Encl: cc: Mr. Wayne Zwickey

MctNT^Re PORCUPINE MINES LTD. A6me\ OPTIONSE 71 TURAM SO!

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IP Test Work,Anomalies 24, 25 and 25A,Abitibi Option,Lots l, 2 and 3, Concession 4,Crawford Township, Ontario,. . .

We have attached preliminary work data showing the results of IP test work on lines 2800 West. 3200 West, 3*00 Vest, 4000 west, 4800 west and 5200 West covering the above listed anomaly areas located In Crawford Township. Work on lines 0. to 2400 West should be completed today. Information on these lines will be available early next week* ; - *

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REPORT ON


CRAWFORD I GROUP PHASE II


on behalf of


Bale d'Urfe, Quebec September 9th, 1973 Karl Glackmeyer, Eng,

KARL GLACKMEYER A ASSOCIATES LIMITED, Geophysical Consultants and Contractors 716 Cornwall Drive Bale D'Urfe 850, Quebec (514) 453-1982

REPORT OK


CRAWFORD I GROUP PHASE II


on behalf of

MCINTYRE PORCUPINE MINES LTD

INTRODUCTION

During July 1973, a geophysical party, under the direction of the author, carried out an induced polar ization survey on a portion of the Crawford I Group, Crawford Township, Ontario, on behalf of Mcintyre

Porcupine Mines Ltd. This work, entitled Phase II, follows previous work carried out in November and

December 1972.

The induced polarization survey was carried out using a Scintrex Mark VII pulse type unit of high

sensitivity, with remote receiver of the Newmont type. The current-on time was 2.0 seconds and the measuring time was 0.5 seconds. Measurements are made from which


INDUCED POLARIZATION SURVEY CRAWFORD I GROUPPHASE II .2


chargeability (that is the I.P. factor), which is expressed in units of milliseconds and the D.C. resist ivity which is expressed in units of ohm-meters.

The pole-dipole electrode configuration was

employed with electrode separations of "a" s 200 for

n s 2, 3 and 4. This survey covered from L-0 to L-52W; from 14N to 14S inclusively.

The purpose of the present survey was to determine, within the underlying rocks, with greater definition and resolution, the distribution of dissemi

nated metallic conductive minerals; such as pyrite,

pyrrhotite, chalcopyrite (but not sphalerite) and graphite. Magnetite and serpentine are known to have

moderate polarization response. It is rarely possible from I.P. data alone to differentiate between these



Drawings 1301-2-IP and 1301-2-R show in plan, the chargeability and corresponding resistivity data on a scale of 200' to the inch. The chargeability has been contoured at 2.5 millisecond intervals while the resistivity has been contoured logarithmically. Drawings

1301-2IP 8. R, A to K inclusively, show the chargeability

KARL GLACKMEYER i ASSOCIATES LIMITED


and corresponding resistivity data in contoured sections

on a scale of 200' to the inch for the pole-dipole

electrode configuration "a" s 200' for n s 2, 3 and 4.

The chargeability data has been contoured at 2.5 milli second intervals whereas the resistivity has been contoured logarithmically.

The present data has outlined three zones of abnormally high polarization response as these have been labelled Zones A, B and C. The corresponding resistivity data has outlined four zones of abnormally low resistivity response and these have been labelled R-l to R-4 inclusive ly.

Zones A S B

The present^ Phase II geophysical programme, employing the pole-dipole "a" e 200' n B 2, 3 and 4 has

confirmed both Zone A and Zone B in the same manner as has been described in the Phase I report.

The only change observed is that the maximum

polarization response within Zone A is 30,6 milliseconds observed at station 8S with the n a 4 electrode separation, The corresponding resistivity data is 67.0 ohm-meters.

f...



Zone C

The Phase II programme covered from L-16W to

L-0; thus, has outlined Zone C not previously known

in the Phase I programme. This zone extends from

L-16W to L-0 and is outlined by the 15.0 millisecond

contour. The maximum polarization response observed

within this zone is 48.0 milliseconds and corresponds

to a resistivity value less than 1.0 ohm-meters. The

bulk of Zone C corresponds to a portion of a large resist

ivity anomaly labelled R-3 enclosing value less than 50

ohm-meters. The contoured sections covering this zone

indicate a slight dip to the north. The maximum

polarization response was observed with the n e 3

electrode separation which would indicate the zone has

potential in depth.

The most probable explanation for the observed response would be a relatively narrow tabular type body enclosing between 20% to 2525 disseminated metallic minerals by volume. Since metallic conductive minerals

could be either sulphides or graphite, it is not possible, from the present data, to differentiate between these

potential sources of polarization response. However, judging by the extremely low resistivity values, massive

sulphides and/or graphite are suspected to be the source.



The following diamond drill hole is suggested

in order to sample Zone C; if this has not already been

carried out.

Collar:- 8+OOW 7+30SDip:- -50 0

Direction:- south or azimuth 180OLength:- 600'

The present resistivity survey has outlined four zones of abnormally low resistivity response.

Zones R-l and R-4

These zones are situated in the northern segment of the area under study and are outlined by the 200 ohm-meter contour. These zones are on strike, and in the author's opinion, are considered part of the same horizon. This horizon corresponds to a slight increase in chargeability, the maximum response being 13.2 milli seconds.

The most probable explanation for the observed

resistivity results, as well as the corresponding increase in chargeability, is a relatively narrow, tabular body,

extending from L-36W to L-0 and still open to the east. This body is estimated to enclose between 535 to 10%

x...



disseminated metallic conductive minerals by volume.

Since metallic conductive minerals could be either

sulphides or graphite; it is not possible, from the

present data, to differentiate between these potential

sources of polarization response.

Resistivity Zone R-2 extends from L-28W to

52W and is outlined by the 100 ohm-meter contour. The

minimum resistivity value observed within these zones

is 82.0 ohm-meters.

The most probable explanation for this

observed resistivity response is a relatively narrow

zone, having a slight dip to the north, enclosing

massive sulphides and/or graphite.

Resistivity Zone^ R-3 is outlined by the 50

ohm-meter contour and is open to the south-west. This

zone is on strike with resistivity Zone R-2; however,

is much broader arid encloses resistivity values less

than 1.0 ohm-meters. The most probable explanation for

the observed effects is a very broad zone enclosing massive

sulphides and/or graphite; This zone may also represent

a number of narrower parallel conductors,


Phase II has confirmed the presence of Zone

A and Zone B with greater definition and has outlined

a new zone labelled Zone C. The Phase II data indicates


INDUCED POLARIZATION SURVEY CRAWFORD I GROUPPHASE II__________________ .7

that Zone A probably plunges to the east under sterile

rock or that the overburden becomes deeper to the east. The recommendations proposed by the author in the Phase I report still remains the same and no further recommend ation can be made for these zones. One drill hole has

been suggested in order to sample Zone C.

Four zones of abnormally low resistivityvalues have been outlined; R-l and R-4 are considered to

be part of the same horizon and are associated with a slight increase in chargeability data. Should the

presence of economic minerals be encountered within Zones A, B or C, then additional work would be required to the north to further delineate the horizon outlined by resistivity Zones R-l and R-4.


Karl Glackmeyer, Eng,

KG/gc

KARL GLACKMEYER l ASSOCIATES LIMITED

INTER-OFFICE CORRESPONDENCE55 YONGE STREET, TORONTO, ONT.

ATTENTION OF Wayne B.ZwiokeyDATE October 10,1/73

SUBJECT Detailed Magnetometer Survey,Anomaly 25 Area, Abitibi Option, lot l. Concession Jf, Crawford Township* Ontario.

Johnson*s lineoutting orew started work in the Anomaly 25 area today, laying out pioket lines at 100 foot Intervale south of the base line between zero and 1600 West* These lines will be 1300 fdot long* ,

Johnson will carry out a magnetometer surrey on these lines to detail the anomalies known to odour in the area* This work should be completed during the coming week.

AS/ A.Skreoky

fcV ,

Budi GuentherJuly 13,1973

. . "' i*c'

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Anomaly 25 and 25A Area,Abitibi Option*Lot It Concession 4VCmwf&rd Townehip, Ontario*

Please plot the attached magnetometer readings on a mag plate that you prepared last Deoember, covering Lots l to 4 inol., Conoeaeion 4, Crawford Township. Some magnetometer work was done here earlier by fi.Collins, at 200 fpot line epaolnga in the easterly part of Lot l, Concession 4. This particular survey was plotted in June,1971. covering the Input 365R area. Use can use Collins1 information to contour in anomaly features that lie between the lines shown on the accompanying work sheet.

Would you send copies of the revised Magnetometerf Survey plan to Zwiokey., Paterson and this office.

AS/ A.Skreoky

r("O

L.BoudriasO.E.Hloks October 20,1972

Bxploration Program,Abitibi Option,Crawford Township, Ontario.

It seems likely that we will be carrying out llneouttlng and geophysical surveys over the north half of Lots 1,2,3,** and 5* Concession ^, Crawford Township* There are tangential Input anomalies in this area as shown on the Input Compilation for Bast Crawford West Lucas Townships.INCO has drilled two interesting holes in the east part of the area described above where rooks outcrops were uncovered last year* Air Photos show other possible outcrop areas which should be checked out as soon as possible* These features lie in the south half od! Lot 12, Concession 4, Lucas Township* the north half of Lot 2 and Lot 3, Concession 4, Crawford Township. These features oan be examined on stereo paired air photos field copies of which oan be taken out of the office* The above area should be given a general examination to judge whether llneouttlng is practical at present or whether a winter program is essential.

AS/ AiSkreoky

REPORT ON


CRAWFORD I GROUP


on behalf of


Bale d'Urfe, Quebec January 26th, 1973 Karl Glackmeyer, Eng,


REPORT ON


CRAWFORD I GROUP


on behalf of


INTRODUCTION

Between November 28th to December 6th,

1972 and December 12th to December 15th, 1972, a geo

physical party, under the direction of the author,

carried out an induced polarization survey on a portion

of the Crawford I Group, Crawford Township, Ontario,

on behalf of Mcintyre Porcupine Mines Ltd.

The induced polarization survey wascarried out using a Scintrex Mark VII pulse type unit

of high sensitivity, with remote receiver of the Newmont

type. The current-on time was 2.0 seconds and the measuring

time was 0.5 seconds. Measurements are made from which


chargeability (that is the I.P. factor), which is express ed in units of milliseconds and the D.C. resistivity which

is expressed in units of ohm-meters. The three-array


INDUCED POLARIZATION SURVEY CRAWFORD I GROUP .2

electrode configuration was employed using a 400* electrode

separation for maximum resolution and depth penetration. Detailed investigation was carried out over anomalous

zones using electrode separation of 200 1 , 400 1 and 600'.

The purpose of the present survey was to map the distribution within the underlying rocks of

disseminated metallic conductive minerals; such as pyrite, pyrrhotite, chalcopyrite (but not sphalerite) and graphite. Magnetite and serpentine are known to have moderate polarization response. It is rarely possible from I.P. data alone to differentiate between these various potential sources of polarization response.


Drawing No. 1211 VII I.P. and drawing No. 1211 Plate VII R show the chargeability and resistivity data in contour form on a scale of l" s 200 feet. The

chargeability data was contoured at 2.5 millisecond intervals; and the resistivity contoured logarithmatically. Drawing No. 1211 Plate VII I.P. and R show the detailed chargeability and resistivity profile over L-20W and L-28W

employing electrode separation of 200', 400' and 600'. The milliseconds, while the resistivity is plotted on a logarithmic scale.



The present induced polarization survey

was carried out in a reconnaissance fashion over the major portion of the area under study; while, more

intensive and detailed investigation was carried out between Line 16W and Line 36W. The chargeability values

range from - 3.2 milliseconds to a maximum of 30.5 milliseconds. The 15.0 millisecond contour has outlined

two areas of abnormally high polarization response labelled Zone A and Zone B.

The corresponding resistivity data ranges from 4.0 ohm-meters to a maximum of 1561 ohm-meters. The present resistivity data has outlined three zones of abnormally low resistivity values and these have been labelled R-l, R-2 and R-3.

Zone A

This zone is more properly outlined bythe 15.0 millisecond contour and the maximum polarization response observed within this zone is 24.9 milliseconds.

The zone strikes in a north-westerly direction and extends over a length of approximately 1,000 feet. The correspond ing resistivity values range between 100 to 200 ohm-meters while resistivity low R-2 coincides with the western edge

of Zone A. The resistivity values enclosed within R-2 are less than 100 ohm-meters and the minimum value observed is 89.0 ohm-meters.


INDUCED POLARIZATION SURVEY CRAWFORD I GROUP___ .4

Detailed investigation was carried out over this zone one Line 28W. These profiles show that the polarization increases proportionally with the increase in electrode separation; while in each case,

peak polarization responses coincide with a slight depression in resistivity.

The most probable explanation for theobserved polarization effects within Zone A, would be

a vertical lens or chimney like structure, having good potential in depth, enclosing between 15% to 2(^ disseminated metallic conductive minerals by volume.

Whereas, metallic conductive minerals could be either

sulphides or graphite; sulphides are favoured as the corresponding resistivity data is in excess of

100 ohm-meters. The depth of overburden is considered to be approximately 50 feet.

Zone B

This zone is located immediately north

east of Zone A; similarly to Zone A, it is outlined

by the 15.0 millisecond contour and the peak polarization response observed within this zone is 30.5 milliseconds. The zone strikes in a north-westerly direction over a

length of approximately 1,000 feet. The south-east segment of Zone B coincides in part with resistivity low R-3.



Detailed investigation over this zonewas carried out one Line 20W. These profiles show that

the polarization response increases progressively with electrode separations. Each peak polarization response corresponds to a slight resistivity depression, with the

exception of the 600 foot electrode separation, where the peak polarization response coincides with a good resistivity depression.

The most probable explanation for thebulk of Zone B, is a lens or chimney like structure having a vertical orientation and good potential with depth. It would require between 15% and 20% disseminated metallic conductive minerals to account for the observed effects. Whereas, metallic conductive minerals could be

either sulphides or graphite; for the same reason as Zone A, sulphides are favoured as the possible source of polarization.

The overall resistivity pattern has out lined three zones of abnormally low resistivity values. These zones have been labelled R-l, R-2 and R-3; they

are aligned in an east-westerly direction. Each of these

zones are outlined by the 100 ohm-meter contour and the minimum resistivity response observed is within Zone

R-3. Resistivity Zone R-l and Zone R-3 are still open

to the west and east respectively; while resistivity depression R-2 is confined to the vicinity bf Line 32W.



The most probable explanation for these

observed resistivity lows would be a sporadic distribution of massive metallic conductive minerals along an east-

west structure. Whereas, these metallic conductive

minerals could be sulphides or graphite; judging by

the very low resistivity values observed within Zone

R-3, the presence of graphite is quite likely. However,

the presence of either sulphides and/or graphite is likely for resistivity Zones R-l and R-2.

A chargeability "build-up" has beenobserved on the base line between 92W and 85W; the peak polarization response observed is 6.0 milliseconds.

The corresponding resistivity data show a slight depression, Immediately south of the base line along Line 84W is

observed a similar chargeability response. It is also noted that the chargeability values along the base line

between 48W to 84W range between 2 to 3 milliseconds. This is considered to be slightly above background. Additional work in this area would be required before conclusion can be made from these results.


A reconnaissance I.P. survey covered a majored portion of the Crawford I Group, while a more

intense study was carried out between Line 16W and Line 36W outlining two zones of abnormally high polarization


lINDUCED POLARIZATION SURVEY CRAWFORD I GROUP_________.7

labelled Zone A and Zone B; as well as three zones of

abnormally low resistivity responses labelled R-l, R-2

and R-3.

Zone A and Zone B have been interpreted

as lenses or chimney like structures enclosing between 15% to 2Q7, disseminated metallic conductive minerals. Both these zones show similar characteristics; and a north-west trending fault has been inferred between the

two zones. Both zones show that peak polarization responses coincide with only relatively weak resistivity

depressions compared with those of resistivity anomalies R-l, R-2 and R-3. Thus, Zone A and Zone B are considered to be related to the inferred north-west trending fault zone rather than the east-west trending resistivity zone

that is outlined by resistivity anoamlies R-l, R-2 and R-3. Judging by the resistivity data and the polarization response, Zone A and Zone B are considered to be most likely caused by disseminated sulphide mineralization while resistivity anomalies R-l, R-2 and R-3 are considered to be most likely due to massive concentration of graphite

and/or sulphides. The author is of the opinion that Zone A

and Zone B are more likely to represent a source of economically important minerals than the east-west trend ing resistivity anomalies. It is thus recommended that

Zone A and Zone B be investigated by diamond drilling and the following drill holes are suggested:



DDH-1

Collar:- 6+OOS; 28+75W

Dip: - 600

Direction: N 35 0 E Azimuth 35 0

Length: 650' to 700'

DDH-2

Collar:- 0+00; 18+OOW

Direction: S 50O W Azimuth 2300

Dip: - 60 0

Length: 650' to 700'

Respectfully/^ubmitted,

Karl Glackmeyer, Eng

KG/gc



DATE February 1*1973

ATTENTION OF Wayne R.Zwlokey

SUBJECT induced Polarization Surrey, Abitibi Option, Lots l to 4, Coaoesaion 4, Crawford Township.

l have attached a copy of Olaokmeyers report covering induced polarization test and detail work over the north half of tots l to b, Concession 4, Crawford Township.

Reconnaissance IP work was carried out along the base line to test a number of north-south striking conductors indicated by an earlier Input survey* The approximate location of these Input features are shown numbered as follows on Olaolmeyers Chargeabilitynap*

1. This Input feature likely reflects on a weakly chargeable zone located on the ground gust to the east of the airborne indication* Additional ground work is necessary to further develop the picture in this particular area*2* The airborne anomaly at this location is likely caused by Zones A and B which are described in some detail elsewhere in this report*3* There is no explanation for this Input anomaly other than its proximity to Resistivity low fi-1 located just to the south**t* This Input feature corresponds to a weakly chargeable cone* Over* burden is believed to be deep in this area where additional survey work is warranted.

Other induced polariiation test work was carried out on lines 4400 West and 5200 West, the north parts of which straddle a magnetic anomaly believed to be due to serpentinlzed peridotite. The peridotite is not chargeable here as it is elsewhere in Crawford Township* The resistivity low (H-l) located south of the base line is probably due to a graphitic zone which is relatively barren of sulphide minerals.

Detailed indvoed polarization survey work was carried out over an area between lines 1600 Utst and 3600 West where a complex chargeability and resistivity pattern developed*

j


DATE

ATTENTION OF

SUBJECT page two

l have plotted IF and INOO drill hole information on a Magnetometer Survey map whioh covers the north half of Lots l to 4. Concession 4, Crawford Township.(Figure 1) Magnetic contours (100 gamma intervals) in the east part of the map were obtained from an old survey mat*. The colour scheme used corresponds to that used for other parts of the map. Chargeability* contoured at intervals of 2,5 milliseonds is shown in red. The drill holes have been plotted from data supplied by INOO. One drilling site was located l on the ground (Bole No.27023). The bottom part of this particular l drill hole Is marked by low eino values the best section of whioh assayed 0.40 percent eino across 15*5 feet.7 A specimen of rhyolite on hand from this drill hole shows heavy shearing and sericitization. No other core material is available from this area.

INCO Drill Bole No.25037 bottomed in a rook logged as andesite and graphitic schist. Rooks south of the peridotite Intersected by both holes in this area are comparable and there is no explanation for a lack of rhyolite in the westerly hole other than through the presence of extreme alteration. Weak copper values are common in Bole No.25037 the best sections of whioh are tabled below.

Footage feet copper zinc

451.5 - 456VO 4.5 0.'43 0.20 5^.4 - 553*0 8.6 0.23

The above diamond drilling results show that economically l important sulphide minerals are present in the IF survey area. l There is some evidence of mineral zoning with copper predominating to the west. The chargeability centres indicated (Zone A and Zone B) are considered to be reasonable targets to explore by diamond drilling. Consideration should be given to drilling the two holes recommended by Olaokmeyer.

AS/ A.Skreoky

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63.4827 CRAWFORD

Haroh 15.1973.

Paterson, Grant and Wat t on Limited

Request for Rat Ing ,Anomaly 30A.North half of Lot 9,Concession 3,Crawford Township, Ontario*

We have laid out reconnaissance lino* and will shortly be carrying out mag and V.E.M. traversing orer an area located in the north half of Lot 9* Concession 3, Crawford Township. These lines straddle a short axis conductor which wo hare numbered 30A.

Anomaly 30 A was picked up by the Input surrey through the following Intercepts.

l*tJ 15K 1180 1190

It flanks Anomaly 30 which was drilled in two places by XRCO and also by Keevll as shown by the accompanying location map. WOO drilling shows a wide band of graphitic tuff mineralised with up to 20 percent pyrite, two percent pyrrhotite. The Keevil drilling showed narrow ssotions of graphitic slats and massive pyrite* Their ground survey work* surprisingly, did not show any conductivity to tho west of thsir drill section.

We would like your rating of ths above Input intercepts.

160

AS/ A.Skreoky

liman Pa erson & Associates Limited l Consulting Geophysicists...^ Suite 2306, The Simpson Tower, 401 Bay Street, Toronto 103, Ontario, Canada. (416) 363-4261. Cables: Norquest.


March 19, 1973.

Mr. Alec Skrecky,Mcintyre Porcupine Mines Limited,Schumacher, Ontario.

Dear Alec:

Re; Anomaly 30A

This refers to your memo of March 15th, concerning the anomaly you refer to as Anomaly 30A, and shown on your attached sketch.

This anomaly was not identified as a conductor in our report as we believe it to be a subsidiary peak of Anomaly 30, produced by a combination of dip and strike. The attached example by Questor shows how this can occur. The presence of conductive material near the main anomaly axis, as confirmed by Inco and Keevil tends to suggest that the conductor responsible for the anomaly is located roughly in that vicinity. If so, a steep, northerly dip would seem to be implied, which would be consistent with the Inoo drilling.

An alternative interpretation is, however, possible, involving a relatively flat southwesterly dip. This, by the way, would be^onsistent with the Kdfewl drilling and would imply that mstPWay have drilled down-dip. Under this alter native, the main conductor could lie as far as 1,000 feet to the northeast, as shown on the attached sketch. This would be within 250 feet of the position of your Anomaly 30A. The conducting material encountered by Inco and Keevil would in this case have to be attributed to minor zones, masked by the effect of stronger conductivity to the northeast.

In summary, we think that you are right in doing follow-up work on Anomaly 30A, and recommend that you locate your Em transmitter slightly to the north of the anomaly axis, Lines should preferably be run in a northeast direction.

- 2 -

Transmitter location position is important, parti cularly when parallel conductors are suspected. The conductor energized most strongly is the one closest to the transmitter, and the effect of this tends to mask any parallel conductors that may exist. This has been the case I think on Anomaly 38, where your transmitter was unfortunately placed 600 feet south of the anomaly axis, and directly over the axis of Anomaly 44, which it picked up very nicely. Anomaly 38 shows very weakly in the form of profile inflections at its correct location. If you have an opportunity, it would be advisable to repeat this grid, situating the transmitter 600 feet further north.

Yours sincerely, PATERSON, GRANT 6 WATSON LIMITED

J VC-*AA*-*.

NRP:smcc: Mr. W. Zwicky,

Norman R. Paterson

South North

45"

N

DIP AND STRIKE - 450 UP-DIP RECORD

Paterson Grant and WatsonLimited March 22,1973

Input Survey Characteristics, Abitibi Option, timmins Area, Ontario*

We have your memorandum dealing with Anomaly 30A, in which you describe subsidiary peaks resulting from aerial traversing at an angle to the ground strike direction of conductive aatera*l. Anomaly 30A is in the process of being checked out in this regard*

Might your explanation also apply to the Anomaly 5L and Anomaly 4L areas located in the southeast corner of Lucas Township* An IP chargeable zone in this instance is located on the ground between Input intercepts.

AS/ AfSkreoky

Paterson Grant and WatsonLimited March 28,1973

Geophysical Data*Abitibi Option,Abonaly 30 A,Lot 9, Concession 3*Crawford Township, Ontario*

l have attached V.E.M. and Magnetometer survey data for Anomaly 30A located on Lot 99 Concession 3, Crawford Township.

AB/ A.Skreoky

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MEMO

TO: Alec Skrecky

FROM: R. Watson May 14, 1973,

SUBJECT: ANOMALY 30A

The anomalywas picked up by the Turam on three lines and resolved into two conductors approximately 125 feet apart which diverge slightly toward the north-west. The vertical loop survey detected the conductor but its position was a little less definite and I believe the Turam conductor axis to be the more accurate. The strike length of the Turam conductor axis is exactly parallel to that of the airborne survey. A 40-gamma magnetic anomaly on Line 6 + OOE lies between the two conductors but may be considered as directly associated with them. The conductor has no noticeable magnetic expression on Line 0.

Conductivity-widths were calculated on the three lines and are very consistent at 17 or 18 mhos. The conductivity-width on the anomaly 600 feet to the south which was drilled, is 47 mhos and the relative values are a measure of the relative amounts of conductive materials. From the consistency of conductivity-width values across the three lines I would judge this conductor to be a graphitic belt similar to the one to the south but probably narrower. The only indication of possible sulphides is the weak magnetic response. However, it may be of more interest than anomaly 130 to the south just because it's a separate isolated conductor off to one side of the main graphitic belt. We would recommend a drill-hole located at O + 20N on Line 6 * OOE dipping 50 degrees to the north-east.

/iRoger K. Watson

/l A AT P ft M . ,

t/ i Wayne R.Zwlckey

Drill Hole Section, Anomaly 30 A Area, Abitibi Option,

July 18.1973

! have attached two copie, o^^^e^cUSn fhSwf ?he covering Anomaly 30A In Crmwford Township. T ^ ^^^ that, the

for propo*;* Hele 90^j^*j B hmn thmt encountered jn at2thie drUl Blte^iU g^ on Keevil drilling ^200 thl southeaat wSere 70 feet of overburden *a* shown,

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REPORT ON TEST


CRAWFORD II GROUP


on behalf of


Bale d'Urfe, Quebec January 26th, 1973 Karl Glackmeyer, Eng.


REPORT ON TEST


CRAWFORD II GROUP


on behalf of


INTRODUCTION

During December 7th, 1972 to December lith,

1972, a geophysical party, under the direction of the

author, carried out a test induced polarization survey on a portion of the Crawford I Group, Crawford Township, Ontario, on behalf of Mcintyre Porcupine Mines Ltd.

The induced polarization survey was carried out using a Scintrex Mark VII pulse type unit of high sensitivity, with remote receiver of the Newmont type.

The current-on time was 2.0 seconds and the measuring time was 0.5 seconds. Measurements are made from which


KARL GLACKMEYER d ASSOCIATES LIMITED

INDUCED POLARIZATION SURVEY CRAWFORD II GROUP .2

chargeability (that is the I.P. factor), which is express

ed in units of milliseconds and the D.C. resistivity which is expressed in units of ohm-meters. The three- array electrode configuration was employed using a 400'

electrode separation for maximum resolution and depth penetration.


map the distribution within the underlying rocks, of disseminated metallic conductive minerals; such as pyrite, pyrrhotite, chalcopyrite (but not sphalerite) and graphite. Magnetite and serpentine are known to have moderate polarization response. It is rarely possible from'i.p. data alone to differentiate between these various potential sources of polarization response.


Drawings No. 1211 Plate IX-IP. and No.1211 Plate IX-R show the corresponding chargeability and resistivity data in contour form on a scale of 200' to the inch. The chargeability data has been contoured at

5.0 milliseconds interval; whereas, the resistivity data has been contoured at the 100 ohm-meter intervals.

Both the chargeability and resistivity contours have

been idealized due to the broad gaps in the data.

The eastern segment, generally speaking,is characterized by abnormally high polarization effects; that is, in excess of 10.0 milliseconds while the back-

KARL GLACKMEYER l ASSOCIATES LIMITED

INDUCED POLARIZATION SURVEY CRAWFORD II GROUP ,3

ground is-1.5 milliseconds. Three zones of polarization have been outlined, Zone A, Zone B and Zone C. Zone A

is outlined by the 20.0 millisecond contour and is

partly associated with resistivity low R-l. Peak polar ization response observed within this zone is 27.9 milli seconds. Zone B is only partially outlined by the 5.0 contour and is considered a "build-up" closely associated with the main mass of polarization that hosts Zone A

to the east. Peak chargeability response is 7.8 milli

seconds. Zone B corresponds to resistivity low R-3. Zone C is isolated and outlined by the 5.0 millisecond contour the maximum polarization response observed is 6.0 milli

seconds. This zone coincides with resistivity low R-4.


The present data has been acquired from a reconnaissance type induced polarization survey; thus,

only generalized interpretation can be considered. The eastern segment of the area under study reflects abnormally

high polarization response which, in general, is associated with corresponding resistivity values ranging from 150 to

175 ohm-meters. The most probable explanation for the observed polarization effects within this area is most

probably due to the underlying ultrabasic mass containing between 10% to 157, disseminated metallic conductive

minerals .

Two other zones, Zone B and Zone C, of weaker chargeability response are observed along the base


INDUCED POLARIZATION SURVEY CRAWFORD II GROUP .4

line in the vicinity of Line 24S and Line 36S. Both

these zones correspond to resistivity lows less than 100 ohm-meters. The most probable explanation for

these two weak polarization responses would be between

5/S to IQ7, disseminated metallic conductive minerals by volume.

Whereas metallic conductive minerals could be either sulphides or graphites,.- it is difficult from

the present data to differentiate between these various sources of polarization response. However, considering the resistivity values, Zone A is most likely to be due to disseminated sulphides while Zone B and Zone C

are more likely to be caused by graphitic shears that could contain disseminated sulphides in parts.

The present induced polarization surveyseems to have successfully outlined zones of abnormally high polarization response as well as zones of abnormally low resistivities. It would then be recommended that additional work be carried out in this area to further deliniate these various zones, as these could have economic significance. A more complete interpretation

could also be carried out.

Respectfully .submitted,

Karl Glackmeyer, Eng.

KG/gc ————————————— KARL GLACKMEYER fc ASSOCIATES LIMITED

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42A14SW0026 63.4827 CRAWFORD 190

March 13.1973

Paterson Orant and watson

Anomaly 38 Area, Abitibi Option, Lot 5* Concession 2, Crawford Township, Ontario*

l have attached the following items concerning the Anomaly 38 area which is oentrod on Lot 5, Concession 2, Crawford Township,l* 1320 soale location plan 2. MoPhar V.B.M.Survey Plan

MoPhar OP ?0 Survey PlanGeological Section Nodwell H Traverse

**

lThe Hodwell traverse has not been tied to the picket line

grid. A Second print of the V.K.M. Surrey plan will be sent to you when the traverse location is established, Nodwell Bole Ho.H-l is approximately located on Anomaly 38, other holes lie to the south*

AS/ A.Skreoky

l:* INTER-OFFICE CORRESPONDENCE

• P.O. BOX 51, COMMERCE COURT WEST TORONTO. ONTARIO MSL 1C1

DATE March 19, 1973 ATTENTION OF Mr - Alex Skrecky

SUBJECT Paterson and Grant's Anomaly 38

Do you intend to complete the magnetometer

traversing on the easternmost of the three lines you show on the

sketches you submitted to Paterson and Grant on March 13?

xWayne R. Zwickey

WRZ:sl

c. c. File

Karoh 30,1973

Paterson Grant and Watson,Limited

Field Conditions,Anomaly 38 Area,Abitibi Option,lot 5, Concession 2,Crawford Township, Ontario.

Thlo area has recently experienced unseasonably warn weather which has resulted in local flooding* The V.E.M. survey crew reports that the Anomaly 38 area lies in a floodplane which flanks the North Driftwood River and is not presently accessible. Survey work in this particular area will be carried out when field conditions are found to be suitable.

AS/ A.Skreoky

March 21,1973

Wayne B.Zwiokey

Additional Magnetoater Traversing,Anomaly 38,Abitibi Option,lot 5* Concession 2,Crawford Township, Ontario.

Anomaly 38 as well as many other anomaly areas In the Abitibi Option area have been straddled with two chained picket lines spaced 600 feet apart. These lines are traversed with the magnetometer as soon as they are completed. v

McPhar V.E.M. survey work is carried out at a later date with the transmitter being set up at one picket line at the approximate location of the Input intercept. Dip angles are recorded on the second picket line and the transmitter is aoved to the cross over from where the first line la profiled. Subsidiary lines are then read at the discretion of the instrument operator. This can readily be carried out in open ground and serves to establish the anomaly characteristics at depth and to determine any strike direction changes. These are reconnaissance type lines chained in by the operator and marked In any way that is convenient. They are adequately controlled to be included on our V.E.M. survey plans but cannot be accurately relocated by the magnetometer operator.

The need for some magnetometer follow up work is apparent in laces. Additional mag work as an example is scheduled in the Anomaly area located in Crawford Township.

AS/ A.Skreoky

-2-

. 3-1

Anomaly 38

As mentioned by telephone, the transmitter was located so as to emphasize Anomaly 44, rather than Anomaly 38, though 44 appears to us to be of much lower interest. The transmitter should have been located some 600 feet j further north, at about 14N of the base line. An additional line 600 feet west of Line 600W should be surveyed at the same time. Neither conductor is appreciably magnetic, so I would not attribute the cause to iron formation, though certainly there appears to be iron formation further north.


ATTENTION OF Mr. Alex SkreckySNTI55 YONGE STREET, TORONTO. ONT.

DATE April l, 1973

SUBJECT Anomaly 38 - Crawford Township

This is written in response to your memo of March 21 concerning the marking of lines. It seems to me that all lines can and should be marked so that not only the lines but stations as well can be relocated.

WRZ:sl

c. c. File

Paterson Grant and

ôiiiar^jMN^•AbltlbtXWw^;|iOt 5*' tô*lii^,-î'-,;-v,:''''Crawford TowniMp, Ontario,

* hart th* following additional

1. V.B.K. profii*B /^6A2. Nodwell drill hole lo

AB/

Anomaly 38As you pointed out, the overburden is very deep

at this location, which probably accounts for the low ground EM response. I am fairly certain that the conductor is not related to magnetite despite the presence of magnetite in drill cuttings near the conductor location. I would recommend a minimum program of three lines on this grid, extending it to five if an anomaly is found.

::^y/^^

t

Paterson Grant ana Watson Limited

W

AS/A.SVcrecky

Paterson, Grant A Watson LimitedJune 12, 1973*

Compilation Nap, Anomaly 38 Area, Lot 5* Concession 2, Crawford Township, Ontario.

I have attached a 200 scale plan of the Anomaly 38 area which shows Turam conductora along with revised locations for Nodwell holes H.I to H.5 inclusive* Hole locations were originally obtained with a partial snow oover and doubts on this natter have now been resolved.

AS/sa A.Skreoky

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42A14SWe026 63,4827 CRAWFORD 192

Paterson Grant and Watson Limited March 27,1973

Anomaly 50,Lot 9* Concession 2,Crawford Township* Ontario*

(Abitibi Option)

l have attached MoPhar V.E.M. and Sharpe MF l Magnetometer survey date for Anomaly 50, located on Lot 9* Concession 2, Crawford Township*

AS/ A.Skreoky

\

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\l formerly:

Noi man Pa ersorji St Associates Limited l Consulting GeophysicistsSuite 2306, The Simpson Tower, 401 Bay Street, Toronto 103, Ontario, Canada. (416) 363-4261. Cables: Norquest.

Norman R. Paterson, Ph,D., P.Eng. Roger K. Watson, B.A.Se., P.Eng, Fraser S. Grant, Ph.D., P.Eng.

March 30, 1973.


RE; ANOMALIES 30A, 50, 6, 29, 17Ay CRAWFORD TOWNSHIP

Dear Alec:

It would appear that you were right in thinking that Anomaly 30A is in fact a separate conductor. The ground geophysics certainly suggests a steeply dipping body almost exactly under the INPUT intercepts. Depth, as indicated by the VEM could be as much as 175 feet, though my guess would be that it is not more than half this value. (Attenuation of the EM signal produces the appearance of greater depth).

I would suggest a Turam set-up as shown on the attached sketch, with a grid of 3 lines, 300 feet apart, as shown. This minimum program will help define the best location for the drill-hole.

Unless I am mistaken, Anomaly 50 has not been covered by the ground geophysical grid. I have shown the approximate position of this grid on the aeromagnetic contour map, which indicates that the INPUT anomaly is some 500 feet east of your easternmost survey line. I would suggest two more lines, as shown in red on the aeromagnetic contours. The weak inflection on the dip angle profile on Line O suggests that the conductor is

-2-

indeed to the east of your grid, and that you are just beginning to pick it up.

It is extremely interesting to observe how well the ground magnetometer survey agrees with the susceptibility map. You will note that the airborne survey simply showed one large magnetic anomaly centered about the middle of your ground survey grid. The susceptibility map derived from the airborne data shows two distinct highs and two distinct lows, all coinciding almost exactly with similar features on the ground survey. This is what we would expect, but it is most gratifying to see that it actually works. It would have been useful to have had the susceptibility map when describing the airborne anomaly, as it now appears to lie in a magnetic low, rather than on the flank of a magnetic high, as previously suggested. We will be mailing you a copy of the complete susceptibility map immediately.

Scintrex reports that they will have a crew available in a day or two. Their Party Chief, Tony Grenier will be contacting you if he has not done so already. Considering the weather, it is most unlikely that you will get much Turam work done before break-up, but you might be able to do Anomalies 3, 9, 8, and possibly 30A. I do not recommend continued work on Anomalies 7 or 17A. Anomalies 6 and 29 appear to be bona fide conductors, and of the two I prefer number 29, which has been drilled about 2,000 feet along strike and encountered some sulphides. Both conductors, however, look very much like graphite. If you are planning to drill them, I would suggest that you survey both grids with Turam, adding an additional line in between the two you presently have on each grid. The Turam loop edge should be placed to the north at a distance of about 1,000 feet from the conductor.

I am still waiting for data on the following anomalies: Anomalies 5 and 13, Lucas Township and Anomalies 24 and 38, Crawford Township.

Yours sincerely, PATERSON, GRANT S, WATSON LIMITED

/Cx~-oV****"

Norman R. Paterson NRP:kn Encl: cc: Mr. Wayne Zwickey

Paterson Grant and WatsonLimited April 2,1973

Anomaly 501Abitibi Option,Lot 9, Concession 2,Crawford Township, Ontario*

l have your comments on the field work carried out on Anomaly 50 along with several plans covering this particular area* l have attached a copy of one of these plans on which is plotted the Input intercepts recorded on lines 1^4-N and 1098* These intercepts lie west of the locations you show and are within the grid as laid out in the field.

This area is rather featureless in the field and we were obliged to anchor the grid on the magnetic anomaly on the east end of which the Input survey shows a 3 channel anomaly*

AS/ A.Skreoky

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Paterson Grant and WatsonLimited April 18,1973

Anomaly 50*Abitibi Option,Lot 9, concession 2,Crawford Township, Ontario,

l have attached a revised V.B.M. survey plan covering Anomaly 50 located on Lot 9. Concession 2, Crawford Township. This map shows V.E.M. profiles from transmitter location No.5 located at 500 North on line 400 West,

AS/ A.Slcreoky

PATERSON, GRANT Si WATSON LIMITED

formerly:nan Pa erson1 St Associates Limited l Consulting Geophysicists

Suite 2306, The Simpson Tower, 401 Bay Street, Toronto 103, Ontario, Canada. (416) 363-4261. Cables: Norquest.


April 24, 1973.

Mr. Alec Skrecky,Mcintyre Porcupine Mines Ltd.,Schumacher ,Ontario.

Dear Alec:

This is further to our telephone conversation and the data I forwarded you by mail on April 20th.

Anomaly 50

n The conductor appears to strike at approximately N 60 E or conceivably N 60 W. Because of the doubtful strike, I have suggested two Turam set-ups, one to the north and one to the west, the conductor detected on the ground is very indistinct and its nature is uncertain, but because of its geological environment we regard it as of high priority.

Peterson Grant and WatsonUnited May 3, 1973

Turam Survey*Anomaly 50 Area*Abitibi Option,Lot 9* Concession 2.Crawford Township.Ontario.

l have attaohed a Turam survey plan covering the Anomaly 50 area located on Lot 9, Concession 2, Crawford Township. This survey work was carried out by the Bointrex crew who today left the Crawford Township area to return to Toronto.

AB/ A.Rkreoky

Paterson Grant and WatsonLimited July 16,1973

IP Test Work.Anomaly 50,Abitibi Option,Lot 9, Concession 2,Crawford Township, Ontario*

Olacktneyer has completed. IP test work on linea O and 800 West In the Anomaly 50 area. Field reports Indicate that the results of the work were negative. Olaokneyer will forward the field data to you In a few days time.

AS/ A.Bkreoky

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ANOMALY 50 AREA

-CARNEGIE- TOWNSHIP. ONTARIO

on behalf of


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Bale d'Urfe, Quebec September 5th, 1973 Karl Glackmeyer, Eng.

KARL GLACKMEYER fit ASSOCIATES LIMITED, Geophysical Consultants and Contractors 716 Cornwall Drive Bale D'Urfe 850, Quebec (514) 453-1982

REPORT ON INDUCED POLARIZATION SURVEY

ANOMALY 50 AREA CARNEGIE TOWNSHIP. ONTARIO

on behalf of


INTRODUCTION

During July 1973, a geophysical party,

under the direction of the author, carried out an

induced polarization survey on a portion of L-0 and

L-8W of Anomaly 50 Area, Carnegie Township, Ontario

on behalf of Mcintyre Porcupine Mines Ltd.

