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AERIAL RADIOMETRIC AND MAGNETIC SURVEY

NATIONAL TOPOGRAPHIC MAP

WILMINGTONDELAWARE, MARYLAND, NEW JERSEY, PENNSYLVANIA

PREPARED FOR THE U. S. DEPARTMENT OF ENERGYGRAND JUNCTION OFFICE

GRAND JUNCTION, COLORADOUNDER BENDIX FIELD ENGINEERING CORPORATION SUBCONTRACT #79-337-S

Geodata International, inc.7035 JOHN W. CARPENTER FREEWAY DALLAS, TEXAS 75247(214) 630-1600 " TWX: 910-861-4359

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LEGAL NOTICE

This report was prepared as an account of work sponsored by the United StatesGovernment. Neither the United States nor the United States Department of Energy,nor any of their employees, nor any of their contractors, subcontractors, or theiremployees, makes any warranty, express or implied, or assumes any legal liability orresponsibility for the accuracy, completeness or usefulness of any information,apparatus, product or process disclosed, or represents that its use would not infringeprivately owned rights.

TABLE OF CONTENTS"WILMINGTON TOPOGRAPHIC MAP SURVEY"

ABSTRACT

AERIAL RADIOMETRIC AND MAGNETIC SURVEY

WILMINGTON NATIONAL TOPOGRAPHIC MAP

DELAWARE/MARYLAND/NEW JERSEY/PENNSYLVANIA

SOUTHEAST U.S. PROJECT

PREPARED FOR THE U.S. DEPARTMENT OF ENERGYGRAND JUNCTION OFFICE

GRAND JUNCTION, COLORADO

UNDER BENDIX FIELD ENGINEERING SUBCONTRACT NO. 79-337-SBY

GEODATA INTERNATIONAL, INC.DALLAS, TEXAS

SECTION

I. INTRODUCTIONABSTRACT

The results of analyses of the airborne gamma radiation and total

magnetic field survey flown for the region identified as the

Wilmington National Topographic Map NJ18-2 is presented in this report.

The airborne data gathered is reduced by ground computer facilities to

yield profile plots of the basic uranium, thorium and potassium equiva-

lent gamma radiation intensities, ratios of these intensities, aircraft

altitude above the earth's surface, total gamma ray and earth's magnetic

field intensity, correlated as a function of geologic units. The

distribution of data within each geologic unit, for all surveyed map

lines and tie lines, has been calculated and is included. Two sets of

profiled data for each line are included, with one set displaying the

above-cited data. The second set includes only flight line magnetic

field, temperature, pressure, altitude data plus magnetic field data as

measured at a base station. A general description of the area, in-

cluding descriptions of the various geologic units and the corresponding

airborne data, is included also.

A. Survey AreaB. Summary of Map Location, Geology and Physiography

II. FLIGHT OPERATIONS

A. Survey Time SummaryB. Line Coordinate LocationC. Test Line ResultsD. Magnetic Diurnal Correction - Base StationE. Altitude and Ground Speed Summary

III. GEOLOGY OF THE SURVEYED AREA

A. Location and General PhysiographyB. GeologyC. Description of Geologic Map UnitsD. Radioactive Mineral Prospects in the Surveyed Area

IV. RESULTS OF DATA ANALYSIS

A. Description of Stacked Data Profiles

1. Multivariable Radiometric Profiles2. Residual Magnetic Field Profiles

B.C.D.E.

F.G.H.

Single and Average Record ListingsStatistical Presentation of Data by Geologic TypeFrequency Distribution of Data of each Geologic TypeData Interpretation

1. Analysis of Geologic Histograms2. Discussion of Anomalies3. Summary and Recommendations

National Gamma Ray Map SeriesLine Printer ContoursStacked Data Profiles and Geologic Histograms

Geodata International, Inc.7035 John W. Carpenter Freeway

Dallas, Texas 75247

PAGE

I-1

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LIST OF FIGURES(Table of Contents Cont'd.)

SECTION

V. GEODATA DATA ACQUISITION AND PROCESSING

A. Data Acquisition System.B. Data Processing

1. Data Reduction2. Description of Data Processing3. Data Presentation4. Statistical Analysis Procedures

APPENDICES

I. PRODUCTION SUMMARY

A. Production Summary TableB. Test Line Results TableC. Diurnal Corrections TableD. Explanatory NotesE. Speed and Altitude Tables and Histograms

II. TAPE FORMAT STATEMENTS

III. COMPUTER LISTINGS

IV. LINE PRINTER CONTOURS

BIBLIOGRAPHY

PAGE

V-1

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FIGURE

I.1 Survey Index Map

1.2 Geologic Base Map

II.1 NTMS Showing Flight Line Location

IV.(1-6) National Gamma Ray Map Series

V.1 Survey Aircraft

V.2 System Block Diagram

V.3 Typical End-of-Flight-Line Spectral Plot

V.4 Data Reduction Flow Chart

LIST OF TABLES

TABLE

IV.(1-6) Geologic Unit Average Value as a Function ofMap Line

IV.7 Mean (X) and Standard Deviation (a) for EachGeologic Type

IV.8 Geologic Units with Significant Variationsfrom Unimodal Distributions, Based on theAnalysis of the eTh Histograms

IV.9 Summary of Anomalies

IV.10 Radioactivity Anomalies per Geologic Map Unit

IV.11 Statistical Summary of Radioactivity Anomaliesby Geologic Unit

V.1 Data Reduction Parameters and Constants forN540S

iiii

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SECTION I

INTRODUCTION

SECTION I.

INTRODUCTION

A. SURVEY AREA

Geodata International, Inc., Dallas, Texas, conducted an airbornegamma ray and total magnetic field survey for the WilmingtonNational Topographic Map Sheet as outlined in Figure I.1. Thissurvey was performed from a fixed-wing aircraft, using a computer-controlled, large-volume radiation detector system to detect thegamma radiation flux emanating from the surface materials. Eachmap line was flown in an east-west direction with an average linelength of 78.2 miles; each tie line was flown in a north-southdirection with line lengths of 69.0 miles. Map lines and tie linesare shown in Figure II.1.

Sections I through IV of this report present information andresults associated with this specific survey. Section V gives thedata acquisition and the processing procedures which are generallyapplicable to any survey flown with the equipment described.

B. SUMMARY OF MAP LOCATION, GEOLOGY AND PHYSIOGRAPHY

The Wilmington map area (N.T.B.M.S., 1972) is delimited by thelatitudes 39000' to 40000' north and longitudes 74000' to 76000'west. The surveyed area occupies parts of Delaware, Maryland, NewJersey and Pennsylvania (Figure 1.2).Two geologic and physiographic divisions occur within the area.Most of the land is within the confines of the Atlantic CoastalPlain. In the west and northwest, the Fall Line Zone and Piedmontunits are very different.

The Coastal Plain is a sedimentary-structural feature with strataranging in age from Cretaceous to Holocene. Much of the surfacearea has outcrops of either Tertiary or Quaternary age. ThePiedmont is crystalline rock, mainly metasedimentaries of Paleozoicor Precambrian ages, and metaigneous rocks of both intrusive andvolcanic variety.

Economically significant deposits of radioactive minerals have notbeen found within the surveyed area. However, rocks of both theCoastal Plain and Piedmont could be potential hosts for boththorium and uranium concentrations.

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FLIGHT OPERATIONS

SECTION II.

FLIGHT OPERATIONS

A. SURVEY TIME SUMMARY

The Wilmington map sheet was flown between July 22 and July 30,1979. A detailed list of dates flown and lines flown on thosedates, as well as average altitude and speed for those dates,appears in Appendix I.A.

B. LINE COORDINATE LOCATION

Doppler navigation system data have been used to locate the posi-tions of the flight lines. These lines are positioned and verifiedby point locations, determined by visual sighting by the navigatoror photographic recovery, and corresponding record numbers displayedby the on-board computer. The data are then plotted as solid lineswith ticks every ten records, circles every fifty records, andrecord numbers every one hundred records. Record numbers andcircles also appear at the end of each line. The points used forlocation reference (at least every 10 miles) are marked with an"X". The flight base is then photographed with the geologic basemap to produce the composite map in Figure II.1.

C. TEST LINES

When conditions allow, two five-mile test lines are flown, one atthe beginning of the day and one at the end of the day, over thesame base. The data are used to check the repeatability of thesystem's measurements, and are presented in Appendix I.B.

D. MAGNETIC DIURNAL CORRECTION - BASE STATION

A base station magnetometer is set up in the area to acquire datapertaining to the diurnal changes in the magnetic field. Thesedata are analyzed to evaluate a diurnal correction to the magneticdata obtained by the aircraft. A list of these corrections appearsin Appendix I.C.

E. ALTITUDE AND GROUND SPEED SUMMARY

The average altitude and ground speed for each line is determined.A list by date appears in Appendix I.A. and is discussed in SectionII.A. A list by flight line is given in Appendix I.E.

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SECTION II

GEOLOGY OF THE SURVEYED AREA

SECTION III.

GEOLOGY OF THE SURVEYED AREA

A. LOCATION AND GENERAL PHYSIOGRAPHY

The aerial radiometric and magnetic survey was conducted over theland area of the Wilmington National Topographic-Bathymetric MapSheet (N.T.B.M.S., 1972). The surveyed area includes a part ofnortheastern Maryland, northern Delaware, southern New Jersey andsoutheastern Pennsylvania. It is delimited by the latitudes of39000' to 40000' north and longitudes 74000' to 76 00 west. Itincludes part or all of the following counties: Chester andDelaware counties in Pennsylvania; Caroline, Cecil, Kent and QueenAnnes counties in Maryland; Kent and Newcastle counties in Dela-ware; Atlantic, Burlington, Camden, Cape May, Cumberland, Glou-cester, Ocean, and Salem counties in New Jersey.

The surveyed area is located in two major Physiographic Provinces(Fenneman, 1938). These are the Atlantic Coastal Plain, and thePiedmont Plateau. The transitional zone between the physiographicprovinces is known as the Fall Line (Fenneman, 1938).

The eastern margin of the United States is a lowland which passesunder the Atlantic Ocean with little change of its gentle surfacegradient (Fenneman, 1938). The shallow, submerged part of thelowland is termed the Continental Shelf. The emerged part istermed the Coastal Plain. The shoreline between emerged andsubmerged portions of the plain is temporary, and significantshifts of the coastal boundary have occurred during the Mesozoicand Cenozoic eras. Seaward of the emerged area, there are barrierbeaches; these are broken or interrupted in places, but extendalong most the coastal zone.