The induced polarization survey was

carried out using a Scintrex Mark VII pulse type unit

of high sensitivity, with remote receiver of the Newmont

type. The current-on time was 2.0 seconds and the

measuring time was 0.5 seconds. Measurements are

made from which are derived two (2) physical properties,

namely, the chargeability (that is the I.P. factor),


INDUCED POLARIZATION SURVEY RE: ANOMALY 50 AREA .2

which is expressed in units of milliseconds and the D.C.

resistivity which is expressed in units of ohm-meters.

The pole-dipole electrode configuration was employed

using an a r 200' n s 2, 3 and 4 electrode separations

in order to obtain maximum resolution and depth

penetration.


map the distribution within the underlying rocks of

disseminated metallic conductive minerals; such as

pyrite, pyrrhotite, chalcopyrite (but not sphalerite)

and graphite. Magnetite and serpentine are known to

have moderate polarization response. It is rarely possible

from I.P. data alone to differentiate between these



Drawing 1301-4A IP d R and Zone 1301-4B IP

S R show the chargeability and resistivity data in

contoured sections for both L-0 and L-8W respectively

on a scale of l" = 200'. The chargeability data varies from - 0.7 millisecond to a maximum of 1.5 milliseconds.

Corresponding resistivity data varies from 131 ohm-

meters to a maximum of 354 ohm-meters. The chargeability

data has been contoured at a 1.0 millisecond interval

l...


INDUCED POLARIZATION SURVEY RE: ANOMALY 50 AREA .3

while the resistivity data has been contoured logarith

mically .


The present induced polarization survey

carried out over L-0 and L-8W of the Anomaly 50 Area has

not revealed any significant polarization or resistivity

response.


Karl Glackmeyer, Eng,

KG/gc


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Remarks

Graphite, po, trace cp \Graphite, py, trace cpPo, py, graphite, . trace cp, Cu up to 0.43/4.5'Graphite, py, poGraphite, pyWell attemptWell attemptGraphite, py, po, Zn up to0.91/6.9'Peridotite -Graphite, pyWell attemptGraphite, pyGraphiteGraphite-GraphiteGraphite, pyGraphiteGraphite, pyGraphiteGraphite, .po, pyGraphite, py, poGraphite, py .Graphite, hole abandonedPo, peridotiteGraphite, py, poGraphite, po, py, Zn up to

' 0.60/5.0'Graphite, po, py, peridotiteGraphite, py Graphite, po, pyGraphite, po, trace cpGraphite, py .Graphite, po, pyGraphite, pyPeridotite, gabbro, tracenative copperGraphite, pyGraphite, po, pyGraphite, py -Graphite Gabbro, peridotite *Peridotite

Total - 40 holes 23,726.0 feet

CRAWFORD TOWNSHIP - SAMPLING RECORD LIST OF HOLE NUMBERS

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SHEET NO,

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0. 6

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PROGRESSIVE TOTALS

FEET X PER CEKT

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z_Ga_(^^^jf?f-t^f_ecL spites Pod'7% med. q 5W cjpjs

blebs /Ô" wJ.Jha 55 r t ^ ?* O? .OS

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LsflCilQ '.~ O5 flboW'. knifyohnw Is P o b/rAs

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Dnriie \- a ha du* II \i bec^f.It'erh i h OWoaeiin u s l ncênseairttJe^J/Jia/raJj aS/'n \vilhvnitiot- Cat-to. S/J/Ca Oflos-es'llrtctfa^-frf am J s n5 o /A:Cat-bombed ftr-odute jnfiflinait////? cjf&in.

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SAMPLING RECORD 8HEET NOS*

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SUMfQ^R^

Pfll**Uverbvrdc* ^.J^--'Ûaci-ie:-L-'/a rbotiar eoup -2- rriefr/i faji'o^

ripaphiiic SOAJ. A^f/t/u^-yHi/u; /?i^ /the/"1 ' : - 5^ illcideej* ratbn*i*fMuyw- Mvw Py

G fl f&onfrcfoos ~Hnie.tTAlA houS-ô/o P\^Po

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fi?' Po Z/e&c

BOTTOM GF POLZ

DATE STARTED :- "3 'AN. ^ /*DjTt: CDMPlFTED-.-FEFl'tODPlL/FD PY : HEATH AMD 'H QLZ A/ OT~ PL(JG(?fDCORE: s/z^r :- ,f"x*{cin TJTS TS -. (2 IRQ - 4-s *

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Q

FORMATION•AMPLE

NO.

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nr.

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4W8T

PROGRES3IVE TOTALSFEET X PER CENT

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SHEET NO.CO-ORDINATES

FORMATION

YfA6**\f^\*i Vtfltn

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NO.

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COPPER NICKEL CU. tt Nl. ABtHVTH-PROGRESSIVE TOTALS

FEET X PER CENT

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f

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lOLE NO.-2TQESLDEPTH-^^7LC?——ANGLE-jfiCO-ORDINATES

f-t-ao w. _i-t-To S.p^" -E -" DIPTHps/ r"T

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NO.

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f *^ . 1 *{ t'i^ts* ^ \6ocoXltA4. ,

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more iVttMcW cUW. CXt . Ctn. . StorCqih'a^l!———————— .^1 — -^ —— .. —————— — —— ——————— ,

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dtwn^ (ÎpU. rHA* . Occ. sl.'P

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w if^ i y .GaÛj; N? V 2Ss*'*G al* W i' A? fc^ as^-sT^;U-cUo" -firpV-.ncU.TniWaUH alH

qalUo . loc cUi Mvt spt-.So-v.t-

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'jt ,'w. ^^v. ums' oct..K*Qvie*;tf v*;** .'FfenJot.-U. l*iJ (OK 5ST-T fi-trora^t*)" "'ijf"""Ul *k- ^T'l' 'J 1- K.'MA coe r 0 IK i *j *w^t^ wen L ' ^ *'itv - v^r 1 v^bk

(gao* (^ wfci-o'.lX*^c|otiK ' **^ tor" 4W'^ ' 0*^-' ****î**5ilo1

\?p\ ' \^-t^5 v^*fC\ 3OlftcC*\^ ^*P^ * *^"J^*t

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flffîC. ' l FOCf fitoffs Cfifft aOlOfl

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NO.

f -2^11 31f- S^tlSU*

f- S^H^sT

?-i^\U*b

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?lt-oyial\j, toacftiffi'c

ift-OHyJii fo&aHeficrfttdc&Jie '-~ d** above -mod. -Sirtynrjlu tvja.q'neiic \ itvjSC.ftytf SrtfQ ^^'ac^t>^ts

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Mm l-tplocenenj Jtyf-fc/o tiie- - - (i s a. b&ue, m,oJ*-^

ter*?- pyi3* "ft? /t ^^ffPfr{t(a{nC'- AS above vi// y/?

ty?rt-ft?s eJ rn?pafi e it'fa ~ Vt/CakliiQ LOCK //y ^jnfffa f -lie J

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pej-Ja.oJ.ue'. as-o.bove \MilJz^set-fyc/ •(rac.'iures q shir, ûi-fxLoceJ hiffi/nfîif - \tsea.k.~Kfod

kjZJri'tiLaJity'- os above .meet-JVjtranf/t'c

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NO.

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C2.*?/^!f5ft-to, S//-/.; U/^J/T le /OCtfdu IIfHoe/Ct-aie Magnetism nf ffi 1(^-2.

Per-ttl&TiJz^- îs ajjoise-deet-fas&ftwaqndics -wta.k . y . ll/^//-^?

A^C/31 (*.a.nhlrn:'..toijffl.-ataihe.rf.\3AiibhoieL -iey-fuirf ^{Jla+c/e

r ti (le 1 1,-/ f?X, a rain t Chutfffsihe,Ji-SJi.-Zjl

t/'tfA- OLmffhihole lajm'CM- 6 --.aclfa ".-J.JH A.-mzf.rjJt..^.4 Met- ea anhtcfi-al ic/as -

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/y&b

t i . j . j j ~t in C-fi'c. \ /y/*; find rfiniac,~i^h dloove Pt H (-1 o-l ileL cry o-bbho \- o.s tikoi/e

\yi{k tft/Wft-OU? le/st'r C/ahd5//-S. : i f w Ca.rh. {/efns

EddjU?aihfc phase -. o f a bnve

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r tot A a hfJ 'f 'f...

d? b 9 O- o' v/iih inJisii'Mci at-e^s o iJ.1f.t.teifcLwh/le fe/ffa znalenlz

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CTOIk-p ,^0/JT// P.I PVAT10M 4-+OOS: J3

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NO.

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/9^rf5e .#f flihovz m 2^-03^1-6f — . y . /y "jl ^J^/*/^* i Qfat&GStilGto AS GLkjQAS 01

î/y CoAfSfr qfaineef /arete^Q^tyfi C*?f 0f*cr Jfyfijf^' Q^Q i t? s yC/f) /5 V/f'jJi f yi /f/ fjf/ Ma 7 tfJ-ff* Crmfe/f/T 5 eat-faff -//'ovs - mi'ttfi- Ifj. /Vrf v7 y f i tli -1 /l \sores J 1

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Pyfoxenilf,- fl3 a.hflue bft?*rVa'(tfk'et- \Afiih cferj-fl)? -fi^ftcea MI t. Sulphicjr spec^

êj-ptnJin i? f^L^PchisLo life ? "'Pqarqi ha l fa od. WlAe/h f jfc*r*0(iV of under /\i ltd PcH'f/oliia.lJer(rll CariTohleo COM "i ad"Zou f Ci f li f Of 'n U - Seiyq'f/ frtu?k/iJh while iniet-s-lflfaJ \efof-ruiniQ * lall in f w em nt.it' J t

IStff- a**il* SCaftftttf zhhohffea ra in j

S ^pC^jiî2^CL—I^Ctlidj?JLis^-~4JL. Q.kQvA-i-l2JAd--.S.i*:atef /.y , ftHjti Stif} f t- ffi f fff, {l#'aCt7^ÂT,f(ff'Cr PlfVV

Qhai'fu : pOLichy \viih Sft-ar/

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FEET X PER CENT

COPPER NICKEL CU. A ML

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'PROPERTY OWL 4--89; CZAWFOXO TWP SAMPLING RECORD SHEET NO-

CO-ORDINATES i

'i.

lf*

1(974-0

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SAMPLING RECORD SHEET NCO-ORDINATE

STRIKE SOW TU PI PV/VTION 4-4^0^ 13

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NO.

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l&elwJ&jJLbbfo-' r/ffh-MA/ne-ffrW\t.lnsf)a. ifaic prjAseF 736-0-7^8.0^COarse QPaiHea ohosfiC9 fi^K.^— *.v- rt-y — iî in . .^ . ^f.i*-. A-JJ — un ' 1 îj ————— f)6O.04-8c?0.5'-?)94I? 1

P\\SQXenL2c :- 9#t/- tnaaneJL&cfroiihKu-l fsseniiftfki tton-tvaciMpJtPH

3&f0A^LKi3^<i^Ju!?^'t'aoî•|e\- II•jytyicai "/If esr)- /dK/f/-*' ': jfiitrjliifcffvlotciftf^'t f'jS. ~ W OQ(!ha.~felii Qio-tf/ie.vir/MAyxe/f'/C Conten-ira-leahi winV^4 , ^ //*9?. 0'- S/ 3 3.0 '-S JrejtJttotten? -lil e VJ

V

ROTTOM OF HOLZ

DATE SJARTFD:- FER PA w,C) ATE COMPLETE o:- MAR gDRIU-ED BY: HEATH AMPCORE S,i?g: :- XfxJjOLZ MO~f~ PLUGGEDrAS/A/c LOST:- Ax -rn'

MX- /o'A C//0 T^5 TS :- (* 1 80 '- 4&.S

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SAMPLING RECORD

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FORMATION

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l*tfei f*r le t f. f S J**.rllri'Hf i'*f J i i . 7

pr* ri'm/Ltf Te S9^rre\A) Sftfm^rj^

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tl*tttrs ^ IL/t'J a/.-u.X Vte./f.Jff /

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4-r-o^.a.

4^-^ t(L

•Vrxie*.

•U-aeÎ.

-Wive...

4-r-oe*.

f OlkM oTHE INTERNATIONAL NICKEL co. OP CANADA, LIMITED

SAMPLING RECORD SHEET NO.i- ' fc POLE NO..

1 "*™p 5 '"" p **!^(k- AJeBif""' ftIr —If k\*,.ol ' '

E" b?sfe eJfr

F""W- tn*. a

1 ————p ————K' * 'i — tta-8BP;"' .

E"t":t"li.. .*tt,ft

i"'-r-

Ir ^nfc 0r

E,. '

CO-ORDINATES A .iXsASi DEPTH fcWe ANGie - **s. STRF^P ^ ELEVATION H***t 7s*"Y^' ;

FORMATION

' 1"

^ "**NrsQ^v a*i ^j F\* - O t (^. \^^ VyvTri CL\V^*\J^^

' ^-T \^ o iî^ ' Vp." 'VT^^. ' *T* A T ft orJr \"t\"pY . J^ l U .^

IT^Q. \T^ w ^ft-U'fe. e^-rirt"\****ftcJcm

fV*. îW cV-r MXrAA'e. ©ê*.Xj y x

Pc:TvA e\x\^-lTxq.Vfteo\\Mesft.'rp-X. V ' ^

i i ^ ^

tWo'-feo'tê.^ 5* - -mod- \TO -mQB

Pe.TÂe\vVe^?Q-^Q- ec.e.\vi

tx-Â "Ae*. 6 P ^ \\f viAVe-Vî-H* *J *A \

-*na. ft X9e.T tAo^\e..9o-'mQ - e tp, \^*. v*AV

ft.e.TpN^Q-r.^'S \L_tV 1^-^VA ^V-

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S^pâÂ^ ®.M|0* "U-i YV*. Viv*tV\ X i

' t t J

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^C-XvAoÂe^Q- oce. I't^XvH^

jsViTiA^Â^cÂi^'i.To @. ^.a

^^ " tl l 1^^^" fm, ~ DOT f 3

Pe,vAo1rAei.Fq. ê.-rpe.-r,V^\7 C.A.x . V y

4 \ * ^^ . ^\Oce.V,QTxd^ ?,f!^^ (SM^*. -mod

\

SAMPLE

NO.

pE^\t V^

^^\StH

fa^fete,

-

^^l*t^{,

Ft'V^tn

Esax&VjJL.

Tf\\^b*\

V^l^To

LENGTH

FT.

\t*.e

.

\fe.o

V ?,.o

ifc.o

\?,.o

\^.o

i^n fe.o")

l&.O

ANALYSISCOPPER

*

M: l

t.o*

/.o*

A MM

-ir.eS

* K.-1

*- o-z

* M;\

NICKEL

c&ri

.'

.re .

.9^

•HO

.BC.

BS

.2*9

• •WE

•sz.

CU. * Nl.

*

"-. '

'

"

~

*****r

^PCWT ^

i

-i.om

1 '

i^.09

*.e*

-S .0*

^.ee

^.os '

^.os

*. os

PROGRESSIVE TOTALS f

FEET X PER CENT

COPPER

4

1

J

NICKEL

'

Ifcl.H^

I(.-\.^H

n*.*H

ne.i-t

ies-*-j

, ea.^l4.

l ^^. IH

i^-,.,^.

J^*Si"

1

. ,. . - ---|

————— . ———— : \M.T' -"11

— . ..^,'. V , J... i

-'•~ ' " . } "

. N:r- ^j-•- " f

;

. . , ' ,M.-V

Nl.'l

i

M.' l

MM

•\rr-ac.*.

1

1

OTHE INTERNATIONAL NICKEL CO. OP CANADA, LIMITED

SAMPLING RECORD SHEET NO.-ii-pr•j.v

POLE NO..

P-- DEPTH•fprjr.-'. -

jlh i' W

fer-- - "*2A- Q

Ei.. '|: ™,ciP'' '

r'' e.prHlsn:i '

IMP-li —— 3itjiIff i "Vie .e

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fc"'

WF'" "

E ôe.o

1: o,v fe.eS'

m **ni *P ——p ——i"P ———H ———

mi. -. ' T

fc— ——————— li

CO-ORDINATES ^SL-lcsAfe DEPTH 9A1.0 AMttl E -Hfe STRfKF . *a E^^VATfOW l***'P ^'•"tA

FORMATIONt

IpÂ.AAp.to.Â*^,.*^\SM" Tt\*^* \^ 'dk \^*kf**TG*'

. ./sJ'O f \

* ^Mvvy^.Pî 4tAo\ê..-rfto. \ecCL\\ufee-Tft

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4 X \ .

V \ ^ î *

^ -ip*. \ e c. (X\\u ^-* 'Afe-HaVJ i x

\. C.. ^

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j \-. y i/. î .

ft J

Pe.xÛ\v^cL.-^Q. ^\|oV^\H ^*?.Tp-\ x*** '

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îtvp . 9i-v\e. cN\T 1^5^,0^x1^. ?Armo-' J , . . \ , -^ "

ex^. e. c. c. rt s, vjvAVêvXc. (S. XSi.C)'/J X

\ x

•AMPLE

NO.

?2qtfe*\i

S?ft\ ftT.2.

Yafti^TSi

r^S^?^^H

^•a*\v?,-\5,

T^v^lb

fiai*ax

itaia*.

ft^^-\^

LCN6TH

rr.

\?..ft

\6.p

1**.*.

Z. "9.

\fe.G

(

^"?L

\fe.o

\Vo

1&. 0

\t, o

ANALYSISCOPPER

(Jta

^.09

l. OS.

*.o*^.es

4. OS

*.off

^.0*

^09

^.0*

*r.os

NICKEL

-tSo

.rt

.Si

.90

.So

.Z-*

.so

.•a*

-HO

MO

."4 O

CU. A HI.

*

-eeewrw

4WEV-

^ o-S

^ OS"

^ . o^

^.09

z. os

*.os

^.t*S. '

i.eys

*.os

PROGRESSIVE TOTALS

. FEET X PER CENT

COPPER

^

^

*

^

^

J

J

*

j

NICKEL

Zoi .-j-*

3rov^.^

ZU.O&

•e 11.1*

Z X.. 0^

•zzo.s^

Z-zS.B^

731. QH

Z-S-7.6-*

*H-5.8S

-^J^î

isi.M

Kl.M

IM; l

M;|

KI;|

M; \

4.-..-.

-V-l-CkCtt.

J

MM i oTHE INTERNATIONAL NICKEL CO. OF CANADA, LIMITED

. SAMPLING RECORD SHEET NO.—SL.

CO-ORDINATEStOLE DEPTH ANfil E - STRIKE .ELEVATION.

DIPTHr err FORMATION SAMPLE

NO.

LCNOTHANALYSIS

COPPER NICKEL. CU. t Nl. LCNOTH

EET

PROGRESSIVE TOTALS

FEET X PER CENT

COPPER NICKEL

isjp^.

*vi. OS •Z—

tf \t..e,\cits^\\e -Vci'Ott T'v'rv*- ^

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"V

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t* t

•oTHE: INTERNATIONAL NICKEL co. OF CANADA, LIMITED

SAMPLING RECORD

fSHEET NO. l.

•OLE NO..|:oIT'S?IFli ri —— *!*Jr- — m ' - *Ai,cm- iip",.. im, , . *. . i1-. , . 1m : - i* i•P- , ' iM: . '•t . iIMlfc *" '•ss"

•If

pr —————

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Ife''- - '- j

if-/I,

S^' ~-fc;

lte;:**-

CO-ORDINATES WP.n 0*\^ nEPTH fe*\T. 0 AMRI P - Ufe gTRIfrP ^ BLEVATIAN *O*' t. ^*" H

FORMATION

w^CkO ^*\ ^* XT\"TTX OT^ LI *i*

!r.\\ arioxtTôT Ae^.! Pe.T\^cj\v*te..

YP O ^ OT ViftAG. i

1ti :'.

•AMPLE

NO.

-

LENOTH

rr.

ANALYSISCOPPER

*

O^W ^

Gtt.\e. to

rb-rv\\e.(4

AY^ r o1* t

dotT-e^*

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0x4 \\feA ,4A KcAti \effi ^*. B .6 1

fe X.%.6.6'

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*

; . .

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*

*,\fe:

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LENOTH

FEET .

- --~

Tvôoi r

-

AT.&. GK

PROGRESSIVE TOTALS

. FEET X PER CENT

COPPER

-

T^^ft, N,^

\\Q-ts*t,

NICKEL

-x\eA

CU. A Nt.

*

m- \form TWO

•'•'A

UNIT GRADE CALCULATIONBOMB HOLE 2 7O 9S~ tZVEL

~7~i*i0.

T*

From

Dili.

Orado

To

From

DIM.

Orad*

To

From

Dill.

Grado

To

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DIH.

Orad*

To

From

Dili.

Orado

To

From

Dili.

Grad*

To

From

Dili.

Grad*

To

From

Dill.

Orad*

To

Fro.

Dill.

Orad*

Length

7 Z S*. 0

/22 OH 3 -0

^?.o7 Z 6l li o

-

ProgroMlT* Total*

Cu.

——

Nl.\

2 20 S-3-

lio- y 56-33

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2lo.S'343. f 8

0.33

GU.+ XI.

(

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Pro0T*ulv* Total*

Cu.

•-

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t

. (

Cu.-f Ml.

* * '

PORCUPINE MINES, LIMITED

April k. 1971

txploratlon Department* P.O.Box 970, Tlralns, Ontario.

Mr. Bill Bondar,Bondar- C l egg and Covpsmy, Limited,?64 Belfast Bead,Ottawa, Ontario.

Dear Mr. Bondar i

Ve have attached 33 drill core reject* nmbered between 291538 and 291583* V* would like theee aaaljraed for nlokel ttclng the ooid leaoh-aioorbio aold hydrogen peroxide •ethod. Ve also wish analyil* for total copper.

Please aend the result e along with your larolee to the address noted above.

Tours very truly,

MoHfTTHE POBCUPIWB NIHE8 LIHITZD

AS/ A.Skreoky

BRANCH OFFICES

If jK— t———— BONDAR-CLEGG & COH' - 768ABEL

PHONE: 23

1; '^ GEOCHEMICALN1 - Ascorbic Add/Hydrogen Peroxl

W"" Extraction...........Cu...-.JNQ,,-HCl.......................................................iiii.Lj.3M™ j. V

ll : - Method.............. AAt................................................................................

'friction Used -IQOrOCkS ^ ^T*0?5"

SAMPLE NO.

291538

K- 39

291540

f' 41

|p';: 42

P- 43

P' 4?

IT 48

1 49

K." 291550

K 51R; 52

p: 53m: 54m 55P 59

291560

p ' 65

•St': ' 669jjf-"~ '•••-rJ^- : .

Ifc 67

K; 291571

It 72

B 73i 74

1' 75

! 76

77

78

1 791 291580

1'- 81

tuppm

8

18

3

10

20

18

45

128

60

75

60

53

25

100

30

14

25

10

10

8

12

68

15

60

50

58

50

35

30

105

20

m ppm

480

550

520

520

400

480

490

350

400

360

540

500

680

470

490

280

300

490

320

360

230

900

1100

1400

760

250

400

500

400

780

510

rtPANYFAST RO/7-JllO

. LAB ide

From

Analy

^^B 1500 PEMBERTON AVE., BOX 487,

^^ NORTH VANCOUVER, B.C. CAMPBEUTON, N.B.

T Try ——iU) (M.R. l), OTTAi

REPORT

A. Skrecky - Me

WA 8, ONTARIOTELEX: 013-9)48

No 156*1

Intyre Porcupine Mines Ltd.April 16 -lofli

- '— ^^16*^"-

st A.A.-6.B.'''Vr:SSilliBt*'

'" l-":,as-...f "iEBSJi*-

REMARKS'.;|||j|^

. *:S|SEP

'-illiil1 ? ' :

•— 'Isili-

• ::

• •'iHiit'':[v*i-uL'-

,::'-*-|S|3*,

-,,;g|||-

,^psp,.

'-""'•'i^SK'-^"'',—— •'^ifeS?!* '-.;'

"""•'iSf-7 :';/

,,,:.4"SiieiniS:,.:.5..r" ' '":';|S?5*'' ~~ L-.' -J" '^Sr,^iJU""' :"*-"•-•stfi&trfm&jz-

^v^pSftS; : '

..

.-;. :.;i,;^-. . : - -

' n

0 . .BONDAR-CLEGG"fic

'-'V'^'tii''^^" ••-i* •P* -r" j i '*-i*ii*P '-f!,*"" 1 -MI

PT

Siff^,j(^-..-V, "; gAJV,7,.^. ,.

SsS

fe

ri*s ^' -'.

^K; *^.-"jli

^•:

it.

m-

i.'A'tt:

" v--"; ifi? . il-'Suv; .i;- uVijf-

42A14SW9826 63.4627 CRAWFORD

August 16, 1972.

194

W, P. Hammond

Deep Overburden Sampling Program,Abitibi Option,Crawford Township, Ontario*

Summary

We have completed a deep overburden sampling test in selected parts of Crawford Township shown on an accompanying plan* Several Nodwell holes are located on Input anomalies the location of which was previously established by ground geophysics. The drilling did not encounter any conductive material. Two magnetlo anomalies were found to be due to magnetite mineralization* One hole intersected till with Y abundant barren pyrite and a nearby bedrock source is o indicated. Chloritic schist was found at the bottom of Bole G-7 and may account for the oonduotive zone present at this location. Somewhat anomalous values in copper* zinc and nickel are common in bedrock Material intersected by the Nodwell holes in Crawford Township* Analysis of till material shows generally background values.

AS/sa A.Skreoky

:, v

August 16, 1972.

W.P.Hammond

Deep Overburden Sampling Program,Abitibi Option,Crawford Township, Ontario*

I have attached the following item* covering a deep overburden sampling program recently completed in Crawford Township. -

Plan of Crawford Township showing Nodwell Bole locations Geological Sections for Traverses P, Q, 61 and H Geochemical Record for Holes in P, O and H series Logs for the Crawford Township Nodwell Boles

The Nodwell holes were grouped in traverses and where possible were spotted directly on Input anomalies.

Some difficulty was experienced in previous deep overburden sampling work in that the coarser fraction sent out for heavy mineral concentration did not always produce a large enough sample for geochemical analysis* Our initial approach was based on the GSC practice and on Dr. B.A.Lee*s advice. Our interest in the sampling prooeedure is to locate anomalous metal areas which should be reflected in a heavy mineral concentrate, values in which can be judged in a relative manner. Our Crawford Nodwell work was therefor based on the analysis of a heavy mineral concentrate from minus 15 mesh (1*23 mm) samples.

1 : . i . - -- ' - -.

Results of the Crawford work are discussed below and are Illustrated on accompanying sections* Details are shown on records which are also enclosed.

Traverse P , ; .'. ^ '.-'^;..' -- . ' ;'', '';}.,

Hole P-i drilled into an Indicated conductor and Bole F-2 tested a flanking magnetic anomaly. These features were recorded, by the Input survey as a coincident mag-BH , anomaly. The magnetic anomaly was found to be due to gabbro. Books to the south consist bf felsic tuff* Bedrock material in this area shows slightly anomalous values In copper, zinc and nickel*' ' . ,/; - -' :.-'.;', \\

Traverse Q^^•^^••••••^^•^^•••••i ^ ^ f - . x

This traverse straddles 4 cluster of Input anomalies the most easterly of which was located on the ground* The Nodwell drilling shows that tuff WrAd andesite is present in this

PAGE TWO

area which is marked by background metal values in bedrock and in the till* Hole G-5 intersected abundant barren pyrite in the till fraction overlying bedrock. A nearby body of this mineralization IB indicated. Bole 0-2 ahows above background values in nickel which can be explained by the finding of metal fragments probably related to bit and rod wear.

Traverse Gl ' ,v \. ' ' r - ' ' ' ' l , '

Holes G-6 and G-7 were spotted on and just south of an EH anomaly. Hole G-7 bottomed in ohloritlo schist which could account for the geophysical feature. There are no significant metal values in the two drill holes completed. ' ,

traverse JB

Five holes were completed in this traverse which . straddled three Input anomalies. Sole H-l bottomed in iron formation which probably accounts for the conductor present at this location. Anomalous metal values are confined to the bedrock in Holes H-3 and

AS/sa A.Skrecky

EXPLAHATORY HOTES

DEEP 0VKHB&HDE8 SAMPLING PROGRAM

The sampling system consisted of a Nodwell mounted drill which weed a trloone cutting bit and produced a continuous sample through dual vail rode* The sample Material was screened at the drill Bite to produce the following fractions*

l* coarse plus 6 mesh (3*352. medium minus 6 Mesh plus 15 **ah (1*?33* fine minus 15 mesh

The recovery of ooarse and medium f raotioni is usually associated with till and bedrock penetration*

She sanpled are* i* Mounted with a varying thickness of clay. Ho attenpt was Made to reoorer this material* Other material was collected at assorted depths* placed in narked plastic bags and transported to our Sohumaeher warehouse for further processing*

The coarse and Bediua cuttings were examined to verify the nature of the sample horieon and to establish bedrock type. The fine fraction in and just abore bedrock was screened to produce the following Material*(a) vinus 15 nesh plus 35 nash (0.50 mn)(b) minus 35 nesh

laboratory work was then carried out aa this material as follows.Fraction (a) Heavy Mineral concentration* pulverizing* then AA analysis for total copper* lead* cine and nickel* This proceedure at times did not produce any concentrate shown on accompanying tables by 1.8* (insufficient •ample)* \ h change in sample prooeedure is being affected to correct \ this situation* l Fraction (b) pulverizing to minus 80 mesh then AA analysis for total copper* lead* elnc and nickel*

^^fî'^W^^ffa'^^filSfsl' • !IP*^W™!f fl'^^j^P^*^^*'* A— -••••.^-•i^jj^^T^-jîj^ .K ' . fridilT jT* 6 i OrCUplil6 fwllllGS/ LI III IT6dK Pf0fffc*|i*ii ^. ^. . ——

l: IXK

Surveys At Dip Bearing

11 | . -iCO T

From

0

3266

m

To

32

66XIX

H7

07

-•-

Description of Core

dayiMtriTillF*l*ie Itaf*. 0v la crloor -*^-^* at. ^PM tm* erf*, p^ t-M^ **r hrf*

' -

Hole N Length Date Stt Core Lo Date......Elevatio

North

o, F"X -ôf Hole... Xirted. ÛD8

17-0 f**l ..27. 197:

fe.2* c

ggnH Ky A .Slfr*cky 4t D •Heuniez*

lieet Mn qjja

ompleted Jtan* 27

July 14, 1972. . . . , ...... .. .........,. n ........................ _ ..,..^.......^....,^^. Datum ..F-*I— - _ -— —

Co-ordinates of Collar•a* clan

East .....—.. ... ............................ .... . ... ....... .. .................... .......

SLUDGE ASSAYS

FootageSample

No.

CORE ASSAYS

Footage Width Au Ozs.

Ag Ozs.

.-

'~ .

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGHole No. .......-^a.........._____....................... Sheet No.x-i.vpui.7— .^j

Location — , C-JCi

•aarzora ^L± — — — — -— — — - -—

•awford Township OntarioSurveys

At Dip Bearingc oil ir verti cal

Prom

fi

ogJ*

81123

To

38

-81 ——123128

128

Description of Core

Clay-

SandTillGabbro, dark green ferro magnesium minerals in fine grained greyfine sulphides

end of hole

Length Date Sti Core Lo Date......Elevatio

North

-. ........j.j^..— ...- ——— . of Hole... —128^ f* "ted June 27 f 19

—. — . — — — ...... .— —— ^ OBBg'"""' —— "~" rt.__._ _ ..............— ...-. _ ........ ......... _ ... _ ,...72* . C

frtrrfi KV A *Sk!rsCKy St D -Keuni^rompleted June 2

n AgB?e as nCo-ordinates of Collar

see plan

alum F — T

East — — — ..........— .. .......... .... — ............ ....................... ....................................

SLUDGE ASSAYS

Footage

green fei*Ispar natrl* fat

Sample No.

t

' dissem.

CORE ASSAYS

Footage

magnet

Width

ite tr

Aa Ozs.

ice vei

Ozs.

y

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGProperty- Location Claiia

Crawford -g-

At

Hole No..— — ..JUJ....—...............--.Length of Hole....— ..I32-*0..feet.

.Sheet No.fflBC..

Surveys Dip Bearing

Core Logged by.....Date ......July. . J&,. ^972.Elevation .... — .. same as . Datum

Co-ordinates of Collar

East

From

—0

-69 ——

89126

To

69— **e ——•J7

126133133

*

Description of Core

I^T ~*r——— i^iay ———————————————————————————————————————————

——— Sand ———————————————————————————————————————————

Till——— Felgic Tuff , grey In colour sheared spots of rust on shear plaaes- ——— end of hole —————————————————————————————————————

SLUDGE ASSAYS

FootageSample

No.i

CORE ASSAYS


Ag Ozs.

EXPLORATION DEPARTMENTProperty---Qrsxfor.

Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGHole No. Length of

Sheet No.

AtSurveys

Dip

Core Logged by--A*Ski!ack7..jt.D-^fenni.er..Bearing

collar vertical Elevation ...— — .... ...- .... .........- ...... ............— .......... DatumCo-ordinates of Collar

East

Prom

0

-4366

III

To

32

66mH?H?

-•-

Description of Core

Clayc***M**t—— Sans ————————————————————————————————————————————Till

Felsic Tu^f , grey in colour abundant otz eves trace cube rrrrite•nd of h*i"J(*

SLUDGE ASSAYS

FootageSample

No.t

CORE ASSAYS


Aff Ozs.

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGProrwtv ^ fZAmj P-o fS-C* it Hole No...... .— yrrL-*2r. _ ,.. .-...— ... _ .————.. ,. Sheet No. —- * (cr* -..,..-Lot

C.fcoH*sfc~O /2.A TOCt/fJA+h D ovT-jê-io


12*0 tc-^v t- yê-*~v c-*-t^

From

(93**i

12.3

To

3^

^1

^

IZ-^f -z

-•-

Description of Core

C.t-A^

5^*A/ O

T.uu^^^r^y #^ ^^^ /-S-*'"^ ^^2-^^ /x^fV

^~*'^sî ^x?//^ 2,.rj-^*?. ^

Length Date Sts Core Lo Date, -..Elevatio

North

of Hole...... .. ... ^.^* fi.^ 1^........ .. . ....- . .-- .irted---.'*^^'.^^!--.-r?t:.^r---'^^^?.,.Czzed bv -*A '5 K *S6 e-c^lfj-f *- "f

ompleted A^C/x*^^ ^X

t; /a/ (fcrt^

tS"*J *-*-/ * i-f * Q -7 z^.

Co-ordinates of Collar 5 GT& P ^-a /J

East .--- ...,——— .— — -— . .—— .. . . . ....... .... . .

SLUDGE ASSAYS

Footage

•^Xic/" y*xi

.^X^^^v

' ^X

"X-/-2

^XV

t^'s

^^^

Sample No.

SS&—&

^ ^Tx

?

CORE ASSAYS

Footage

V^x-1^-^S X""xJ

Width

^y,v*-1^

Au Ozs.

^xcv^^"^•^

Ag Ozs.

- x^-^

^.^,

—^2^,

^-^^•^ i'

^

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOG

Location ,...C.laosi..P*35335I..

AtSurveys

Dip

Hole No. .........f^g.............—-.__.............__. SheetLength of Hole.-—-228*0—f e*fc——-——-———-——Date Started--..-5fen9..27*.--I9.72*.----.-..............Completed .JunC-27-Core Logged by—~

Bearingcollar vertical Elevation as Datum


East

From

f

^a81123

To

33

RI123128

128

Description of Core

Clay

^™*Till

Gabbro, dark green ferro magnesium minerals in fine grained greyfine sulphides

end of hole

SLUDGE ASSAYS

Footage

green fei Is par matrl x fat

Sample No.

r dissent

CORE ASSAYS

Footage

magnet

Width

ite tr

Au Ozs.

ice vex

Ag Ozs.

7

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGPro Loc

oertv ^ /2^Â* P~ea /a-Ci 1 )ation ÛW/M P. '5536''S2L

CT*a!Vt*jp:d?(a.^ T^w/A^J^/yo ^^TN*^.,^


jC-tf Ut-^ f*-- \Jif-ten &&L*

From

0

^

tz.^

To

^

^f

^^

133/33

-•^

Description of Core

C UA-f

sôri c i- ^s*s?#*^^^^T^ -ts^^z S?*^,S 'f ^-^^^ s-c;-7-J- f-

^^ ^*C

Hole N Length Date Sts Core Lo Date......Elevatio

North

o. . JZ'-J? SIof Hole......... ..L3-3.....*?..^.e...e7"! ...irted.--.^^.'±??f...^.^^.^./?.^^ ....... Ceeed by. ^* * * ^~- fc^ . ^*\

icet No.

ompleted

^#s~^-

tJisAS^-ef


East - -— . . . ...... ............ ......... ..... ............... .. ... ............... -

SLUDGE ASSAYS

Footage

^ SSS~ - e? s. ' ^-SS•^^

Sample No.

: S2S^

CORE ASSAYS

Footage

^^v:

Width Au Ozs.

Ag Ozs.

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited

At

-collar

Township, Ontario- Surveys

Dip ________ Bearing

--vertical-

DIAMOND DRILL LOGHole No. __...5^.3..^.......................^.. ..........Sheet No- qn^length of Hole.....---.I33-*Q---*e*t.....__.......... ... ............... ..^Date Started..June-J2S^..1972-- -Completed June .28.Core Logged by- . A...Skrec^y^ ?t .vL^eigiierDate... StaSy-I-4,-1972Elevation ... .... ....SaBJe...a3. ..... .........^........ Datum ..f-X.......

Co-ordinates of Collar North East ....

Prom

0

—69 ——

8yT5/Xicw

To

69

89

1^6133133

-•-

Description of Core

Clay

——— Sand ———————————————————————————————————————————

Till——— Felsic Tuff, grey in colour sheared spot g of rust on shear planeg- ——— end of -hele ——————————————————————————————————————

SLUDGE ASSAYS

FootageSample

No.

CORE ASSAYS


Ag Ozs.

EXPLORATION DEPARTMENTProperty-

Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOG

Crawford TownsMp,""Ontario"Surveys

At Dip Bearing

Hole No.-.^— -.. ..__-.——........———Sheet No.Length of Hole ...I??.-P.. feet __...,. ...,.___.__...Date Started... ^H1.8...2?.* ±?Z?.'..... . . .....CompletedCore Logged by—A*Sferecky..5t..D. JieunLer.....——..Date..........?^^..^...A972v ,............ . ..............

one

collar rerticalElevation ..............-.............................................. Datum

Co-ordinates of Collar North

G-I

From

-J*0

49

. 50102.!

*

To

^950

102.110

110

-*-

Description of Core

Clay

Sand

* TillIntermediate to felsic tuff threads dark qtz. Trace cube pyrite

end of aole

East .— ......... .......... ...... ............ ......... . ... .

SLUDGE ASSAYS

FootageSample

No.t

CORE ASSAYS


Ag Ozs.

-

*" , l ' '

^ *. - ' !' Vn ' " - r '' t

Footageit - .' vi

; ' 75-80- . - '".,. . 'V . - 'k '"k": "'' '80-85 . :

1 'L ", '

kv . 85-88 ' ' --' ' i ' '" '

••v-'^'"' ' ' : ,'. 88-93 ; ' .

1 ; 'k ~. '93-100! "- "|" ,, - '' '"'

100-103•; , 103-105

105-110 ;J1

, /" ; ; ' i'' ' ;' - ; :- : -:, ''- ' ( J,j.,V •'•''"i!, i'' i "-' '' y.'-'- '' - 5: ; -i,"'1 ', ' * - . ' '

' . : ' ' ' •| 'i; . ; '

NODWELL HOLE NO. 0-1•"': ''' '-' '' : -•':r ; ' 1' ' ' "•"•V:.';

Heavy Mineral Concentrate ," ' CU' ~'2n ,'../ " : 'li k ! . ; '

. . ' ' , ^ '''' ! -I/' ; 'L ''

,. -56 ' ' 62 :-'. ;,'' i ..,/^-. .V"* ' ' '' ' r!*' i' ' '' ' - L- i : ' "'

. 56 , - -37,; -. - "".' •. :'^'*#-; ' . ,1 "'- ' /. . , ^.'- : f,'} ' - - '72 , '.'' 3^ •,/' 1 .-/ .•r';**b. .;. ' :

111 ' " :;' — -^ "- ; ' l "'*

51 ' ;~*7 ; .'.'•,-; ; 3650 92 60

67 98 , i 11590 12^8 ' 160

,. '131 ' . ' ^ao-,.,^^ :"'--"-:.-.98.'-".' ;--..r -'"' ' . ii / ; '" ' - 1 -'

•T: ^

Fraction

Till

Till

Till

Till

Till

Till

Inter, tofelsic tuffInter, tofelsic tuff

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGProperty... Ab Locs**!**" i*O

ildJbi-Optifln—-.-----------—-..-——-—--



collar vertical

from

-•L0

84

121 ——

-•"

To

82

84121

TOO**^ 7

129

^-

Description of Core

Clay

Sand

Till

end of hoj**

Hole No. . r"~ . .. .... ..... .......... . . . Sheet No. **^Length Date Ste Core Lo

Elevatio

North

of Hole . -I?9.?0...f jeet..

eeedbyA " s^rec'^~ - ''•^f-riierompleted June 28

n .....— -.-.r^.....?.T— — — — ,— — — .—..— ...... Datum .V*.~?—— ..,..— — ...— —Co-ordinates of Collar

East ......— . ..... ,...... ............. .....— .. . ... ..—

SLUDGE ASSAYS

FootageSample

No.4

CORE ASSAYS


Ag Ozs.

Footage

NODWELL HOLE NO. 0-2

Heavy Mineral Concentrate Cu 2n Nl

Fraction

104-106

106-109

109-111

111-113

113-115

115-11?