The Coastal Plain is comprised of many sedimentary strata, rangingfrom Cretaceous to Holocene in age. The strata dip downslopetoward the Atlantic Ocean, and pass beneath the sea onto theContinental Shelf. The dip of the sediments increases with depthof burial and with age of origin. Many of the sediments weredeposited under shallow water conditions.

The landward limit of the Coastal Plain is generally considered tobe the inland margin of the Cretaceous units. The altitude of theboundary increases from sea level near New York City, to greaterthan 300 feet in Maryland.

From Cape Lookout, North Carolina northward, the Atlantic CoastalPlain is deeply indented by bays and estuaries. It is little more

than a fringe of peninsulas (Fenneman, 1938). Two "peninsulas"make up the Coastal Plain within the surveyed area. BetweenChesapeake and Delaware bays, there is the Delmarva Peninsula;north of Delaware Bay and south New York Bay is the New Jerseycoastal area.

From the Hudson River to the Potomac River, there is a lowland, 5to 20 miles wide, at the inland margin of the Coastal Plain. Thelowland is formed in the less resistant beds of an Upper Cretaceousclay. More resistant sediments of younger age overlie the easilyeroded strata. These more resistant strata are marl formations andindurated limestones; the more resistant beds form a cuesta seawardof the lowland, and constitute some of the highest topographicpoints of the Coastal Plain.

A variety of Pleistocene terraces have been delimited for theAtlantic Coastal Plain. In places, low scarps separate one terracefrom another. The terraces were first described in Maryland.Cooke (1931) lists the terraces by name and elevation. They are,in descending order and decreasing age, the Brandywine, the Coharie,the Sunderland, the Wicomico, the Penholoway, the Talbot, and thePamlico. The origins of the terraces have variously been ascribedto both coastal and fluvial processes. In recent years, lessemphasis has been placed on the significance of the terraces ininterpreting the Pleistocene and Holocene geology of the area.

The Piedmont Plateau is one of six physiographic provinces of theAppalachian Highland. It is the non-mountainous portion. Thesurface is eroded into deformed crystalline rocks of Precambrianand Paleozoic ages. The Piedmont surface generally slopes awayfrom the Appalachian Highlands toward the Coastal Plain. At itsseaward edge, the resistant rocks of the Piedmont pass beneath thesediments of the Coastal Plain. The steeper margin of the Piedmonthas been termed the Fall Line.

Typical landscape of the Piedmont is a gently undulating surface ofminor local relief, cut by steep-sided valleys. Interfluvial areasare of limited areal extent; valleys are steepest in the Fall LineZone.

B. GEOLOGY

Piedmont Plateau - Precambrian and Cambrian Rocks

The Piedmont is a gently undulating plateau bounded on the west bythe Blue Ridge Hills and on the east by the Coastal Plain. It isan erosional surface cut into deformed and metamorphosed synclinalrocks of Late Precambrian to Early Paleozoic age (Fisher, 1970).Intrusive rocks are common. The older Precambrian rocks appear in

New Jersey in a series of anticlinoria and recumbent folds. South-ward, they reappear in Maryland. These basement rocks are mainlyquartzofeldspathic gneisses and migmatites, but include anorthositeand hypersthene granodiorite (Fisher, 1970).

The oldest of the Precambrian formations has been termed theFranklin (Buckwalter, 1955). In Pennsylvania, the bulk of theformation is a group of graphitic gneisses and graphite quartzschists. The Franklin Formation has been correlated with thePickering Gneiss of the Piedmont.

Gabbro gneiss, hornblende gneiss, and several other types of basicgneisses occur in the Piedmont. The gabbro gneiss is a dark-greyto black, medium-grained rock, with little gneissic structure. Itcontains some 50 percent labradorite and 50 percent ferromagnesianminerals, including hornblende, augite, hypersthene and minorbiotite. The hornblende gneiss is composed primarily of labra-dorite and hornblende with local minor garnet (Buckwalter, 1955).

The granite gneiss is light-buff to light-pink, and fine- tomedium-grained. The gneissic structure tends to be ill-defined oralmost absent. Essential minerals are quartz, microcline, withsome five to ten percent of biotite and hornblende gneiss combined.In some localities, the ferromagnesian minerals are few, and therock is leucogranitic. Orthoclase and albite may occur in minorquantities. Accessories include magnetite and zircon (Buckwalter,1955).

The Port Deposit Gneiss is a moderately to strongly deformedgneissic quartz diorite, hornblende-biotite quartz diorite, andincludes biotite granodiorite. It crops-out in southeasternPennsylvania.

The Wissahickon Formation is a thick sequence of metamorphosedgreywackes, shales and submarine slump deposits. It overlies thindeposits of metamorphosed quartz sandstone, potassic shale, and theCockeysville Marble. These three units comprise the Glenarm Seriesin the Potomac area (Fisher, 1970b).

Southwick and Fisher (1967) in Maryland divided the Wissahickoninto five informal lithofacies. These lithofacies are: (i) ametagreywacke; (ii) a boulder gneiss; (iii) an upper peliticschist; and (v) a metaconglomerate lithofacies. In Pennsylvania,the Wissahickon Formation is subdivided into: (i) an albitechlorite schist, which includes the octararophyllite and somegranitized members; and (ii) an orthoclase mica schist, whichincludes hornblende gneiss members, augen gneiss, and some quartzand feldspar-rich members, which show varying degrees of meta-morphism (Buscom and Stose, 1932).