117-119

119-121

121-123

123-125

125-129

40

82

5360

52

51

40

72

100

214

127

48

42

5532

29

60

28

4?

68

9528o s;

600

560

270

600

380

390

370

280

162

73132

Till

Till ,;

Till

Till'

Till

Till

Till

Till

Inter, tuff

Inter* tuff

Inter, tuff


Location...--.Lot 7 Concession 3

AtSurveys

Dip Bearing

DIAMOND DRILL LOGHole No.—— ,G-^3———-—————--- — ...———Sheet No.—oneLength of Hole ......I4I-.3...rec1t........... ........^.......^...... ..Date Started--^-^JiT?.-- .....CompletedCore Logged by.-.J^5*rec*7 J'.?'!,?'ouniorDate .-Elevation —...?.?*i!?..**—.—...—.....——.—..———,. Datum

Co-ordinates of CollarM L See ?!North East .

From

-•-071

III

127131

~W

To

TIII

127

—— l±L-140

140

4

Description of Core

ClaySand

Till

Boulder of criart^ dioriteAndesite or gabbro a dark green medium stained rock

end of hole

SLUDGE ASSAYS

FootageSample

No.*

CORE ASSAYS


Ag Ozs.

__——————

"..'1: ;

Footage

NODWEJ.L HOLE NO. 0-3

Heav.y , Hlneral Concentrate'' ''" Fraction

116-121121-123

123-125 :,

125-127

127-129

129-131

131-138

138-140

53 : : :;557068 "~" . ;176.-7370173

,-, :-' ' : . v.r ' ' 40 "W ; 49 L

iii20 -' ' -. 81 '..•"'"' : '

" ' ^7,': ,- ", ' 63:Vv : .' * ' ' - " .- .

^''59 ..- - (d ~' ,

./^:- ;? '^^^••.•"•S* -' ' : . " : 51 . J

:^*V i:; :-v.'5p' : : i ^'' r7^ "'''., . ^.67 ; J : .:.

; " , T1^1 •'•'•v .i ,: : ,;;'^tui;'"""'^ '- ^..''rf- -fuiiV';^':.,.;-!".

* ' ' '"' ' f ,^- f "' - '- 'x ' "K - '

'' :'' ; i ::fl3!l' : : "' '*; : -' . '. f::. ' '' ^ . . '- .

'•-. : .',..';^ouild*v. : of,' ; .- ,. v :'\, 'c^wartB.^iorJLte'

j , v1 ^; Andealte :. r( ;, . .•', ' '. k - - ' ;- ' ';-- ' t : ' -{ :; ;

r,-,- '.'^ Arjd^tltQ . ^ :

Andes It* '

•.'^•:.-

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGLocation ....-.-....-.L.qt...?.. C.Qn.c.ession..3.

Hole No. ..........fek..... .. . ^ ....... .......^........... .. ..Sheet No. .....o?® .Length of Hole J?^ feet

AtSurveys

Dip Bearing

Date Started-----.---July..J!4.,..J[9-72--Core Logged by..... . A.,,Skrecky.Date . . .. ..JWLy.!?,, .1972.

Completed ...... July..5——

Elevation — —— -— — — — — — - DatumCo-ordinates of Collar

North East -

Prom

-•-0

—JLOi.T O1—— L-f.fi

—9

To

105

122

—— I33E- 131

^-

Description of Core

Clay•r-m

————— Felsic tuff yellow groen in colour rock stained with limonite — end of hole

SLUDGE ASSAYS

FootageSample

No.

CORE ASSAYS


Ag Ozs.

^

—

Pootage

NODWELL HOLE NO. G-4

Heavy Mineral Concentrate Cu Zn Nl

Fraction

105-110

110-115

115-117

117-120

120-122

122-124

124-127

127-131

62

90

89

7370

^3

38

104

5066

58

62

78

59

5593

, 54

66

60

48

73

50

22t

110

Till

Till

Till

Till

Till

Pelsio tuff

Pelsio tuff

Pelsio tuff


Location..Crawford Township

SurveysAt Bearing

rt.r*4-v— -*

Hole No..............Length of Hole.... JSQ*C reel—---- —---. — --Date Started^.........................^..............................CompletedCore Logged by.......A^e^LAl' 3^^................Date . ....Julr 6^. IS72 .. ......... . .. . ...Elevation ———?5?!?—^.?.————.——-.-———..... Datum

Co-ordinates of CollarNorth ^^aeeEast ......—.....^...

From

^•L. 0

80

108

117118

124

128I-?8

~*

170

To

8010!

irin121

12!

13

171

I8(

Tft(

*~

Description of Core

—————— clagc ————————————————————————————————————————) sand

Gravel or till

S da yGravel or till

J clay

J till

i Qii /sy With Vtt^*y ' P^ ff^j[^. f^nn prtonj^f^ ij* flMT-ttw^j. ^ Mst^ft^jJ st. | ^n^^^jj jjsulphide content with snail bell like and cubic forms* Many c

average 25 percent sulphides.

t Basic tuff - a chloritic rock showing distinct bedding or she*

l w** of* hoi**

SLUDGE ASSAYS

Footage

nfQ offhrpubes are

ring

fco bi*1alter

•Vtffl \,IT

Mi tot PT^CTdark 1

Sample No.

in colo^piont't-*'-!

CORE ASSAYS

Footage

IT. It "Entire

Width

oo/il TT^sec tic

Au Ozs.

showsD WOUl*

Ag Ozs.

a M rrKi* aai&^Bi

1

NODWELL HOLE NO. 0-5

Footage Heavy Mineral Concentrate Fraction: 'CU '., . Zn ' ' ' Nl ; "^"'U .

138-140

140-142

142-144

144-14?

147-149

149-151

151-152

152-154

154-156

156-158

158-160

160-164

164-166

167-168

168-170

170-173

173-176

176-180

50

175

215

190

180

248

185

15

20

13111

6547

112

72

297

197

513

28

184

142

142

95

43

52

12

1*

14

38

4763

7341

15*131115

112

no* ,

150* 96

92 ' . '100

15*

122

1231 .

112

95.113 /'. : v

M 85 r,-:

108 '; ' .67:--;,,.'-

209118

. ; 87 ( ;

Clay and till -•locally heavy pyriteClay and -till.*locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and fclll -locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and till -locally heavy pyriteClay and till - Jlocally heavy pyriteBasic tuff

Basic tuff

, Basic tuff

; .f

v." -- * """ ;: ''' f ^V ' ,: l'

: 'S


d Township, Ontario

Surveys

At Dip Bearing

Hole No. ... Length of Hole Date Started....Cote Logged by Date . -.. ....

DIAMOND DRILL LOG. .. . . Sheet No

H6mQ feetCompleted

vertical Elevation ...— —. ....... ^... ....... ... ....... ................ Datum —C— 6-Co-ordinates of Collar

North East .

see plan"

From

-*0

.2534

88

97110

~9

-

To

25

3488

97

110116

116

*m

Description of Core

OTcrbttrden clay; ^rey

————— silt.; gmy —————————————————————————————————————gravel

sand and gravel

————— clay; grey —————————————————————————————————————altered tuff grey green in colour,, carbonate, *h^r^ an'1 chlor

end of hpl**

SLUDGE ASSAYS

Footage

ttie ———

Sample No.

t

CORE ASSAYS


Agr Ozs.

Pootage

NODWSIX BOLE NO 0-6

Heavy Mlneiral Obnoentrate Cu Zn Ni

Fraction

34-40

50-66

66-80

80-88

88-100

110-113

113-116

45

60

48

4354 ;860

53

^3

29

35.'W

• .'•'•Iftj •^.'•-,

; -.r 0 i'"•r?8'W-;

40

38

45

44

50

l - ,39 ''* "51 .. ;i.

Till, sand and clayfill* sand and o lay

fill* sand and clayTill, sand and clayTill, sand and clay

Altered tuff Altered tuff

'\

EXPLORATION DEPARTMENTftopetty S6KI Locatlon -tot 6 -Grewferd Township, Onfeario

Surveys ____At________Dip Bearing

Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGHole No..... _ .g,..!*............. —. ..............................Sheet No.-0jje-— —Length of Hole ^ JJ^CX. feet———————————————————— -DateStarted.... Jyly...7,..I5.72.^.. .......CompletedMy 7Core Logged by— —A*i3arecky...at-i;.BiirtQn.——— .. ........ .........Date... .... ............. ..^. ,. .,...........^.^.,....... ............ . .....Elevation ... .^^ as . . ... . ..... .. .. ... Datum

Co-ordinates of Collar North East

From

-•-—— 0 ——

— tft— — v-

80

83

^*-

-

To

ZiOi+w

——— 55-

PO

83

95

9^

a-

Description of Core

———— gut ———————————————————————————————————————— gravel ———————————————————————————————————————

gravel and bedrock mat.PTH alG tJ t- tp /Z- rf t c, Se/V/s"

————— end of hole ————————————————————————————————————

*

SLUDGE ASSAYS

FootageSample

No.

CORE ASSAYS


Ag Ozs.

d •' . "'5 f '. ", i ' .HODWPLL HOI^E NO. 0-7

Footage jieavy Mlnefeal Concentrate FractionCu ' ; Zn l Nl

5'^- 60

60-70

70-80 ;i i1 "

80-83

83-88

88-91

.74

99

135

133

370

102

75K,.';^

77 '

88

42

275

63

, vv' 77 " -'1 ? *"'' 71 '

, : v87*8113

53

Tillr

Till

Till

Till

Chloritic schist

Chloritic schist

fr^-,

in H-a-1

•t-i

l

•4-•H-•t-—" l M

*" "J HMH.

O'

cf. O '

i l

Tfiat

•i

i--

"Sij

[j

O

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGproperty Abitibi Locarion Let 5,

f.-rawfnrd

-one~2

AtSurveys

Dip

-Ontario

Bearing

Hole NO.......H.I.-..............——.......... ..Sheet No.Length of Hole...---2(X)-JO..J!eet.---.----------------------..-Date Started—.^^^...g——...——..........—...,. Completed JttlyCore Logged by—..-A*Skrecky-i-iU3urton ---Date .. . ........ ,... .

G-ol4a-p————— -vertical— Elevation -ag—— Datum Co-ordinates of Collar

H-I-

North... ..............see .planEast .——— .

From

-•-0

sn90

ICC

109130

140195

~W

To

SO

CO

100

109

130140

195200200

*-

Description of Core

overburden clay; grey

very f*3fV ^qn^ afiri frivol

gravel

clay; f^rey

————— gravel} II7-IIg quarts vlih pjrrile —————————————————————— clay; ^ey

gravel; 17^-18? sand pell Rt q

siliceous tuff, a grey yellow rock with I5& disseminated iragnet-end of hole

SLUDGE ASSAYS

Footage

te aa de ATI t.T ny pnHTI?

Sample No.

CORE ASSAYS


Ag Ozs.

Pootage

NODWELL HOLE NO. H-l

Heavy Mineral Concentratt Cu Zn ,

Fraction

115-120

120-130

140-145

145-150150-160

160-173

173-180

180-190

190-200

9064

64

69

3? : i

22

27 "

81

57

70

50

^01

37** '*

16163164

133 ; .106 '

"M " 76 '; i PI

120;- '/ v ;'': 81

l"68

760

460

510

Till

Till

Till

TillTill

Till

Till

Till

Felsic tuff ant

'.t

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, LimitedAbltibi-eptlon

Location .....Lot.-^-CoiV^&Si^fV 2 ——Crawford Township , Qrytario

Surveys _______ At ________ Dip _______ Bearing

.-collar-

DIAMOND DRILL LOGHole No. H-2 _——.....————— Sheet No.Length of Hole_-2QQ*Q—fc**k~~~~"_~~~—__—~———______ Date Started———July—IQ———————. .—— Completed -,JttlyCore Logged by——A-.-Skreefcy'--Sr S-ri Date— Elevation .

North .—— East ——

as ....._—..———_—..... Datum Co-ordinates of Collar

From

-*-0

QT

140

- 195

-*

To

—— 9J.T^O

195

200

200

A^

Description of Core

—————— overbttrdon clay ——————————————————————————————————

90^ cl.Tj; 10^ aand ft graTel ...,— .

—————— gabbro- a dark green aeditm grained rock with d--rk — ferronagnoi —————— end of hole ————————————————————————————————————

SLUDGE ASSAYS

Footage

t™ i" ^txuni L fTflfl l J^A \J\*n -ff.1,EX -t v^ ^ 1 *tTV^T* T

Sample No.

i6LuJrj.3C

CORE ASSAYS


Ag Ozs.

NODWELL HOLE NO. 8-2 ;

Footage Heavy Mineral Concentrate FractionCu Zn Nl

91-100

100-120

120-140

195-200

108

95198

69

85

82

47

37

668930081

V Till

TIUTill

Gabbro

J


Location .-Lot 5 Concision 2Crawford Township, Ontario

Surveys ^^^^^^^At_________Dip________Beating

DIAMOND DRILL LOGHole t*o...........??3..--....~————..._-..-__ Sheet No.Length of Hole . .JTO-OJ*^ ........ . ..... .. ..^..Date Started. July.II ......^ . , ... . .Completed July..I2-Core Logged by..-A^Skreeky-feSrSitrtoaDate...—...................... . ..... .. ,-,. ... ........Elevation......?™? ?3 . -.... Datum .. H-l.........

Co-ordinates of Collar North .. East ..

Prom

-•-090

160

"T

To

90i5e170

170

-*-

Description of Core

overburden clay; 7^-76 bedrock of B-2gravel; 96-98 bedrock of H-2; 104 pyrite in black roc|; II3-IE

felsic tuff green in colour, serlcitized, carbonated rrfn t.r- mil

—————— end of -bole ——————————————————————————————————————

SLUDGE ASSAYS

Footage

green gr

*t py*rlte

ey TO :k wi1•h some

Sample No.

pyrite

CORE ASSAYS


Ag Ozs.

Footage

NODWELL HOLE NO. H-3

Heavy Mineral Concentrate Cu Zn Ni

Fraction

93-100

100-113

113-120

120-128

128-140

140-150

150-160

160-170

52

141

70

188

143

158

55

135

43

108

60.122

87

70

103

2250

52

86

149

133

300

400

370

74

Till

Till

Till'

Till

Till

Till. ^i/V/^'-v'

Felsic fcuff

• , f i

s A


Locarion..-...-.Lot5^ ..g

AtSurveys

Dip Bearing

Hole No. .........Length of Hole....Date Started.. -July-lZ....-...—......Core Logged by.. Date......... .........

..... .Sheet No....... -j™-—

.....Completed Jv^y..

collar vertical Elevation ..... SSSie ,,aft.. .................^........ .. . DatumCo-ordinates of Collar

North East .. see pTa n

From

-•-0

60TOO

— H5-I?A

132

I4S

~V

To

60

—— 100-

—— U5-"r*-* rt- 128 13?I4S

154154

^

Description of Core

overburden clay

————— gravel ——————————————————————————————————————————

sand pellets

————— gra-val ————————————————————————————————————————

cisy* ^Knn** finr3.Tr^l And s&ndsand and gravel

felsic tuff with scattered clear qtz eyes rock grey to light grend of hole

SLUDGE ASSAYS

Footage

*wi in co Lour i "horo B6A&— {7

Sample No.

ilorite J

CORE ASSAYS

Footage

.0 evideti

Width Au Ozs.

*k Til?*-

Ag Ozs.

f— .-..xWA \*blA^ 5 IT

NODWELL HOLE NO. H-4

Pootage Heavy Mineral Concentrate FractionCu Zn Nl

60-80

80-100

100-120

128-138

138-140

140-148

148-154

W

62

?8 ,

34

61

210

1890

49 '; 36

* ,j 69* "-

120:"A' *6 - v ''

166

1690

# *'' .'" ' 'T6 :

' 236

120 -^! '- ; ' \ ' \i

126

228

129

590

Till

Till

Till

Till

Till

Till

Pel s lo

••t

v y , ,-

tufftrace pyrite



BearingAtSurveys

Dipcollar vertical

Hole No......Length of Hole...ISO*-0-iect— — — — — — — — — — — — — — —Date Started.---, .^yly 12 .-...-...-. . CompletedCore Logged by^A'^^y b ^.MeunierDate ——. - .. .— -.-- , - —- . Elevation ......sase...a.3... ..— — ......... .— -— Datum B-5

Co-ordinates of Collar North , East . . — .

From

-•-——^CL—

84

I^n164

L 166

167169

172175

To

__ 24-120

I6A166

167

169172

175ISO

ISO

9

Description of Core

nvnrbiirden clay-

gravel

claywhite clay, some quartz chipsyellow clay

white clay, some cnart;". chipsy boulder of bedrock

————— white clay somft quatrs and bedrock ————————————————————Cleared felsic ttiff or rhyolite grey to green in colour latter csericitic end of hole

SLUDGE ASSAYS

Footage

ue to zeeessor SL-Cbli )rite.

Sample No.

Rock mi

CORE ASSAYS

Footage

1 tT* C1

Width

* pvi'j.t

Au Ozs.

p Hoc

Ag Ozs.

c high]y

NODWBLL*HOtE NO. H-5

Footage Heavy Mineral Concentrate FractionCu J5n Nl

8^-100 57 51 56

100-120 263 225 123 Till

178-180 115 1^0 70 PelBlo tuff

,t ' -*. 1

OVERBURDEN DRILLING LOG

SAMPLE NO -

2cZ- /u HtLf3"

LINE:

^ S E L ///E

OR ILL MOLE NO:

7^/SAMPLERS :ea /raSTATION :

l* J

DATE: , 1

a^ /3/72JCON TRACT

/tc/^r//?^

* * "^k -" .M,


SAMPLE NO:

.2, ci ?^Z-SAMPLE DEPTH:^3 ~2*

LOCAT1 ON: j LI NE:

CRAt#p6 K&TrtP A-4 S F l "f* Z

OR ILL MOLE NO:

^ 3uSAMPLERS :

C. L fi. LSTATION :

#-3-*

-

OVERBURDEN DRILLING LOG ^^

DATE: ; V i "M "L t MO:

^5/^^ i ^^^-CONTRAC/ ————— ————————————— i SAMPLE DEPTH:

ft c //y r y x F 1 x 'TxJwFeKD r*r ^ s 2'^

^3/f/. /? ^

3^3

^u /^flcs#77tfg-CfiJXJFoRP 7*P

POINT STARTED: Q* '

POINT STOPPED: J 6 ' b 3

POINT EXTR ACTED:^/^

DRILLING TIME

SAMPLER STARTED:

SAMPLER STOPPED: /'QQ

SAMPLER E XTR A C T ED: /l* C- ^

POINT STARTED: S- f * Q

POINT STOPPED: 3- '

POINT EXTRACTED:^.. ^ 5

DRILLING TIME5"ya. l &T 6* CsnJ

SAMPLER STARTED: ^ ' O

SAMPLER STOPPED: ^ l 3~ O

SAMPLER EXTRACTED: f'

POINT STARTED:

POINT STOPPED: '

POINT EXTRACTED:

DRILLING TIME JTXjZ. J- a T6

SAMPLER STARTED:

SAMPLER STOPPED: *——~

SAMPLER EXTRACTED: (^

FOOTAGE

FROM

O'f*

!3*19'

W 7"25 'S"

TO

/'

J3-

/y2 i' ?"2S-3"

OVERBURDEN DESCRIPTION

0 A S A "'C-c IA/

f/ Af E S A * bg c L P ^/?S~T, J-JL

-S v # at/'T' c y? a#

SAMPLE j

DESCRIPTION

ORGANIC r.

CLAY r.;

SILT -,,

FINE SAND ".

MEDIUM SAND *1 i

COARSE SAND r.i

GRAVEL 1 1

PEBBLES

REMARKS:

FOOT;

FROM

0 '

/-

/S.'?"

j 8- y2.2 "7"

P5\2"

REMARKS:

iGE

TO

/ '

/2'7"J Z" 7"2Z7"33 '3 "

6 /f G ^ *r t cc J~siy

TIME 3*4*0ft s J. /9^/fS

fsJL^

y V x3 0 o'7~~ C /f^^

SAMPLE ' FOOT/

DESCRIPTION j FROM

ORGANIC -. i S\ *

r.; g '

-i /? -

FINE SAND ~. ! 25

MEDIUM SAND ", ! ^ O^

i/ J '

GRAVEL -. !

MtMARKS:

XGE

TO

a-;j-as-5a*^/-

i ————— — — — — ——————— -- ———— ,


0 K G /4 ///ccuy

F s //z SJ#P s c LAYc t fi ^zTiLL

S f 8 a uT c, /f Q&

SAMPLE

DESCRIPTIC.'

ORGAN' C

CLAY

SILT

flN E SAND

MEDIUM SAND

GRAVEL

PCBBLCS

OVERBURDEN DRILLING LOG OVERBURDEN DRILLING LOG OVERBURDEN DRILLING LOG

SAMPLE NO:

SAMPLE DEPTH: -y/ 'OR 'L L HO LE NO:

C. Z, H L

l

/CONTRACT:

LOCATION:

POINT STARTED: S f "V

POINT STOPPED: f Ci '2-

POINT EXTRACTED: f Qi 5~ @

DRILLING TIME 5 Xz. J- e~7~(p

SAMPLER STARTED: *———~

SAMPLER STOPPED: *-"'

SAMPLER EXTRACTED: ^-

do

FOOTAGE

FROM

0'2. '

13'2.5-38'f/'

TO

2. "

/3'25"se-?/'


OK G A x'c-ctsr

F/// f S^HQ* cJ-^yQ /Ul/^L7//^

5 ^ 13 a is~7~ c /? a ^

SAMPLE

DESCRIPTION

ORGANIC r. i1

C L AY "V f

SILT •'.l

FIN E SAN O ". .

MEDIUM 5A*4O ",.

COAHSC SAND r.

GRAVEL ".

PEBBLES

REMARKS:

SAMPLE NO:2/^- ySAMPL E DEPTH :

39'

LINE:

d^ 5 E Zx/v^r

OR 1L L HOLE NO:

#*iSAMPLERS:

/?^, RLSTAT.ON: ^^

OATE: 11

6/6 /7 |CON TRACT :

ftcwry RE.LOCATION:

c fi /}W Fa fi 070 P

SAMPLE NO-

POINT STARTED: 8'3 ®

POINT STOPPED: /C ' J

POINT EXTRACTED: /f '

DRILLING

SAMPLER STARTED: l 2. '

SAMPLER STOPPED: t

SAMPLER EXTRACTED: f r

FOOTAGE

FROM

0 'a-

S3'3VS B'

TO

a-S3'

3V38'


G RG A xi c.c t y

F/s/Z S^ISSPTs IL

S a *6 a u~7~ C /?a S

SAMPLE !

DESCRIPTION :\

ORGANIC r.i

C L AY ".

SILT ". :

FINE SAND

MEDIUM SAND ".

COARSE SAND r.

GRAVEL -.

PEBBLES *v :

R EMARKS:

S

SB'

DRILL MOLE NO:

SAMPLERS : CONTRACT:

LOCATION:

POINT STARTED: ^*~

POINT STOPPED: ^**

POINT EXTRACTED:

DRILLING TIME S^^L.

SAMPLER STARTEC: /'

SAMPLER STOPPED: J *

SAMPLER EXTRACTED: y

FOOTAGE

PR OM

O"2.'

S3'3?'y Q ' j (j

TO

2~ '/3'

3Vse-


C /f &A A* /^cis/

p/S^Z ^s* #P7-,*^

S t/ t7#7~~ c^/Ta/?

SAMP LE

OESCPflPTiO"

ORCANi c

CLAY

SILT

FIN C SAND

MEDIUtw* SAND

COARSE SAND

GRAVEL

PEBBLE5

REMARKS:

3


J2l"/)-32'

/BASF JLSM&

#*?

"/?J-s /?Z™'~ ** fOATE: y .

F/&/72L,


2LA- 6

/*lCSAf7~yS!*E. 13 *

C/f/Qt&fafifi ~7s#P r^~ '

DR'LL MOLE NO: ~' ———

3* /3

6J-, /SsL——— ^/3

"V/6/7Z'

.

*OVERBURDEN DRILLING LOG

2iA- rM C //ST/ ftJE. 3^ ' 7"

LOCATI ON :

CRAujfaRD Tx/P-^ s

™^ , #j- , /rz-

^ /r-. . . . r\s.

"-' t: l l7/^/7^

Mc;*TyjZCftAUsfaftP Trt; , ; ,,-7-yi r^mj S*

POINT STARTED: &J l

POINT STOPPED: ^f f f

POINT EXTRACTED: G,

DRILLING TIME.J}^L

SAMPLER STARTED:

SAMPLER STOPPED:

SAMPLER EXTRACTED

CcnnJ

' *POINT STARTED:

POINT STOPPED: f ' ^ 5"

POINT EXTRACTED: 2- *"

DRILLING TIME S Xi, * o

SAMPLER STARTED: 2

SAMPLER STOPPED: 2.* ' -1

SAMPLER EXTRACTED: 5' 3

FOOT

FROM

Q'

a-B'36'

AGE

TO

e-B'

36'32."

0 /f &/1 */ cC t /)/

p/S/Z S^ *D

(^ Rjy^l-

SAMPLE '

DESCRIPTION i

1 ORGANIC ". j

CLAY *i!!

SILT r.;

FINE SAND ".

MEDIUM SAND *i .

GRAVEL

PEBBLES ".

FOOTAGE

PROM

o -

rZ 8 '37'Y3'

TO

/*

26"37'ys-


^ R C? A /*J zc j. Ay

^/*z s**p-rsj-L

cS^/5* o o-T" d /? a g

SAMPLE j ! 1

DESCRIPTION j

ORGANIC r* i

CLAY

SILT

F 1 N E 5 AN D ". :

MEDIUM 3AWO ". :

COARSE SAN D r. ,

GRAVEL r.

PCBBLCS ".

REMARKS:

POINT STARTED:

POINT STOPPED: f j

POINT EXTR ACTED: /

DRILLING

' ^ SAMPLER STARTED: /' ' *SAMPLER STARTED

SAMPLER STOPPED: /J

SAMPLER EXT

5"

POO T AGE

FROM

C'

t*

W33*

36'7"

TO

X "

/y53*^'^


G R (^ /t#ic-c^^y

p /H E 5^ "0 * Ci A/~7 s JLL

S#s# a o~7~ C/TSS&

SAMPLE

DESCfiP':C;

OWCANt C

CLAY

SILT

FIN E SAND

MEDIUM S AM O

COARSE SAND

ttWAVEL.

PEBBLES

R EMA R KS:

X L S


-2LA- 7*tl'7"

#- /

^ y STAt, An*

l* /S

8 /^/7^

OVERBURDEN DRILLING LOG i OVERBURDEN DRILLING LOG

2.L A-Me s //T y x g s vCRAwFoRb To/ P ^ S

#- s t.SAMPLERS: —————

#1. XL/to

DATE; X J SAMPLE NO:g/^/7^ ez^9-^///77#Z 7VLOCATION: . "LINE- ' ————————— ™" ——

C ft A IV po K l? 7&P ^ S

OR 'L L HOLE NO:

**/?

SAMPLERS :

fil, fi LSTATION:

/7

DATE: , ,

8/6* /72sCON TRACT ;

M c wry # E.LOCAT1 ON:

CffJtvFoftPTte;DRILLING TIME

POINT STARTED: li l J SAMPLER STARTED: l* ~~ ~*

POINT STOPPED: O ' 3 SAMPLER STOPPED: 7* D ^

POINT EXTRACTED: . 2- O SAMPLER E X TR A CT E D : / O ' ^L. O

FOOTAGE

FROM

O'a*

e^-37'Va.-?'/

TO

e.-2.^3?'yz'7"


0 RG A /v/ cC l /4/

P / A/ ^ SA ^ oT' J-L

5" u B a u~7~ c ft o 8

SAMPLE |

DESCRIPTION 1

ORGANIC -.i

CLAY

———————————————————— i

SILT r. j:

fIN E SAND -. ,

MEDIUM SAND ". !

COARSE SAN D ~. :

5RAVEL -. ,

PEBBLES ",

REMARKS:

POINT STARTED: J O f ^ O

POINT STOPPED: //* / 5

POINT EXTRACTED: ^— """~""

DRILLING TIME /*/ J- a7~6

SAMPLER STARTED:

SAMPLER STOPPED

SAMPLER EXTRACTED:

FOOTAGE

FROM

O'2'

3o'V7'

S?*

TO

2*so:V 7'

5V


o 8 G** J cC L A f

Py/y^ SA*D-7~s^L

StiS oes-r~ C.S?oB

1SAMPLE

DESCRIPTION ;

l ORGANIC •Si

j

CLAY -. l

1S 1 LT ".j

FIN E SAND **. i

MEDIUM SAND ". i

COARSE SAND r.

GRAVEL

PEBBLES r..

M*'5

DRILLING TIME 5 X^- ^ aJ- fe

POINT STARTED f 2- J 5 SAMPLER STARTED: ^—*

SPOINT STOPPED: 4

POINT EXTRACTED

SAMPLER STOPPED:

SAMPLER EXTRACTED:

FOOTAGE

FR OM

0*2*

33'

5VGb*

W

TO

a-33'

sv(?b*7V


0 A fi y* /v; cc //4X

p/ ^^" (5 Ks4lS^LG ft*4iS^L-T' t L

S t/ g c tT7~~ ^ X a g.

SAMPLE

OESCRIP^'O-

ORGAN! C

C L AY

SILT

riN E SAN D

MEDIUN* SAND

GRAVEL.

PEBBLES

REMARKS:

OVERBURDEN DRILLING LOG OVERBURDEN DRILLING LOG OVERBURDEN DRILLING LOG

SAMPLE NO :

- 8

X

OR 'LL HOLE NO:

SAMPLERS :

SAMPLE NO:

CON TRACT. SAMPLE DEPTH:

LOCATI ON:

DRILL HOLE NO:

SAMPLERS :

/f

DRILLING TIME

POINT START ED: /*3^ SAMPLER STARTED: l* ' '

7 * SAMPLER STOPPED: /O* f

Y' 3 5 SAMPLER EXTRACTED: [O ' L

Gem!

SAMPLE NO-

CON TRACT

LOCATION:

POINT STOPPED:

POINT EXTRACTED:

DRILLING TIME 5)^2. J~a7~6 GfrJ fa

SAMPLER STARTED: /*- f 5

SAMPLER STOPPED: /, 7-5

POINT EXTRACTED: X S.*/ 5" SAMPLER EXTRACTED:2'

POINT STARTED: f f *

POINT STOPPED: //,

REMARKS:

FOOT

FROM

o-f

3k'57'6,2'

\GE

TO

/*

34*

57'^a*

^5 /? a /4 /V X ^

c /^yT/^^r s*#*TsLL

S u g a vr- c X 06

SAMP L, E i FOOT /

DESCRIPTION i FROM

ORGANIC ". /** *

CLAY -. O *

SILT -i p ry *

ri*J E SAND ". JJ f? *

MEDIUM SAND "i tj Gt *

*

GRAVEL T.

*

kGE

TO

2-2.7'

vr-yf

^5 R C* A * 'C

C J A/F ///^ ,S ^A'^^x ^^.

6* ^^5" 0 v ~7~ c fi a 8

SAMPLE j

i

DESCRIPTION '

1

O ft C A N 1 C "* j

iCLAY ". *

Js t LT r. ,

FINE SAND ".

MEDIUM SAND ".

GRAVEL ".

REMA RKS:

X -T /r

SAMPLE DEPTH :

5 9' Sb*

DRILL HOLE NO:

. XL CONTRACT-

M c/ # ~r y js zLOCATION:

POINT STARTED: — '

POINT STOPPED: O*1 ' ^

POINT EXTRACTED: 3 *

DRILLING TIME

SAMPLER STARTED: 3'

SAMPLER STOPPED: V*

SAMPLER EXTRACTED: '

FOOTAGE

FROM

0 '

y2*"5^'5f'5"x

TO

x-a-y*5a-5^5"


O K G* /4 //' cc i A y

P/ /v *f S s?S/ ^~7~/ 2- L.

^ -^x5 a tr~7~ C. /? (? S

SAMPLE

oescRip~'C-

ORGANI C

CLAY

SILT

FtN E SAM O

MEDIUM1 3AND

COARSE SAND

GRAVEL

PEBSteS

REMARKS:


SAMPLE NO:

2//J-OR'LU HOLE NO: tf. — y

SAMPLE DEPTH : SAMPLERS :

AA.CONTRACT;

LOCATI ON:

P

*7 "2 OPOINT STARTED. (' -1

POINT STOPPED: 7* f S

POINT EXTRACTED: /(J* /O

DRILLING TIME 5Xi L a 7~

SAMPLER STARTED:

SAMPLER STOPPED: ^

SAMPLER EXTRACTED:

FOOTAGE

FROM

0 '2.'

W72'73'

TO

a-yf7^-'7^'


o* (^/) # )tC J- A y

p //J& S S) # *

y/ JLJLS t/ 4 av7~~Crf6#

SAMPL.E

DESCRIPTION :

O R CANT C ** \

CLAY

3 1 LT

FIN E SAND ".

MEDIUM SAND -.

COARSE SAND T.

GRAVEL ".

PEBBLES *1

REMAP KS:


SAMPLE NO : DRILL HOLE NO

SAMPLERS l CON TRACT ;

LOCATION:

DRILLING TIME 3 Xi L o7~ 6r ffirW b

POINT STARTED

POINT STOPPED: f f

POINT EXTRACTED f'

SAMPLER STARTED:

SAMPLER STOPPED:

SAMPLER EXTRACTED:

FOOTAGE

FROM

o-a*

55*60'78*9V

TO

a-?5*&6 1

78'

&V


o K G* A M l cC l A/

Ft //g S*"*P /x e GKAI/ZLT, z lS u k o u7~ c /? G S

SAMPLE 1

DESCRIPTION

ORGANIC ".

CLAY

SILT

r IN e SAND -v

MEDIUM SAND ~.

COARSE SAND

GRAVEL

PEBBLES

P EMA RKS:

7

\e.

lF *1

/9 S8 /7 /f /S

®45 ®tt Q'* O54 O&-

\\ ^

'oV^^DTV ^ ,

W*'. \\

A\ ;** OV - : -: ^ :-:

^ -\ : : :

K ^©Q^/o ^ *?r?) v-x x . ..^ * 0 Q

O. C/.0/S1 J* - 33-3S-?/ r\

:. 1O

i-- -^

-i Q

/5 /^ /X A?i

37 ©431 O O O HFSlJ^ *j^ i.

: ' L:::: v: 1 " ' . : : :.::j.. :| : ' - :; : • ::: -1 ; - ' . : . . . . ; . . . - ;

i.:::...:;..:.: j -r : : : -'-;: ':: " : - : : " ; : : . - :

/3

6

7 CJLff/fl P-33*3f7O

8

9

Co*. 6

COM y ;

, - .

C ftofrtV TT CiA*f*Z. . ..- -- ' ..j. i.

OBO//DAR -

6DXILL HOLES

3~ 6

l T -'im^r^i.^g ^r

MINERALOGICAL DESCRIPTION FROM OVERBURDEN SAMPLES IN CRAWFORD TOWNSHIP, COCHRANE, ONTARIO

t4e L C wo. lSample #1

402 Hornblende 302 Pyroxene 152 Garnet 102 Epidote

3/0 Magnetite 12 Pyrite, mostly all

sugary and some cubic

Trace of Zircon and Mica

Sample #4

502 Hornblende302 Pyroxene102 Garnet 52 Epidote 32 Magnetite 12 Pyrrhotite

Trace of Zircon,Pyrite, Mica

Sample #7

502 Hornblende 3525 Pyroxene52 Garnet52 Epidote32 Magnetitel 0/ Mica

Trace of Pyrite, Hematite, Zircon

Small sample

Sample #2

302 Rock fragments 252 Pyroxene 302 Hornblende

52 Garnet52 Epidote32 Magnetite12 Pyrite

Trace of Hematite l grain of Chalco

fjfei.6. U O. 1*4-

Sample #5

502 Hornblende 302 Pyroxene 102 Garnet 52 Epidote 22 Magnetite with

Pyrrhotite 22 Pyrite, mostly

fresh, some sugary

Trace of Hematite, Zircon, Mica

Hot.s uo. '8Sample #8

502 Hornblende 302 Pyroxene52 Rock fragments52 Pyrite52 Garnet32 Magnetite12 Mica

Trace of Pyrrhotite

aoSample #10

Hornblende 305^ Pyroxene l O 0/ Garnet

535 Epidoteyjo Magnetite135 Pyrite135 Mica

Trace of Zircon

Sample #3

402 Hornblende 402 Pyroxene 102 Garnet52 Epidote32 Magnetite

Trace of Pyrrhotite, Hematite, Zircon

Small sample

Sample #6

40& Pyroxene 452 Hornblende

52 Garnet5'/ Epidote311, Magnetite135 Pyrite

Trace of Hematite, Zircon, Tourmaline

w o. * 9Sample #9

502 Pyrite, mostly all cubic, fresh and linear

302 Hornblende 102 Pyroxene 52 Garnet 52 Magnetite

BDNDAR-CLEGG SL COMPANY LTD.ROAD, OTTAWA. ONTARIO. K1B OZ5 PHONE: 237-311O TELEX: O53-354B

Geochemical Lab ReportExtraction-

Method—-

Fraction Used __

Cu, Zn, Ni - HN09-HC1

.... ..JLA..........

^ -150 Soils^ _...

Report 467-2

From Mr. R. Cormier.

Date_ -Ju J9 72

SAMPLE NO.

2CL - 1

2

?CL - 3

2LA - 4

6

78

9

2LA - 10

i

Cuppm

11

8

20

23

11

10

516

28

29

In ppm

21

15

16

108

25

28

1125

37

69

N1 ppm

17

36

27

28

16

14

928

24

32

Mo ut rOo.

1 j

2.

3

-4

14-

'3

i5

\B

/9

zo

REMARKS

-150 FRACTION

BRANCH OFFICES

1500 PEMBERTON AVE., BOX 487,

NORTH VANCOUVER, B.C. CAMPBELLTON. N.B.

BONDAR-CLEGG 8t COMPANY LTD.760 BELFAST ROAD (M.R. 1), OTTAWA 8, ONTARIOPHONE: 237-3110 TELEXt 013-3 548

July 8, 1970

Mr. A. Skrecky, Exploration Department, Mcintyre porcupine Mines Ltd., P.O. Box 970, TIMMINS, Ontario.

Dear Mr. Skrecky:

Enclosed are the analytical results for the over burden drill sample.

Examination of the heavy mineral fraction has in dicated the following estimated concentrate composition:

hornblendepyroxenegarnet (mostly pink - a few brown)fresh pyritesulphides attached to rock fragments -unidentified rock fragments magnetite

i-;i-;

i-;

As indicated over the phone, we expect to have a drill available sometime about July 20. Charges for the drill and two operators would be $100.00/day with Mcintyre to bear the cost of any lost rods while drilling eskers or boulder beds. Additional charges would include a vehicle at $15.00/day and food and lodging charges at standard hotel prices if staying in a hotel, or ^.SO/raan/day while camping.

Sincerely yours,

BONDAR-CLEGG S COMPANY LTD.

W.F.B/ml

W.F, Bonda

i^' x * BRANCH OFFICES

ISOO PEMBERTON AVE., BOX. 487,

NORTH VANCOUVER, B.C. CAMPBELLTON. N.B.

KONDAR-CLEGG k COMPANY LTD. t. l^-l-flti^^ ***l*^lJiiyis*:**WB(*J4S

76SA lihl,l AST ROAD, (MR1) OTTAWA ONTARIO - 237-3110PHONK: 237-3110 TELEX: 013-3548

GEOCHEMICAL LAB REPORT No : 21?-0

Cu,Zn,Ni - HNO--HC1rrom

Mcintyre Porcupine Mines Ltd.

ii IL j Cu,Zn,Ni - A. A.

P ,. ..j as receivedFraction Used— ......— ....... ......— .... ....................... ....... ... .....

SAMPLE NO.

OGR - 3020

Heavy mineral

concentrate

OGR - 30?0

Cu

9

97

Zn

13

18

Date ... July A.......... 19 ..79...

Analyst. A..T.A..' .........J.'.M.r... ................................

Ni

15

77

REMARKS

——— --•j

gbr~z""..: "

Department, 970.

Tlramlns, Ontario.

May 23, 1972.

Mr. W.F.Bondar,Bondar-Clegg and Company Limited, 760 Belfast Road, M.R.I, Ottawa 8, Ontario.

Re: Corraler Timmins Work

Dear Mr. Bondars-

We have enclosed sample 2 CL 1001 from 71 ft 9 inches in a hole located at 700 East 150 vSouth on our Townsend option near Timmins. This sample was recovered from lower till material by Cormier's deep overburden sampling crew. Would you handle this sample as outlined in recent telephone conversations with Cormler.

We have also attached screenedsamples 111 to 125 some of which are also from the Townsend property. Would you analyse these for total copper, zinc and nickel.

Would you send the results to and invoice us at the address noted above.

Yours very truly.

MCINTYRE PORCUPINE MINES, LIMITED,

AS/sa A.Skreoky

BONDAR-CLEGG Si COMPANY LTD.BELFAST ROAD. OTTAWA. ONTARIO, K1G OZ5 PHONE: S37-311O TELEX: O53-354B

Geochemical Lab ReportExtraction

Pu, 2n, Ni,-HN05-HCl 389-2

,. L J A. A.. r Mcintyre Porcupine Mines Ltd.Method From

c . ,. . - 100 Rocks nt May 29 1Q 72Frprtinn UsfiH Pate " 19

SAMPLE NO.