111-2III-i III-3

The Settlers Formation is present on the flanks of the Woodvilleand London Grove-Avondale anticlines. It consists chiefly ofquartzite and quartzitic schists. In places, it may be a micaschist. The formation is estimated to be about 1,000 feet thick.

The Cockeysville Marble is exposed on the flanks of the Woodvilleand London Grove-Avondale anticlines and, in small areas, scatteredalong the southern side of the Poorhouse Prong and the Baileylineament. It is a medium- to coarse-grained, saccharoidal rock,which ranges in color from white to light blue-grey. It is oftenbanded with flakes of phlogopite. Its thickness is between 100 and500 feet (Bascom and Stose, 1932) to 1,700 feet (McKinstry, 1961).

The Peters Creek Schist is found in the central part of the PeachBottom Synclinorium. It is distinguished from the weakly meta-morphosed phases of the Wissahickon by its abundant quartzite beds.It is a fine-grained, finely laminated, non-fissile mica schist,with numerous thin beds of quartzite, interleaved with layers ofmuscovite.

The Glenarm Series were deposited in a shallow marine environment.The sea extended southeastward of the present Piedmont, and includedmuch of the area now occupied by the Coastal Plain. The two upper-most formations were a limestone, some 200 feet thick - Cockeys-ville Marble, and some 5,000 feet of shale - Wissahickon Formation.No local record exists in Delaware of the Glenarm Series above theWissahickon.

During the Paleozoic, one or more of the orogenic disturbances thatformed the Appalachian Mountain System metamorphosed the Glenarmsediments. It is thought that this occurred during Middle and LatePaleozoic times (Ward and Groot, 1957).

During metamorphism, magma was intruded into the marble and schist.Much of the eastern and southern Delaware Piedmont is underlain bygabbro. The gabbro was also regionally metamorphosed.

Although Bascom and Stose (1932) consider the gabbro to be intru-sive, McKinstry (1961) states that in the Wissahickon, he has seenno gabbro that is clearly intrusive. McKinstry (1961) suggeststhat the gabbro may be volcanic in origin and possibly of post-Glenarm age.

Within the Wissahickon Formation, and elsewhere, there are irreg-ular masses and tabular bodies of amphibolite. They may representsmall apophyses of gabbro pluton completely recrystallized duringmetamorphism.

No metagabbro is found in the zone of low grade metamorphism;however, a greenstone schist that is present may be its equivalent.The schist is composed of very fine-grained amphibole, plus epi-dote, plagioclase, biotite, chlorite and quartz, and would berepresented in the high grade zone by a hornblende gneiss.

Small bodies of serpentine have been intruded into the Wissahickonand metamorphosed. Pegmatites occur in northern Delaware. Theyare largest and most abundant north and west of Newark. Generally,in the eastern Piedmont, they are small and uncommon.

In the very northwestern portion of the map area, there is atransition from flysch-like, locally volcanic, highly metamorphicrocks, of eugeosynclinal origin, to Early Paleozoic rocks ofmiogeosynclinal origin. This line of transition is termed theMartic Line, and is generally drawn along the junction of knownCambro-Ordovician rocks, mainly the Conestega Limestone, with thepelitic schists of the Glenarm Series. Rapid facies changes areinvolved (Wise, 1970). The line marks the edge of a deeply sub-siding paleo-basin to the northwest of the surveyed area. Alongthis basin edge, the effect of several stages of deformation areconcentrated (Wise, 1970).

Coastal Plain - Mesozoic and Cenozoic

The Coastal Plain is underlain by a series of dipping layers ofrelatively unconsolidated sand and clay and lesser amounts ofgravel. These are deposited upon an eastward continuation of thecrystalline rocks of the Piedmont. The interface between the twotypes of rocks dips to the southeast (Vokes, 1957).

The nature of the crystalline rocks is not well known, exceptwhere they crop-out near the Fall Line. The Hammond Well, inWicomico County, reached the basement at a depth of almost 5,500feet. The drill hole penetrated a mica gneiss similar to theBaltimore gneiss of the Piedmont (Vokes, 1957).

The Bethards Well, in Worcester County, reached the crystallinebasement at a depth of 7,154 feet. It penetrated a dark, greenish-black rock similar to the Baltimore Gabbro(Vokes, 1957).

The interface between the crystalline rocks and the overlyingsedimentaries is irregular. The general level of the surface tendsto slope steeply away from the Fall Line. Maximum slope is about125 feet to the mile; however, it is only about 43 feet to the mileunder Calvert County, and under the central and western counties ofthe Eastern Shore. It steepens as the Atlantic Coast is approached.

The sedimentary rocks of the Coastal Plain comprise a wedge of LateMesozoic and Cenozoic deposits. These strata thicken southeastward

and eastward from a feather-edge at the Fall Line to as much as8,000 feet near the Atlantic Coast Line (Pickett, 1976). Theycontinue to thicken seaward to as much as 40,000 at the edge of theContinental Shelf. The strata dip to the southeast, and becomeless steep with decreasing age of the geologic unit (Pickett, 1976,p.2).

The depositional area lies astride the axis of the SalisburyEmbayment, at least through Miocene times. The orientation of theaxis is not precisely known, and almost certainly shifted throughtime.

The Coastal Plain strata display major up-dip/down-dip facieschanges within the emerged segment of the wedge. Such facieschanges are a source of confusion in nomenclature and correlation(Pickett, 1976).

At a depth of 5,300+ feet in the Hammond Well, and 6,700+ feet inthe Bethards Well, a series of red and green conglomerates, sand-stones, and shales were encountered. They are similar to those ofthe Upper Triassic Newark Series of the western Piedmont. They arethought to be an easterly extension of the Neward Series, and arethe oldest known sediments in the Coastal Plain section (Vokes,1957).

The sediments of the Potomac Group, the basal sediments of theCretaceous in Maryland and Delaware, are of continental origin.They are fluviatile, lacustrine, paludal and swamp sediments. Theyare some 600 feet thick along the edge of the Piedmont Plateau, butthicken to 5,380 feet thick near the coast line (Vokes, 1957).

The basal unit within the Potomac Group is the Patuxent Formation.It is comprised of unconsolidated sand and gravel.

Superimposed on the Patuxent is the Arundel Clay. This is composedof red and brown clay, and includes layers and concretionary massesof sandstone, cemented with iron oxide or iron carbonate, andgeodes and nodules of iron carbonate and limonite (Vokes, 1957).

The uppermost unit of the Potomac Group is the Patapsco Formation.It is comprised of sand and clay, which are highly colored andvariegated red and brown. The clays tend to predominate, andlocally contain iron carbonate. Lignitic beds occur in the unit.The Potomac Group is considered to be Lower Cretaceous, perhaps,some 120 million years old. It is the thickest sedimentary forma-tion in Delaware. The deposition of the Potomac Group was followedby a period of erosion or non-deposition. A non-conformity exists,which represents the encroachment of the sea over much of Delaware(Pickett, 1976).

111-4111-6111-5

Most of the Upper Cretaceous formations overlying the Potomac Groupare named from sections in New Jersey. Fossil leaves in the twolower units suggest the strata were deposited under continentalconditions. The upper units have marine fossils.

The basal unit is the Raritan Formation. It is difficult todistinguish from the Patapsco, in Maryland, and is comprised ofwhite-to-buff sands and variegated clays.

The overlying Magothy Formation consists of light-colored sandswith minor amounts of clay. Lignite beds occur. It reaches amaximum thickness of 130 feet in Maryland. In Delaware, Pickett(1976) suggests the unit is transitional from stream to marineenvironments.

The Matawan Formation is the first truly marine unit in the Mary-land Coastal Plain section. It consists of dark micaceous sandyclays that contain an abundance of glauconite (Vokes, 1957).Concretions of clay and ironstone are common. It is thought thatthe marine seas were shallow during Matawan time.

In Delaware, Pickett (1976) elevates the Matawan to Group status,and includes within the group the Merchantville, Englishtown andMarshalltown formations. However, Pickett (1976) states that theseformations are not distinguishable south of the C and D Canal, andthe Matawan assumes formational status in the down-dip surface.

The Merchantville Formation in Delaware is a dark-grey to dark-blue, micaceous, glauconitic sandy silt and silty fine sand. Itwas deposited in a fairly shallow, perhaps marine environment(Pickett, 1976).

The Englishtown Formation is a well sorted, micaceous, glauconitic,fine sand with thin, interbedded layers of dark-grey silty sand.It is thought to have been deposited in a low energy sand flat nearthe intertidal zone (Pickett, 1976).

The Marshalltown Formation is a dark, greenish-grey, massive,highly glauconitic, very fine sand. The inferred environment ofdeposition is inner marine shelf (Pickett, 1976).

In Maryland, the uppermost Cretaceous Formation is the MonmouthSandstone. It is comprised almost totally of glauconite. A rich,well preserved fauna of marine invertebrates has been collectedfrom the unit. In Maryland, the Matawan and Monmouth Formationscan be up to 130 feet thick.

The equivalent to the Monmouth, in Delaware, is the Mount LaurelFormation. The unit is glauconitic, fine-to-medium quartz sand,with some silt. The depositional environment may have been embayedmarine (Pickett, 1976).

The Brightseat Formation, Paleocene age, is widely present in thesubsurface of the Coastal Plain. It does not crop-out within themap area (Vokes, 1957). The dark-grey micaceous and sandy clays ofthe Brightseat are unconformable with the Monmouth Formation. Theycontain in their lower portion some reworked Upper Cretaceousfossils. The Brightseat is some 70 to 100 feet thick.

In Delaware, the Rancocas Group spans the Late Cretaceous to EarlyTertiary time (Pickett, 1976). It is a heterogeneous array ofmainly glauconitic, marine units. In the subcrop area, the groupincludes the Hornerstown and Vincentown formations. Down-dip,these become a thick clay-rich sequence that has not been formallynamed (Pickett, 1976).

The Hornerstown Formation is a fine-to-medium, greenish, highlyglauconitic sand and sandy silt. It is the Delaware equivalent ofthe Brightseat Formation, and was deposited on an inner marineshelf environment.

In New Jersey, the Manasquan Marl rests unconformably upon theVincentown. The lower part of the Mansasquan is composed chieflyof glauconite, but the upper part is made up of very fine sandmixed with greenish-white clay. Total thickness is some 25 feet.It is generally succeeded unconformably by Tertiary or Quaternarydeposits, but locally may be overlain by a bluish marl of laterEocene age (Kummel, 1940).