2CL 1001

2CL 1001 H

Cuppm

18

34

Pbppm

16

13

Znppm

65

23

f .--"

Ni ppm

45

45

REMARKS

-80 Mesh

feavy Mineral Concentrate

BONDAR-CLEGG S COMPANY LTD.BELFAST ROAD. OTTAWA. ONTARIO. K1G OZB PHONE: S37-311O TELEX: O53-354B

Geochemical Lab ReportExtraction.

Method —

Cu, M, 2n-HK03-HOl

A.A,

Fraction Used-100 Rocks

Report No. 329=2

From—NfiTntyre Porcupine M^nfiR Ltd

Date May 29 197?

SAMPLE NO.

111

112

113

114

115

116

117

118

119

120

121

122

123

124

125

Ouppm

32

27

21

21

17

1Q

16

20

25

25

44

6

10

7

v10

Zn ppm

10^

80

57

101

10Q

100

20

83

64

83

136

14

25

10

10

Ni ppm

—43 ——

44

25

36

37

"51

32

31

30

30

41

11

12

11

12

REMARKS

J0-/& /0-Jt#

6O S&& 60

JT0-4S0 ^0*4/0

f 0-4*0 4/0-^0

^-#-60 St -60

BRANCH OFFICES

1500 PEMBERTON AVE., BOX 4B7,

NORTH VANCOUVER, B.C. CAMPBELLTON, N.I

BONDAR-CLEGG & COMPANY LTD.,764 BELFAST ROAD (M .R. 1), OTTAWA 8, ONTARIOPHONE: 237-3110 TELEX:OU-S548

June 13, 1972

Mr. A. Skrecky,Mcintyre Porcupine Mines Ltd.,P.O. Box 970,Timmins, Ontario.

Dear Alex:

The lines referred to on the overburden drilling logs as baseline is actually the north-south line on the mag. anomaly. Line l is the east-west line and line 2 is the one by the road. The station numbers are as they were flagged by your men in the field.

Yours truly,

BONDAR-CLEGG Si COMPANY LTD.

/J Roch Cormier.

RC:ml

.ploratlon Department, t.Q.mp 970, Timmms, Ontario*

June 16, 1972

Bondar - Clegg and Company Limited, 764 Belfast Road (M.R.I), Ottawa 8, Ontario.

Dear Mr. Bondari-

We have enclosed assorted samples which we wish handled as follows.

Samples 126 12? 128 129 130 136 139 140 141 11*5 146 149 150 151 152 153 154 155 156

Heavy mineral separation with an analysis of the concentrate for copper, zinc and nickel.

Samples lil 132 133 134 135 137 138 142 141 144 147 1^8 157 158 159 160 161 162 163 164

These samples consist of minus 35 mesh material to be analyzed for copper, zinc and nickel. Material can be pulverized if you feel this is necessary.

Samples Bl to B25. Handle as is and analyze for copper, zinc and nickel.

Please send your results along with invoice to the address noted above.

Yours very truly,


AS/sa X.Bkrecky

IP

30i i

131, /SI

IM t IH t

l VVi*tr

v?

/rt

ATI tft

Ut

M oue 100 , AM

*\ * l

ft - l

A -tn-i

A -4 ft -.3 ft *4 ft-J

A * J"

A-r

A'-r A-r

rt-r rt -jr

t* r - .fei -

l. 6 3 - i *^

i qr * xoo

- AO

j-o * x 7 j*f ^ 60 60- 6 3

60 --60

* T67-69

67- 7 l T- 15T* -7V

7 T- 79 "? 9 -ffiir-fi67-6?

73 - 7V 7 V

frtJLtH**Wu

a it

i/

itn

11a

1 1

* *

V

V

V

s

V

V

V V

B -i8 - x4-3B-HB-JTfi. ta-TJ-r.J R

fi -leB -lifl-UQ -Idff-IWfl-irj-/ 6n-ne-*/i -19f- 4.0fl-tlfl-i*0-4.3J -1.VC - V

P Ay t c.ft*:e (Sett(rTtfx*.e- Ifli M fi |i

U -

,g,l

.. If 44 - ,.t P

1 * "M " *l II

II i^ II

li " / , II

" * *' ^11av "" /^ "

lVx" ' "

I'/x" " " 3 y"

/2. "" " " /t"

/'/X/'/t" " " tt, "" " " /J. "

6 w" *t t, j^ /*

6 "tt '' /* A

•S t^ /* T ft C ^

z. ac^ O 100 tv)1.5 i ** o eVJ B u|^ f4p0 t^J

S^ r oo et* Sk*6^ **-

y - PL

1

^^ S 1-J 5 foo t*r

b f -S 1*0 ef fe 5 ffi/6 ^ f*o fti. /O J top 6la vS eo^c(2.^ /*o fef *f 5 20o E/V ^ 3 do E/63 y**e/6^ 2** e/{^ UfttC*- J+tOftfr

^ f i^tf* fftoAt/9sT L#**r s#c*a-Z-O^y tAlf+'S'&o&t*

BDNDAR-CLEGG S. COMPANY LTD.BELFAST ROAD. OTTAWA. ONTARIO. K1B OZ5 PHONE: S37-311O TELEX: O53-354B

Geochemical Lab ReportExtraction Pu, J2n, li

Method _____A*A,—^——-.

496-2Report No.--—Mr. A. Skrecky

From Mcintyre Porcupine Mines. Limited.

Fraction Used -100 Bocks H.M.S. June 23 .19.7!

SAMPLE NO.

126 H

127 H

128 H

129 H

130 H

136 E

139 H

140 H

141 H

145 H

146 H

149 H

150 H

151 H

152 H

153 H

154 H

155 H

156 H

Du ppm

73

54

- 6?

48

54

30

... 6J^

1^5

139

300

120

63

46

51

50

24

51

81

28

•Zti ppm

270

95

92

50

50

280

95

300

60

100

136

68

40

41

54

75

118

32

148

Ni ppm

72

74

82

155

150

156

104

228

64

100

64

76

94

6^

89

145

11*5

42

24

REMARKS

HRAVY MTNfiRTAT,

CONCENTRATES

Extraction

BDNDAR-CLEGG S. COMPANY LTD.BELFAST ROAD. OTTAWA. ONTARIO. K1B OZ5 PHONE: S37-311O TELEX: O53-354B

Geochemical Lab Report496-2i, Ni Report No.

Method ____ A. A.

. _________________________ Mr. A. Skrecky

Mcintyre Porcupine Mines. Limited.

Fraction Used -100 Socks H.M.S. June 23 J9JZ2.

SAMPLE NO.

151

132

133

134

135

137

138

142

143

144

147

148

157

158

159

160

161

162

163

164

B- 1

2

3

4

5

6

7

8

9

10

11

Ou ppm

13

11

26

88

73

10

83

24

54

73

16

62

7

3

4

4

6

28

52

34

8

7

10

10

5

8

4

4

7

4

5

'Znppm

21

21

40

88

ioo

15

135

38

120

175

16

90

13

4

3

8

12

78

125

88

19

23

35

25

12

28

13

13

22

6

13

Ni ppm

8

8

8

140

86

7

83

23

92

42

13 .

48

6

4

5

4

6

11

14

14

13

12

16

19

6

12

8

10

12

6

13

REMARKS

Samples B1-B25 Analysed

as Ree' d, per instruction

-some were very coarse.

s.

BONOAR-CLEGG S. COMPANY LTD.

Report No.- 496-2Geochemical Lab Report

Page No. -

SAMPLE NO.

B- 12

13

14

15

16

17

18

iq20

21

22

23

24

25

Cuppm

8

20

8

8

8

8

6

fi

6

24

7

5

^

5

3n ppm

20

14

14

16

Ifi

16

12

17

17

13

12

9

5

7

M ppm

14

12

10

16

1^

14

14

10

710

12

10

fi

6

REMARKS

BONDAR-CLEGG S COMPANY LTD.BELFAST ROAD, OTTAWA, ONTARIO, K1B OZ5 PHONE: 237-311O TELEX: O53-354B


Method

496-2Report No.__ _ __Mr. A. Skrooky

Fmm Mcintyre Porcupine Mines, Limited*

Fraction Used "10Q Rooks Date. June 23 .19 72

SAMPLE NO.

126 E

127 H

126 E

129 H

150 B

176 E

139 E

140 B

141 B

145 H

146 B

149 B

150 B

151 B

152 B

153 B

154 B

155 B

156 B

^.ttffrfWeS,

J 9 **ve^*vs.S?

3?

3J j&sv/ytg y/7 s/,*?. s*/*

e *0J,

r *z*s*.ev,v

ve

**?*?*&/0USS

Ouppm

73

54

67

48

54

30

64

175

139

300

120

63

46

51

50

24

51

81

28

rf/"fcf^^*ZL

*/jf

Zn ppm

270

95

92

50

50

280

95

300

60

100

136

68

40

41

54

75118

32

148

*9

s?/fi

J3?r.

^#6.

Hi ppm

72

74

82

155

150

156

104226

64

100

64

76

94

63

89145

11542

24

06

r*"o'S90

'f

**t* ft*

*, s*'//y./*0.S

#.t

&Z#.3#3i#.3

^.^

*.y0.S"

*~r*sf*#f#.r/?.fa r#.jr

REMARKS f&ifri&si

*f?'*S?

**?~*e*/

tss-^sj

Z6f~JVf

*4S- *'7

/?f~'200

st-s-?*7'6e4 e -43

J-*F-*o

#0-63

Sf-*/

*7~6?

*?~7/

P/- 7J

?S~7y

?*-7S'

?r-7?9 f-?/BEAVr MIiraRIAL

OCarOKHTRATES

BDNDAR-CLEGG S COMPANY LTD.BELFAST ROAD. OTTAWA. ONTARIO. K1B OZ5 PHONE: S37-311O TELEX: O53-354B


Method

Report No 496-2_________________Mr* A* ftortdgr Mcintyre Porcupine Him. Liaittd*

Fraction Used -100 RockB I,KtS t Date. Jun* 23 .1972,

SAMPLE NO.

151

152

133

134

135

137

138

142

143

144

147

148

157

158

159

160

161

162

163

164

B- 1

2

3

4

5

6

78

9

10

11

Oupprn

13

11

26

08

75

10

83

24

54

73

36

62

7

3

4

4

628

?2

M

6

7

10

30

5

8

4

4

7

4

5

Zn ppffl

21

21

40

88

100

15

13538

120

X75

16

90

134

3

8

12

7*5

12568

19

23

35

25

12

28

13

13

22

6

13

HiPDR

8

e8

140

66

7

6323

92

42

1348

6

4

5

46

li

1414

13

12

16

19

6

12

6

10

12

6

13

'i

-

-

-

--

-

-

x****? A*".

S-/

*'/

S?./

#-'

4.,

#.Z

*2

S-f

0.3

**'3

#.y*y#-r**r*r*'f*e.r/#r*r*.f

REMARKS /KtoTVA*-

*s-?**j~?*S7-**S

j * /- #6 y^fj'jsjr3*f-Jt7

/r0~sS0/?S**"

S*-*7Jr?-Se

*e~*i3

J-J-60

Se- J4

4S'-4?

*7'*?

6?-7/

?''?J

7S-?y

r**-?r?j~-?f*9-?/

Sa^ltf 11*125 Aaftlyttda* K*o* dt ptr instruction

**OM wtr* rtiy ooars*.

i*

BONDAR-CLEGG a COMPANY LTD.

Report No.- 496-2 Geochemical Lab ReportPage No.-

SAMPLE NO.

B- 12

W

1415

16

17

18

19

20

21

2223

24

K

Cu — ppo-

e20

8

8

8

8

6

6

6

24

7

5

3

5

Zn PPM20

14

14

16

1C

16

12

17

17

13

12

9

l7

VipnM

14

12

10

Ifi151414

10

710

It10

6

(

/

•'

REMARKS

Department, 976,

Timmins, Ontario.

June 23, 1972,

Bonder - Clegg and Company Limited, 76** Belfast Road (H.R.I), Ottawa 8, Ontario.

Dear Mr. Bondars-

We have expressed two parcels to you today containing samples we would like handled as follows.

Samples 165 to 2*f7 inclusive and 354 to 376 inclusive

Heavy mineral separation with an analysis of the concentrate for copper, zinc, lead and nickel*

Samples 2^8 to 353 inclusive

These samples consist of minus 35 mesh material to be analyzed for copper, zinc, lead and nickel. Material can be pulverized if you feel this is necessary.

Please send your results along with invoice to the address noted above.

Yours very truly,


AS/sa A.Skreoky

M OJJL 100,

1 fc3~f ttf fc7Ifeff' feql TO' 7 /(74.

1 TSI1H1 T*~

1 7 V

J TT

'7*(So181i ^7.

C.-/ 6^(L- f 70C - f 7tf"

c ~/ f dc. - i S* 3*--i 5*4C -o. *? t ~C. - a 7 / ec -X Ii3~t-a. ii9c- -a * i 3 -t -J ^~oc - J J-rf- -

C. ~3 li -1C -V Jro ~.

C.-V 5~0. -^^ -V ^6 "A

J"- TO

- # S*

-STY

193- *- -5If b C --ST 4 o - 6 2/* 7 C. - 4s V7 -\T A/ f f e - fe xTO. ~^V

C-feCL-fe 5-4 *

C.-'y V 6 '

- f V

2.a Z, C - 2-0 3 c - ^

c- /oc ~/ o /c*e -^ C-/0

4.07 c.~fo2.0f *i-^0 *'tf"' '/T

Q. -/, -j? 9 - y*rC - M J^ ~ ^ 6

l/11

'l

M

li

li4 - CxP

li ,^.TO7o -'"

*an

2.1 U

2. j d

up * j?

2.VJ

CM i

C -H

C-i-i.

c ~tx c-i^ c -it .0- i

o -i O -i .6-1

.0-2.

ft'x

0-30-3

J-vJ

D-3 D -So -f 0-4

ft D -li

*? -l

*-~ -7.

e- -i

6 t -,T* - 60 -63

- 6?-70

70-77.

- Vfc

a -

6 •f'-

i t, e -i- /a. r

•i^11 it 11 t,H

l'

K

-70

Z.-TV

ifeo

2.6V

tfe?

i'72. 2.7J

2*2. if J

iff

j. r?

C- ~(c -i

c-i.C-7.

t-3C-3t-3 C-3

C-H ^ **STc-ar

c-^r t-fcC-4c-c,

t -*r t-7

C -7 c -J

c -?c-S c-8

c-q

c-qfc -*?t~(0

c-i oC - l O

C -lo

C- - J (c - 11o - il

e s -st*

-//fH9-

6 J -4V

/CO ~.

/OxT "//e//o -,

II

h

li

II

M

l'

l'

II

•Joo Jo,

t-ll

t -li

C-l j.

c ~TIC -12.

fl-l

So?

J/oJtf

3/4

3 Z. f Ji? •J Jo,

O -a.

s -T.o-z

o ~i. 0-30-3

0-3

o-s o -^ o-^o-j-

G- -l e--iB-l

f--i

tr-z.IS-t a-i

US-/

t l -7V

l-Vy

-C o

9 7 -

~/ vy

(l

K

ir

a. -i(3-3 G-3 15-s

6-V Q. y

X9-S--ZOO2.00-

V 6 ~

X J- 6 -

a**.

36? C- 3 Q-3 XJ-Vc~ v e-v

2. od-

o -

if*

rt

(t

If

H

(l

li

BONDAR-CLEGB S COMPANY LTD.BELFAST ROAD, OTTAWA. ONTARIO. K1G OZ5 PHONE: S37-311O TELEX: O53-354B

Geochemical Lab ReportExtraction Gu, Pb, !Zn, M-HNO -HCl

Method A. A.

Report No.— ___ Mr. A* Skrecky

From Mcintyre Porcupine Mines Ltd.

Fraction Used -100 Socks H.M.S. June 30 .197.2.

SAMPLE NO.

165 H.M.

166

167

168

169

170

171

172

173

174

175

176

177

178

179

180

181

182

18?

184

185

186

187

188

189

1QO

191

T Q?

TQ3

194

195

Ou ppm

I.S.

56

117

900

I.S.

.541-

80

94

177

I.S.

I.S.

57

45

62

63

I.S.

L.S.

I.S.

70

60

I.S.

I.S.

670

148

118

352

110

I.S.

618

53

32

Pb ppm

10

17

29

18

18

16

120

20

15

40

24

10

51

30

49

30

48

10

200

10

48

Zn ppm

48

98

53

198

63

82

125

56

50

69

128

48

34

492

120

163

245

85

463

56

48

M ppm

\50

142

2,5800

———— -*

.2900

122

85

190

70

60

78

200

86

67

394

452

530

304

70

.2500

52

53

A

-A —

fV-±\-f-tiry-t-:t\ .

i

t*

^

^~

-hC/*

r 1,6\*r

i pi —-t^

•'

REMARKS

I. S. InsufficientSample

Heavy Mineral Concentration

' 'BONDA

9Report No. —— 532=2 ———

SAMPLE NO.

IQfi TT T M,

197

198

1QQ

pnn

201

202

203

204

205

?0fi

207

20R

209

210

211

212

913

214

215216

217

218

21 Q

221

992

223

?94

225

99fi

227

99R

229

930

231

I.S.

T.S.

I.S.

I.S.

I.S.

I.S.

I.S.

I.S.

I.S.

T "?

T.S.I.S.

I.S,

I.S.

R-CLEGG S COMPAKt

Geochemical Lab ReportPage

Cuppm

647

538

104

152

63

97

680

264

113

72

83

52

73

116

68

73

30

65

65

92

58

160

Pb ppm

27

53

10

10

45

20

850

10

17

6

95

175

98

10

1112

R

30

10

10

8

10

Zn vm

154

245

56

51

42

50

440

97

80

42

636

472

1000

72

48

62

4R

72

80

82

44

125

Ni ppm

.7500

.6120

82

61

79

466

3940

98

98

67

40

27

21

90

48

48

43

70.55.-

66'-

53 '

184

l C

J"\

];V-i-*

A

-JL

\

j

y(J\

1(r)\ifyj

g

6/1

0o 1

16 1

c-o

li

pi

f)^

^

IV LTD.

o

REMARKS

BDNDAR-CLEGG S. COMPANY LTD.BELFAST ROAD, OTTAWA. ONTARIO. K1G OZ5 PHONE: 237-311O TELEX: O53-354B


Method

532-2

A.A.

R . unMr. A. Skrecky,

FrnJIcIntyre Porcupine Mines Ltd.,

Fraction Used . -80 soils. June 30. .19??.

SAMPLE NO.

?4ft

249

250

251

252

253

254

255

256

257

258

259

260

261

262

263

264

265

266

267

268

269

270

271

272

273274

275

276

277

278

CuDDltl

64

14

17

6

22

32

28

16

16

16

6

3

50

52

19

22

12

2

4

20

13

27

18

33

284

15

14

7

3

Pb ppm

74

6

6

9

13

6

12

16

9

15

6

5

8

10

10

19

23

7

7

19

13

7

8

11

107

22

15

6

8

In ppm

1112

16

19

16

28

35

39

44

75

75

11

8

64

50

20

36

23

7

12

60

54

29

20

28

288

50

43

8

12

NT ppm

14 ^11

15

170

24

26y43 N

42

20

3

5^/,I N10

83

81 V

15 \

16

15 1if

9 N

10

10

12.X

16 A23

33

si y10

14

10

10 N

12

\^TzrfF-

*\T*i-pr

\ ^rL^.

\H

!/

\ Cu*

**

REMARKS

., 'BONDAR-CLEGG Si COMPANY LTD,


SAMPLE NO.

279

280

281

282

?R3

284

285

286 --287

288

289

2Qn291

292

2Q3294

295

296297

298

299

300301

302303

304

305

306307

308

309

310311

312

313314

uu ppm

2120

12

6

6

31

27

16

45

43

16

?3

16

8

22

12

16

54

9

33

12

12

14

13

6

23

12

10

8

11

13

22

10

22

57

6

KDppm

1410

10

9

711

12

4012

10

12

fi

8

5

2155

14

87

8

10

1012

116

8

7

45

6

12

108

6

136

^n ppm

16495

18

11

1280

70

4850

52

65

fin60

11

211244

233

4515

124

200

211211

22215

36

27

1220

20

28

2428

28

7512

m ppm

85 \30 J

""S

20

10

n .15 .

24 .

16 X33 V

50 A

4

?R -. ;

20 y10 \

A410 J46 /)13- \

10

11nn . 1n X14V

25 \*LL\15: \

46. j

T/24 -\29

13

19 ,

16 X10

cS

F1 -*- U7r1-

S )0L* 1

-ei!

C. ri

\-^l

3 f

t±3

7^,

REMARKS

. BONDAR-CLEGG S, COMPANY LTD.

Report No.-532-2 Geochemical Lab Report

Page No.-

SAMPLE NO.

315

316

317

318

319

320

321

322

323324

325

32fi

327

328329

330

331

332

333

334

335

336337

338

339

3dn341

342

343

344

345

346347

348

349350

uu ppm

53

3618

21

6

16

69

8 .

l?ft

28

4

83

67

6417

76

73

12

1916

.1440

580280

520

22

inn6

20

28

12

11

7673

14

1216

rb ppm

6

98

8

6

9

12

8

148

6

106

12

118

9

8

29

1432

76

5346

42

7

11

8

12

16

12

12

1112

8

97

Znppm

45

5024

36

1632

148

20

3fin172

12

390

123

5524

95

59

27

43300

.3900

277244

255

12

156

18

147200

26

24

14880

20

2316

INIppm

26

3951

32

13 \ 13 —— i50 j

27 X

Mi)c l

^7^\15 1—44 J

- s 96 '25, .

183

137 ^

20 \

25 :19 --

187 -

199171 .

183 .

19

24

15

1212 y25 N

25

54*y25 \ Z5\

26 ]

tri *\j*2-1fs '

b6

K\

s-V-\t^-\

J}^-pV6 '

^18 J

t

REMARKS

, BONDAR-CLEGG SL COMPANY LTD.

Report No. 532r2Geochemical Lab Report

Page No.-

•zrr-ppmSAMPLE NO.

u ppm ppm

m ppm REMARKS

351 8 8 12 15352

353 26 12

15

131

'BONDAR-CLEGG S COMPANY LTD.

Report No.- 532-2Geochemical Lab Report

Page No.-

SAMPLE NO.

232 H.M.

211

234

235

236

237

238

24.0

241

242 A H. M.

?4? B

243

244

245

246

247

354

355

35fi

357

358

359

360 *

361

36?

363

364

365

366

367

368

369

370

371

37?

373

I.S.

T.S.

I.S.

I.S.

I.S.

I.S.

I.S.

Cuppm

1400

820

1350

66

93

1175

66

233

709

1300

536

124

97

98

4750

705

492

565

103

99

89

109

67

—— 70—

79

117

89

R9

161

Pb ppm/

19

88

35

12

24

124

11

27

28

21

24

105

19

105

800

135

100

101

19

11

11

20

12

1213

1?

13

n10

Znppm

1000

1750

269

75

115

3150

81

144 .

810

666

343

105

135

1400

\3750

2375

550

1600

58

138

98

165

71

—— 72—

115

10?

102

123

176

Ni ppm

510

900

L8400

172

90

75

65

180 .

335

376

166 .

105-C\9

.0162

364

566250

335 '

800

100

97

72

51

R2

172 '

158 '

98

90

86

4JLj{\ .yJi—-t-#*Ji tfit3—1C 'J-y

T P\

J

*\4u y

U-

x6^i-2 —

,'l^

r,*

f X

-fr

it-

3

^

REMARKS

* indicates urganic Samples

: v 'BONDAR-CLEGG S COMPANY LTD.

Report No.Geochemical Lab Report

Page No.-

SAMPLE NO.

374 H. M.•57S

376

Cuppm

67

69

330

^

Fbppm

12

36

26

2nppm

83

250

430

Ni ppm

70

55

22

-4J^ x y/07, C

REMARKS

,i ,6f j

BDNDAR-CLEGG Si COMPANY LTD.7fl^BELFAST ROAD, OTTAWA, ONTARIO. K1B OZ5 PHONE: S37-311O TELEX: O53-354B

Geochemical Lab ReportExtraction ^ **, ** N

Method

Report N" ? ~ *—————————^———Mr. A. SKreoxyFmm Mcintyre Porcupine Hin*a Ltd*

Fraction Used -100 Rooks H.M.S. June 30 .1972.

SAMPLE NO.

165 E. M.

166

167

168

169

170

171

172

173

174

175

176

177178

179

180

181

182

183

184

185

186

187

188

189

190

191

192193

194

195

Cuppm

I. S.

56

117

900

1.8.

347

80

94

177

I.S.

I.S.

57

45

62

63

I.S.

L.S.

1.8.

70

60

1.8.

1.8.

670148

118

352

110

I.S.

618

55

32

Pb ppm

10

17

29

18

18

16

120

20

15

40

24

10

51

30

4930

48

10

20010

48

Zn ppm

48

98

53

198

63

82

125

56

50

69

128

48

34

492

120

163

245

85

46356

48

Mi PPI

50

142

*5800

2900

122

85

190

70

60

78

200

86

67

394452

530

304

70

250052

53

c-i

^j ——C.*(

t,*-10

10*75"

If 'fO

C.- 1

C* 1

C- 1

c-1

t-1C-l

c.-*

C- 2.

C-l

C-3

C-3

C-3

c-v

c-v

c-v

C'f

c-rt-rc-rc- 1c-4

l- 6

C*4

C -7

C-7

C- 7

C-*

C -P

REMARKS

I.S. InsufficientSample

Heavy Mineral Concentration

fra - f*

P3 -tft

^6 - 9 f

96-?rU* '/iS

113 -tlf

1 1* * 1 10

1X3 -tlf-

re - s-rS-s- - io

^ 6*.-,^

f/- 7J

f 6 -^-i

fi - i-V

i- 6 -,T7

y? -rvf V -5-4

*T6 - f f

to . 63

V7.i*2

5-2-J-V

4"y-i-6

J" 4- J-^

^^ -^U

J-o-j-y

sS-i -.ft^

iTf -^

^^ -^ V

BONDAR-CLEGG S. COMPANY LTD.

Report No.——532-2Geochemical Lab Report

Page No. —— 2-

SAMPLE NO.

IQfi H. M.

197

198

1QQ

200

201

202

203204

205

206207

208209

210

211212

213 ' (:- t- ) . '

214

21?216

21?216

219

220221

222223

22422?

226227

228229

230231

I.S.

i.a.1.8.

I. S.

l.S.

I.S.

1.8.

I.S.

l.S.

l.S.

1.8.

I.S.

I.S.

I.S.

Cuppn

647

B38

104

152

67

97

680264

113

72

83

R2

7313.6

68

— 73—

3065

65

92

58160

Pbppm27

53

10

10

4520

850ID10

17

6

95

17598

10

1112

530

10

10

810

Zn -MB —

154

245

56

51

—— 42-?0

4401Z-97

80

42

636

472

1000

72

48

62

4ft72

80

82

44125

Ni PPa7500

612082

61

79466

3940**o 98

98

67

40

—— 27-21

—— 90-

4848

4370

55

66

55184

(L-S

C-*

c- *c- ?c- f0 9

c-9

t- 1C- 'O C -/t)

c-/*c -to

C- It

C-/0

c-//

t. x/

c. -lit-ll

C -)l

t-ll

C. - IX

(.•11.

C-ll

^•11c . l 1.

ft-/

O-l

O "1

A - 7

O ~/

o-/

O .2

0-2,

O - X

0-1

0-1

0-J

REMARKS

x^-^s-^#'^0

TO - rr^r- *o#o-l*V

*V-*4

^i *ff*

^*-9l^c) -^S ^^ - /oe

X o o - /o i-

/o J- - //o

//e - f /4'

/r .r - t f 7

39 -v.f- 1

,r 2 - J^6 1J-6 -^-P '

r* -60"™"" l! lj\ *I^

^o - 1& J *

Hi. s*J-a-vj-4 ,

F* 'f fJ-^-4O X

to *6J

6s -4s- t*1 ft-it

6 i . LLii-tf^-P-^c

7a - 7^

>a. -7V•J F- va

Vd-V2

Vl-Vy

Vy-v*S ^ * y^*j-J"^ NT ?


Report No.——552-2Geochemical Lab Report

Page No. ——5-

SAMPLE NO.

252 5T M,

—— 255 —— — — ——2^40ic;

^6

—— 257 ———————95^2.31 -" — "--~ 240941

242 A E. H.

OJO b——— g^g J ———————

243r^4424^216

247

^^'54

?55

356?57

558WQ

?60 *

5^1

—— 562 ——————56556456B

566

?fi7KCfi

569

570571

572575

1.8.

1 C

ItSt

I.S.

I o-rO* —

I.S.

I.S.

Cu -J&® —

1400

8201350

66

Q?

1175

66

235709

1^00

^6

124

—— 7-98

4750705AQ2

565105-

9989

109

67

—— 70-79

—017-69RQ——— Di* —

161

Pb -ppm ——

J9oa —— S9 —

35

1?

•J- I^nta.

— 24—124

11

2728

21

24

105

— 19—105

800l^S100

301

1211

1120

12

19

13

12

15

11

10

Zn -4*pa —

JOOO1"7RA*7yO —

269

TK ——— 4P —

•' Mil

11?

5150

SI

144810

66*

745105

1551400

15750257P

500

3600RA—— po —

156

9816?

71

—— 72-115

102102

125176

Hi PP"510

900L8400

172

9075

65

190

?'5

?76166

105- — —

112162

564^66

250

555

800100

9772

?lCO—— 9* —

172

15898

9086

0-5

ft-3

A'3

0-3

o-**D- M

C-fb-fc**r ô-s-p -f

klc**l

tf-le-*e -2.ff-z

fr'i*'l4 -i

is - 113 - 1

13 -i

Q-l

W * 1

IS -1

ft -*Q -\

B-1

A- S.

/? ' *

K -.3

# - i

C-J

* *-5c -va -v

K -V

REMARKS

i-?' 60

t to - ^2

4* -4**

4v.^s-.J-

3f - 24. J-

36- r-^.ri^-s- - V/.sT

fel- 6?4T . tt

fro - 7^'

————— yr'/oo . ———

/op - /OJT^1 1.0 * i 7.^*

Its- - i x*1 1.1 - 1 IS114 - Ut

Itolff -/O? .4" ——

1 NX* IWt^

'MS * wtIS t - iro

J Jro - if x

\f\ -i^w* IBaioaids organio

fi*n|pl*B l f w - 1 f L

i ft ' Iff

1 A-6 - /J-J-

/^•s-xô

/66 ^*r'*5-- *7T)

/TO - 1 tf

1?.?* i 3o

/ae - /•ar'3j"-;-f*

———— LSJ* w^r/ yTf - 2Bfe

ree ~ êJ-

ioj-- i/o

^

1

,' BONDAR-CLEGG S COMPANY LTD.

t.532-2 Geochemical Lab Report 4

Report No.————————— Page No.———

fl.i DV ffin VI

SAMPLE NO.

374 H.M.

375376

ppm67

69330

ppm12

3626

ppm83

2^0430

ppm70

5522

i? ^R - V

fl-V

REMARKS

7. 1C * 2./JT

ilf - 1/JP

T 1 4? - i l r

BDNDAR-CLEGG S COMPANY LTD.ELFAST ROAD. OTTAWA. ONTARIO. K1B OZ5 PHONE: 237-311O TELEX: O53-3548


Method

Cu. Pb. Zn. Hi - HN03-HC1 Report No. 532-2irt NnMr. A. Skrecky,

F mcintyre Porcupine Mines Ltd..

Fraction Used -SO SOUS. June 30. .1972.

SAMPLE NO.

248

249

250

251

252

253

254

255

256

257

258

259

260

261

262

263

264

265

266

267

268

269

270

271

272

273274

275

276

277

278

Cupprc

64

14

17

6

22

32

28

16

16

16

6

3

50

52

19

22

12

2

4

20

13

27

18

33

284

15

14

7

3

Pbppm

74

6

6

9

13

6

12

16

9

15

6

5

8

10

10

19

23

7

7

19

13

7

8

11

107

22

15

6

8

ZnDDK)

1112

16

19

16

28

35

39

44

75

75

11

8

64

50

20

36

23

7

12

60

54

29

20

28

288

50

43

8

12

N1 DDffl

1411

IB

170

24

26

43

42

20

3

5

11

10

83

81

15

16

15

9

10

10

12

16

23

33

3110

14

10

10

12

C.I

C.-I

C.-I

c.- i

CM

ft -J

C-2

C.-*.

C-3

C-i

t -1C.-&

t-s

t -J

c-ac- fc,-v

c-w

t-r

c. -r

C.-JT

C-5-

1-4

c- tL- L

C-6

C-1

t -7

C-7

(-•f

t-e

REMARKS

65-70

ire -W

73-- PO

50 -6 3

JP a- *fe

ft -reW**t

Mo -113

1 1 3 - //p

Mff- l*o

us - 1* r•ro-.jar

JT^" - it^J

tJP-'yo

7r - isJ-6-S2.

fZ-S-'i

j-i -f r

*f* -*V

JTW-S-4

^•4-irJ?

46 - 6^

f 7 -W

*r^-f^5-V-J6

^•wV4-J8

Jft-.rv

**-,r^

f*-t*

63-6 v


Report No.- 532-2 Geochemical Lab ReportPage No.- 2

SAMPLE NO.

279

280

281

282

283284

285

286287

283

289

—— 290 ——————291

292

?Q*294

295

296297

298

299

300301

302303

304

305

306307

308

309

310311

312

313314

Cuppm

21

20

12

6

p31

27

16*.*/ 45

43

le2316

8

2?12

16

549

33

12

1214

136

23

12

108

11

13

2210

22

576

Pb ppm

H10

10

9

711

12

-f——G

12

10

12

88

5

2155

14

87

8

10

1012

116

8

7

45

6

12

108

6

136

Znppm

164

95

18

11

1280

70

48A~C)

m52

65

6060

11

211244

233

4515

124

200

211211

22215

36

27

1220

20

28

24

N1ppm

ftR

30

20

10

1115

24

1544*33

50

4

2520

10

1211

10

46 Oiif~

10

nn111114

25

15

*n

y

J

?4

'9

28 b

28 p

75 9612 |lO

vi (T

i-j?

^ *ffc.-qc.-*C -9

C-9

C-9

C-9C- lOc -/aC-/0

C-J6

C*fO

0/0

t-//C.'/'

c-//

Cr-ll

C.-/0

C -li.

C-/1

C-11.

i -li.

c - it

t -li

0- i

0 -J

t* -'

0-f

6 -X

0 -1

O -^

/)-2.

0-Z

o-gi

B-2

0 -3

REMARKS

^4,-4J?

d^'-ro

7e - *7f

7s--.?o

*o -#V

^V.#6

*^-#ff

ftp *9/90 -e?,S^^•-/oe

/ao -/64'

l e A- -I/a

/f o * U&"

its- * //y

39 -V.J'

,ara.*f 4

J"^-r*

^JP" ft O

90 ^ 9^-

Wi -ri.

vT2 - i- 4

*4 -^JP

lv i e

60 -t.T

6 a - 6f

4-t- i/

^/-^A

^ -tJ5

^*- 9-0

76 " t^

?a. - 7*v

39 -ve

Vo-va.

*14-SS

*yy-^6

V 6 - V/'-j-J-^-vT?



SAMPLE NO.

315

SIP317

318

319320

321

322

32?324

325

326

327

328329

330

331

332

333334

335

336337

338

339

340341

342343

344

345

346347

348

349350

cu ppm

53

as18

21

fi16

69

8

12828

4

fi3

67

6417

7G

73

12

1916

1440

580280

520

22

1006

2028

12

11

7673

14

1216

Ft)ppm

6

08

8

fi9

12

8

148

6

106

12

118

9

8

29

1432

76

5346

42

7

118

1216

12

12

1112

8

97

in ppm

45

en24

36

1632

148

20

360172

12

390123

BS24

95

59

27

43300

3900

277244

255

12

IBS18

147200

26

24

14880

20

2316

m ppm

26

39

51

3?

1350

27

24

?627

9

IB

44

9626

183

137

20

2519

187

199171

183

19

2415

1212

25

25

5495

25

2618

p. x

D-S

0-X

D - S

o -wn-W

P -*Y

D -i"

O-ll

o-V

f -t

e- i

f'l

1-2

ff " 2-

f -t

cr-i

C-l

8* i

fl - 1

Q - 1

B - 1

fi ' 1

a 'i

c-?,

13-2

o- *

fi -2

fi -2.

13-3

B -J

G -2

R ' 9

a "V

fi-V

0- V

REMARKS

5-9 . Lo

4o -62.

t?. - 4H

fcH - 4i-. l-

24" - 3fc.,T

JA'J-J^-J

J*'^- V/.J"

fc2 - 67

4 ^ - 70

i 7 b - fs

*1 - JOB

/eo - /os-

1 to 7'tr- Ion-

11 o * / i f

'^J" - ; tt

UT ' /l 9

1 19 -is)/**2 -/W

/WV, /V4

/M4-li-o

/50 '/S2

/tf"2 -* /J"V

/•TV" /fi

/A-4-/^-^

/tfto - /J-r-

X *T4~ -StO

1 &C - 1 fei-

/tJ--/?**

/7e - /7^"

/a 5* "/^o

f.* a - /^^-

/ .? .r - 1 J#

i s 4? .,1;j^* * **

/ t -S" * * ao

200 - 'ifti-

JZ6J- - 2./0


Geochemical Lab Report

SAMPLE NO.

31)1352

353

CI!ppn

87

26

PD

88

12

zn ppm

1215

131

ppm

1514

15

*** 541

fc-H

ft -M

REMARKS

•a. j o * 1. 1 f

a,^ .^,P

ai* . ^.i..r

tIon Departwent, 970*

s, Ontario,

Bondar Clegg ft Company Unit td. 76^ Belfast Soad, Ottawa, Ontario*KiG 025* ' ••••:. ' f ^;:/, •''•••'.

1 ' * HT V, t .,.''^'?Y '^ '. ,,' '; '" '.-'4^W^'-

Dear Sirs i-

.soil samples. These are numbered 377 to Inclusive. . "'.. ./.-:v. • 1 -" s -.;. 1 '•^'..V,;^ •• " " ' ; "

•; "' .' Would you wake . concentrate from each sample and run eadh fo)r total copper^.sine and nickel. . ;;\\'. " '''

Please send your related InvoloeB to the

l *ASve*r

AS/sa

*:. L ' ..y 'i:."'**7 ,.- r ; ~, '"^i.^' 1 "'';'; 'V '''/I'"-' 1 . ""Vl'&v "' ;'

34" l 3 f

3*7 s?t

3 ^ H

3T ^3*1 T

3' H

Hoi

4 or*Wo4

F -l

P -f

P -'

F-/* -f

* P -iF- '

. p. -.

-z

t* -

1^- - i. F -3

P -3(^ -J

3T -MiVt - 47

M Til fX -T7 J-T - t t

6 Y-7/

ff l -II - ^^?4 - /o/

/O f - /6 (a til - U3li 3 - M r.

.J-

^ to -J 13, l t.3.r - i

r *

lil- 1M J- - M 7/l 1 ^19 /^ 9 - i t*/ izs -i 14 ; tt - r

BDNDAR-CLEGG SL COMPANY LTD.7B4"E1ELFAST ROAD. OTTAWA. ONTARIO, K1G OZ5 PHONE: 237-311O TELEX: O53-3548


Method

Report No. 622-2Molntyr* Porcupine Mines Ltd.

From Ki*t A.

Fraction Used - 100 Date —— July 17,

SAMPLE NO.

377

78

————— 79 ———

80

81

A2

83O4—————— 64 ——————

____ 85 -

86

————— 87^

88

no——————————— 99 —— ——— —— ——

90

9192

93————— 94 —————

———— 95 ———

96

97

98

99

400

01

02

03

04

05

06

Cupprc

66

60

^64

44

44-

34— 44—

13?*SJ

129

— 70—

—63

— 95to —— ©e —

-470....

297

690

57

60

-BS

84

171

170

171

60

94

, 16 L ...

64

186

80

84

2n— pjan—

60

58

ieo66 .

70

..-60—

55or

-109^

AT—— O-f ——

45 —

55—55—

J03

85

570

89

—80

ac —— S^ ——

58

34

34

32

50

50

. -52

40

55

62

95

Ni PPffl i

6?

66

— 54

51

53

-45

KT—— W —

Afi

—^6

GA—— B4 —

— 70-

— 97—

GC— Se —

283

250

1050

— 90—

76

-100

57

95

82

69

79

60

83

74

62

56

68

REMARKS

Heavy MineralConcentrates

'

BONDAR-CLEGG S. COMPANY LTD.76-^BELFAST ROAD. OTTAWA, ONTARIO. K1G OZ5 PHONE: 237-311O TELEX: O53-354B

Geochemical Lab ReportExtraction—

Method A 'A *

Report Nn 622-2Mcintyre Porcupine Mines Ltd.

From Mr. A. Skrecky_______________

Fraction Used - 100 rocks HMS Date July 171 19 72

SAMPLE NO.

377

78

79

80

81

82

83

84

85

86

87

88

R9

90

91

92

93

94

QR

96

97

98

99

400

01

02

03

04

05

06

Cuppm

66

60

... 64^

44

.-..44...

.34^..-

..- 44

133

129

_ 75

63

93

fiR

470

297

690

57

60

85

84

171

170

171

80

94

76

64

188

80

84

2n ppm

60

58

180

66

...TO

60

55

^85 ...

109

87

45

55

103

85

570

89

80

-85 -

58

34

34

32

50

50

52

40

55

62

95

Ni ppm

63

66

54

51

53

A5

.51

.BS -

96

84

70

97

Rfi

285

250

1050

90

76

inn

57

95

82

69

79

60

83

74

62

56

f?8

REMARKS

Heavy MineralConcentrates

Department,970,.; . - ' Ontario.

m"?'f, . V*. '- .' , . i ; ' - .V.''i': -.', 'vR' . - - . ..,Sondar Clegg A Company Halted,

764 Belfaetj; .Boiul,' : "-'- : . ,' ..Ottawa, Ontario,' - 'v":-.?:,v . .-...•

OZ5. . - ' !