The Lower and Middle Eocene Aquia and Nanjernay Formations havelong been among the best known of the Eocene formations of theAtlantic Coastal Plain. The Aquia is a clayey glauconitic sand-stone. The unit is up to 100 feet thick in the subsurface ofMaryland.

The Nanjernay Formation is also comprised of glauconitic sands. Atthe base, there is a pink clay, some 10 to 30 feet thick, which isknown as the Marlboro Clay (Vokes, 1957). The Nanjernay unit isgenerally less than 100 feet thick. It was deposited in an innershelf environment.

In Delaware, on the up-dip side, the Nanjernay passes into a sandyfacies, the Vincentown Formation. The Vincentown is a green andgrey, fine-to-coarse, highly quartzose glauconitic sand, with somesilt. It is more quartzose than the Hornerstown, and was depositedin a shallower portion of the shelf (Pickett, 1976).

In Maryland, the Aquia and Nanjernay formations are unlike otherCoastal Plain deposits. They are not blankets of sediments. Theywere deposited in a channel or trough that crossed the northernpart of the Eastern Shore (Vokes, 1957).

Oligocene age deposits are not known in the Maryland, New Jersey orDelaware portion of the Atlantic Coastal Plain.

The Miocene deposits of Maryland are referred to as the ChesapeakeGroup. The lowest formation within the group is named the CalvertFormation. The lowest member of the Calvert is the Fairhaven, adiatomaceous earth member. It is comprised of microscopicallysmall tests of diatoms. The lower 20 feet is almost wholly diato-maceous, and is grey-to-white in color. The upper beds contain amixture of clay and diatoms. The Fairhaven Member may be as muchas 60 feet thick. Overlying the Fairhaven is a series of darksandy clays; forminifera and mollusca are abundant. The uppermostmember is known as the Plum Point Marl, and has a thickness of some135 feet in the Calvert Cliffs (Vokes, 1957).

The Choptank Formation is the middle formation of the ChesapeakeGroup. It is easily distinguished by its yellow sands. Generally,the formation is buried beneath younger deposits; it dips to thesoutheast at about ten feet to the mile. The thickness ranges from50 to nearly 100 feet (Vokes, 1957).

The St. Mary's Formation crosses Maryland from northeast to south-west in a belt immediately to the southeast of the Choptank Forma-tion. On the Eastern Shore, it is buried beneath a mantle of LateCenozoic deposits, and does not crop-out within the Wilmington maparea. It is comprised of bluish sandy clays and fine sandstonesthat are extremely fossiliferous, and is especially rich in gastro-pods (Vokes, 1957). The St. Mary's is some 150 feet thick, anddips seaward at 10 feet per mile.

The Chesapeake Group was probably deposited under inner shelfconditions, with shelly, fossiliferous zones that represent shallowmarine conditions. The Chesapeake sediments are generally verysimilar to the overlying Late Cenozoic sediments, and, in part, maybe younger than their assigned Miocene age (Pickett, 1976).

In New Jersey, during Miocene time, the sea invaded the southernportion of the state. During this submergence, sediments nowgrouped under the term Kirkwood were deposited (Kummel, 1940).These beds are predominantly fine, micaceous quartz sand, and, inplaces, they are banded in pink and yellow hues. Black ligniticclays occur, locally, near the base. In Salem County, the Kirkwoodconsists of thick beds, 80 to 90 feet, of brown and drab-coloredclays. Above these beds, there is a fine clayey sand with abundantshells. The unit is termed the Shiloh Marl.

111-8III-7 111-9

In southern New Jersey, the Kirkwood is overlain disconformably bythe Cohansey Sand. The Cohansey is composed chiefly of quartzsand, with local clay laminae, and occasional lenses of gravel. Itforms the surface of the Coastal Plain in New Jersey over a widerarea than any other single formation (Kummel, 1940).

The cycles of deposition of the Miocene Epoch were terminated inEarly Pliocene time by the arching of the Appalachian Region(Kurmel, 1940). The erosional surface of the Appalachian Regionhad been deeply mantled with weathered residuum. This residuum wastransported by the rejuvenated streams over a wide area. TheBeacon Hill Formation of New Jersey and the Bryn Mawr Formation inPennsylvania, Maryland and Delaware were formed at this time(Kummel, 1940). They are units of gravel, sand, silt and clay withcoarser sand, cobbles and boulders near the base. These "gravels"cap some of the higher hills of the area. The Beacon Hill Gravelis chiefly quartz, but contains chert and pebbles of sandstone andquartzite (Kumnel, 1940).

Overlying the older Cenozoic deposits, there is a series of gravelswith sand and silt. In the past, these gravels have been consideredto lie on terrace surfaces cut into the Coastal Plain. The miner-alogical composition of the gravel units are generally similar.Differences are essentially textural, and are enhanced by varioussedimentary structures.

In general, the sands are subarkosic with minor chert and mica.Composition of the gravels vary with size. Generally, the gravelsare quartz, sandstone-quartzite, chert, and a few are crystallinerocks from the Piedmont. The sand-size, heavy minerals are gener-ally ilmenite, magnetite and leucocene. Non-opaque heavy mineralsconsist of zircon, epidote, staurolite, kyanite, garnet, amphi-boles, sillimanite, chloritoid, pyroxene, andalusite, apatite,monazite, sphene and spinel.