, . f 4972.

.80il"8anplee,V These are numbered-

concentrate from each sample and copper, fclno and nickel.

, ' "" v"''- "'' ' V'' •"'* l ' ' ' V' "'' 'r "' '* i ' i,.^,\i'.-;if j^" 'j . , ^-',:.n'"'',; 'i: !iv^'.' ' ,- -.;' :*

Please eend yo^r repoirt along related Invoices to the addrete noted above.

•:ry. ; -

AS/na- ,'

.:.T. : ' -' ; J^::''Ji^''?;":; :,;vS

^^^|l.^vV

'

"'^'"v ':H :-''. '-.v'' J '.

408

4.14

G-,55

6-. 5

- K"7

- l SG

no - \TS ns~176 -

li i 6 G^17 SS i O y-** OVr? GS 30 0Vj; SM 34 C?

yjj s.vjy s.vjr e-VJ^ G-V 5 7 G .V *i C

•JCT "5 '

y T? G-, V^d G-i VV/ C-

VV^ G' 1 ^VJ G-

WV CW*T C- VV6 S-v^ 7 eWrf* SW? s

V -r* ^VJ"/ S

- f•#•( •(- (•1•(

z.Lz.1.ii. ^iz.z.z.

.3J3•3•3•3•J•3

f o -SfPa-- f fBjb . a ^Ta TO9 3 -/ao/GO - 1 o J

/o 3 . /*jr/or - x /o

/oy -/o 6/c 6 - /of/c 9 -ttt/tt -1/3it 3 - *vr//*r ~t("j tt f 'tt ftt ? - t*.tt^i -/ij/w - /ir"-j~ - / if

//d -/^/I/r/ - /ij; 1.3 -/ivT/IJ-- /i-T/2-7 -/i?/It '/J/t y/ - /*S*/JcP-XV*

V 4 Ov (t

3 V

6

S.yC-V S-v s -v 5. t/g. Vs -v

-//e-/AT

l - /^ Vt if "i.

- f

-/oo

BDNDAR-CLEGG S. COMPANY LTD.764 BELFAST ROAD, OTTAWA, ONTARIO, K1B OZ5 PHONE: S37-311O TELEX: O53-354B

Geochemical Lab ReportCu, Zn, Ni - HNO,-HC1 D K1 672-2

Extraction_______________ o_____________ Report No. ^^^—^——.^—-^-—^—————^—^—————^

Method____A.A._________________ Frnm Mcintyre Porcupine Mines Ltd.-Mr. A.Skrecky.

potionu^ -TOO rocks H.M.S._________ Date July 28._______________ 19-72__

SAMPLE NO.

407

08

09

10

11

12

13

14

15

16

17

18

19

20

21

22

23

24

25

26

27

2829

30

31

32

33

34

35

36

37

Cu ppm

50

175

215

190

180

248

185

15

20

13

11

65

47

112

72

297

197

-5Ja -

56

56

72

. .51 —.50

67

90

131

40

82

53

60

52

Znppm

28184

142

142

95

43

52

12

14

14

38

47

63

73

41

154

131

,^US-

62

37

34

47 ^92

98

248

920

48

42

55

32

29

Ni ppm

112no150

96

92

100

154

122

123

112

95

113

85

108

67

209

118

87

57

46

40

. 36 -.60

115

100

98

600

560

270

600

380

x ffjf *)

6-t

SAMPLE NO.

438

39

40

41

42

43

44

45

46

47

48

49

50

51

52

53

54

5556

57

58

59

60

61

62

63

64

65

466

Cu ppm

51

40

72

100

214

127

53

55

70

68

170

73

70

173— — — — — 62

90

89

-Z3 -70

43

38

104

45

60

48

43

54

860

53

Zn ppm

60

28

47

68

95

280

40

128

67

59

96

38

53

75

50

66

58

^278

59

55

93

43

29

35

34

72

40

78

Ni ppm

390

370

280

162

73

132

49

81

63

69

51

51

50

67

54

66

60

48

73

50

22

no40

38

45

44

50

39

51

*jt*

G 3

0*

6-6

BDNDAR-CLEGG S COMPANY LTD.7B4BELFAST ROAD, OTTAWA, ONTARIO, K1B OZ5 PHONE: S37-311O TELEX: O53-354B

Geochemical Lab Reportnn Cu, 7.n, m - HHyHCl_______ R Nn 67?-2____________

Method. A.A.

Fraction Used -TOO rock f H.M.S.

Kclntvre Porcupine Mines Ltd.-Mr. A.Skrecky.

Date Jlllv 28.______________________ 19 J2___

SAMPLE NO.

—————— 407 ——— ——

OB

09

innrti?14

15

1C

17

It;H1

2021?223

24

2b

26

27

2829

3C

31

32

33

34

35

36

37

C,'PPI"

— W) ——175

215

190

100

248

185l'.i

20

13

1!

6b

47

112

.22- -

297

197

513

56

^

7K

S3

50

67

90

131

40

8?

b3

60

52

Zn PPM'JO— te ——

184

142

142

95

43

52

12

14

14ifi,-HJ

47

1-3

73

. M—

154

131

4U

62

37

34

4702

98

248

920

40

4?

155

32

29

M ppm

112noISO

9fi

92

100

v;41?2

1:3112M! ^' *J

VI 3r ; O l*

108

67

209

118

B7 -t'7

^

40

60

11R

100

?f;C 09

&OU

270

600

380

SAMPLE NO.

43B39

40

41

42

43

W

45

46

47

48

49

50

51

52

53

54

5556

57

5f;

BS

60

fi

f.2

6?

f.4

66

466

Cu -ppm —

^140

72

100

214

127

53

55

70

C8

170

73

70

173

62

90

89

7370

43

38

104

45

60

43

43

54

860

53

Zn PPm

6028

47

68

95

280

40

128

67

59

96

38

53

75

50

66

58

5278

59

55

93

43

29

35

34

7?

40

78

Ni -PPm —

3QO370

280

162

73

13?

49

81

63

69

51

51

50

67

54

66

60

4873

50

22

no4C

38

45

44

50

3S

51

ploration Department,0.6ox 970,1 r,j' ; , ,. : -f

TlmmlnB, ' Ontario, ' . . ..

Bondar,.

ottawa, Ontario.'

.r .f

Jtilj^ 20, :;*972.

J^-'iW'M!.'ite:'.u",V -J l

soil sftaplee.We hair* •nolottd 3J ^*^.. ^ Wp.., .

These are numbered 467 to 503 Ineluslv*.

:*. -' : ^-\" ; ." , Would.oonoentrate from each vaaple and run *aoh for total *: eltvo and nickel. ; " : -,v v ,,:- \-- i '--.,,/' : :; ; ,

,; Please aend jrottr rejjort along with relate^ Invoices to the address noted above.

^•'v-fW^v;

MoINTIRB POBCUPmE NINB8. LIMITED,

' .f f, *'"' t ' . 'l " '.'l* ''•''^• L '^'"i 1 -;..- 1 ' 1 ,-?'-'"'/

AS/sa A.SkreokyP'.'. : ' i

*'v; ",,v i://-::,' 1 :.:.': 1 ';^;'

r

\i

i

t5*

VST to

rft' Or?toJ/t Z. J3IHi 5"iti 7ste**[90SI^i^3\HSH^rHITU 90

e -TS - 7S - 76 -7G- 7

W - /

H - tH - 1

H -Z.li - ^H**~

H -21* -JN -3H . 9

H --JW'J

M -J

f^ -V

y j ^*

/j ** ^^

N-HH - H

/v -J"

l 2. 0

-LO -

M s -fvo

/6o - / 1 O,60 -80 -

- 138

to -

l 9 o -

BDNDAR-CLEGG S COMPANY LTD.7B4T3ELFAST ROAD, OTTAWA, ONTARIO, K1B OZ5 PHONE: 237-311O TELEX: O53-3548

Geochemical Lab ReportExtraction Cu, Zn, Ni - HNO^-HCl_____________ Report Mn 68U-2_^_______^^^__

Method. A.A.

Fraction Used -100 rooks, H.M.S.

Mr. A. Skreoky - Mcintyre Porcupine MinesLtd.

natp August l,_____________19 72.

SAMPLE NO.

1*67

68

69

70

71

72

73

Ik

IS

1*76

77

78

7980

81

82

83

81*

W

1*86

87

88

89

90

91

92

93

9h95

k96

97

Cu ppm

Ik

99

135

133

370

102

90

6k

6k

69

32

108

95198

69

52

11*170

188

11*3

158

55135

kk62

78

3U

61210

1890

22

Znppm

77

77

88

1*2

275

63

70

50

1*0

37

28

85

821*7

37

U3

108

60

122

87

70

103

2250

1*9

36

69

120

26

166

1690

16

Ni ppm

77

71

87

98

113

53*. — ma

133

106

76

120

81

66

89300

81

52

86

11*9

133

300

1*00

370

71*

76

236

u 120

126

228

129

590

168

~-v

1J

*\4x\

J^

i,— j

,^s

r^u* b

f

V ^,(

"7

-t

f

±i—

d- -f

REMARKS

. BONDAR-CLEGG S. COMPANY LTD.

68U-2 Geochemical Lab Report

SAMPLE NO.

1498

99*X)

0102

*W

Cu

27

81

5757263

11*

Zn ppm

16

31

6k51

225

li+0

Ni ppm

760

1+60

510 y56

123

70 "

l ) L\r

}y te)

c

r aye

REMARKS

BDNDAR-CLEGG SL COMPANY LTD.764"feELFAST ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: 237-311O TELEX: O53-354B

Geochemical Lab ReportFvtrartinn OUt Ztl, Ki * HNOyHQl

Method ______A*At__________

Report No..

Prom Me, At EQnftoVr ~ Poi?OTffitFraction Used -100 rookB, H.M.S, August l f 19 72,Ltd,

SAMPLE NO.

1*67

68

69

70

71

72

737U

751*76

7778

7980

81

82

83

8U

85i486

87

86

89

90

91

92

9391*95

1*96

97

Ou ppm

71*

99135

133

370

102

90

61*

61*

69

32

108

95198

69

52

11*1

70

188

11*3

158

55135

14*62

78

31*

61210

1890

22

Zn ppm

77

7788

1*2

275

63

70

50

1*0

37

28

85

821*7

371*3

108

60

122

87

70

103

2250

1*9

36

69

120

26166

1690

16

Nippm

7771

87

98

113

53133

106

76

120

81

66

89300

81

52

86

11*9

133

300

liOO

370

71*

76

236

120

126228

129

590

168

REMARKS


68L-2Geochemical Lab Report

SAMPLE NO.

U98

99

#X)

02

Ou PPB27

81

*7*7263

IT*

Zn

16

31

fit51

225

-11*0 —

HI

760

L60

510

56

123

70

r aye

REMARKS

Department, 970,

Timmins, Ontario.

July 26,1972

Bonder Clegg A Company. Limited, 76k Belfast Boad, Ottawa, Ontario*

RIO 025

Dear Sirst

We hare enclosed 48 minus 30 nosh soil samples* These are numbered 50^ to 551 inclusive.

Would you make a heavy mineral concentrate from each sample and run for total copper, zinc and nickel.

Please send reports along with related invoices to the address noted above.

Xours very truly*

HoINTTBE PORCUPINE MINES 1IMITBD

AS/ A.Bkreoky

5045036066 67

5 l O * 1 l B U-

E 13Si*6 15 '5/6 . 5/7 5 18' S/ls io-SKs n ^ -

62.5-5-2^ 52-7-

533534535

5.39 54 P 54- f542--

645 54-f547

A-lA-\A-/A-/A-/

B-fD -l8-1 8-1 B-/ B-l8-15-18-1C-2- C~Z-

c. -e.

c- ^C. 2. C. "2- C. Z.c. 2.C. 2L

C -7

P--J 15-3P-^ P-3

aoo-ô ^ -jt o-f 2 ^ 3 -X ISz n- z ao z ô - z, mt ?f3 - ^ 2 52. 30 - 2. 3 Z Z 3 2. - 2 3f Z Jf— Z36 239 —

75 — PO

/oo\ 02.f 09

- l 0^- l 08-II*-l/ fe

II ^ ^

-60(To - d S

- "7 O - S--7 B.S

- ffo- ^?^- 9o

ô ~ /oSf 0=5 .|IOno ~ /^ a

53-S S-S 55.S - tf e 6e ^ rf-S 6 o -70

-rf 2-

BDNDAR-CLEGG S. COMPANY LTD.76WE3ELFAST ROAD, OTTAWA, ONTARIO. K1G OZ5 PHONE: 237-311O TELEX: O53-354S

Geochemical Lab ReportExtraction_____Cu, Zn. NJ - HNOg-HCl_________ Report No _____^ 735-2

Method. A.A.

Fraction Used___-100 rocks H.M.S.

From Mcintyre Porcupine Mines Ltd-Mr.A.Skrecky.

Date August 8, 1972.___________ 19____

SAMPLE NO.

504-H

05

06

07

08

09

10

11

12

13

14

15

1617

18

19

20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

uu ppm

35

29

41

64

270

32

191

83

80

75

57.^...

41.

3957

65

72

67

63

69

36

59

500

40

51

100

73

64

305

105

128

117

L\\ppm

70

58

77

63

167

390

660

88

189

74

57

. 182 .

7657

79

127

97

42

108

93

36

400

38

43

57

54

48

227

79

1Z4

inn

N1 ppm

41

40

44

58

98

135

73

79

77

67

39

43

3332

65

51

55

60

59 ,

55

49

147

47

34

44

44

76

113•66

64

ft.V

\~\ ———

fH ——

^ 4-i

-i __

\

7A\FW -f-"-i l\

E7

V1

\

3

Jf

SAMPLE NO.

535-H

36

37

38

39

1 40

41

4243

44

45

46

47

48

' 49

50

551 -H

C* 2

Cu ppm

125

115

43

56

156

145

43

26075

800

1170

860

60

2200

860

470

167

zn ppm

85

138

59

55

100

40

31

R653

550

980

680

58

1590

1180

610

240

N1 ppm

68

59 ^

36

40

53

42

30

??36

290

385

540 ^

39

530

275

1350

400

^\\

~/—

fyit/' d 'y

^

7'

1

Mcintyre Porcupine Mines Limited,Exploration Department*P.O.Box 970,Timmins, Ontario,P4N 7H6May 16, 1973*

Bonder * Clegg * Company Limited,768A Belfast Street,K.R. l,Ottawa, Ontario*

Dear Billi-

We have mailed you a small parcel which contains 38 samples numbered M73*l to M73*38 Inclusive, These samples consist of till and bedrock material screened to minus 10 plus 100 mesh* Would you make a heavy mineral concentrate from each sample and analyse for total gold, copper and Elnc*

Please forward the results along with your Invoice to the adtress listed above*

Yours very truly,

MoINTYRB PORCUPINE MINKS LIMITED,

AS/sa A.Skreoky

B ^ Fo ft*uxc*fVO frOs'"

5.4 (VAL- t N) o .

M 1 5j. l ^

M 1 3. Z- ^

*n i?). 3 ^

M "73. 4- ^

H 75. S ^

H. 75,^ ^

H. 7^, 7 ^

H. 75.^ "^

H.7S-^ ^

K-7S. VO ^

H. "IS, u ^

H TT^ 1 i— S t*^•(B.I© ""^

H-7-5.13 f

. K -7^S - v^ ^

K-T5 .15 *^

K .*T^ . t^ *^

K ,TS . \7 *^

K-7-S..^ *S

K- 7? . ^9 ^

H-lS.SU^ •-

K-7-S. SL^ *^

H-75.a5 ^ K. 7^ a? *^* \ | ^J * v^*O

K-IS,^^ ^

H-7S .as rH TTL O^ ^

. 1 O ' C**O '

K-"TS.*5T7 ^

K.ns.-as* v

•** Ô^/OAA. v\*vy it Cp/t* ^ w ^**^ i W 1

"D ^Sc^ (2-i pr. o*0

c . l 7*5 ~*S"0

C . \ go -ê

C- 51 U^ — KV^

C-SL US- i^S

CV5 60 -SS

C. *5 5*5-^0

C- "5 6^^7|

C.-^ 5o-Sa

c. 4 Sa-57C. S 6^5 -^Sl

C.6 ^51-^4

f" ^* ^:54- ,- ':fe?^^^. *o -^^r *"" ^-Ôi

C.6 5^--5i8

C/7 ^^-ô

C-7 ô-^^r

C-1 6S--56*

C.S" 6^~e^

c.e ^-6eC.^ 66 -70

C-^ 60-6G

C.^ 6/5 -76

C -^ 76 -60rv -a 5S4-~- trZC?^ — - / CrT CTTCT

C. 9 ^-^c ac *fe * looC.\O IO)0- KbS

c-\o los-tvo

C-VO UO- US

H -is

K-

K-

K-13

c.\o"59 -AS

c.

C .

-ST

K-

H

K-

t56~

-Ito

\3*SA \-So^ t

t^^——\4J5 ^-50-

/K.

A\,

/K-TS

-

IX A

IX.--5X

VX.-5.

AA A.QL

AS 'So-'ST

A-V

A.S

A-?

s.

M T-S i If-/ .4

HO

i/K-TS .

-86

v Hi/K-TS.89

K-T5 . 1' K -75. 95

J

v.

b.-s t.-s

68: - 70

"756 /S -'"755

Sg .S —

V5 "76 -

O^W^k /o M O

nrt- 7.3*

m - 73

fv? - 74 - /o/

/vi i 7,3 ' 'o 2.

7 a - /oy

73

f a

- 2. li o ~/

f 2.7--

/T) i 7

/V7 , 73 - /o?

JVJ , 7J - //o

#7 * 7 J - l u

fa . 73 . l' Z.

fa . 7 3 . /; 3

xn- 7J . /y V

-l

-x

t

2.

-x o/

x z-^-'sT- x ^7•'v^

99 -/oy

-J /o ? - x/

73

m ' n

i/?

' 73

7.3 '

e -z

6-2.

9 3 -

l "i l - l Z.

38 ~ l 1 O

l f f - i ^.-z.

K-

K T5^\-TS

K--73

VVT

a-s*

H6r-

Extraction

Method

BONDAR-CLEGG S. COMPANY LTD.ELFAST ROAD. OTTAWA. ONTARIO. K1B OZ5 PHONE: S37-311O TELEX: O53-354B

Geochemical Lab Report______ Report No. _________735-2_______________Cu. Zn. 111 - HK03 -HC1

A. A.

Fraction Used . -100 rocks H.M.S.

From HcIntyrQ Porcuplno

Date August 8, 1972.

Ltd*MriA t SkrccKyt

SAMPLE NO.

b04-H

05

06

07\^ 08

\ 09

H 10 ——— 4 ———— UJ ————

{ n——— ————— U —————

12

13

14

IS

Ifi

17

18

19

20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

Cuppr.i

3i

29

41

64

270

32

151

83

80

7B

57

43

39

57

65

72

67

63

69

36

59

500

40

51

100

73

64

305

105

128

117

ZnPirn

70

56

77

63

167

3SO

660

88

189

74

57

182

-76 —-57

79

127

97

42

108

93

36

400

38

43

57

M

48

227

79

124

inn

N1ppni

41

40

44

58

98

135

73

79

77

67

-39

43

3332

65

51

55

60

59

55

49

147

47

34

44

44

76

113

66

64

A3

s*,?***

Zee '2e2

teg-**}/

2/f'J'j

4t9~je*e

t2f'MZ

tfJ'tSS

zre-ff2

*S2'fsS

tt****'

JSSf'*fro

SAMPLE NO.

535- H

36

37

38

39

40

41

'. ————— 42 ———

43

44

45

46

47

48

49

50

551 -H

/0 7?#?s*ie!SP

S0 V"?***'*f**F

CUppm

125

115

43

56

156

145

43

OCft 60U ——

75

COO

1170

860

60

2200

860

470

167

&PSF

zn ppm

85

13659

55

100

40

-31 —

tUL- — o9-

53

550

980

680

58

1590

1180

610

240

'•rs

mppm

68

59

36

40

53

-42 ——

-30 ——

-22 ——

36

290

385

540

39

530

275

1350

400

rf

BONDAR-CLEGG S COMPANY LTD.7SWiBELFAST ROAD, OTTAWA, ONTARIO, K1G OZB PHONE: S37-311O TELEX: O53-3548

Geochemical Lab ReportFvt,..*inn Clt.Zn.Au - HNOg-HCl_______________ Report No.___________420-3___________

Method A. A. F rom Helfllyff

Fraction Used Hegvy Mineral July IS, .1921.

SAMPLE NO.

M-73-78

79

80

81

82

83

84

85

86

87

88

89

90

91

92

93

94

95

96

97

98

99

100

101

102

103

104

105

Sample Weight

0.26g

0.330

0.26Q

0*30

O t 08g

O.OSg

0.225

0.24g

0.1 8g

Cu ppm

56

36458

400

141

308

I t S.

I, S.

1890

3290

2038

587

613

94

1110

2089

106

780

938

114

27

23

569

810

810

287

280

226

< mea

In ppm

60

463BS

5S9

98

145

6300

1550

2885

1133

938

95

1650

4578

128

2800

3396

90

66

44

372

560

760

108

191

143

is less

Au PPb

5

20

I. S.

I.S.

1820

25

I.S.

^

I.S.

I.S.

I,?,

40

i t s,ItS,

^

50

ItS t

N.P,N,D.

6

I.S.

15

N.D.

25

I.S,

I.S,

than

REMARKS

I.S.-1nfufficiant sample

N.D.- not detected ———

BDNDAR-CLEGG S. COMPANY LTD.ROAD, OTTAWA, ONTARIO, K1G OZ5 PHONE: S37-311O TELEX: O53-3O4B

Geochemical Lab ReportFvt,artinn Cu,Zn,Au - HNOg-tiCI_______________ Report No.___________420^3.___________

A. A. From Mcintyre Porcupine Mines,

Fraction Used Heavy Mineral July 13, 19 13-

SAMPLE NO.

M-73-78

79

80

81

82

83

84

85

86

87

88

89

90

91

92

93

94

95

96

97

98

99

100

101

102

103

104

105

Sample Welaht

0.26g

0.33g

0.26g

0.3g

0.08g

0.05g

0.225

0.24g

0.1 8g

Cu DDm

56

36

458

400

141

308

I. S.

l.s.

1890

3290

2038

587

613

94

mo2089

106

780

938

114

27

23

569

810

810

287

280

226

^ meal

Inppm

60

46

385

559

98

145

5300

1550

2885

1133

938

95

1650

4578

128

2800

3396

90

66

44

372

560

760

108

191

143

s less

Au ppb

5

20

I. S.

I. S.

1820

25

I. S.

^

I. S.

I. S.

I. S.

40

I.S r

1. 55.

^

50

I. S.

N.D.

N.D.

5

I. S.

15

N.D.

25

I. S.

I. S.

than

"X

Wf\ i

^

jCo*

)\

yrnr

)11 134H'"}(•'06

\M

trr'\1—\ tlr~

c*\~SL

54-41

tf-lo

70-lZ

It'14

/ID-42-

42*44

M-4L

ft-4*'S

5?Ui

6*-*'

AH4

*4-tf.J

3^36#4^5S-fr*(4W-41tf-7o

1*-1ttf'W

f^toO

10 ^-/O^

io5*/^MteW

f/0- dOI?^it1

•ZT-^

I2/H3/

REMARKS

I. S, -Insufficient sample

N.D.n not detected ———

June 28. 1973*

Bondar - Clegg ft Company Limited,768A Belfast Street,H.R. l,Ottawa, Ontario.

Dear Bllls-

We have mailed you a shipment which contains 28 samples numbered M.73*78 to M.73.105 inclusive. These samples consist of till and bedrock material screened to minus 10 plus 100 mesh. Would you make a heavy mineral concentrate from each sample and analyse for total gold, copper and Kino.

Please forward the results along with your invoice to the address listed above.

Yours very truly.

McINTTRE PORCUPINE NINES, LIMITED

AS/sa A.Skreoky

BONDAR-CLEGG S. COMPANY LTD.ELFAST ROAD, OTTAWA, ONTARIO. K1G OZ5 PHONE: 237-311O TELEX: O53-354B

Au - Fira Assayl Fvtrartinn CU. Ztt - 11110 .,-HCl

Geochemical Lab ReportReport No. 305-3

Method.A. A.

Fraction Used H.H.S., -100 RookB Date.

Molntyre-Poroupine Mines Limited29*

SAMPLE NO.

C-l-75-80-80-86

0-2-113-118

-110-125

0-3-50-55

-55-60

-68-710-l*-50-52

-52-57

0-5-55-620-6-51-5*4

-5U-5B-56-58

0-7-146-50-50-514

-56-58C-8-58-61{

-66-6B

-68-70

0-9-60-65-65-70-75-80•814-88-88-91

0-10-90-100-100-105-105-110-110-115-115-117

0-11-39-1*5

-52-56

CUppm

19ii1150

151,766

76

1L905800

637

555161310322li i J250

y//

1.6

119

217

1*2

IciG

Itf

#5

I.e.

166

163

I.r..82

109

66

77

'/.nppia

132

860

15553li8?

63

1?2

181|0

Hi5o1733

11517822790325

695

67

*75

h35W60

62

315

I. S.

80

87

i. a.),5o371

65

1020

Au Ppt

30

I. S,

1.51.8,

30

K. D,

30

I. S,

I. S,

I. S,

27005ijOOi^tioo3)i2^I.F,

I.r.,50100

I.S,

H.D,

3030I.S,

100

12

18

I.S,

I.S,

I. L.,

N.D,

168

SAMPLE NO.

C-ll-56-58-56-60

C-12-U7-57-56-58-58-60-60-63-63-65

I.S. - Irani

H. D. . Hot I

UUppo

1|0

w50

660351WiO197

fioiont

otooted

aa ppa

595663

614

1500

928

UilO

886

r*ainple

AUppb

112

16

12

i.e.I. S.

I.S.

I.S.

BONDAR-CLEGG S COMPANY LTD.ELFAST ROAD, OTTAWA, ONTARIO, K1B OZ5 PHONE: 237-311O TELEX: O53-354B

Geochemical Lab ReportAu - Fire Assay

Extraction Cu. Zn - HUO..-HC1 Report No. 30^-3

Method.A.A.

Fraction Used H.H.S.. -100 Rooks Date.

Mblntyre-Poroupine Mines Limited

May 29,

SAMPLE NO.

C-l-75-80

-80-86

0-2-113-118

-118-125

0-3-50-55

-55-60

-68-71

O-U-50-52

-52-57

c-5-55-620-6-51-5U

-5U-58-56-58

0-7-1*6-50-50-5J,

-56-58

0-8-58-6^-66-68

-68-70

0-9-60-65

-65-70

-75-80-814-88

-88-91

0-10-90-100

-100-105

-105-110

-110-115

-115-117

0-11-39-1*5

-52-56

Cu ppm

195

1150

15U

766

76

.JI

90

5800

637

555161

310

322

11 (0

250

597

1*6119

21?

1*2

186

U9

525

l. s.

186

163

I. S.

82

109

68

77

Zn ppia

132

880

155531*

82

63

122

181*0

11,50

1733

115

178

227

90325

695

67

275

1*35

1*6

60

62

315I. G.

80

87

I. S.

1*50371

65

1020

Au ppb

30

I.S,

1*5I.S

30

X.I),

30

I.S,

I.S,

I.S,

270051*005800

3U25I.S,

I.S,

50

100

I.S,

H. D,

30

30

I.S,

100

12

18

I.S,

I.S.

I.S.

N.D.

168

SAMPLE NO.

C-li-56-58

-58-60

0-12-1*7-57

-56-58

-58-60

-60-63

-63-65

I.S. - InsuJ

N t DT - Not I

CUppffl

i*o1*8

50660

3511*1|0

197

fioient

ateotad

Zn ppm

595

663

61*

1500

928

11*10

886

Sample

AUppi)

112

U5

12

1.8.

1.8.

I.S.

I.S.

BDNDAR-CLEGG S COMPANY LTD.7S*^ELFAST ROAD. OTTAWA. ONTARIO. K1G OZ5 PHONE: 237-311O TELEX: O53-3548

Geochemical Lab ReportAu - Fire Assay Cu. Zn - HHO,-BC1 Report No..

Method.A.A. fram Molntyre-Poroupine Mines Limited

Fraction Usad H.M.S., -100 Rocks Date.May 29,

.19 73-

SAMPLE NO.

c-i-75-80-80-86

0-2-113-118

-118-125

C-3-50-55

-55-60-68-71

c-l*-5o-52-52-57

c-5-55-62C-6-51-5U

-5i*-58

-56-5b0-7-146-50

-50-51*

-56-5,8

C-8-58-61;

-66-68

-68-70

0-9-60-65

-65-70————————— voVtV — ,

-75-80

-8U-88

-88-91

0-10-90-100

-100-105

-105-110

-110-115

-115-117

0-11-39-1*5

-52-56

Cu ppm

195

1150

151*

766

76

37

90

5800

637

555161

310

32211*0

250

597

U6

119

217

1*2

186

i*9

525

I. S.

186

163

I. S.

82

109

68

77

Zn ppm

132

880

155

53U

82

63

122

181*0

11*50

1733

115

17b

227

90325

695

67

275

te*1*6

60

62

315

I. S.

80

87

I. S.

1*50371

65

1020

Au ppb

30

I. S,

1*5I. S,

30

N.D,

30

I. S,

I. S,

I. S,

270051*005BOO

31*25I. S,

z. s,50100

I. S,

N.D,

30

30

I. S,

100

12

18

I. S,

I. S,

I. S.

N.D,

168

Sfi,*-^w^^ftfts

6^

f j t-tfL

A*-

^W"

ft'l,*

1^

W

W-

^^•v-//' 'w* y

,\s<^v'; V'

\ A'

V)V

Jw

SAMPLE NO.

C-li-56-58

-58-60

0-12-1+7-5^

-56-58

-58-60

-60-63

-63-65

I. S. - Insui

N.D. - Not I

i

/J004 -' ' * fs s

uu ppm

1*0

U8

50

660

351

W+o197

fioient

eteoted

003*-. . ^

Zn ppm

595663

61*

1500

928

11*10

666

Sample

:"V*.s

AUppb

112

1*5

12

I. S.

1.8.

I. S.

1.8.

,*V**s r

^

^

^P)tj

^

fit*

ffi

9A/

OVERBURDEN DRILLING LOG o H S"

el- /DR ILL HOLE NO:

*MPLE DEPTH: SAMPLERS :ra^fa s E L; y E. X

LOCATION:

i-

*OINT STARTED: O* '

POINTSTOPPED:y'i'''^5

SO1NT EXTRACTED:/^ * ^

DRILLING TIME

S AMP LE R ST A RT ED:

SAMPLERSTOPPED.

S AMPL ER E XT R A C T ED:

CcmJ 6

: /X ' 2 J

*-' FOOTAGE

l" FROM

T 6 '

f; rU3'l'/?'

WJP} Jt* '* 2 S fa *± t,j ^2\tf ' si

ri- -s*- ———Sir ,,

jlf '.

TO

/'

13'!9'2il?"25*3"


C K O A *}^C ) A y A fi f

p/ M E SAN og 6 L ^xT/fST/ Jit

o u a G t/*?" C, fi G^

SAMPLE

DESCRIPTION

ORGANIC %

C L AY *

S 1 LT 1,

F IN E SAND %

MEDIUM SAND 1,

COARSE SAND 1.

GRAVEL 1,

PEBBLES t.

^REMARKS:


•AMPLE NO: DR IL L HOLE NO:

• AMPLE DEPTH: SAMPLERS:

C. L fi. LME

LOCATION:

DRILLING TIME^/S. x" ^7"*^ GsrU k

POINT STARTED: oi- , 3 S AMP L E R ST A RT ED: f'

Q -y opOINT STOPPED: J- *

POINT EXTRACTED:^, ^ 5

SAMPLER STARTED:

SAMPLER STOPPED: ^f ' **- ^

SAMPLER EXTRACTED: Y' 5"

FOOTAGEOVERBURDEN DESCRIPTION

SAMPLE

DESCRIPTION

X ' 6 /? (3 S) X ife'7" CJ Z'?" J i M E1X7" JB A J. FIN C SAND

MEDIUM SAND t,

5* f COARSE SAND

i.,

REMARKS:

t.


AMPLC NO: DRILL HOLE NO: : .

9- 7 4SAMPLE DEPTH: CONTRACT:

LOCATION:

DRILLING TIME S^Z.

POINT ST ARTED;

POINT STOPPED:

POINT EXTRACTED:

S AM P L E R ST A RT E D :

SAMPLER STOPPED:

SAMPLER EXTRACTED:

FOOTAGE

l PR OM

0'^3 *

yro c *

iri

TO

e-/3*25*50*^/'


C K G A NICc l /i y

P i HE S/IXP y c /MXtC /f A i/^LTiLk

S u S o vT OXC&

SAMPLE

DESCRIPTION!

ORGANIC 1,

CLAY *

SILT 1,

r IN E SAND *h

MEDIUM SAND *lt

COARSE SAND 1,

GRAVEL t.

PEBBLES -T.

REMARKS:

A/

•nOVERBURDEN DRILLING LOG

DR IL L HOLE NO:

• AMPLE DEPTH: SAMPLERS :

j J-*

CONTRACT:

INE:

DRILLING

IPOINT STARTED: Q-Q v

•OINT STOPPED: /O * 3

fifOINT EXTRACTED:

SAMPLER STARTED: /2 *

SAMPLER STOPPED: f *

SAMPLER EXTRACTED: /y

f: FOOT)'fi

|. FROM

s" 0 ''K p t |.—5r

F3?'f S S 'F1liifi-ii - — — 'fREMARKS:

lF

rvi"1"

kGE

TO

e*/^'3-y38'

7 ^

t5 y?^ A X/ C

C L A?

F/SSZ SslVP

7W^cS" ^ ^ a u7~ C/^&fe

'^^ L

SAMPLE

DESCRIPTION

ORGANIC 1.

CLAY f.

SI LT %

F IN E SAND - K

MEDIUM SAND %

COARSE SAND t.

GRAVEL %

PEBBLES 1,

s!..w

fc 'OOVERBURDEN DRILLING LOG

•AMPLE NO: DR IL L HOLE NO:

SAMPLE DEPTH:- SAMPLERS: CONTRACT:

C. L ft L

f*————————————————————

fPOINT STARTED: O , *1 f

"i"OINT STOPPED: ^ O l C- ^

EXTRACTED: /0; 5"^

DRILLING TIME S/A ,lo7~6 Grrx/6

SAMPLER STARTED: C

SAMPLER STOPPED:

SAMPLER EXTRACTED:

* FOOTAGE;ii.

| FROM.1* —————————— 't -

f 2"

ls.5'

l' y, t

I..f'

tft

TO

2. */t— *

^5 *t^" *

^8'f/'


OX G A /*' c.ct*7

FJ'H E ssiNv* c lAyQ K/ti/^Lr/t^

S P B a (/T c /7 o ^

SAMPLE

DESCRIPTION

ORGANIC r*

CLAY *

SI LT *h

FINE SAND 1.

MEDIUM SAND ft

COARSE SAND f.

GRAVEL 1,

PEBBLES i,

REMARKS:

i p -r/1?;^^

jt-'l:' : i:f:|r

1l:'


•AMPLE NO: DRILL HOLE NO;

/•AMPLE DEPTH: SAMPLERS:

LOCATION

f

|fOINT STARTED: ^

jjtiPOINT STOPPED: ^~

JJJFPINT EXTRACTED:^!

DRILLING

SAMPLER STARTED: /* f J

SAMPLER STOPPED: J" *

SAMPLER EXTRACTED: *f*

f- FOOTAGEtp!.

f FROM

0*

l Z '/3*

i 3?'2S'

:ti''

TO

2- '/3'3?'se-


c fi &A/V/CC2/)/

p///^ S A X PTV^

S t/ av7" otfag

SAMPLE

DESCRIPTION

ORGANIC 1,

CLAY *.

S ILT *h

FINE SAND 1.

MEDIUM SAND . 1,

CO ARSES AN D ^

SRAVEL 1,

PEBBLES 1,

REMARKS:

3


SAMPLE NO: OR !L L HOLE NO:

•AMPLE DEPTH :32' SAMPLERS : CONTRACT:

LINt:

DRILLING TIME CcrrU b

IPOINT STARTED: O/ 7

STOPPED: ^Jf S

EXTRACTED "*

SAMPLER STARTED:

SAMPLER STOPPED:

SAMPLER EXTRACTED

|| FOOTAGE

•|f" FROM

f 0 '# a -l s*! 3 o '

t|:l-iy.i.r! |.

Ss "!'.!

1-'

TO

e-e*

5^-sa^


6 K G*A fi J cC ) /} V/

A /i f

p/S/sE 5/4 /Y#

(^ ft /t l/ S L

SAMPLE

DESCRIPTION

ORGANIC ft

CLAY ft

SILT ft

FINE SAND , ft

MEDIUM SAND ft

COARSESAND ft

GRAVEL ft

PEBBLES ft

REMARKS:

X

?


, SAM PL E NO: OR IL L HOLE NO:

SAMPLERS : CONTRACT:

tiHE:/J

LOCATION:

AIPOINT STARTED:

*OINT STOPPED: /* ^ 5"

*OINT EXTRACTED: 2 ""

DRILLING TIME 5

SAMPLER STARTED: C- * r ft

o j-i *rSAMPLER STOPPED: ii* ' ~l

SAMPLER EXTRACTED:^' 3^

f; FOOTAGE

1. FROMi" '

O '

1 /*i 2g*1 37't V3'|:.

f"f.-,

si'.' t,?

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/'

2^'

37'V3'


o/r^/4 /y/cc? ^ AY

p/*^ S * rf o-r/n

S U # 0 aT e /l 6 g

SAMPLE

DESCRIPTION

ORCANIC 1.

CLAY 1.

SILT ft

FINE SAND . %

MEDIUM SAND f.

COARSE SAND f.

ORAVEL Si

PEBBLES r.

'-REMARKS:

1;; ^ 7~/?/^ ik- it' . IK.- SS.p -Sf : ..


r DRILL HOLE NO:: f- .W5" f T1-

AMPLE DEPTH: SAMPLERS : CONTRACT:

C ft AW f a X t)DRILLING TIME.5X2-

JPOINT STARTED: f v ' ~? S AMPLER ST A RT ED: /' ' 3 '"E

P*OINT STOPPED: /f SAMPLER STOPPED: //' J J*

IPOINT EXTRACTED: /f 'fi Q S AMP L E R E XT R AC T ED:^2* X 5^

rl" FOOTAGE

1; FROM

i, O '

l r

l3k"J"L'-

rE :

\ .

Ir

TO

/ .

/^'

33'

36'?v


6 P, G- A rf it.c i A y

P/&6 s ** p x c;/}/-7* ILLS#^ carr cs?*#

S AM P L E

DESCRIPTION

ORGANIC f.

CLAY 14

SILT %

FINE SAND , ft

MEDIUM SAND 9,

COARSE SAND ft

GRAVEL 7*

PEBBLES *7.

REMARKS:


IAMPLE NO:

- 7DRILL HOLE NO:

SAMPLE DEPTH: SAMPLERS : CONTRACT:

LINE:

DRILLING TIME 5 /A- A 6 T& fryyj

POINT STARTED: /4~J SAMPLERSTARTED: J ' t*- -J

IjPOINT STOPPED: ^' 3^ SAMPLE R STO PP ED: ^' ? O

•POINT EXTRACTED: ^* 2.6 SAMPLER E XTR A C T ED: / Q ' pL 0

; FOOTAGE

FROM

O'a*

1 e ^'i z?'l -7^

ig

TO

e-2^'3?'yz?*


0 KG A A'/ cc 2 ^5/

p / ^ E S A ^ T( LI*

S t/ x5 o t/T' c K o S

SAMPLE

DESCRIPTION

ORGANIC T.

CLAY 1,

SILT W

FINE SAND , t.

MEDIUM SAND 1,

COARSESAND %

GRAVEL 1.

PEBBLES 1.

REMARKS: -7-

l'''l'!' 1:.

:*,,


: lAMPLE NO:

\2LA-DR ILL HOLE NO; s b

SAMPLE DEPTH: SAMPLERS :

, XL

'"•OINT STARTED: X O f 3 ^t

|**OINT STOPPED: //* / St;.iiPOINT EXTRACTED: '-"""^

DRILLING TIME 5X2/ A"7~6

SAMPLER STARTED:

SAMPLER STOPPED:

SAMPLER EXTRACTED:

6

f'' FOOTAGE

i FROMOVERBURDEN DESCRIPTION

SAMPLE

DESCRIPTION

o B

5*" FINE SAND

MEDIUM SAND

COARSE SAND

'^REMARKS:

x

13


SAMPLE NO:e* d DR !L L HOLE HO:

• AMPLE DEPTH:

7VSAMPLERS:

M c wry fi E.tr LOCATION:

DRILLING TIME 5 X*2~ b

STARTED : f 2. 1

f. s\JSPOINT STOPPED: C- *I-"

pfOINT EXTRACTED:

3iy

SAMPLER STARTED: l

SAMPLER STOPPED: C

SAMPLER EXTRACTED:

l" FOOTAGE

|; FROM^T". c?'

f 3 'rsvj ^^ 'r 7fi-

i' rf ^ J 1^j j,,,, .1 |:.' .

i L:

TO

a-35-5^'bb*

7V


Q K &A # ) cc ji^y

p/ ME Q KAl/ZLQ? RA J/^L-r/ 1 L

S v 8 c v7~~ c- X o B

SAMPLE

DESCRIPTION

ORGANIC 7.

C L AY ?.

SILT *

FINE SAND , 1,

MEDIUM SAND 7.

COARSE SAND 1,

GRAVEL 1.

PEBBLES 1,

1


SAMPLE NO: - g DR IL L HOLE NO:

SAMPLE DEPTH: SAMPLERS: CONTRACT:

Mcwryxz-/B LOCATION:

Gemi j?

POINTSTARTED:

POINT STOPPED: 7

POINT EXTRACTED J ' 3

DRILLING TIME ^/^ *

SAMPLER STARTED: 7*7.5

SAMPLER STOPPED: /O' l Q

SAMPLER EXTR ACTED: fQ t *-j O

FOOTAGE

FROM

o-t'

3k'57'

^

TO

r3^57'

6,2.'


6 fl G rf A /cc i/ty

F///F S*XPTsJLL

S V 3 d v7~ CAoA

SAMPLE

DESCRIPTION

ORGANIC f.

CLAY ft

S ILT Tit

FINE SAND ; *

MEDIUM SAND 7*

COARSE SAND 1.

GRAVEL 1,

PEBBLES 1,

.REMARKS:

X

l: l'

f;


i CAMPLE NO:

e ) A -~ " f*l S AMP L E DEPTH:

DRILL HOLE NO: /j*- /^

SAMPLERS :

/fLOCATION:

DRILLING TIME 5^2. 6 CcmJ faPOINT STARTED: (f *

POINT STOPPED: //, y^

POINT EXTRACTED:/^./ 5"

SAMPLER STARTED: /* f 5

SAMPLER STOPPED: /, *J C*

SAMPLER EXTRACTED: 2* /O

FOOTAGEOVERBURDEN DESCRIPTION

SAMPLE

DESCRIPTION

a K G A /v/c

•y r x FIN E SAND

MEDIUM SAND 1,

COARSESAND

REMARKS:

S T


•AMPLE NO:

S Z /4 -DR IL L HOLE NO:

' 5 SAMPLERS :" RESTATION :

3 .- J*OINT STARTED

!l.i FjifOINT EXTRACTED: 3*

STOPPED : 3

DRILLING TIME

SAMPLER STARTED:

SAMPLER STOPPED: V' '

SAMPLER EXTRACTED:

r6 Ccrvi/

?. V5"

:sr.;-

f" FOOTAGE

l FROM

f 0 'i x-;i 2t -y*j ..rfitz —p^'l:5f'5^f; 1 —————ff-

s- t--Et

1* V

f,

TO

/*

a-y-5a-5^5""


0 rf G /4 S/CC t/)?

P/ A/ g S J

-T/^LS. u ti avT' c fi aS

SAMPLE

DESCRIPTION

ORGANIC 1.

CLAY 1.

S 1 LT It '

FINE SAND : 1,

MEDIUM SAND ?.

COARSE SAND 1.

GRAVEL 7.

PEBBLES It

JBEMARKS:

*- X -7-J/^ts..


BAM PL E NO:

PAMPLE DEPTH:

' 78*JLlNC: , .

DRILL HOLE NO: . ; - l jP J-/

SAMPLERS:

STATION:

DATE: J l

f d y w f y 3jCONTRACT:

Mc/j/TyfiELOCATION:

C f? d Ut rt) n P /*0ir\ DRILLING TIME 5)^ X o T 6 Gcmf fe

JJPOINT STARTED: f i 3 SAMPLER STARTED: ^"""""^•l'1

i|*OINT STOPPED: 7'

•OINT EXTRACTED: /C*

SAMP LE R STOPP ED:

SAMPLER EXTRACTED:

j. FOOTAGE

FROM

0'

l p\W\7l*1 O'tf 'Ir-

:fe

S.

Ir

TO

a-J^/fi 4

f~J *\ *

/jf /T) *


O /? (^ /Q /^ r ^

c j- Ayf //Sg- J^A'Z?

r, ILB f A 01/7^0*0,8

SAMPLE

DESCRIPTION

ORGANIC ft

CLAY ft

S ILT ft

FINE SAND ; ft

MEDIUM SAND ft

COARSE SAND ft

GRAVEL ft

PEBBLES ft

,

REMARKS:

t.-'OVERBURDEN DRILLING LOG

••A DRILL HOLE N 0 :

AMPLE DEPTH: SAMPLERS : CONTRACT;

DRILLING TIME 3X2- L of k QfrJ b',OINT STARTED:

f*OINT STOPPED:'. V-S

EXTRACTED:

SAMPLER STARTED:

SAMPLER STOPPED:

SAMPLER EXTRACTED:

' FOOTAGEf-

'f.. FROMH ———————————

O *

\- 2-'35*b*'7 B"8V

b

TO

a*?5*^0'F7 f^ t

^^ J-J '


o K G, A M 1 cci A y

pt rt z SAWp J M f G- R/) l/ EL*T; 2.1O6//S o u J c, /? A S

SAMPLE

DESCRIPTION

ORGANIC ^

CLAY 1.

SILT 1,\

FINE SAND 1.

MEDIUM SAND %

COARSE SAND % i

GRAVEL % :

PEBBLES %

REMARKS: .

r

INTER-OFFICE42AMSW0026 63.4827 CRAWFORD 195

DATE July 1. 1971

ATTENTION OF

SUBJECT

V.P.HajuBond

Exploration Program, Input 365 V Area, Abitibi Option, Crawford Township, Ontario*

l hare attached a log for the drill hole recently completed in Crawford Township* This hole tested Input anomaly 365V whloh had been earlier detailed by a ground surrey. The moderate IN anomaly outlined here Iles at the south edge of a avail isolated magnetic anomaly* These features in turn lie about 1500 feet south of a large body of niokeliferous serpentinite.

The BM anomaly was found to be caused by graphite* Core reoorery was particularly bad in the anomaly area - no important mineralization however, was noted in the recovered Material. There are no magnetic Minerals present in the rook types interseoted by the drill hole and the magnetic anomaly remains unexplainedt

AS/ A.fikreoky

EXPLORATION DEPARTMENTPropertyT . North Half of Lot 3, Concession 2,Location.... ' 'Claim No. Location of Core


north along picket line

PORCUPINE MINES LIMITED 650.O Teet .Sheet No.,— —..---—. .^^Crawford" Township

... ___ ... _ ......— ....... ___ ... .Schumacher Warehouse

Input Anomaly 365 W

collar - 60 o

-6ee- feet

Hole No.Length of Hole.———...-r--,-—,——.———————....——....... ,..—- ^ . June 20,1971 , JuneDate Started——————..———————...———Completedr* , j. A .Skrecky CoreLo^^l, 1971 ^Date...——.-...———...........-.-...——.....—————.......-.—.....Elevation ...—....................——.......————........ Datum

Co-ordinates of Collar South 3100

400nEast

From

0t I. -3 C' t J * S

18!? .0

294.0

To

143.5 IPS 0

294.0

306.0

Description of Core

casing - drillers report clay then a thin layer of sand and gravel near bedroc

of calcite the main ones of which trend at 35 o to the CA.tufi - rock sectioned as follows 1S6.0 - 19#.0 - a grey locally cherty hard rock thinly bedded at 45 o to the C

calcite. Much of this calcite is leached out leaving blocky eaIn r?5arm*t.**r- FI •rat 5- O ff.t*. nrln ^ pyT-ite and i? barfly gronnd .

1V^ *U ™* ^\J\) .u ^ ^i ovuid core 200.0 - 205.0 - tuff as in section 1S8.0 - 19S.O feet Rock rain trace pyrite204.0 - 2O6.7 - chloritic schist - a green sort rock ftigaiy sheared at 45 o te

qtz and qtz-carb. Rock rain tr pyrite206.7 - 240.4 - ground core p7,n^/, - yjtQ rff - rraphl'''-!'* sf'M.^t- — A bla*^'*' *^"*if *5h**gf*4ri ^t- /,n ^ to t.h** f!A fp*r240.6 - 241.0 - chips of qtz and sheared tuff min 5^ pyrite

— 241*0 - 246.0 - ground core ———————————————————————————————————— 246.0 - 264.7 - tuff - a carbonatized grey sonewhat muddy rock thinly bedded z

localiy. iiock nan trace pyrite. Short, sections are hi.ghly brec planes are partly plated with a thin film of graphite.

264.7 - 268.0 - dark grey tuff bedded at 45 o to the CA oin 10 1 fine pyrite ?6fl.O - PQ4-0 - tuff ss in section 246 .0 to 2^4-7 feet. Scattered inch thick tagglomerate - a tuffaceous rock with abundant irreg shaped fragments of a fin*

———————————— to 45 o to the CA. Rock Bin trace eube pyrite, scattered foot le 297.4 -0.2 ft .calcite at 45 o to the CA296.5 -0.4 f t .qtz-carb 299.2 -0.2 ft .calcite301.6 -0.3 ft .irreg dark calcite

Sample No.

k. No mat n oction \

A. Rock ivities. F

12740

1274ffithe (JA. 12742

^rn^T T T"vit12743

t 35 o tcciated lie

12744 eds are igrained

v^xw — J-*.a*..At ** ^4A^, *J^-\* U^.L

FOOTAGE

From

erialhat fo

s highock ni

irs.o200.0

HOCK s 204.0

240.4

45 oaled w

264.7 ery ehgreeniTHt flTT* 'UO Cat^c

To

(*as re4

Ly bre(n with

193.0

204.0flatter* 206.7

f h**ma1241.0

bo theith ir:

268.0 erty.jjxlcjr US

^^i^ a*h *-firt.i ii w.

Width

overec

ciatec12 py

5.0

4.0td thre

2.7

ite0.6

CA. a;•eg cal

3.3

teria]

CORE ASSAYS

from ' nd 4. Ro*

heale*in bri,

nil

niladed w:

nil

nil

all qticite . i

nil

. Rock to 10*

-he ov*tlr gTI^

1 withTJ& cal

0.02

o.osLth nfal

0.06

0.01

t, grailvidely

0.02

poorlycube j

lrburde by a f

very i•es up

y thin

is arescai/te

beddeiv r*! t f* ,

n frad iw thi*t

rreguLto 1/S

vein!"

5OB3S3OI1red bel

d at 3:

don. fc**^ j _*VL*M9 ————

irinch

;ts

Ettng-

; o

EXPLORATION DEPARTMENTProperty.————— Location ——._.. Claim No................Location of Core.

At

PORCUPINE MINES LIMITED

Surveys Dip Bearing

DIAMOND DRILL LOGHole No.""'"-"": 1 -"-....——....... Sheet No- Length of Hole——....—-—....—.——........-..————————..Date Started.—————————————... . . CompletedCore Logged by————————— ————___—_..............Date — ——— —————————....—————.—...—... . —- .....Elevation ...——.....................—...—————......... Datum

Co-ordinates of Collar North..--...——-....———...—............———..—————....-.East ————-,.———————........—————.—————. ——.

From

306.0

}'JX*J

346.0

420.0

To

332.3

346 .u

420.0

P*- S.!

F^HJ

650.0

Description of Core

tuff - a grey relatively massive i-oek poorly bedded at Ô o to the CA . T?net i 9312.8 - i inch calcite at 25 o to the CA 314.0 —— 0.7 f t .at z -carb at 55 o to the CA ————————————————————————————378.3 - C.2 ft. " " at 60 o to the CAgraphitic schist - a black tuffaceous rock highly graphitic sheared at 40 o to with scattered tiny cubes of bright py at times in clusters up to 1 inch in diatuff - a grey mud like rock thinly bedded at 35 o to 45 o to the CA. Hock is qt g^sttt^rî tiny ctib^s of briiyht pyrite at titt^s clusters in HIHSSOS UT? to 1 inch is developed.346 iO - 4.4 ft .breccia healed with irreg qtz min tr pyrite 350.4 -7*1 ft .shear zone at 45 o to the CA mn with irreg qtz and tr pyrite

361.4 -4.6 ft.irre* qtz (7*JO min tr pyrite382.0 - balance of rock is highly sheared at a. small angle to the CA

L-îo^fe *s ev:3"dent in other fragments. Several, inch long sections eonsist of gojjr)rrlLtJ. Only 6.0 TeeL of core was recovered from thisl.9.0 foot sSCtiin.

rhyolite - a grey hard rock with abundant glassy qtz eyes. Rock nay be a recrystto 55 o to the CA* A general brecciation is healed with thin seams of qtz and q Rock becomes progressively more sheared towards the bottom of the hole where thin the highly sheared material. The rhyolite is mineralized with tiny irreg sha

650.0 - end of hole.

Sample No.

:arbonati

the CA. B seter.z rich so: In diaraet-±2755 —— 1274612747 12748

1 V \slU^ fJH

ags. Rock12749

illized ttz-carb. : i colour iaed mauve lero with

FOOTAGE

From

zed *nd

edding

ne chei

3**o.O 350.4357.5

-361-4,*j.*^^ ^* m.atut JJig^sôws401.0iff wit

To

i someW

or she

•ty bed•If TO 1

350.4 357.5361.4 366.0

•p— nm 1J. A. \JUl .3

irrsg420.0 h reli

teck rain with ;hanpe!| to Acoloui

In And•ed phe

Width

hat br

arong

s areocolly

^..ij. 7.13-9 4.n

u O &Oqtz veL9-O c bedd:trace

felloTOCrys' it to :

CORE ASSAYS

?.cciate

LS loca

jresent

-nil —— nilnilrvH

^60-oHJiing jnil jog orto locrrev. 5,s whic

d* Hoc

lly co

. Rock^ ..u —\X if 14 1* i

0.02 C. 010.02 0.0?

o the nd is

;J .01 weak sally 3 ericith are•.^1. ^m—* WTtr goir

f min. -

Qtortet

min w:* — 9OXuG~

uAi Colain wil

hearinj1 f in*

e i^ e*partici

;race p

li Rock

.th widr*..—û^XU3C7IU

.h trac

: at 45! cubektlHIVjh^

ilarly

yrite

imr^

elyfee ———

•L —j j a .UÂ\O^.e

0pyrite

E ———

^M v ; - ; : ..i " !-" "- ; . ' :.' •r"---" ' : ~ ~'- ' . . Jl^fJm. JLJLÎ JL JL JLVrJLJU ^ ^ ** *'" "~"-ir ^ * J*.-'-- ,-,. ... ,- m,—-

* " ; - ^. _ Nor L h 'Hfrir of l*ot 3* Ccnc08 sion 2^

Claim No. . . ............ .. .. - - . Location of Core .......... ......~. .'

r, -r-^. __ A *-*^—— .fc '*.—. ~5^Lf- *'purveys .tT/yy.v f-TXMCjsj^? J*O^ 'S At Dip P-fflrin.g

' """"'collar"" """- SC o ' ' ' rôrih slorj; picket, lib-^20u Fe^st - tJ. o 30 f

-----600 feet - -54 o — -- -- •-••--. .-.. , ' - - ' j

ij Frow To : Oesc^-.ion o! C "r e ;

^^ j 0 143.5 casing - driHerr report, clay thor? ^ *.hir. layer of sand -srxi gravel near bedrock.

j of calcite the as&in on-9s of which trend at 35 o tc t c* CA. |

i IP^.O - 19o.O - a grey locally cherty hard, rock thinly badded at 45 o to the GJA.

LenEth of Hr,j., Wv.O leet.

D^te Started " '.. -'- : *t?d .... . .

D?f; ^--'-v

FOOTAGEVo. ~ ^^^**i X^

Ne âtsrial vas rswcrered fro". t.a? ^-e^s.Mrden fr-anti,-?- ,.

Hock is highly breccia tedj healer? with êry irregular1 calcite . Hach of this calcite is leached otit learing blocky carities . Rock sib with ! 1?? py IB bright caoes up to 1/8 : iseh

" : ....... l ......... 1 ... ... .... _ r. in î.*!F**t**r- First ^*'"^ feat iein 53* r^rr5tft and Is barfly gr"**1*^-! : i, - ' -^- —- -,—:i: j " 12740 i?e.o 193.0 5.0 nil c,02 ' j i" : 1 200.0 - 205.0 - tuff as in section 1S?-0 - 19^.0 feet Rock sdn trace pyrite 12741 2OQ.OJ 204.01 4.0 ail u.OC : i i '

I 204. C - 2o6,7 - chloritic scMst - s *3reen sort rock highly sheared, at 45 o td the CA. Hock shattered thraadec wit,l? ss^ly tain Teinl^ts : ; i qte and ots-carb. Rock adn tr pyrite " 12742 204.01206.7: 2-7 sil C' .06 i : : 1j 206.7 - 24C.4 - ,?TOTind cor*

'~: \ 240.6 - 22^1.0 - chips of qts am sheared tuff rain ^ pyrite ]

^^1 246.0 - 264.7 - tuff - a carbonatised prey soiaeirhat 'ruddy rock thinly bedded at—--y ' locally. Rock rJj5'"!;raee Barite. Short ?e'ctibhS~ar* highly bredeS

l planes are partly plated with a thin fill? of graphite. :

\ sail p*f;ehft*t o|f hespftiitft . i i........... ..i. . ,,.,JJ2743 240.4 241.0 0.6 nil O.C1 ; j j 1

35 o td 45 o |bo the CA. Staal! qtt graiJiis are ccaraoni ;::ît©^ healed wjltlrlrreg esliclte. VWely ; scattered bedding r 1 """"*

fi . !

j 264.7 - 266.0 - dark ^r&r tuff bedded at 45 o to the CA ads 10 * fine pyrite 12744 264.71 268.0 3*3 nH 0.02; i \ L . 26ifi.O - 2O4.O - t.nff MA Jr. section 246. 0 to 26*4.7 feet. Semttared inch thick l|flda ara êry ehjart-*-. |j 294.0J 306.0 agglomerate - a tuffaceous rock with abundant irreg shaped fragments of a na4 grained green prey s^terialU Ikx^c! poorly beddejd at 3^ 0 {

, . ——— j —— . —— j ————————————————— to 45 e- tc-th*; CA i. -j^gif-â-trace eobe pyrite, seattered foot l^Pg seetic^M arei ndn *iith ap- to 10^ i cube gyrite. ————————— —— — t J ; j 1 297.4 - 0.2 ft .calcite at 45 o to the CA | ; , . j

:r , ! i 299.2 - 0.2 ft. calcite 1:~- \ l 3O1.6 -0.3 ft .irreg dark calcite

j . ,.,..,. .. ...,... . .-.-.. — -..-,- . . , ,, ,. — — — l:: i il\

;i : \l i

—————————————— , ———— , ———— j ————————— , ————1 j i . "1li 'i . --

deration ——.—,— - .. ^ ...... ..,,....,,..__...,. . Datum

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGPro

'Locp&ty Abitibi Option

. north half of Lot 6, Concession 6,Crawford Tovmsnip, Ontario.


collar - 50 o north along picket line

Hole No. ..904-73-3. ...... .. ........ .... sheet NO. one

200 Teet - 4"9~o 30 T400 feel - Z*A. v yu

From

0

200.0

To

200.0

469.7

Description of Core

casing - drillers report clay to 30 feet then sand gravel and boulderwhich Was encountered at 160 feet. A tricpne bit was used for most of recovered other than from the section between 30 and 160 feet. Threesection. These boulders consist of biotite gneiss, pegmatitic pranite mareial and is min wi,th 2 percent po. The drillers report a heavy watcharged from this section causing some difficulty in piping operation

— dacxte - a green grey massive fine grained moderately hard rock showl scattered sections are weakly sheared, the main shear sections are t ausually at 45 o to the CA are partly plated with a thin film of po-cp threads and veinlets of dtz and qtz-calcite. The ma-5n vein! Pt.?? A™* t.a238.3 -0.2 ft. chloritized shear at 45 o to the CA

— 249.0 - 0*5 f t. section as above ————————————————————————————272 .4 -1.3 f t. section as above— 290.0 -1.0 f t. section as above —————————————————————————— 3H.1 - 0.5 f t. shear as above316.6 - k inch qtz-calcite at 20 o to the CA 318.5 - i inch " " " "323.0 -0.1 ft .qtz-calcite at 45 o to the CA no vis ndn 350.0 - 0.3 ft.ohoar at 70 o to the GA chloritic ——————————————371.0 -0.4 ft .chloritic shear at 70 o to the CA407.0 - rock to 469*7 feet is highly chloritic, somewhat sheared at 6 431.2 - 10.4 f t .shear zone at 60 o to 80 o to the CA. Rock highly chl

434.5 feet shows limonite stained shear planes. Rock cut by a 433.0 -o.l f t .Qtz-calcite at 90 o to the CA467.0 - 0.8 ft.qtz at 80 o to the CA no vis min 463.0 - |- inch at z at 80 o to the CA468.1 -0.9 f t. section min 1 percent fine po-cpy with a central 0.1 f

— 469.0 - 0.3 ft.qta at 70 o to the CA no vis adn ——————————————— 469.3 -0.4 f t .section ndn 1 percent fine po-cpy

Length Date Sts Core Lo Date ..Elevatio

North..East

SLUDGE ASSAYS

Footage

s to bedrthe over

aouldersand brec

er flow fStng rare pj jled beloy. Rock s sled belo

D o to 80 oritic. Gfew thre

t. sec t ion

jck. 'jurdei sach:iatec mm b(

*. Rotlows i •r.

0 to )re biids at

showj

'he bouldersi drilling w 'our ijnches1 andesite. )tweeri 65 ani* or seams o :k is min wiL gene

the C idly bid 0.1

ag 5

ral we

A. Hoc roken.f t .ve

percen

of Hole........ 537.0 feetirted-..J.one . H*1973 . C

j, A.Skreckygged bvompleted June 18

MJune 18,1973

n . ....... .... ... . .. .... . . . DCo-ordinates of Collar

410

atum /5)4-73-3

300

Sample No.

are up 1Lth the : Long wenFhe ande 1 70 fed

f a yell* ih rareak chlor

le ndn wii Rock ndijilets o:

t po-cpy

CORE ASSAYS

Footage

X) 5 feet•esult tt \ recoversite is d ;. A full

m±sh epi Tains od.te heale

h trace i trace i1 qtz-cal

in an ir

Width

. in ditat no •ed fro;eamed

eaain

dote 1' PO-CPd brec

po-cpy o-cpy.cite a

re gula

Au Ozs.

ametertsoulde] ILihiiidth reg of w;

ike milr-py. iciatioi

-py. A 0.3

s tabl*

r seam

ASOzs.

the lay mate ^articnor ea ter wa

leral. •cattert. Roc

f t. secd belo

at 50

rgestrial w ularrbonac s dis-

Widely ed frak cut

bion a1ir.

D tO tl

)f13

SOUS

:sJ7

9

ie CA

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGProperty- Location..

AtSurveys

Dip Bearing

Hole No.. -r-.:-.. . -.- .-..-.. . ———-Sheet No. Length of Hole... — -....— _ ...........-.............—............— ............Date Started-^—— ...........................— ............ .^Completed .Core Logged by—————.—.——-———.-.-———————.———Date —— —— . ........ . . — — . .——————— .Elevation .— — — —— .... —— .— ........... .... —— ....... Datum ..

Co-ordinates of Collar North.............-..-....--—— .——————..—.—— ———.——...East .... — ..———— ...... —— ...— —— —— —— ——. ....... .... ... .

From

-^*-469.7

^W

To

537.0

Description of Core

dacitic tuff - a green grey massive rock composed as previous rock witscattered tiny qtz~eyes and By occasional small 'round bomb's of dense l of qtz-calcite. No visible sulphide mineralization present.537.0 - end of hole.

SLUDGE ASSAYS

Footage

h poor beore acid ~

ddingtoater:

at 6CLal. S

i o toock we

Sample No.

70 o toMcly ser

CORE ASSAYS

Footage

;he GA. }.citized

Width

lock ehand cu

Au Ozs.

aracte:t by s(

Ag Ozs.

•ized bkattere

jr wided thre

17ads

EXPLORATION DEPARTMENT DIAMOND DRILL LOG-A.V.A. M 1 ^ -A~ JL. .A. ^*A—f

r

Locatio Claim Locatio

n north half of Lot 6^ Concession 6, Crawford TownshipNo. ..... ................. ....... ....n of Cor

At

e __ ........... ,... . .. .....- — —. . -Surveys

Dip Bearingir '-50 ^ . .JtiDi!tii...alon^..picket. line

200 feet -49 030'

-

-

400 feet -44 O30 f

Fromm 9

*—

To Description of Core

Sample Record

I Ir c rE

pE

Sample No.

12949

iole No. -ength ol )ate Star Tore Log] )ate .. 'Elevation

'forth

904-73-3 Sheet No thrS*Hole J37.-0 ^.... . ..... . . ......T —— ————

. Jxine II, 1973 ^ , .June ISHhy A.Skrecky g|June 18, 1973. ^

Co-ordinates of Co410

. Datumliar

904-73-3

200

FOOTAGE

From

467.0

To

469.7

WidthG

2.7

CORE ASSAYSold Silver Copper

nil nil 0.06

-EXPLORATION DEPARTMENTProperty?— Abitibi.Qption..-.-..-----.--------------- . .—~.~ -~~~

DIAMOND DRILL LOGPORCUPINE NUNES LIMITED

Claim NoLocation of Core

AtSurveys

Dip Bearing

Hole No. ....Length of HoleDate Started.... June -21, 1973.Core Logged by—Date..... June 26. 1973*

.Sheet No.

Completed

?-.?-U.a.-r---------------.---— -.T--5..9...rL?g,-^^ picket line20C) .f e^ - 44 d eg. 30*..^,,,.,.^,. ^.^.......,...

J ".-42 deg. 30*

Elevation ........sam.e..aj5...—........———............ Datum .904-7-3-3-Co-ordinates of Collar

North . ..100.0.....-—-.-................ . ....——...............

From

0

200. 0

312.0

To

'00 f

312. 0

328.1

Description of Core

—— casing - Dfillefo report clay to 28 feet then sand, gravel and boulders to be* at 170 feet. This was followed by abundant sand then large boulders from 19

—— frgaments from 190 feet to bedrock consist of brecciated andesite with carbtpegmaticUtic granite, gabbro and one boulder of magnetite rich gabbro.

—— andesite - a green grey to locally dark green relatively soft, fine grained hi at 60 deg. to the C. A. Many fractures show slickens id in g. Core is badly birregular veinlets of qtz-carb up to 0. 1 ft. wide. The more prominent vein!

—— scattered grains of pg^py ——————————————————————————————————————s? C^ ^* f y

210. 0 - 0. 4 ft. sheared breccia healed with paper thin veinlets of py at 70 d

^32, 2*0?!"^ ** ^^î*1**? i* *? a bov^ H^ftled "with 5?^fr UO~OIF trsco CDV227. 3 - 0. I ft. section as above healed with 5^ po-py trace cpy

237. 0 - 5. 0 ft. sheared breccia at QO ri*g- to th** C. A. m\n tr py239. 0 - slickens ided fracs plated with graphite

25L 5 - 0. 4 ft. qtz. at 65 deg. to the C. A. walls min with an epidotite like n

—— 288. 3 * 0. D IU qtz. at 55 deg. to the C. A. no vis min ———————————————— tuff - sectioned as follows

—— 312. 0 - 319. 0 - agglomerate tuff - a green black tuff with a few rounded Crag diameter. Rock thinly bedded at 65 deg. to the C. A. , min t

Sample No.

0 feet to

n*i weouis

ghly alte: roken up.ets are t

eg. to C

iineral ti

ments of r po-py.

FOOTAGE

From

lîrge bedrot

l^CLL VZ'^

•ed ro Roc!

abled

A.

cpy

light* rodi a

To

Ixûlil' :k. R*

LTcttti

:k. R. t lacec)elow.

r cAlou omewl

Width

\Zf WdS

covers

fed eLr

rcfc-irs- with iRock

red m at she

CORE ASSAYS

eiicou?d bou

u d tr*

tiigbly lumertmin TS

SEtertat ared

nteredo'er

ice pO|

fractu ms thrith wi*

up to

blotll

red m; eads ael y

2 Inch

e rich

i inly nd

53 in

EXPLORATION DEPARTMENTProperty—————. Location._————..Claim No. _—._... Location of Core.

At

PORCXJPINK MINKS LIMITED

DIAMOND DRILL LOGHole No.. .904*73*4-—— ---.—— -Sheet No.... — .Length of Hole————.—..———.....————...................—...........Date Started.— ——.——.. ......—.—...——— —-——.—. Completed .......Core Logged by—...—.- _ .....— —— —— — ...........—— ........— ____ .

.T.W0-

Surveys Dip Bearing Elevation ...... ——— ..... ........ — .... —— ..... .....— ... ..... Datum

Co-ordinates of Collar North-.——...........................————..———.............-.........East ——— . ........ . . .... ........... . . . ....

-

^

From

328.1

*-396 5J 7V* -J

-

To

396.5

44LO

Description of Core

319. 0 -J23. U - graphite zone - a black masSiv* graphite rich rock min with 5 ?0 py-po tr sph. Section includes 0. 5 feet and 0. 7 feet inclusions of medgrained dark green gabbro. The gabbro is min with 10^1 po

323, 0 - 327. I - gabbro - a dark green medium grained rock highly shearedmin tr py

327. 1 - 328. 1 - graphite zone as in section 319. 0 to 323. 0 feet

—— fcfigsf — diorite - a green grey massive fine grained rock. — Rock is relativety-h threads of feldspathic material tip to 1/2 inch wide min with tr po-cpy

388. 0 - 0. 7 ft. section as above

peridotite - f* dark green to black highly g*rpeotinized rock in contact withprev section at 60 deg to the C. A. Rock cot by numerous slickensidedfracs at 25 deg to 50 deg to the C. A. these often seamed with 1/4 inchpicrolite RtK'k m i t with a^**rfanf- magnfcilt*, *rinrr MAction* shrvw 2 ^disseminated po-py . Rock seamed with minor magnesite and witha few very thin threads of asbestos

44L 0 - end of hole.

Sample No.

— 12670

ard min

12 67112672

1267312674 12675

FOOTAGE

From

•9.TQ — e-•J** 7. w

wp*tfe-4*

383.1388. C

396.!42^. C 436. C

To

--i. J.

-pe-^y

38^388.

401.425. 44L

Width

9 ——— 4-V *I.

i — Ree

6 07 0.

5 - 5.5 2.a s.

CORE ASSAYS

-e ——

k cut \

q7

0-5 — —

0

vy j* fa v ———

EXPLORATION DEPARTMENT Mcintyre Porcupine Mines, LimitedProperty—.. Location.—.

AtSurveys

Dip Bearing

SAMPLE RECORD

DIAMOND DRILL LOGHole No. 904^73*4- Sheet No. .three.Length of Hole—.———.._—..—...—.———. —..—— ——.———...—— Date Started————....—....————————.CompletedCore Logged by———————.———————.......................—————.Date-——...--.—.....--———...... .... ———...——————————.....——.Elevation ——————.————.————..—————... Datum ........——....

Co-ordinates of Collar North....-...———————..--——————-.----..——————————East .-.————.........——.———————.....——... . . .——... ....

From To Description of Core

Sample No. from footage to width gold silrer copper

12670 319-0 - 323.0 4.0 trace 0.025 0.0412671 383-1 - 383.6 0.5 0.05 1267? 3#fl.o - 3f?s,7 0*7 0.04512673 396.5 - 401.5 5.0 0.0612674 ———— 424*0 - 425.5 —————————— 2*5 ————————————— 0.105 — 12675 436.0 -441.0 5.0 0.08

SLUDGE ASSAYS

Footage

zinc r

nil

tickel

0.30 *rfj0.35niJ^ 0.21

fv

,/^ *mz*-

Sample No.

/S- t?~ ,-

CORE ASSAYS

Footage

^•V-*-''-- ,~~f

Width

~~ ^s'tf ^".-

Au Ozs.

^~St^" S

Ag Ozs.

, —— T-S'f'"*"^.'

- ~

EXPProper) LocatioClaim Locatio

IXMLtv"

&TION DEPARTMENT ^ ^ __ _ f\. m m\Jf^ uJKr Tf*.m\. 1 ITIEI^ 1 -j^ /rc*T^WT' 1 i V^T5 TTIl ^B ^^^ B JJ^M J. if BT* MiJ

n..— — —. — — -— — — — — — — — — — — — —- — — — — — — — — — -~No. . ....................... ..... .n of Cot

At

e ............................................... . .......................Surveys

Dip Bearing

^JSVISH) SAI1PLE RBCX)RD


Sample No. from Footage to width gold silver copper zinc nick*

12670 319.0 323.0 4.0 tr 0.025 0.04 nil12671 383-1 383.6 0.5 0.06 nil 1967? 3&.0 2S8.7 0.7 0.045 nil12673 396.5 401.5 5.0 0.06 0.35

12675 436.0 441.0 5.0 0.08 0.21

r l E C E E

^E

Sample No.

iole No ,ength ol )ate Star rore Log: )ate ..elevation

tforth

DIAMOND DRILL LOG904-73-4 fonr

- . —. ....................... ............ ..... ...........Sheet No. ..................... -,-—Hole........ .... . ....... ........................ ....

•jfA hy ^^


]ast . ........... ........ ......... . . ........ . .. ... .. . ,. ... .. ... .

FOOTAGE

From ToWidth CORE ASSAYS

EXPLORATION DEPARTMENTAbitibi Option

Property Location CrawfortT , OhiJario.

Surveys..At——collar

.630.

Bearingazimuth o-—— -~ — -56-0— ~

Mcintyre Porcupine Mines, Limited DIAMOND DRILL LOGHole No. ?Ot-73-5 L. ........ Sheet No .Length of Hole *** fecfc

Date Started -....... ..CompletedKCore Logged by Date... y

——,1973.... ...same as

Elevation ...— — ..... .................. ........, .................. DatumCo-ordinates of Collar

Core stored at Schumacher warehouseNorth East -

From

"O"To Description of Core

casing - The drillers report that they intersected the following ove Q - 34 - clay

lot oejg-i exaa Lned ait yet

CORE ASSAYS

34-220 - sand, gravel and bouldery op to 7 foot thick. SeveralThe drillers report that they

220 - 250 - yenow coloured clay

320 .C 663.0250 - 320 - sand gravel and very smalldacite — a erer to locally green __ __ ________—————————————————""—— *--*——w——— —— w——*-* ~t^— ~w —————————~" — f "' ""^ (j™ -^——x^imr*.* **A "C

the CA. Rock mln with widely scattered grains of po, py, cpy* Rock

shearing or bedding is evident particularly in the sectionhighly sheared, some shear planes are slickenside end liaoniteto the CA. These tuff sections healed brecciation.

327.7330.6

- 0.7 ft.basic dyke at 35 o to the CA. Reck is dark grey in— 2J+ rt.ntvi-chlorlte at 45 o to the CA no vis niLn

333*7 ~ 20*0 ft.basic dyke first contact at 35 o to the CA lowerana aassive. Rock cut by scattered slickensided fracs usua

353.7 - O.S ft.qtg'-chlorite flrat contAct g*-HMf*rt, l^fr contact at 3J 370.0 - A6.0 ft .weak shear zone trending at a snail angle to the CA

thin film of407.0 - i inch qtz- at 90 o to the shearing adn tr or 409,0 - - - -- -- ^-nl inch tiLz. paralleling shearing here at 'y? o to tfte CA

- 1.0 ft.qtz-epidote at 40 o to the CA min with a few tiny563.0 - u.ii rt.qtz-epidote at 10 o to the CA 674.0 - 1.0 f t.section showing 3 inch in

gra: as of po-epr

683.0 - end of hole.

EXPLORATION DEPARTMENTProperty,.... ^

DIAMOND DRILL LOGPORCUPINE A4INKS LIMITED

Claim No Crawford Township, Ontario.Location of Core......._.....—....—,——._._. _._.....

Surveys Dip Bearing

Hole No. 5ytt-72r**. r ........ ....Sheet NoLength of Hole...—..—.:*^-?-~—f-:*?—-..-—.--—.——————...Date Started———.—Z?... Jt ...^b..iia.. js1..a.................. Completed

Core Logged by....Date-—......—.....—.

Atcollar 200 feet4~00 feet

.-..50. e......- *? ? 30-48 o

-P43-0.Elevation ..............,.........—...—......_......_.......... Datum

Co-ordinates of Collar70 ^

904-73-3

East^

^

From

•^0

185.0

353*0 389.6

/i35*0

*-

To

185 .C

353.0

389.6 435-0

660.0

i-

Description of Core

casing - drillers rctxsrt sniskag to 14 feet followed by clay to 150 feet then swas (iriren to IS 1? feet f'roE which point coring began. rhyodacite - a prey siassive relatively hard rock flecked with snail grains of

usually i inch square. Rock cut by a few chlorite healed seams, scattered open 19Q*3 — 6ifi ftipfction of c fowl, y rhRclite win tr iw. A central 0.1 ft*s*^ction222.0 - 0.1 ft.qtz at 60 o to the CA no vis nin

graphitic tuff - a black rashed looking rock usually bedded at 45 o to the CA.Tvlfi't4v* flllpH shoving f*cw* slickfrwriWing. ^ock Bdn tr to locally 10 prcpnt- co^Scattered open frae* Are partly plated with Hmnrrfte. Sock i*, ctrt. by wa-jy thre

— dacite - a light grey to locally dark grey coloured Bujgive reck aarked with B of qtz nsaic ones of which are tabled below. Rock min trace cube pyrite.445.0 - 0.3 ft .section cut 5y thre* i inch qtz veinlets at 45 6 to the CA 450.0 - 1 inch qtz at 45 o to the CA no vis min481.7 - 0.1 ft.qtz at 35 o to the CA adn tr py 429.5 - O.? ft.qlz At 2O o to the CA artn tr py534.2 - 1.9 ft.irreg (70i) qtz adn tr py

— 574*7 - 0*1 ft.qta at 35 o to the CA ne vis irfja ————————————————————— 594.5 - 10.5 ft.irreg (50*) qtz in irreg shaped znasses and in later 1 inch v

veins ^t ?^ o to the C!A .odC tain tP W attendant wall r^ock ciAit^Pi Al* — — - —— ^- -*.- A — y, n n ---^ .*is sojoewnat sneareo

635*2 - 1.1 ft.irreg qtz as above 641.5 - 1^.2 ft. Irreg qts *s* above

654.7 - balance of rock consists of flow contact material somewhat brecciatedof qtz tnese isually ain witb a trace or pyrite. Core badly broken.

Sample No.

FOOTAGE

From

md gravel and l

ntz and feldspalracs sho

* Rock nil Bedding

t pyrite ids and n12695

my qta f

1260612697

12951-12952 —

12Q5312954

md shear

* a bitbh a fr

t wi\.-n .s looap to ;

400.0LHod (

/,fi9.S534.2

594.5600.0

A/,1 .5644.7 649.7

sd at t

To

loulder

hie ma. of se i* ?Tai

illy CGr inch sinlet405.0jr.iyjj.dul

/,90.0536 JL

600.0605.0

6U.7 649.7654,7•O o tc

Width

s to b

terialrtcite

small itorte(squarea of q'5.0

0-51.9

5.55.0

3*25.0

the C

CORE ASSAYS

Bdrock

. Fockalters

Ryrtte- I. Kociand atte.

ik cut

0 n~~T

V-

0.00*

0,00,

0.0*0 . 'J e "

- n .. C

i. Roci

at 180

min wition.

cut b

feet.

th reai

f auaeisHsall toy cutx

by sea

cut b

btored

f a f ei

Casing

r cubc-

"ous grt clast

throat

f threa

pyrite

aphiteers .

9 ————

ds

—-1

-

EXPProper) LocatioClaim

Locatio

'L&lttv

AT10N DEPARTMENT ^^^.^J^^JL JLJLî JL JL JL VrJtZj

n — . . __ _ — ___ —

n of Cot

At

e... _ . .. __ .. _ .......... ............. ......................Surveys

Dip Bearing

——————

From

^—660.0

671.0

t—

To

671.0

609.0

——————————————————————————————————————————————— — - — - ————— — — - — — ——————————————

Description of Core

graphitic tuff - a fine grained black rock bedded at 60 o to the GA. Rock hi -hi;

r E E C E E

f E

Sample No.

r breccia,

tuff - a dark grey then grey highly altered rock bedded at i. 5 o to the GA. Rock! is felsilocally aggloroeritic wit* an eroded fragment of dense graphitic material noted In one pi threads and veinlets of otz.689.0 - ens of hole.

iole No. /ength oi )ate Star ôre Log: )ate ..Elevation

ôrth

DIAMOND DRILL LOC^....--?TT— ir."!!:?...-.------....--..,.............-. ..-Sheet No...— .......... .... ,.... — ...Hole........ ........ . .... ............... ............ ... ...... ...

;edby... . ............ ......^^,..


!ast ..... ............ .... ... .

FOOTAGE

From

;ed cal

s withace. R?

To

a few

a prou!ck mi n

Width

threa

Inenttr py

CORE ASSAYS

!s and

!lne ci•ite at

Teinle

ert cod is c

bs of t

itent*ut by j

itz.

Rock iL few

s

EXPLORATION DEPARTMENT*

Property——^bit-ibi -Qptioa-^AnoBaly-- 3QA-)-—--—-MCINTYREPORCUPINE MINES LIMITED

Claim No... Location of Core

AtSurveys

Dip Bearing

..c.O-llar......200 feet "400"feet"

"600""feetr

.^O...o..........-4? o 30' ~33T6"~~~

.043-0.

DIAMOND DRILL LOGHole No. ..90.4-73-6 ,.,.^ sheet No three

L f r^ , 688.0 feetLength of Hole ..Ju^.....27;..T973vDate Started...................................................... .....CompletedCore Logged by—.. Date___............—....Elevation J3^6...^........................ . . ............. Datum 904-73-3.


East


CORE SAMPLES

Sample No.

[2695

[2696[2697

[2951

T?Q5?