The Columbia Formation of Kent County is a medium- and coarse-grained sand with abundant gravel; cobbles and boulders are common.The coarseness of the unit decreases from north to south. Beddingis distinct, and different textures tend to segregate into distinctbeds. The beds exhibit some cross-cutting. Cut and fill and slumptextures exist. The sediments are generally oxidized. Limonite isabundant, and black wad staining is common (Jordan, 1976).

Early in Pleistocene time, the streams in southern New Jerseyceased eroding, and began to aggrade. The Bridgetown Formation wasdeposited. The unit is essentially gravel and sand, with a maximumthickness of 30 feet. The materials are derived from various olderformations. The unit occurs as outliers, capping hills and inter-fluves. After deposition of the Bridgetown, there was reneweddown-cutting and general degradation.

The Pensauken was deposited in southern New Jersey during post-Bridgetown time (Kunnel, 1940). The unit is comprised of sand,and smaller pebbles that are mainly quartz. Pebbles of shale,sandstone, quartzite and crystalline rock occur. In addition,pebbles of chert, water-worn ironstone and glauconite occur, andwere probably derived from erosion of older Coastal Plain sedi-ments. The average thickness of the Pensauken is 10 to 20 feet(Kummel, 1940).

A subsequent period of prolonged erosion partially removed thePensauken Gravel. In southern New Jersey, terraces were formedalong the coast. Deposits of sand and gravel occur at low ele-vations. These deposits extend up-valley to elevations of 140 or150 feet (Kummel, 1940), and are known as the Cape May Formation.

Along the coast and lower Delaware River, terraces of Cape May ageare not more than 40 feet above sea level, and are lower than thePensauken terraces (Kummel, 1940). Along tributary streams, theyrise to greater elevations than 40 feet.

In latest Pleistocene and Holocene times, alluviation along largerstreams and silting of shallow lakes and ponds occurred. Beds ofpeat formed. Along the coast, barrier beaches have been built fromManasquan southward. Broad and shallow lagoons have been formedbehind the barrier beaches (Kummel, 1940).

C. DESCRIPTION OF GEOLOGIC MAP UNITS

(Modified from legend of "Geology of the Wilmington Quadrangle" -Mineral Resources Development, Inc., 1979).

Cenozoic - Quaternary

Qma: Marsh and Alluvial Deposits

Qbs: Beach Deposits

Ql: Lowland Deposits

Gravel, sand, silt and clay; medium- to coarse-grained sand andgravel. Cobble and boulders near base.

Qcm: Cape May Formation

Sands and gravels, with clay and silt, locally, at the base.

Qpb: Pensauken and Bridgeton Formation

Deeply weathered gravels and sandy gravels.

Qup: Upland Gravels

Gravel, sand, silt and clay. Mostly cross-bedded, poorly sorted,medium- to coarse-grained sand and gravel.

Cenozoic - Tertiary

Tbm: Bryn Mawr Formation ( Type not encountered during survey.)

High level terrace sands and gravels; some silt.

Tbh: Beacon Hill Formation

Tch: Choptank Formation

Interbedded, brown-to-yellow, very fine-grained sand, and dark-greyargillaceous silt.

Tco: Cohansey Formation

Tc: Calvert Formation

Dark clays and fine-grained sands, with prominent local shell beds.

Tk: Kirkwood Formation

Ta: Aquia Formation

Green, argillaceous, glauconitic, well sorted, fine- to medium-grained sand.

Tra: Rancocas Group

Includes Hornerstown, Vincentown, and Manasquan formations.

Mesozoic - Cretaceous

Kmo: Monmouth Formation

Dark-grey to reddish-brown, micaceous, glauconitic, argillaceous,fine- to coarse-grained sand.

Kma: Matawan Formation

Dark-grey, micaceous, glauconitic, argillaceous, fine-grained sandand silt.

Km: Magothy Formation

Loose, white, cross-bedded, "sugary", lignitic sands, and dark-grey, laminated silty clays.

III-10 III-11 III-12

Kp: Potomac Group

Interbedded, quartzose gravels, argillaceous sands, and multi-colored silts and clays.

Pal eozoi c

Ocs: Conestoga Formation

Bluish-grey, thin-bedded, impure, contorted limestone with shalepartings; conglomerate at the base.

Gu: Cambrian Sedimentary Rocks, Undivided

Xgr: Granite Gneiss and Granite

Unit includes the Springfield granodiorite, granitized Wissahickonand related rocks.

Xs: Serpentine

Serpentine, steatite and associated products of alterations ofperidotites and pyroxenites.

Xhg: Hornblende Gneiss

Unit includes rocks of probable sedimentary origin; may be equiv-alent to the PGg unit.

Xcs: Cockeysville Marble and Settlers Formation

Marble, feldspathic quartzite, mica schist and mica gneiss.

Xpc: Peters Creek Schist

Chlorite sericite schist with quartzite.

Xw; Xwc: Wissahickon Formation

Xwc: albite chlorite schist; includes octararophyllite, andsome hornblende gneiss and granitized members.

Xw: Orthoclase mica schist; includes some hornblende gneissmembers, some augen gneiss, quartz and feldspar-rich membersshowing various degrees of granitization.