[2953

[2954

FOOTAGE

From

+00.0

+S9.5534.2

594.5

too.o341.5

i44.7

^/,9.7

To

405.0

490.0536.1

600.0

605.0644.7

649.7

654*7

Width

5.0

0.51.9

5.5

5.03.2

5.0

5.0

CORE ASSAYS

eoldNil

0.007Nil

0.0090.0070.008

0.007O.O08

silverNil

-

EXPLORATION DEPARTMENTPORCUPINE MINES LIMITED

DIAMOND DRILL LOGHole No....-.?.9^~?:?r7......———...,.-.......——.Slieet No.—L

Ix)cation........Lo.t,. 8^ .Cojric^Claim No. ,...~-.. ... _ ....... ____ ,. _ ..— . _ . __ ...... ....... — — _ -Location of Cote ,. ...Mine., C.pre Shacjc, , ^ , , . .....

Surveys At Dip Bearing ______

Length of Hole ^-501 .Q .f.eet.., .......... ........... .... ...Date Started... 11. Au^st .1973 ,.,... ........... ...Completed . .I8...Au.?Core Logged by..... W

"200'-5X30-

-50 deg. True North "Dip" "Te st" only

INPUT ANOMALY NO. 8

Elevation

JJ/U SOUTH7/7/7 WBDT - if// ————-

Surface . DatumCo-ordinates of Collar

28 and 70

From

0.0

110.02

TI5-5

T22.5

133.0

163.0

To

no

115. 5

T??^

1^.0

163. C

263.0

Description of Core

Casing

Andesite, greenish - grey, massive, secondary quartz in fractures and as

grains in wall rock.

Fault. 7.nne. Brown., si i ppery mud f fault gouge) on slip surfaces andfractures, brecciation in places. 10^ lost core. Attitude doubtful

———— because- of lost ooro and varied attitude of fractureo. — Occasional — —— —piece of barren milky quartz up to ^" in width.

Andesite, slightly ruggy in places, occasional fracture annealed withbarren, glassy quartz.

Fault zone. Broken^ brown, oxidized pieces of core^ only 20# overallrecovery. At 133.0, I" barren milky quartz. The hole is running almost parallel tn some of the fractures.

Andesite

Sample No.

FOOTAGE

From ToWidth COKE ASSAYS

EXPLORATION DEPARTMENTProperty.—.Abitibi--Option- PORCUPINE MINES LIMITED

DIAMOND DRILL LOGHole No. ....? OZt;-?3-7. ...... ....... ..... ....... Sheet No. A.

Location._...___. Claim No. —————. Location of Core.

AtSurveys

Dip Bearing

Length ofDate Started.— ————— ——-..————— .———CompletedCore Logged by—————..———.—.—————————......Date .. ——— ——— —— — . ........ ...— — .. ........ . .Elevation ...— — ........ ——— ...... ——— — . __ — .... . Datum . ...

Co-ordinates of Collar North ..........—— — ......— —— . .. . .... . -.— ————— .......East . —— - .——————— .... .. .———— —— —— .


163.0 - 181 .0 Up to 5^ VURS. i" barren, vuggy milky quartz at175 '5, 85 deg. to core axis. Core has numerous fractures at various

——————— angles . —————————————————————————————————————————————————

181. 0 - 200.0 Approximately 5# vugs, numerous fractures, somefine, barren quart z -carbonate stringers or threads up to i". Occasiona trace pyrrhotite, pyrite and rare speck chalcopyrite.

200.0 - 214.0 less fractured than preceeding

21/1.0 - 223.0 somewhat brecciated and finer grained than preceed-ingedge of flow? IOJ& barren, irregular quart z -carbonate stringers and

——————— carbonate throughput ——————————————————————————————————————

223.0 - 239.0 10^ quartz-carbonate threads in places. At 236.2i" U.0% pyrrhotite band at 60 deg. to core axis in |" quartz-carbonate stringer .

239*0 - 263.3 more massive, less altered than preceeding,carbonatized throughout but very few distinct carbonate tnreads. Occasional epidote, rare trace pyrrhotite.

Sample No.

1

FOOTAGE


EXPLORATION DEPARTMENTProperty.——-Abit-ibdL-Qpt ion...

DIAMOND DRILL LOGPORCUPINE MINES LIMITED

Location—————.—Claim No. _,._—... Location of Core.

AtSurveys

Dip Bearing

Hole No..

Length of Hole——..——....-..........................-..—...——.—..Date Started———...—.__———_—._———........CompletedCore Logged by———————————.—————————.Date————————.-.....-....—————————-....—....-..Elevation ————.................—.......————.......,... Datum

Co-ordinates of Collar North .-...———.....————..————.————..————.........East ———.....—.........,—..............,——..—................———.

Sheet No. ...3................

From

263.3

26S.O

To

265.0

501.0

Description of Core

Veins. Two - 13", 2" milky quartz-carbonate veins at 50 deg., 60 deg.——————— to core oxio, barren except for a. few fine hairs of rutile or tourmalir

Rest is andesite, very little altered

Andesite265.0 - 280.0 traces pyrrhotite and rare chalcopyrite280.0 - 300.0 coarser grained in places than proceeding, sualleryd carbonates as threads and blebs.300.0 - 400.0 fairly massive, accasional slight schistosity or banding at 80 deg. to core axis, carbonatized throughout.400.0 - 426.0 15^ quartz-carbonate stringers at 75 deg - 80 deg to

throughout .426.0 - 440.0 highly^'Car'btrtiatlzed throughout, slight schistosity at 70 deg to 80 deg to core axis440.0 - 460.0 moderate schistosity at 75 deg to 80 deg to core axis, carbonatized throughout. A few threads along schistosity containingpyrrhotite and traces chalcopyrite. 5" barren quartz-carbonate vein

460.0 - 480.0 highly carbonatized, chloritic, traces pyrrhotite,rdrc cnculCupyi i oC ciiong sllgiit schistosity dt Su uyg Lo Cux~ts GLX~LS. 480.0 - 501.0 slight schistosity, carbonatized throughout, chloritic,Traces pyrrhotite, rare chalcopyrite along slight schistosity at 80 deg. to core axis, 10/5 quartz-carbonate stringers.

Sample No.

te-j —————

FOOTAGE


EXPLORATION DEPARTMENTAbitibi Option

DIAMOND DRILL LOGProperty- Location..——.-....-...Claim No. __.—— Location of Core

At

PORCUPINE MINKS LIMITED

Surveys Dip

Hole No. ....904-73.-7-——-—-——-————-Sheet No.~Length of Hole,....—...._—————_......_.............—__..—....Date Started....—-—-———————————————CompletedCore Logged by———~...——........———~—...————————.Date ....... ........ .—.-...—— -. ———————

Bearing Elevation —.— —...——....—..— Datum Co-ordinates of Collar

North East -

From To

501.0

Description of Core

End of hole

Note: This is an interesting hole. There is much calcium carbonate——————— and chlorite in places and minor amounts of pyrrhotite, pyrite and rart

chalcopyrite occur as platings along schistosity planes. The hole didnot go through the zone of alteration but did apparently check the extension of the two surface conductors. Consideration may be givento drilling a second hole, possibly the additional one recommended by Pnttrr-inn and Grant at a later date. How**vT 4 morp ppophys-ios shouldbe done on the extension at the condustor to the East before adecision is made.

Sample No.

FOOTAGE


EXPLORATION DEPARTMENT JVL^INTYRE DIAMOND DRILL LOG

^^—.^

Propeti Locario Claim Locatio

ty — --..AQltxba...Qp!til.OJX— — —. —. — — — — — — — — — — — PORCUPINE MINES LIMITEDn Lot 8, Con. 5 f Crawford TownshipNo.n of Cot

At

e ~- Schumac&er— Warehouse— — — ——Surveys

Dip Bearing0 -50 o 360 o azimuth200 ~^4"9~ o400 -44 o


SAMPLE RECORD

I l t C I E

7/t

Sample No.

120-57

12958

lole No. -ength oi )ate Star 3ore Log )ate AUilevation

W/th S

904-73-7-.-------————— -Sheet No.. -5-— — ——Hole....5PI..O..f eet............................................. . . ...^

ted - ...^^?L?5*..I973.. .............Completed.^.?.- ..?.?......~A i.r W . H . Thor oe g^'gust 19, 1973 ^

SurfaceCo-ordinates of Co

OUTH 2870

.. Datum liar

r

FOOTAGE

From

TT •i.';263.3

To

T22.5

265.0

Width

7.01.7

CORE ASSAYSGOLD

0.005

0.005

EXPL DEPARTMENTProperty Crawford Township* Ontario

taim----^^^^--js^--Qf-y^--^---Q lgjjc^^^"^--Claim No.——————gcht———,—— ————,———— Location of Core........

]VLCINTYREPORCUPINE MINES LIMITED

DIAMOND DRILL LOG9O4— 73*"8 one

11 AtcollarSurveys ™fc-50 o Bea

o a: th-.o——.o-30 o

.6.00 feet .........- 42- o- --.... BOO feet - 37 o 30 *

Hole No. Length of Date Started— J1??11?* ^4/73 Completed .S*pt *7ri ,, A.SkreckyCore Logged by——————————:.Date S®^611^ 3JL*1?73

Elevation .. . . .. ..... ...——— Datum . ?9^7?.7?..Co-ordinates of Collar

South

From To Description of Core Sample No.

FOOTAGE

From ToWidth COKE ASSAYS

0.0 -84*0-

84.0165.0

casing - we have no report on the overburden fraction intersected oy this drill hole.~ fine grained rock showing local

C A. Rock ain with trace fine po at times associated with grains of epy. Rock cot by scatteredup to \ inch wide these usually trend at 60 o to the CA100.1 — 1.5 ft,.breccia v-nn* *t "W) M t*

brecciation (c ilorit* threat s and

or Jcelnlej^S-DiL

si earlrfcz

.rig) iz-and

at 60 jqtz-Cjirb.

o the

165.0

114*0 - 2.0 ft.breecia zone at 30 o to the CA healed with 252 qtx-carb tr po -162^ - - -

287.0 dacite - a green grey aassive fine grained relatively hard rock showing a general chlorite he; tied bicpy grains and is eat by scattered 201,0 - 0.3 ft .splash of qfrzOcarb

ecciatLon. Rock gjj with a- po few,,and reinlets of qtz-carb

203.0 o 3.5 ft .chloritic breccia healed with irreg qtz-carb as sinuous veinlet s paralleling tiie CA"y\f\ C\ — T -*7 *H- Kl^^-rr^" *-— ~^ nmm __________________________________________________________________________—HMMH^— Mfw^ M. w .^P^T^^WWJUJl ru rT~^TwnTT^^~ —'————————™———'—""""""^—"—~~~~———"——~~~~—~~"~~~~~~~—————————————— —

213*7 - 3*0 ft.breccia as aboveection min 1 po-cpy

of lighter coloured harder rock.2.0 ft.section snows 3 inch in diameter txaadb like aaises

243.6 - balance of rock shows a general brecciation which is seamed with 2O? qjtz-carb vsinletii the i ain onts of the CA or almst Darmllel the CA. "Sock h l^hlv ; 60 o

283*0 - 4.0 ft.acicidic rock showing pepper like limonite staining. Sectionthe CA

287.0 291.3 wit i

291.3 323.0

graphitic breccia zone - section consists of brecciated rhyoldacite healedIpdcr contact glHIUIHl. The r-hyodAC^t^* i.i Highly ffftyj[gj[^^ Cl0aTag^ Of wfajgh ~IJ3py trace cpy along with a few grains of sph. Rock cut by a few irregular threa isrhyodacite - a relatively hard grey rock largely altered to sericite whicht.Mn fllma nf py. Rpek ent. by many gr^phjâ plat*M ff^^pff t-**** "Îff "*1*S Of îrregular. Rock is locally aggloaneritic and is min with about l percent py.322.8

323.0 427.0 tuff-a green grey relatively hard highly altered and recrystallized rock si sericitized where rosettes are common qnd where a yg}lawj.ih Îng** ^** b^gn These are due to local brecciation which is chlorite

EXPLORATION DEPARTMENT DIAMOND DRILL LOG

-

-

LocatioClaim Locatio

No.n of Cot

At

e ... _ _ —— . _ .. _ .... . - . . ... ...— .Surveys

Dip Bearing

Fromm*

427.0

^58.0™

i.oe n•*7O *V —

684*0

To

458.0

498.0

JJ*Lf\ "vOK^BV

713*8

Description of Core

l E C E E

P E

Sample No.

348.5 -3*6 ft. breccia healed with black chloritic material. Last 0*5 ft .ndn tt- po-cpy354.0 -0.5 f t .breccia healed with 40?5 irl-eg qtz-Carb | 359*7 - 0.5 ft.qtz-carb at 70 o to the CA n6 vis min383*7 - 0.2 ft.qtz at 50 o to the CA ndn with one grain of sph

39O.5 - 4*8 ft .basic dyke at 45 o to the CA. A nassive black coloured very fin

398.3 - balance of rock generally chloritic and markedly sheared at 50 o to thgraphitic tuff - rock sectioned as follows

diameter nodules and as i inch streaks paralleling the b)eddin

443*7 - 458.0 - aggloneritic tuff a green to locally black rock where graphitQ rcccist viOH * IvOCn Mift î In jLO/v D^"~1D9r filff fll fi jul9 d L ^ Hflfflt JntffctJbont *

agglonerate - a green grey hard rock showing abundant lighter coloured ayigntgrweakly brecciated and chloriti zed ndn with 155 to locally 3^ po-py rare grains 458.O - 0,4 ft. black bftsrfe dyke flt 6O o to the C*460.3 - 1.9 ft. dyke as above

abundant eyes of sugary qtz up to 1/8 inch in diameter. Scattered chlorite rim504.6 " 10.0 f t .section streaked with very irregular sinuous 0.1 ft.dyKelets o

to the CA553*4 - 0*3 ft.qtz at 45 o to the CA no vis ndn574 1- 9 ** 4*8 M-r -Hfla|c A y If a at ^0 O t** t"-*1** 0^594594*9 - 0.1 ft. seam heavy fine py at 75 o to the CA

— rhyolite breccia - sane rock aa previous - showing heavy brecciation healed wi later weakly sheated at 45 o to the CA. The breccia Is locally healed with a 1dissemination and as i inch disks paralleling the shearing. The po is at times

710.0 - 3*8 ft .section ndn tr very fine sph

iB^d*iAmz—Z*•^^ — **B grained

B CA. Roc

with abog .Contact

B is abun

to subancpy

,.t i . •t.* i —^toC 1. 1.A.P

faed veadef which p

.ength oi )ate Star rore Log )ate.. —Elevation

•forth

y***— r^— o- -- -— -- - ""^' x,,^,^— — —— -

ted— ————— —————— ————Completed — ——— — . —— — —gedby— -—— . ^p......

Co-ordinates of Co. Datum

liar

ast ......— —— —— —— — .... — ——— . ...— —— —— — — —— —— .—— ...——— ...—— .

FOOTAGE

From

Bar fjjrock :

c ndn i

ttt *I O4*with ]

dant tt

eolar i

ni^ li -lil |T^| i

Les an)rcelad

To

*tt\. gqg

locked

dth tr

u'eviot

inningk

,T J — T- UL IS f* finen like

Lh dark gi-ewu XJLUO gra iter rhyojLite. ôck adassociated witl

aa at 70 b to tlt tracete CA

Width

tacV4 with

PO

tt. t*i njis sect

the aa

to of

resent dtwithrhyol

CORE ASSAYS

m f*fmflH\9 Um.ÔfV

:hlori1

di.ia t Ion is

,rix od

icie ct

:alclt*it* trc

ined -c:|LBPC3.w D 1 ^ po Iocscpy

lated-- ,e and

sirfn^Mgradat

' a ver

gnposit

i. Bockmding

i miner Uy 10

ndn tr

rtp psLonal.

T irre,

Ion. Ri

i t i.- tujLerxvndn t]

at a si

alizat. t po ai

po-py

4 ITV-V

Sectio

^CLar

*ck is

id by j " po-FStall at

ion. Bc i a fin

n

airly

gl*

ck ——e

EXPLpRAtlON DEPARTMENT DIAMOND DRILL LOGProperty.-.._——— Location.——————.Claim No.————.. Location of Core.

At

PORCUPINE MINES LIMITEDthree

Surveys Dip Bearing

90^.73-8Hole No. ....^.'L^. -...,... ...........Sheet No..Length of Hole.—.—...—._——.. —_—,._...._........._..........Date Started————————.—..—.......—.........Completed .Core Logged by——————.———.—.——.....——.—. ——...Date .. . .. —....... ..... . ...Elevation .......................———————_—.......... Datum

Co-ordinates of Collar North.........———.......———............—........—— .———..——...—.East ...——................, ————.... —......—...........————... .——

From

713.6

819-0

To

819.0

912.0

Description of Core

rhyolite - a hard grey to greenish grey fine grained rook peppered with smallitic and brecciated where an increase in chloritization is noted. Rock ndn wit

726.2 -0.8 ft .section as abore

quartz diorite a hard green coloured fine to medina grained eren textured rotHock is somewhat epidotized adn with }ocal trace po-pgr-cpy. Rock cut by a few feet is cut by many slick-flnsidad fracs and is badly brokim-ap*- Two fracs.are j

821.5 - 0.1 ft.qtz-chlorite at 60 o to the GA no Tis nin623.1 "4.5 ft .section ctrt by rery irreg qtz*earb reinlets trending at many anj 902.8 - 4*5 ft.weakly sheared zone locally adn with 5^ disseminated po trace ei912.0 - end or hole.

Sample No.

patches th trace i. phlftTH'H—— V***W*. Jk WJ

k showingthreads t raphite i

les to tty

FOOTAGE

From

•f brieo-py-c o rnel

a unind Y*i lated.— fi A ——O V/i

To

it gre jy. Lau

tom d;diets (

Width

SI Chic [t 6.0bVl-l MUb^

.B'semlrif qtz

CORE ASSAYS

rite. f t. sheT^r ^*-*^P*^ *J.L V.

ation iand qt

tock li pfs roptCJIHB—Hm-i VVUX —— UL7

^r tinsc-carb

t local7 mate

qtz 6First

ly amt]rial at

yes.5.0

loner -Lxed

EXPLORATION DEPARTMENT DIAMOND DRILL LOGLocation Crawford Township, Ontariol /-i - ~'~~'''''''"~Claim No

PORCUPINE MINES LIMITED one.

Location of Core.

At

Scliumacner" warehouse

BearingSurveys

Dipcollar"200"feet" J.60...Q-.azimuth

- 48 o 30•- ~48~b"

Hole No..... ?0A-~73"9T .....,.,,. Sheet No.. ,-. , 644.0 feet

Length of Hole..—..........—........................................................Date Started ...September 12,1973 CompletedCore Logged by September 20,1973 A.Skrecky Date September'24,1973j—---""~--~-™~~~~

Elevation .........Pl^S J-P;..f eet..................... . Datum 904-73-8.Co-ordinates of Collar

ck South 450-West 1950

From

0•cw.w

105.0

n5.o

255.U

To

20. C105 *C

•Mr; f]

255.0

Zfff.B

Description of Core

casing - drillers report clay to bedrock

Sample No.

rhyolltic agglomerate - a very hard fine grained massive blue grey to locally kreen tin Non agglomeritic sections show abundant qtz eyes and a general brecciation heated withcoloured fragments up to 1 inch in diameter. The fragmental rock exhibits weak

— evident. Rnck is min with trace to locally 10 porcont po in thin ooamo, smallassociated with grains of cpy. A few 1/8 inch seams of chlorite cut the rock a

5 3 *v -^ 1.0 ft.glftjt to Cjreaili Culuujred felsite at 75 O to the GA56.7 - 0.6 f t .as above at 70 o to the CA86.7 - g incn qtz-chlorite at 45 o to the CA 94.6 - 0.1 ft .qtz at 30 o to the CA no vis min97.7 -1.4 f t .highly chloritized rhyolite

—— 99.5 - 0.5 f t. grey felsite dyke at 80 o to the CA ndn tr-po —————————————104.0 - 0.1 ft .qtz-sericite vein at 20 o to the CA min tr cpy

quartz diorite " a flue to medium grained even textured massive rock showing qt: gradational. Rock is very hard at first gradually becoming soft at 115.0 where ilui?.0 - u.j it. patch of light dissemination po-cpy peridotite - a dark green to near frlack soft massive basic -rnck inp.giiy min witlserpentinized sectuons. First half shows many ribbons of magnesite up to 1 inch Rock ia min with rare tinv rraine of nv nnd iiri-fch trmcp f-in*. nnn nu jn*t i ^ r^n. TJ.-^•""•• 1 "J-"" i d* w VJ.1JJ b^ 1*1.110 w J. py cuiu WJLUII ui Qt\*ti JLXUe HOU daguc i* J.vi pO . HOIground. Last 3*0 feet badly broken up and ground.237.0 - lLc.7 f t. section min with 5^ to locally 20^ disseminated non magnetic

po along with a few grains of cpyrhyolitic agglomerate - same rock as in section 20.0 to 105.0 feet. Rock is Iocssections are tabled below.256.8 -3.2 ft. section of spherulitic rhyolite min 8# dissem po tr sph-cpy 260.0 - 2.7 ft.broooia min 20# pe 5# py trace cpy&ph ——————————————————262.7 -3.2 ft .brecciated spherulitic rhyolite min 15# po 2^ *py 1^ sph tr cpy

disseminated and healing a weak breccia

shearingirregular ; a small

i phenocr; iccessory

wide. Loi•K OUl/ uy1297712978 12979lly sphei

12980'"" 12981

FOOTAGE

From

;ed rocn-inor jat 45-patche angle

•sts ir qtz is

Ey^Q^I^'^f

rer ha3scat t e237.0241.0 2/^.0ulitic

260.0 262.7

To

k the o. Theo to ts arid to the

a dio: not e

. Rookf of t:red si 241.0245.0 249.7min t:

262. 7 Z65.9

Width

latter-AgglOlhe CA -ias a d:CA.

rite 3J irident ,

io hi| le rocl.ckens:

4.04.0 4.7

- te l.

2.7 3.2

CORE ASSAYS

cSioLO S'iUV4K'C0|9^*lvC 2/ve- MiCtCff

colour aeratertiere sLssemir

ke roc

•hly al is hi

sed fr .0o*f.c****''

callj

.fv*w*fft-..:'- y-''---

due t showsome eh.at ion.

k. Botl

tered -\ ghly s(acs. Ix

JC^ pc

***A.4fr4-

a. ^^5"

3 accei tbundaiLoriti;The pt

i contc

n.th tc srpent5)wer cc &.07~.*r&-AJL-, The n

0 .SO 0*0"?*y. ^^5

jsory cit ligh ;ation\ is lo

cts ar

ilCOsdnized.ntact :

ain sxi

^•^e.- v -,~

hloritU^—i.

iscally

3

3Q3d ———

LS*?.xVC?. X4fo.*oLphide

~.4-

3

EXPLORATION DEPARTMENTProperty.—————— Location.______. Claim No..__........Location of Core.

At


Surveys Dip Bearing

DIAMOND DRILL LOCHole No.... 904-73-?.,, .................. Sheet No....twoLength of Hole...———.—.—.—..—......—..............——..—............Date Started—-———.———-...————.-—-—.—.——Completed .Core Logged by—...——————.————............—...........———...Date .- ........... ........ . . ...........................—Elevation ....————....—.——.——————————,. Datum . .......

Co-ordinates of Collar North..--————.-.....-.——..—————— .,... ,. .. . .East .——————.....-—————..............—..—...—...——......—.....

From

287.8

322.0

359.0

381.8

To

322.0

359.0

381.8

644.0

Description of Core

265.9 — 21.5 f t .section min 10/5 to locally 20^ po disseminated and in streaks ismall, splashes of cpy

dacitic flow breccia - a grey moderately hard rock finely fragmented and seamecpart graphitic. The groundmass as well as some of the fragments are min with f d

tuff - an alternately grey and black fine grained rock the black colour being clabled below. Souk is~ bedded at 45 o to 55 o to the CA". 'Light coloured phases i rare grains of cpy. The graphitic rock is min with 5# to locally 20# po as thiiin diameter (some of which are partly rimmed with a thin film of cpy) and as dj grains and is cut by scattered graphite plated frans^322.9 -2.1 f t. graphitic tuff 325.3 -0.2 ft.qta at 45 o to tho GA no vio min ——————————————————————329.8 -0.1 f t .seam of chlorite-po at 75 o to the GA334*7 - 10.7 f t •graphitic tuff ————— - ————————————————————————— 345.4 - 2.7 ft. section min with 80^ py (marcasite) - po in a felsic to graphs

nodules up to 2 inches in diameter at times rimmed with a 2 inch layerwide streaks trending at 60 o to the GA. Section m-^n w^th t** cpy assQCwith the po. Section also min tr sph

Sample No.

t 45 o tc

with bisnely diss

ue to abxf the roc

. seams pisks up tc

12982 tic tuffof po. Tt 1?0*3

-nWdacitio flow breccia —— ao in ooetion 287*8 to 322*0 feet* Rock min 2# to locally O.W./P ^ i thick trending at 50 o to the GA. Rock min with a few grains of cpy j370*0 — trace sph 377.0 - 4.8 ft.shear zone at 65 o to the GA min 3QJ6 po tr cpy few grains sphquartz diorite - a massive fine grained grading to a medium grained pale green Hole 0,04.— 73**^* OoTrt-^^t- with pi***v~Loi|is faction gToXTrvit Rock l""smj' min trace po-387.0 - J inch shear at 40 o to the GA min with heavy po light cpy"3 Aft .16 — J- ini-h -m-T-tr 4*rr*v tn^am m frra — srl — 3-C)--n +/-1 +V.C. PA .—— -. . ......

412.3 - 0.4 ft.qtz-chlorite at 35 o to the GA min tr po4^1.7 - 1 inch ankerite vein at 25 o to the GA 426.0 -0.6 ft.shear at 40 o to the GA426.6 - 0.1 ft.qtz at 60 o to the GA min tr cpy

even text cpy- — —

FOOTAGE

From

the C

ck careminat

indantk are j-allel

4 inc

341.7 matrixe po o 34.5.4

finely

ured r

To

A. The

bonaceied po i

graphrimin wi Lng thi thid

345^. The tc cur s 348.1

sck six

Width

po is

*us locfhich j

,e the;h up t j beddi:. Sec-l

3.7larcasJ'inely

2.7

dlar t

CORE ASSAYS

/Ju X?*? Cu~ 2*7 Afo'

at tim

king mIso oc

main so 5# v ngj noion m±

0-033te is :dissem &.&S3

CU1U JU

o the :

ss assc

iteriaJ:urs ir

3ctions3ry I'ir iules ili with

XW'4~in fin*.nated0^2

-L SCcUUC

*ock a1

^ciated

whicht patch

i of whte po aip to iscatte

0-07iljr layand ir0.0?

i Up bo

, the b

with

is ines up

ich* arnd wit inch

red cp;

ered1 inc

1 JLtiol

ottom <

X}

si

r

•r'**

l

i

)f

EXPLORATION DEPARTMENTProperty————_. Location——————Claim No. ————. Location of Core,

At

PORCtTPINB MINES XJUMITED

Surveys Dip Bearing

DIAMOND DRILL LOGHole No......904-73-9-————————.——..Sheet No.-thrjLength of Hole.__........_——.————._,_......—._._..,___.Date Started....—.—————..————....————.Completed .—Core Logged by—————————————....—...———————...Date-...---...-....-.-...---———————...—-....—————————.Elevation .———...—....-——....—.————————— Datum

Co-ordinates of Collar North......-..——-....-...—..-----.——--—-.-----.--......——————.East ———————————————————...........—— —....——


450*0 -6.0 f t .weak shear -breccia zone at 40 * to the GA min tr po-cpy474*4 - O O rt .qtz-epidote at 40 o to the CA 535.0 - 0.1 ft. shear at 15 o to the CA min tr Do-cpy554.6 - 0.1 f t. qtz-epidote at 45 o to the CA 563.5 - 0.5 ft .qta-ohlorite at 15 o to the GA —————————————————————————594.0 - 0.5 ft.qtz-carb at 40 o to the CA.644.0 - ene of hole.

Sample No.

FOOTAGE


EXPLORATION DEPARTMENT DIAMOND DRILL LOGLocation North *** *** ^* Cancession 4,

^awTord'TownsHip," "Ontario."PORCUPINE MINES UMITED .0 feet Sheet No. .on.e.

ri - MClaim No Location of Core

At

A.Surveys

Dip Bearingcollar 200~f eet j

"feetvertical

Hole No,Length of Hole..Date Started ......SeP^.f.r...20,l?.73. Completed Sept.28.

Core Logged by- Date.........Elevation .. ..same as. . . . . . . Datum 9Q4-73-..-9

Co-ordinates of CollarSouth....................71QL.M......................... .. .. . ..

From

0— 30.0

85.5

138.3

3?3.0

332.0

To

30.085.5

138.3

323.0

-332 .0

366.0

Description of Core

casingdacite - a grey to faintly green coloured relatively hard fine grained highly a! showing a mixture of dark and light coloured fragments. Hock is rain with tt to "treneing at a small angle to the GA. The po is at times associated with blebs c at various angles to the GA. Rock is min also with ocattorod grains of sph. ———48.0 - 2 slickensided fracs at 5o to CA slickensiding trenes at 45 o to the GAr*-**- — u.^ it. section seamed wo-tn i. inun velnlets 01 po at 20 o to the CA.

The po is in places associated with 1/8 inch veinlets of cpy. Two suchveinlets trend at 85 o to the CA

rhyolite breccia - a grey to cream coloured very hard rock showing ii*tense brecclization.The fragments in the first half of the rock are rounded showing a rim c

streaked with some cpy. Scattered short sections show weak sph mineralization.

dacite - as in section 30.0 to 85.5 feet. Rock i.* highly brecciated min tr to 1scattered ragged qtz veinlets at 30 o and 80 o to the CA. Rock weakly chloritizsulphide zone - rock consists cf dacite AS in previous section which is very hi of po trending at a small angle to the CA. Section contains 35# po partlyfinely disseminated in the rock .Rock also min trace cpy-sph dacite - as in section 138.3 to 323.0 f eet. Rock is Tnr.aliy ^gglom^ritic min witaltered. There is a 0.1 ft.veinlet of qtz at 357.2 feet trending at 75 o to the

Sample No.

.tered ro(oeally ?')f cpy wh:

JL^VVY 1299812999

•iation ttf high a"13000 — 1300113002

12989 1300313004±3005 —— 1300613007 Him14102

oeolljr 1Ceel. arid highly brec 14103

h tr to 1CA.

FOOTAGE

From

sk sect# pn aeh als

72.2 76.380.6

e matr ter at i

85.5 90.093.3 96.897.9

105.0110.0

To

ions o: s a f iio occui

76.3 80.6

^ 85.5

on. Fri90.0 93.396.8 97.9

105.0iio.o115.0

115*0 LltS*4.118.4 123.4123.4 128.4 128 J* 133.4133.4 b8.3 SJ-po-b— - - JShly aciated 327.0

30 ally

.au e uj

.tered ,healec 332.0

10# pc

Width

' whici le diss-s alor

4.1 4.34.9

rfll rth r*-* AT* B T V

igments4.5 3.33.5i.i7.1i op. w5.0J*k 5.05.0 5.04.97~-few~

with 5.0

-few--g

CORE ASSAYSgold silver copper zinc nick

are h •eminatg thin

nil nilnil

j~Li~t ga T LI t vZ13JL9w

in thsilnilnil

sent t.i0.010 nilnilnilnilnilisliU*rvt.

^rajjis

lumeroTK^tb.

rains t

Lghly 1 ion ancfracti

nil nilnil

a tf\f---fa* y \Jj, Ut

2 lowe:nil nilnil

t T^roi0.036111 * nilnil nilnilW*V-ItfiL.

sph. f

is inct•/vL.

ip^-t.pi]

)reccial -. -. Tt as J.ires tr

0.12 0.170.12

!avy po - half

O.T3 0.070.17 to 5-" s "0.500.18 0.210.23 0.260.216.09O.fO

.ock la

thick0.01

. Ruck

ted inch siending

miner; are

r\ n/i-renil

tr trtr

cut b}

seams

highly

?effis —

i

/•oanil

Af II.

y*cu

EXPLORATION DEPARTMENT DIAMOND DRILL LOGProperty—————.Location——————Claim No................Location of Core.

At

IKJRCUPINE MINES IJUMITKD

Surveys Dip Bearing

Length of Hole- ... — ——— — ——— ... . —— ——— ... . ...——— — ....Date Started— ————— ————— ——-—— ——.-...—.Completed .Core Logged by———.-.————.. ..— — — — — — — —— ——Date-.——————————..———————.———..—Elevation ..... .. ..—— ... ..——— ...—— —— — — — ... Datum

Co-ordinates of Collar North...————. ... . . . .East —— — ......——— — —— — —— ...— — . ...——— —— ——

From

366.0

413.2

428.3

To

413.2

428.3

533.0

Description of Core

agglomerate - a dark grey soft rock showing many fragments which vary considerthese are typically sharp edged disks oriented at a small angle to the GA. Sev fragments indicating^ a complex depositional mode. Other frags are rounded, ligfragments consist of massive po. Rock is min with 2^ po finely disseminated an

— also min with a few grains of opy and sph. Rook out by scattered \ inch qta-casulphide zone - an acidic highly altered agglomerate showing fine bright green35^ po as a fine dissemination and in Inch streaks trending at a small angle t sections are min with finely disseminated sph.

dacite - as in section 332.0 to 366.0 feet. Rock is highly brecciated locally ,grades locally to a rhyolite. Rock min tr to locally 10# po as a fine dissemin CA. Rock also min with trace cpy - few grains of sph.433.0 -0.1 ft.qtz at 45 o to the CA 457 .ft -* 0.1 ft.qtz at 90 o to the CA480.0 - balance of rock is highly altered locally s sheared at 20 o to the CA. A

— patches of fuszy spots. ————————————————————————————————————————— 533.0 - end of hole.

Sample No.

ably in csral pale it grey i:i in thin"b veinle1 fuschite

•3 the CA. 1410414105 1/11061410712990 —— igglomekiition and

.teration

FOOTAGE

From

xmposilgreen

i coloistreal

/s wfaic and aHock j 413.2414.4 417.2420.84i^.U ;ic wh*in a J

indue

To

ion. CfragmeT and;s tren'h para variabs nan 41A.4417.2 420^-422.042S.3 re aciew inc

es the

Width

arbona*nts sh of anling aIlel a Le sulwith t; 1.22.8o L 3*O ——

1.2-613—i fragili wide

develt

CORE ASSAYSgold silver copper zinc nickt

;eous i?w sma3 ic id cc, 20 oweak s Jhide clin sti

Wlt.MV*-

uvk.

WlU

.003 j are cstreak

ipment

ragmenler ea mposit.to thehearJLrij ontenteaks o

^*

^y,*ii^0.036ommon.s tren

of ser:

bs are"bonaci ion. ACA. S*

g al 2( . Rockf cpy .i o.i4O.iT. o t ^O.M0.20 Rock :ling a1

tcite {

commonsous fewsction) o to min wiShortr*\\-

nil .tself, 20 o

nd szna

Bft ——— th

0.1D

to th

LL

EXPLORATION DEPARTMENTProperty Abitibi Option (Anomaly 25) . """"3x)t""r, '^6nc'4is'sI6n''^'''CYa^ford'lLocation..Claim No...... ....................................— ...— —— ,— —Location of Core ....??.hu^cher Warehouse

Surveys At Dip ________ Bearing

Township, Ontario. POR.CUPINK MINES

DIAMOND DRILL LOGHole No. ....--9.Pjfer73-!S-----.-.-............ Sheet No. ...one........Length of Hole ........1P36.0 feet

Date Started... Core Logged byDate November 9A973

collar - 55 o 345 9 azimuth. "200 "feet ""~~"-"52"o"~"~""

Elevation ........^.^ a^ .... .. . .... .... .... .... ........ Datum 904-73-11Co-ordinates of Collar

800 feet - 44 1000 feet - -^

From

046,0

181.5

207.5

309-5

3/1 1.0519 .6

583.0

To

46.0101.5

207.5

309.5

341.0

519-6583.0

605.0

Description of Core

casing - drillers report clay to bedrock on which a small boulder of pink granddacite - a green grey hard massive rock cut by a few threads 'of "calcite 67.0 - 1 inch qtz-carb at 25 o to the GA min tr po67.5 - 2.0 ft .qtz-carb ppppfcjs at 35 o to the CA 69.5 - 6.5 f t .f low contact maternal76.0 -5.3 f t .porphyry at 40 o to the CA rock is very hard dark grey in colour

— 7^3 —— balance of rock highly brecciated frags feealed with a black hard materl pillow lava - a light coloured very fine grained grained hard rock showing pillis agglomeritic . dacite as in section 46.0 to 181.5 feet. Rock is locally amygdaloidal min tr pc267*7 - 1 inch qtz-chlorite at 15 o to the CA no vis min272.5 — 2 inch q-f-,9:— carb chlorite as ahov**276.4 -2.3 ft.irreg (30#) qtz carb no vis min 286.0 —— 2*0 ftichcrty tuff bedded at 35 o to the CA ————————————————————tuff - a grey to near black cherty rock thinly bedded at 50 o to the CA Rockcontains scattered pea sized sherds of black carbonaceous material. Rock min tr 331*3 -0.1 f t .bed po showing tr cpy332.7 - 2.8 f t .section min 2C# po tr cpy andesite - a relatively soft green massive fine grained rook -out- by a few threaagglomerate - a grey to locally near black fine grained intermediate to basic rLuff&ceous with the fust i ri sections tabled below. Rock nrf.n tr po rare grains cpy. 519*6 - 5*8 f t .contorted graphitic tuff min 20# irreg qtz 5# po trace cpy540.8 -2.3 f t .graphitic tuff bedded at 45 o to the CA first 1.0 f t .is agglomer

the top of the formation faces south.548.5 - 4*4 ft. section min 30?S po disseminated and in 1 inch thick seams at 60^tt 6 7 O ft Atrrrl nmri-wt f tuff u-itb ahnnrlant rrranh-i t* m-i vi t f- ru^

560.6 - 22.4 f t. section showing progressively smaller fragments towards the botcarbonaceous material. Rock min 10^ po. Rock shows a bit of fuschite al

aeelomeritic tuff - a pale green coloured massive rock weakly bedded at 60 o to

Sample No.

te restec

14185

massiveal .rock n ow selvag

-py

1418714188 — 1U89po-py

14190ds of qta ock showi

14184itic min

o to the

bom of thberation.the f.A F

FOOTAGE

From

67.0

cut byin tr es and

276 .4*coo.u309.5

332.7 and silg abu:

519.6br po-i

:A3 sect:

"Apmer^

To

69-5

a fewx? fewsmall

278.328^.0 314.0

335.5

Width

2.5

threadgrains pillow

2.32.0 4.5

2.8lowing a g,^ii^ idant fighter

525.4:py. Be

.on* Re

.s aria

5.8dding

ck mat

lignin

CORE ASSAYSgold silver coppernickel

nil

s of q1cpy outlii

nilTttl — nil

nilral ws;colou:

nil;radat:

:ix mai

*nl mvp*

nil

;z min

les. Fi

nilnil nil

nilik carb •ed fra

nil.on her

•ked by

"^ daci

tr po-

rst 3.

0.04onatiz gments

e sugg

abund

+ •^f -in

spy

D feet

nilition. . Rock

ssts tt

mt

comT?o e

is

at

•^ ^ j^ on

EXPLORATION DEPARTMENT DIAMOND DRILL LOGPORCUPINE MINES LIMITED

Location........__....Claim No. ————— Location of Core.

AtSurveys

Dip

Hole No. -.-3^18 .. Shcet No twoLength of Hole........ ...................— ................................................Date Started—— ...——.—...............................—.—Completed ......Core Logged by————————..—— _ — —— ..—— .......... ...... _ .Date....-......................—————...................-................——..—.....

Bearing Elevation

North East -

———————————..... DatumCo-ordinates of Collar

From

605.0

631.3

t jj*f-

rtl f\ rr OfrU. f

901.0

Q18.7

971.0

To

631.3

755.2

040.7

901.0

918.7

971.0

L036 .0

Description of Core

-ropey volcanics - a peculiar black and grey stripped rock consisting of streaks

Sample No.

and shercmatrix. T^e light colour fragments afe aligned at 6U o to the GA. Section includes scatt* Other small bomb like masses consist of po showing sooty graphite. 1rhyolite - a grey hard rock marked by abundant sericite which occurs in the fon yn^ Tn - 7,. A ft. TaD-gir,mpraif712.6 -5*4 f t .ropey volcanics as described above Rock min tr po few grains cpyperidotite - a soft grey maasivy rock showing abundant ~talc and magnesite seams as tabled below."797.2 -8.6 ft. section of green hard jade like materialin sharp contact with thi

sulphides819.2 - 31.5 ft. section as abovetuff - — a groy to locally grron tinged rock the latter colour due to weak aerpenl due to an extremely fine dissemination of a brown mica. Rock is weakly beddedat 45 o to the CA. Contact with previous section is gradational. graphitic tuff - a black graphite rich rock bedded at 50 o to the CA. Rock min :at times rimmed with a thin film of cpy. tuffaceous agglomerate -ma grey to green, -grey to near black rock the latter colecontaining many light coloured fragments. Tuffaceous material is bedded at 60 0dissemination as nodules and as small irreg shaped masses. The pa is associated agglomerate - rock as in previous section with less tuffaceous matrix. Rock min1UJLU.5 -1.0 f t. section min 20^ po trace cpy 1036.0 - end of hole.

i of cornp;

interbanc

i talcose

;uiiza"bioi 1A191

.0^ po as

UT due t(to the CJwith a ti 5^ po as

FOOTAGE

From

Is of cjred sn

ict ros

led wit

perido

i. Othe 851.4

a fine

* abundL. Rockace cp in pre

To

aciticall bo:

ettes.

h sect:

tite. i

r sect: 856.4

dissei

ant gnis mi]yvious i

Width

mater:nb likf

.ons oJ

Sectior

ions ai 5.0

nina.'ti

tphitei tr tc

sectior

CORE ASSAYS

gold silver copper zinc

,al in^ fragm

hard

min w

e ting nil

n and

in thelocal

a bla*ents o:

jade JL

ith tr

ed a f ; nil

as fla-

ly 1(#

:k cartt cherl

.ke mat

extren

idnt br

itened

- nf A

po as

onaceoy mate

erial

ely fi

own In nil

nodule

a fine

usrial.

le

coloui

i

EXPLORATION DEPARTMENTAbitibi Option ' (Anomaly 25)

Property———————————————————————--.-——————Location **ot ^* Concession 4, Crawford Township, Ontario.


Claim No. _ ... — ......Location of Core

Atcollar

..Sc.humacher..;Warehouse.Surveys

Dip Bearing- 45 o——

DIAMOND DRILL LOGHole No. . .............504*72-12 - -....— ———.Sheet No...O.ae.Length of Hole-. J^..^..---.-..--------..-.Date Started --.NOVSldDel:..^1?Z3.- Completed Nov

Core Logged by-.. --A.Skrex;ky—----—-------—Date NPYei*er 15^ 1973

azimith north" Elevation Saffie .aS -——— .——— . Datum

Co-ordinates of Collarr~-W—-rr-———————————-—————

From

033*0 84.5

130.0

298.1

^fcifctf316.5

3?6.u

399.0

422.3

To

33.0— 84-75- 130.0

iVo.J.

316.5

2pasfcpe-376.0

jjyy.u

422.3

542.0

Description of Core

casingperidot ie - a grey to near black massive sort rock threaded with many Jrreg mas tuff - a green grey highly altered intermediate rock bedded at 60 o to the GA arhyolitic material. Rock min tr to light sulphides the main sections of which a — 96.0 ~ 1.0 ft. section min 15# po-py. ——————————————————————————————106.7 - balance of rock min 5^ to locally 20^ po disseminated and as seams up tc

agglomerate - a highly fragmented rock showing abundant compact dacitic and a ' inches thick layered at 60 o to the GA. The rock is in part a flow breccia. Ttsomewhat carbonaceous. The more acid frags show alteration with the developmen healed locally with 15^ po. Scattered acid fragment.* show fjpp/ly f} i sswni nat"rfor replacing fractures through po masses. A local weak breccia is chlorite hea

— acid frags towardo tho lower contact where the rock can be called a flow breccgraphitic tuff - a black graphite rich rock bedded at 60 o to the GA. Rock shemineral is at times finely disseminated in tne rock. The section from310.S to 3 this section also shows a weak brecciation which is healed with a smallamount of cpy. 0.1 f t. sections at each end of the intersection show trace amounts of sph,.agglomerate as in section 130.0 to 298.1 feet. Rock min tr to locally 5# po tr

- —where-^bhe-rock- can- be cai±e±-a-ficnr"breccia. This latter section is marked by that follows is gradational. First 5.0 feet shows a weak late brecciation healdacite a weakly amugdaloidal massive green grey rock min with trace po 387.8 - 3.9 f t .felsic tuff bedded at 60 o to the GA Rock shows qt.* eyes anrt -i*tuff - a green grey dacitic rock poorly bedded at 65 o to the GA Rock min tr t 415*6 -0.3 ft.qtz-carb at 70 o to GA no vio naa —————————————————————quartz diorite - a pale green massive fine grained rock cut by scattered threa— 542.0 - end of hole. —————————————————————————————————————————

Sample No.

nesite ve nd showirre tabled

1 inch tfew rhyol e matrixt of fine po.Rock irled. Therla. ws scatte16.5 feet 14221

ace cpy.abundant ed with t

fleckedo locally

is of qtz

FOOTAGE

From

inlets g scatbelow

hick pitic f is dargrain

JLn wite is a

red nois no.

310.8

Fragmecalcit race s

with t;5# PO

and 1

To

. Rock bered :y

aralle;rqgmenl ic i n c3d fus( h scatlprogr*

jlules ci with 316. s

its be(s fille ffi.

jay fus

)cally

Width

locall'ragmen

Ing th.s vary olourbite. ered gssive

isks a30 per 5.7

ome led amyg

chite

min wi

CORE ASSAYSgold silver copper zinc

y #alc(ts of :

e bedd:ing in with olSock si rains tdecreas

nd thiicent ptM li-

s s disliules.

K^S ———

bh 2# J

)seL-isrhtei

Jig. Resize i .ackLjxlows a)f opyse in 1

i beds* as de ft vL*

;inct iContac

'ine po

colou

ck minrom mi r&ionsweak b uouallhe abu

of poscribe O.l?

n lastt with

y-ftri

few g]lute t(beingreccial

idante

md th:i abov(

20 f e*sec tic

•ains c* 3

-ion•ng of

.3!.

t

n

py

EXLORATION DEPARTMENTProperty" -. . .

Lot l/'Conce'ssion 4, Crawford township, Ontario. PORCUPINE MINES LIMITED

DIAMOND DRILL LOGHole No.. 9Q4--73r?21—————— -. -..——.Sheet No. ..jone Length of Hole ....494.0..f eet

Claim No. _______ ........ __ ... __ — _ ..... ___ — _ —Location of Core .. ......Schunaacher ..Warehouse


Date Started " U.V -"^.C4-.^^/^........ CompletedCore Logged by-

Elevation .same as

Datum904-73-1:1

collar - 60.p 360..o..azimuth...TooTeet""" - 58 o """"~""~'

Co-ordinates of Collar923

flikkk--.Hest.

From

0f .w

337*7

To

17.0337 o

3oy.4

Description of Core

casingandesite - a grey green to green rairly ftarci massive fine grained rock min tr p 47.7 -6.5 ft.ttiff bedded at 45 o to the GA69.4 -0.4 ft .graphitic tuff bedded at 40 o to the GA min 5# dusty po-cpy AQ T ft — '*5 ftt^hlori'tized tuff min tr po— ctry85.8 - 0.4 ft.qtz-carb at 50 o to the GA min tr po-cpy

112.8 "1.0 f t .agglomerate sheared at 40 o to the GA matrix min 5^ po tr cpy 121.3 - 0.3 ft. graphitic tuff at 45 o to the GA. Section is min with heavy dust

to the contacts.124.0 - pillow selvage pa-rail ft! s f.A for 1.0 feet, anrf f.np? at l^.Q wh^r* it is

fair cpy.

171.8 - 0.3 f t. graphitic tuff at 55 o to the GA as at 121.3 feet179*6 - 0.2 ft.qtz-carb at 45 o to the GA min tr po-cpy 180.0 - balance of rock shows scattered 0.3 f t .bands of andesitic tuff bedded a215-J -0.4 ft.qtz-carb at 45 o to the GA Min tr po-cpy 255.4 - 0.2 ft.qtz-catb at 45 o to the GA no vis m-in271.4 - 1.4 f t .andesitic tuff 318*0 — 0*2 ft ats^Cfirb at 7O- o-tn thr fA nn iH ^ min335-0 - 2.7 f t .andesitic tuffgraphitic tuff — bedded at 45 o to the Cft 337.7 - 21.3 ft. section min 25^ po-py disseminated, as nodules and thin streaks

Section min with a trace cpy 340.8 — 3.2 •ft-di aba*?e dyke rontgfKc qt. l^f\ n -^O th*1 CA

Sample No.

o-py rare

y po ligh

JverlaAa-

.uw ux t^^c

; 40 o to

parallel

14222142231A224 14225

FOOTAGE

From

grains

t dusti

with Oi

JLCl.

50 o 1

Lng th^

344.0346.8351.8 356.0

To

i Of C]

' cpy.t* r* i v,*c ft,t

.0 the

i beddi

O/ ^. O-

351.8356.0 359-0

Width

y. Rock

Mater i

lack t

CA

rig whi

-2^ —5*0^

-ttT^ 3 "0 1

CORE ASSAYSgold silver copper

locall

i^shca

iff or

:h here

. oo^

w t(-

U.L,

. 00 ^

.y grad

[S-pola

mud ri

showsO.o3

iJit.

MiL

o. 04.

es int

pity ni

eh in

Romfi iO.OZ.

O. 02.

0.02-0.02-

3 a dac

*t rel*

xa and

ihfiarin

it e.

ted

cr *

EXPLORATION DEPARTMENT- Property..———......

Location..——...——. Claim No..........——Location of Core.

At

PORCUPINE MINES UUMtlTED

Surveys Dip

DIAMOND DRILL LOGHole No. ........964r!?3.r?l.......... -...-... ...........Sheet No..twp.Length of Hole...- ............................... ..............................................Date Started— —.——...-—— .—————— ——.......—..Completed ...— ..Core Logged by... ... — — ............ .....— .. ... ..... ...........— .... ....... ..... .... ...Date . ... .. ............ ........ ...... .. .....

Bearing Elevation .— ... .......... ..... ...... .... . ............... — ....... . DatumCo-ordinates of Collar

North ........................... ....................East . . . . ..... .. ..... ...........

From

369.4

398.1408.7

464.2

To

398.1

-408.7464.2

494.0

Description of Core

flow breccia - a dacitic rock showing irregular shaped fragments of uniform comtlocally 2# po trace py~cpy. Last 2.1 f t. shows smaller dacitic fragments as well us matrix but min...with 2G3& po as a fine dissemination and as irreg shaoed streakconformable to a weak shearing at 45 o to the CA.The shearing is also healedWth a late trace of sph. ———————————————————————————————————————— graphitic tuff bedded and weakly sheared at 45 o to the GA Rock is min with tracagglomerate, sectioned as follows. 409.7 - 419.0 -a highly altered ropey volcanic showing rounded acid fragments?

tuff indicating a complex mode of deposition. Rock shows sonsrgb———————————— to the GA. Section is min with 15ff po trace epy ——————————— 419*0 - 435*5 - dacitic agglomerate showing many fragments of uniform compositio

cuii^gdules. Section is min with tr po 435*5 - 438.2 - ropey volcanics with agglomerate fragments some showing sherds o438.2 - 439*9 - graphitic tuff bedded at 50 o to the CAmin 25# po as nodules and

film of cpy.439*9 - 444.8 - ropey volcanics as in section 435.5 to 438.2 feet .Rock min 5# po 444-*8 - 4/^6.0 — - graphitic tuff bedded at 50 o to the GA min 30# po tr epy few ——

grains of sph446.0 - 451*0 - sulphide zone — highly sheared rock nan with 4u^ grading to mass

sections showing a trace of sphalerite451.0 - 457.0 - ropey volcanics as in section 535.5 to 438.2 feet min with 3# po4*5?*0 ^ 464.? - dap-it.if. agglomerate aa -i^ ****f*t-ion AlQ .n "fro 435*5 feetquartz diorite - a green grey massive fine to medium grained rock showing scatte/.Q;, .Q , ^yyj f.f finl IBH-7H-.V **H\J. WO. JL1UJL7 .

Sample No.

osition ias light er "I4?06

e to loca

and dar.-itEight gre

n (flow b

f graphitirregula

tr cpyJUf-SJ*

Lve po ab 14227trace cp

red qtz e

FOOTAGE

From

n a thr colo 396.0

lly 8

•in ph**en fus

reccia

ic tufr snap

444*0

out 1 - 446.0'

7

res ant

To

m carlured ri 398.1^70 *.L.

oercenl

rds. she:hite i

these

f Sectd;d stre

446.0

jercenl 451.0

1 min 1

Width

onaceoyolite 2.1

PO

wing cnd is

marke

on minaks so

1.4

fine 5.0

r po r

CORE ASSAYS

gold silver copper zinc

us mat:fragm

ontain*highly

i by al

tr 130ne par"

4.02.

cpy anc.01^

are gr;

nx^-Ecsnts a] n rt4-

id^frajsheare

undant

few gi/ly rin

. OZ.S

l scatt 0-08

tins of

nlf minso wit a-o^

pient-s•d at 4

calci

?ins coued wi

o- 'O

ered 0 e). 3o

cpy.

t.r -Kni a cai o. t* a

of grqiD o to

be fir

Wbh a tt

.1 ft. Tt

•bonace

)hitic50 o

.ed

tin

o

EXPLORATIOH DEPARTMENT——Property. JJbitibl. Optior (Anoataly ySi ) - --. - - lAy^tiotôt.JjCoo.C9ssio^ 6,CrsLwfordTownship OntarioClaim No..

DIAMOND DRILL LOGPORCUPINE MINKS LIMITED

Location of Core '

At

collar200 feet

Schu*acher ViSurveys

Dip

*50 .-50

arehouse

Bearing

3^0 Aztwnth

Hole No. 904-73-27 Sheet Length of Hole 536.0 feet Date Started0*0**061" 17,1973

Core Logged by G^J.Date January 4,1974t~i - BSJ1"'" 8. t Elevation ^ " ^

Co-ordinafes of Collar

North 1330

East Line O

Completed DeC 3

— r ————— t —————

From To Description of Core Sample i No.

FOOTAGE

From ToWidth i CORE ASSAYSi

~^^ ' ; j wpyzi- -iu.\rKvj.

^ PO,O casinir-no report o" nverburden type, no boulders cored l L ., j -----, .- i j.^*.90.0 116.0 ultrabasic-a grey-green massive altered rock,possibly a feldspathic pyroxenite .NJm-nagnette to locally magnetic with specks magaeti.e.

iUarbonate, serpentine and chloritic alleration present .Magnesite str s .Numerous disoriented! laths eg f eL" "basic intrusive s.

aspar present near contacts wit.n

104.8-3.3 feet light green fg massive dioritic rock.Contacts hazy .Several strs rpddish-brpwn mineral ((garnet .. —— [108.1-7-^9— f-e^t ultrabasic with f-ine speck* sulphide ..-in-magr.etite.Le>* than lg ^ i;.?AA ill -O ,nA-CL^^^D ,

[sulphides.J-XOeU ?Ô.U

.1 .. .LperiaoviT^*— a oj.acK-green ^,o uj.ue— grey ,ig \,o mg msssj-ve aio.gi.ie o j.*; ruwn. a-jêrea T,O K serpeir&j-nx&w .r*g rexi after olivine, locally evident .Locally ag sections to 1 foot speckled with white toagnesitej.0ccasional astrs grenish-*hite asbestos fibres throughoutjusualljr fine, less than 1/16", to a maximum 7l***fMnnw.Mfti*n*-M^ m-B*wnt. a* nnAcV* and wt.f* ATX! nsiiallT- Acrnmnan-? ft* asbast.o* *T.r * Cftl ci 'Isometiraes with stains brown iron carbonate .Fine disseminated specks sulphide present thro

—————————— than IjCtSulphide is probably pj but there is locally a few fine hairs sulphide o- r — •-* — ibroken.jj.b.u-^ root saanpie witn specKS suxpniae,xess t nan jjb suxp

^j^ 190.0-5 foot sample with specks sulphide, less than 1^ sulp

H ——————————

—

——

208.0-21 foot section with 37 strs asbestos, maximum fibre length 1/81*, fibre cont 24*1.0-75 font bailed bracci A zone of lighter grey rounded fragment* In a tfl|*rk fTor strs magnetite .Occasional non-brecciated band speckled with magnesite and losfrom 295*0 to 310*0* ————————————————————————————————————————— 359.0-30 foot section with fibre content I& and with maxLmtai length 7A6" in str3^9*0-19 ôot- section with itartmt fibr* content 6;? and mrin!PW( l*ngt-h 1/4".408.0-47 foot healed breccia zone of rounded light green fragments in a serpent iolirine .Locally numerous fine asbestos strs;fibre content 2-3/K.Core locally bad!|/. tCt /V fc"\ f^.^4- jâxlr uvxtar* iBxo4i^* fa Vi^wM^r TWiT-l H/vf.1 -K* -Uiwn*rn-in . fvar'+irr'am i*1 t.h i*a

fine asbestos strs; fibre content 1-2^. Fine disseminated specks sulphide (py);l^536.O-wid of noli. —— - " -- . .... ~- ,,,,..-.... .

14267 14268

Bnt 256 jL. sen serpeB magneti

at 368.0

le matrixT broken. i-it-o and

sulp

1^16" .Fibre co be as $trs anighout i in var H* thai oould

116.0 121 .-e-190.0 195.0J. 220*0-222. it in* ipAtTHx.: than normal

.

.Frojninent mg

1

ct gral trs pi*

) with few specks JB cpy.

lular texture j serpentine :rolite.Strs and discontinuous

ntent about Z& but higher in shor d f lin "r slip? or fracture *.ying qi be mi!

5- C0 Fragme:.Fibre

relic

irbcna'

lantity but never greater.lerite.Core locally- badly —————————

T/C, o- 1~7 : --- TT2* O-3O

If wmlly rjipnoed by speckscontent 2# to 295.0;55f

: grnular texture after

^ o+o-Sr, TâlW

; i i :

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LEGENDQUCSTGR INPUT ANOMALV EAST-WE^T FLIGHT UINE.S

QUESTOR INPUT ANOMALY NORTH- SOUTH TLISHT

MelNTYRE PORCUPINE MINES LIMITEDCRAWFORD TOWNSHIP ONTARIO

INPUT ANOHALV DIRECT MAGNETIC

SCALE. T INCH s aOO

©ROUWD CONDUCTOR

42A14SW0026 63.4827 CRAWFORD 204

SCRAWFORD ^TOWNSHIP

6 A 5

IV

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N

0 32 E 36 E 4OE 44E

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EM |6 SURVEY

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LEGEND

Measurement station along picket line

North dip angles to the left of line South dip angles to the right of line

IOOO cps (in phase)

5000 cps (quadrature)


Conductor axis - IOOO cps " " - 500O cps

INSTRUMENT: McPhar IOOO/5000 E.M. (E.M. 16)

Profile scale', l" = 200

ELECTROMAGNETIC SURVEYON THE PROPERTY OF

MCINTYRE PORCUPINE MINES LIMITEDCRAWFORD TOWNSHIP ONTARIO

BY

SHIELD GEOPHYSICS LIMITED

SCALE400 800 1200

JULY

42A14SW0826 63.4827 CRAWFORD 205CI)

one inch to one-half mile

52 E

B.L.

LEGEND


East dip angles above the line West dip angles below the line

1000 cpt

5000 cps


"••"•* Conductor axis - 1000 cps .-O—— " " - 5000 cpt

INSTRUMENT-. McPhar IOOO/5000 E.M.

Profile scale-, l" = 200


MCINTYRE PORCUPINE MINES LIMITEDCRAWFORD TOWNSHIR ONTARIO

BY


SCALE4OO 8OO

-A1200

FEETJULY 1970

9 l O

42AUSW0026 63.4827 CRAWFORD (3)


NA

O

LEGEND


North dip angles to tht left of line South dip angles to the right of line

1000 cps

5000 cps


Conductor axis - IOOO cps " - 5000 cps

INSTRUMENT: McPhar IOOO/5OOO E.M.

Profile scale: l"- 200

O 4E 6E I2E 16 E 20E 24E 28 E 32 E 36 E 40 E 44 E 48 E 52 E

B.L

24S

26S -

42AI4SW0026 63.4827 CRAWFORD

DETAILED



BY


SCALE400 800 1200

FEETJULY 1970

(3)

CRAWFORD ^TOWNSHIP

e ,X 5


N

o 4E 8E I2E 16 E 20E 24 E 28 E 32 E 36 E 40 E 44 E 48 E 52 E

4S

8S

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16 S J.n*

20S

24S

26 S

-j-^*.

l-

f ii.

B.L

LEGEND


East dip angles above the line West dip angles below the line

1000 cps

5OOO cps


* -1" Conductor axis - 1000 cps O—— " " - 5000 cps

INSTRUMENT : McPhar 1000/5000 E.M.

Profile scale: l" = 200

DETAILED



BY


SCALE4OO

t——eoo

4I2OO

FEET

42A14SWee26 63.4827 CRAWFORD 208

CRAWFORD j, TOWNSHIP

6 , 5

V

!V

AT)

KEY MAPon t: ifK,h Tt* ^r.e-

LEGEND


Relative value of the vertical component of the earth's magnetic field in gammas

Magnetic contour

Magnetic depression

INSTRUMENT; Sharpe M.F-I fluxgate magnetometer

O 4E ?E

MAGNETOMETER SURVEYON THE PROPERTY OF


BY


SCALE800

i

FFI

42A14SW0026 63.4827 CRAWFORD 203

X x x' -i"' xFelsic to interMediate Pyrocldstics ^a FlowsX X x' x

KEY MAP Scale: l" s 1320'

LEGEND


Relative value of the vertical component of

the earth's magnetic field m gammas

Magnetic contour

Magnetic depression

INSTRUMENT: Sharpe M.F,-l fluxgate magnetometer

MAGNETOMETER SURVEYON THE PROPERTY OF


BYSHIELD GEOPHYSICS LIMITED

4OO

SCALE eoo 1200 1600

FEET

APRIL 1971

"42A~14SW0a26 63.4827 CRAWFORD

•o,

POWER LINE

TlK.K-1-

O

- //' / > x x''

Felsic to Inter

POWER 4LINE

KEY MAP Scole: l" s I320'

.X B

LEGEND


North dip angles to (eft of line South dip angles to right of line

IOOO cps

5OOO cps


Profile scale l" * 200

Conductor axis - IOOO cps - 50OO cpsII M

INSTRUMENT: McPnor IOOO/50OO E.M.

N

C?)




400SCALE

8OO I200 I600

FEET

APRIL 1971

42A14SWC026 63.4827 CRAWFORD 211

Mofic/^o Ultf6maflMhtrusiv*' Roc

Felsic to Interjnfediate/Pyrocla'stics # Flo POWER ALINE

KEY MAP Scale: l "s 1320'

FOR LEGEND: See Electromagnetic Survey.

N

(S'j

DETAILE D


MCINTYRE PORCUPINE MINES LIMITEDCRAWFORD TOWNSHIR ONTARIO \


40OSCALE

eoo 1200 1600

11 FEET42A14SW0026 63.4827 CRAWFORD APRIL 1971

3 CHANNEL

3 CHANNEL

p CHANNEL

^——— XAv*——

TWP cm:

INPUT ANDMALr SOUTH FLIGHT LINES

INPUT ANOMALY

42A14SWaB26 63.4B27 CRAWFORD

2. CHfcNKJEU

2 CHANNEL.

P35356S 3 CHANNEL 2. o H^KjKie L,

P 3535^

\

\

LEGENDDIAMOND HOLE

CONDUCTOR

QUESTOR INPUT ANOMALV MORTH SOUTH FLIGHT LINES

QUCSTOR INPUT ANOMALV EAST

DIABASE.

GRAPHITIC .SLATE

M'lNTYRE (9QRCUPINE HINESCRAWFORD TWP

-SCALE, l s 2-OO

l42A14SW0026 63,4827 CRAWFORD

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LEGEND

22 +OON —

18 +OON —

14 +OON —

10 +OON

00 N —

2 -f DON

BASE LINE

2 4- 00 S —

AREA 3Recommended drill hole

Existing drill hole

Conductivity - width in mhos

Conductor axis

PHASE

O -f I0(

\l

Rotio \

l/' ^

t i i! Phase

i i

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Near side of loop at 24

Near side of loop at 4


CRAWFORD TOWNSHIP

ANOMALIES No. 3, 9

TURAM SURVEY, 400 Hz

8 O 0/*

N.T.S. No- 42 - A - 14

DRAWN BY : o.A.V.

APPROVED'

SCALE: = 200

DRAWING No P - 12/1

DATE : MAY 1973

PATERSON, GRANT S WATSON LIMITEDCONSULTING GEOPHYSICISTS, TORONTO, CANADA

N

Near side of loop at 44-

26 + 00 S

400 Hz DETAIL

oos

200Hz DETAIL

l

\V

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; Phase

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POROTPI S*E MNI'MG (DIVISION, JCJNT

E w W.- BAZINE1 P. ENG.

fiCTKOMAGNEIIIC SURVEY

LEGEND}

gtatifons Along Picketi s

Jj^.P3iasje.iCQmpo-nfiiit jj ;l ;

put Of Pljase campor|enti

Coil Separation i 300

Gonductor Axiss

Instru40nt: Scinltrex S.B.6CIO

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42AI4SW00S6 63.4827 CRAWFORD S33

63

AREA 30A

BUSH ROAD

UJO O4 ro

UJO O+(O

NEAR SIDE OF TRANSMITTER LOOP AT 12 + 00 N

10 + OON —

8+OON —

6 + OON

4+OON —i* i

2+OON —

BASE LINE

.'d \\

l' O t l

DDH 25057

T\

i t O

tl

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o

\

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6+OON —

4+OON

2+OON —

4 +

12 +

BASE LINE

2 +OOS/ -

6 + OOS

8+OOS —

10 + 00 S r

14 + OOS —

63.4827 CRAWFORD23-4

0+00

2 * OOS —

4 * OOS —

6+OOS —

8 + OOS —

10 4 OOS —

12 + OOS —

16 4- OOS —

18 * OOS —

20-1- OOS —

N

LUO O4- o

UJ Oo4-ro

LU O O•f

AREA 29

AZIMUTH 86 0OLD DIAMOND DRILL HOLE SETUP LOCATED AT 17 + OOE ON LINE 6+OOS


CRAWFORD TOWNSHIP

ANOMALOUS AREAS 8, 24, 29, 30


N.T. S. No: 42- A- 14

DRAWN by : O. A.V

.PPROVED

SCALE: l - 200

DRAWING No : P- 12/2

DATE : May 1973

PATERSON, GRANT a WATSON LIMITEDCONSULTING GEOPHYSICISTS, TORONTO, CANADA

LEGEND

Phase - 400 Hz

- Ratio - 400 Hz

Phase- 200 Hz

- Ratio - 200 Hz

NPHASE

I0 0 0 +I0 0

^ N\

Phase\\

Ratio

807o I207o

RATIO

a = lOO'

VERTICAL LOOP

Recommended drill hole

Ex is t in g drill hole-"


Contact of magnetic rock type MConductor axis

AREA 8

16+OOS —

8 + OOS

20+005 —

22+00 S —

24+OOS —

26+OOS

28+OOS —

30 + OOS —

32 + OOS —

NEAR SIDE OF 2000X1500 TRANSMITTER LOOP ON BASE LINE 14+OOS

N

3o ot

AM o M vi us i*| A 46 ITI fti OPTIOM LOT M cone* tt i *M t

42A14SW0026 63.4827 CRAWFORD 235(/D

IOOOIO

l

l

il

>

ISSI&

1000 c. p s.l' - 2.0*

LOTc

V IMC

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UJ

CM

a fi W

*f-~

tt i

If

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42A145Wee2B 63.4827 CRAWFORD S38

42A14SW9036 63.4B27 CRAWFORD

AREA 30A

LUO OH-

UJo o•4*

NEAR SIDE OF TRANSMITTER LOOP AT 12 +00 N

O BUSH ROAD

10 + OON —

8 + OON

6+OON — M

4+OON —i

2-l-DON

BASE LINE

\ b\\

7l

\s

-

DDH 25057

/9/' x

Ov\ l \\ \l

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\; 530' - - \\\

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8+OOS —

10 +OOS f l \

12 + OOS — \

14 + OOS —

UJo o

LUo o

to

LUOo

0+00 —

2 + OOS —

AREA 29

4 -f OOS —

6+OOS — AZIMUTH 86 Q

8 + OOS —

IO + OOS —

12 + OOS —

16 + OOS —

18 + OOS —

20+ OOS —

NEAR SIDE OF LOOP ON LINE 6+OOS


CRAWFORD TOWNSHIP

ANOMALOUS AREAS 8, 24, 29, 30


N T S No 42 - A - 14

DRAWN by O, A V

APPROVED

OLD DIAMOND DRILL HOLE SETUP LOCATED AT 17 + OOF ON LINE 6 + OOS

CONCESSION LINE

CONCESSION IV

NEAR SIDE 2000 X 2000 TRANSMITTER LOOP AT

6 + 00 N —

4+OON —

2+OON —

BASE LINE

CORRELATION

WEAK CORRELATION "TREND"

N

VERTICAL LOOP

AREA 8

6+OOS —

18+OOS

204-003 —

22+00 S

SCALE l ' 200

DRAWING No : P- 12

DATE May 1973

PATERSON, GRANT a WATSON LIMITEDCONSULTING GEOPHYS ICiSTS, TORONTO, CAN ADA

24-1-OOS

26+OOS —

28+003 —

30 + OOS —

32 + 003 —

NEAR SIDE OF 2000 X 1500 TRANSMITTER LOOP ON BASE LINE 14 -1-00 S

42A14SW0026 63.4827 CRAWFORD

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42A14SW0026 63.4827 CRAWFORD

^6 t y - /" " 7*0.o

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A - 200'

vied, —

.. 3 etectroatc* to t/re. north

MclNTRE PORCUPINE MINES LTD.ABITIBI OPTION

( CRAWFOR D l )

CR AWFOR D TWP. ONTARIO

INDUCED POLARIZATION SURVEYDETAIL PROFILES fa*

KARL GLACKMEYER A ASSOCIATES LTD.Geophysical Consultants and Contractors

716 Cornwall Drive Baie d Urfe 850, Que (514) 453- 1982

.DATE

JAN. I973

SCALE200*

APPROVED BY

SURVEYED BY

K. G.

DRAWN BY

G. G.DRWG. NO.

12 l \/ PLATE "211 l Pt R

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lil

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2.000 S

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12A14SW0026 63,4827 CRAWFORD

LOO'

200'

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200'

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300'

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300'

l l f#00

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42A14SW002B 63.4827 CRAWFORD 258

3&O*

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42AHSWC326 63.4827 CRAWFORDf

200'

300'

- f O/*//f feet

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•A m^/00'

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//•,jft/" O. iff -/l//-

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Me INTYRE PORCUPINE MINES LTDABITIBI 0 PT iON

(CRAWFOR D II )

R A w F 0 R D J W P, ^ ....- ......^. .,. . ... .. QfNLTA


RESISTIVITY 8)

NKARL GLACKMEYER A ASSOCIATES LTD

^ \. :

r S - ti'-. .i?

'

'DATE ! SCALE

JAN. i 97 3 : 'APPROVED BY

1 " s 200'

SURVEYEDBY

K. G. NO

DRAWN BY

G. G.

2, f P LAJ E. IX -R

Z O IN E

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MCINTYRE PORCUPINE MINES LTD.ABITIBI OPTION

(CRAWFORD II )

CRAWFORD TWP. ONTARIO


CHARGEABILITY65

V*)

'KARL GLACKMEYER 4 ASSOCIATES LTD.Geophysical Consultants and Contractors

716 Cornwall Drive Bale d Urfe 650, Que (514) 453-1982

DATE

JAN. I973APPROVED BY

SCALE

200

SURVEYED BY

K. 6,

DRAWN BY

6. 6.DRWG NO.

I2II/PLATE IX -IP2Z1

5 CHANNEL

CHANNE.U

CONCESSION

S CHANKJEJ- COKICESSION 3

ZCHANKJtLto ol s

i i

5CHANNEL

R 3535*57

CHANME.L

3CHANKJE.L

5 CHWN&L

LOT A

CM: 3 DIAMOND Dft ILL

42A14S*e026 63.4827 CRAWFORD

QUESTOR INPUT ANOMALY WORTH SOUTH FLIGHT UMC.S

EA5T WEST FUfrHT UNKS

GRAPHITIC

TO &ASJC VOLCAMlC

GRAPHITIC VOLCANIC ASM

TUFF

MelNTYRE PORCUPINE MINES UMITED

CRAWFORD TOWNSHIPONTARIO

SCA.UC i INCH s 2.00 rttr

O rcouA " ro^l JZC

/^l f

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TO BASIC VOLCANIC

VOLCANIC ASH

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F OR D TOWN SHIP

J

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o f-*.2

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\

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C)

C)

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l

l

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i l WCM s.' 2.00

COtJCtSSlONZTOW W SHIP

(lo)

LOT 5 COM et t* t*tt t

SCA.LB) t IMCM t.OO if

42AHSVIIM26 63.4627 CRAWFORD 2804-1

H-00 N

10 + OON

8+00 N

6 + 00 N

4 + 00 N

2 +OON

0 + 00

0 + 00

2 + 00 S

4 + OOS

AREA 50-

SQUARE TRANSMITTER LOOP 20OO X 2000

6 + 00 S

8 + OOS

o+oos

l 2+00 S —

14 + 003

16 + 003 —

OO4-00

-J

oo-t-o o

o

LJ

o o

-10'PHASE

O

Phase \ Ratio

800X0 !007o

RATIO

a ^200'

I20 0X0

AREA 38

400

GNO.I 400

No.2\Q

o o

oo

oo O

O4- o

42AHSW0C26 B3.4B27 CRAWFORD 281

LJ O O

+00

o o o

Oo owa. o o

a: u

CC

AREA 50-2

o o4- to

o oo oH-CM

O O

UJ O O+OJ

LUoO

LU O O

L- 12 + OON

X"\

Xl—————————l——————————l_________L L-8 + 00 N

\L-4+00 N

L- 0-1-00

M0 0Xo-,

I007o

90

T+5

Ratio

a ^200'

LEGEND

Recommended drill hole


Q

Zone of low conductivity

Conductor axis

O)


CRAWFORD TOWNSHIP"CWnflf

ANOMALOUS AREAS 38, 50 ( 61 l c'\vTURAM SURVEY, 400 Hz

N.T.S. No: 42 - A - 14

DRAWN by : H. Ricketts

APPROVED: ' ' iv . ^

SCALE; l'^

DRAWING No:

DATE : May

200'

P -

1973

12/3

DATFDQnM CDAMT ft XA/ATCnM 1 IKjIITm

CONSULTING GEOPHYSICISTS, TORONTO, CANADA

1'

fei*

42A14SW0026 63.4827 CRAWFORD ass

4!

L - 0

110 326 33* 307 /94 v jo* 2t*/

JfeJ fjfy W

1*0

3" 4" t0*

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•n !

s*. -

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?

J9 * SOO '

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X////////

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L - 0

MCINTYRE PORCUPINE MINES LTD.Anomaly SO drea

T*/p. 0ntat~t'o

C**)INDUCED POLARIZATION SURVEY

KARL GLACKMEYER * ASSOCIATES LTD.Geoprt^ca/ Consultants and Contractors

Df.v* B*i* d Uff* 830 Ou* (514)453-1982

SURVEYED BY DRAWN BY

42A14SW0026 63.4827 CRAWFORD 283

i. - S W

233

w/ /J/ /j? /XT^J}?

ft r o

/f /////////x

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a s

/3

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-0.}

/-s t?, f

jr. a -0-7

284

/o " /a"

-0 f-

r 200'

si^ ^

L- 8 W

MCINTYRE PORCUPINE MINES LTD.Anomaly


KARL GLACKMEYER A ASSOCIATES LTDGeophysical Consultant* 9nd Contractors

Ba.t d Ur(* 8 SO Ou* l 514 (453- 1962

SUWVEYfOBY

/(.a.

DWVVG NO

DRAWN BY

z. c.

- i

o o00

3 oQt

i lo o S

LkfcA*MT 1-1 C

*O

LOT * CO* C ftC*.*WPO*O0*4TSCAU& t IKCM. 2.00 P-tfeT

,-^63.4827 CRAWFORD

S85

TP '

3; Q

J i l Ci

'

.

lp' '

i. l'.''-i

-i

W \

i

^.. —— .~... .......,. , .

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j i ""'

-

i

-i-! -7

—*-4

rt MOM A us 5OA&ITtBl OpTtOMLOTS COM C t Sf 10*4 t CA*v* PO*D row M SHIP

l/WCMa. ZOO FfiGT

AREA 50- AREA 50-2

SQUARE TRANSMITTER LOOP 2000' X 2000*

O O±CD

8-f-o o-\-CM

o oLJ o o

UJo o

LUoo

l +OON

10 + 00 N

8 + 00 N

6 + 00 N

4 + 00 N

2 + OON

0 + 00

o o oCM

x"o o o(M

Q. Oo

irUJ

5 Vt

cc

o in

O O+ CO

l

o o+ o

l

UJo o

-I00PHASE

O + IO*\\\

Phase \V

V

x

if1

/Ratio

/

\

800Xo IOO 0Xo

RATIO

a = 200'

120 7o

AREA 38

0 + 00

2 + 00 S

4 + 00 S ——

6 + 00 S

8+OOS——

10+003

12 + 003 —

14 + OOS

16 + 003 ——

SQUARE TRANSMITTER LOOP 2000 X 2000

o o+01

5o o

o o+ro

l

o o

L- 12+OON-x\\

l—————————L. V-^" J———————-^ L-8 + 00 N

\\

L-4+00 N

li

-^————' L- 0 + 00

UJ OoOD

l

90 0X0

T+5'

Ratio

Phase-..

UJtn

a =200 I

AREA 61(CARNEGIE TOWNSHIP)

LEGEND

Recommended drill hole ••••-


Zone of low conductivity •••-

a

Conductor axis

J


CRAWFORD TOWNSHIP

ANOMALOUS AREAS 38, 50, 61


frit.T. S No: 42 - A - 14

OTRAWN by : H.Ricketts

APPROVED

SCALE ; \ ^ 200

DRAWING No: P - 12/3

DATE : May 1973

PATERSON, GRANT ft WATSON LIMITEDCONSULTING GEOPHYSIC1STS, TORONTO, CANADA

42A14SW9826 S3.4H27 CRAWFORD 287"

•d•f Ogd*n ' Dnlwo Sho* ^Co'mon Thoino?) Sf*'trtoo Egor

Ttxxrwloi—— l/ X'Den'or - -' /

''Keel*' /' J'

INDEX MAP

,,....25057

ABITIBI PROPERTY

II25074 25070

THE PRICE COMPANY LIMITEDPRICE MINERAL RESOURCES DIVISION

ONTARIO

ABITIBI OPTION CRAWFORD TOWNSHIP

0 H C. IMCM 2.00

42A145W0026 63.4027 CRAWFORD 589

O O D

42A14SW0a26 63.4827 CRAWFORD 230

O 5

O '

Q 7

o 8o *

^ orjr d 7

/r* 200'

42A145W0026 63.4827 CRAWFORD

O54

K i

/4

- -

--i-

231

LOOKM4G* NORTH

WEST E1FIST

, Co in Ni

89 58 6O73 62. 4©

.100 68 \6Z

ML IZ7 290 (32.

190 14Z 9680 96 9Z

248 43 100186 62. 1545 IZ 122.

20 14 IZ313 K HZli "58 75

IIZ 73 108 7Z 4t 67

Z09

MCINTVRE PORCUPINE MiMCS UHlTfiOOPTION

SECTION

LEGEND

SCALE INCH - lo F

tn V-o

42A14SW0026 63.4827 CRAWFORD 232

LOOKING WESTNORTH

LEGEND

SAND

SILT

GRRVEL

Q6.

u- u-

OWo;Luh or

G7. SOUTH

PORCUPINE MINES LIMITED aemei OPTIOK

MOOWELL Q, TRAVERSE GEOLOGICAL. SECTION

H Ofi. U

SCPXt-ET INCH r. to FEE.T

42A11SW0a26 63.4827 CRAWFORD 233

wes-r LOOKINQ WORTHP.3 FI. FZ.

64 95

.^. Co Zn Hi 66 60 6

60 60 66

64 160 64

44- 6k SI

4-4 70 63

34 to 46

44 66 ^57

129 109

70 07 04

Oin-i uu.

li

i Co

57

Hi

90

fcO 00 76

100

SS 57

lil M 96 HO 34Hi 32. 69

SCO

LEGENDCLflY

TILL

TUFF

42A14SW0026 63.4827 CRAWFORD 294

MCINTYRE PORCUPINE MWESUMlTtOf*8lTl6* OPTION

NODWELL F TftRVERSCSECTION

OHkE. tNCU s (OD FTCTOME (it)

WEST H L

63.1827 CRAWFORD

LEGENDSS5

CLRY

SflMO

[——j

(——[

SttNO

BOULDER

FELSIC TUFF

. ; . CAI 3trt

90 7O

64 93 106

N.S.

64 40 76

69 37 120

32 20 01

I6O

Z7 16 760

B) 31 460

57 64610

Ui

UOOKlWG NORTH

H*,

,.. Cu Zn Ml 2

109 95 66

95 Si 09

iK

;:

196 47 300

N.S.

69 ST 0I

,.. CM; Zn Mi

362,36

44 49 76

MB.

Co Zn N(

57 61 66

225

U6 WO TO

M*INTV*fe PORCUPINE KIN** UMlTiOrteiTlBl OPTION

HOOWCUU H TR^VC^SCatOLOClC^L SCCTIOH

. SCflL-E ONK IMCH i VEfc-tlCAU SCA'tX OWE. INCH a IOFCET

Laidlaw; MoMt ' Dorgov*!

27017 (O'SOVoZn 0-I60I ftg/ton)

-M?i .C2J^ I!*NE:~f| ^IMlskAMINS" "t

W IBlOCUtod ! McCvoy

SLDBURY"-; —r ^ '^

ABITIBI PROPERTY

THE PRICE COMPANY LIMITEDPRICE MINERAL RESOURCES DIVISION

ONTARIO

42A145W8026 63,4827 CRAWFORD

63.4827 CR..FOBD237"

DRl UL M O LE SECT IOWOPTION

S A ml M

0MB l*MCH

t j. y

0B/T/0/ 00T/0/7ra w/?f s*

CO/). Wtor ter-s

PROGESS RPTS FEBRUARY 1971 TO MAY 1973 - Geology ...

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Transcript of PROGESS RPTS FEBRUARY 1971 TO MAY 1973 - Geology ...