Xpd: Port Deposit Gneiss

Moderately-to-strongly deformed gneissic biotite quartz diorite,hornblende-biotite quartz diorite, and biotite granodiorite.

Precambrian

PGgr: Granite Gneiss

PGg: Gabbro Gneiss

Includes rocks of probable sedimentary origin. It may be equiva-lent to Xhg.

PGv: Volcanics

Metamorphosed andesitic and dacitic volcanic rocks.

Miscellaneous

unk: Unknown Geologic Type

D. RADIOACTIVE MINERAL PROSPECTS IN THE SURVEYED AREA

Delaware

"There is no production of uranium in Delaware and no known uraniumdeposits..." (Southern Interstate Nuclear Board, 1969). However,radiometric anomalies have been noted in the clays of the PotomacFormation, the Rancocas greensands, and in the Miocene brown clays(Southern Interstate Nuclear Board, 1969).

Maryland

There are no known uranium deposits in Maryland (Southern Inter-state Nuclear Board, 1969).

New Jersey

Thorium-rich minerals have been noted in certain of the beach sandsin Atlantic, Cape May and Ocean counties. They are not of economicsignificance (Cooper, 1958). In Burlington County, radioactivityhas been traced to the black and blue-black glauconitic sands ofthe Hornerstown Formation. The deposits are not of economicsignificance.

Pennsylvania

Radioactivity occurrences occur in both Chester and Delawarecounties, but none of economic significance appear to occur withinthe confines of the map area (Cooper, 1958).

111-13 111-14

SECTION I

RESULTS OF DATA ANALYSIS

SECTION IV.

RESULTS OF DATA ANALYSIS

A. DESCRIPTION OF STACKED DATA PROFILES

1. Multivariable Radiometric Stacked Data Profiles

These profiles are presented at a horizontal scale of 1:500,000.The vertical scales are:

Altitude: 100 feet/div.; aircraft altitude above the surface

TL(208TQ)* .75 ppm/div; 7.24 c/s = 1 ppm/eTh

BI( 2"4Bi)* 0.25 ppm/div; 13.85 c/s = 1 ppm/eU

K (40K)* 0.15 %/div; 105.0 c/s = 1%K

BiAir 2.5 c/s/div. 50 seconds averaged

Residual Magnetic Field 100 gammas/div. (See Sec.V.B.1)

GC (Count from 400 keV to 3.0 MeV) 250 c/s/div.

Bi/TL 0.07 /div.

Bi/K 0.5 /div.

TL/K 1.0 /div.

Geology Strip: An approximate six-mile width of the geologymap, containing each line, is displayed abovethe profiles.

* 7-second average weighted 1:2:3:4:3:2:1 is used and plottedat center.

2. Residual Magnetic Field Profiles

Altitude: 100 feet/div.

Temperature: 1.0 C/div.

Pressure: 3 mm of Hg/div.

Base Magnetic Field: 10 gammas/div.

Residual Magnetic Field: 10 gammas/div.

IV-1

Geology Strip: An approximate six-mile width of thegeology map, containing each line, isdisplayed above the profiles.

All profiles appear in Section IV.H.

B. SINGLE AND AVERAGE RECORD LISTINGS

Single and average record listings are provided on microfiche.Samples of each type are presented in Appendix III.

C. STATISTICAL PRESENTATION OF DATA BY GEOLOGIC TYPE

Tables IV.(1-6) contain the average value of each variable as afunction of line number and geologic type. The tables are in ordereTh, eU, K, eU/eTh, eU/K, eTh/K.

D. FREQUENCY DISTRIBUTON OF DATA FOR EACH GEOLOGIC TYPE

Table IV.7 contains the mean, standard deviation, and number ofevents for each geologic type encountered over the entire mapsheet. Histograms for these data appear in Section IV.H.2.

E. DATA INTERPRETATION

1. Analysis of Geologic Histograms

The radioactivity data is shown in histogram form with partsper million or percent plotted against number of events(Appendix I). The histograms for 2 08

Te and 40K were examinedfor conformity to a Gaussian curve. It is generally assumedthat a geologic map unit, which encompasses a fairly homogeneouslithology, would have a unimodal distribution. Where mapunits vary significantly from a unimodal distribution, afurther subdivision into more homogeneous lithologic types maybe recommended. Table IV.8 shows the map units, which varyfrom a unimodal model, and for which separation of two or moredistributions is feasible. Only units with excess of 200events are considered.

2. Discussion of Anomalies

Introduction

The 218 T Q , 2 14 Bi, and 2 1 4 Bi / 2 0 8 T (ratio) data were examinedfor anomalous values. An anomaly is defined by a minimum oftwo adjacent, two-standard deviation values, or a single,three-standard deviation value. The anomalies were listed byflight line in Table IV.9; by geologic map unit in TableIV.10; Table IV.10 is statistically summarized in Table IV.11.Only positive anomalies were examined for 2 08Th and 214Bi, butboth positive and negative values were studied for the ratioanomaly.

IV-2

OBS )L 0CM OPB OIJP5

12101618131010895

1225

363443

ML 14L 2ML 3ML 4'L 5ML 6ML 7ML 8MI. 9MLA0Mbl IML12TL 1TL 2TL 3T[ 4TL 5TL 6

OMA191418123216

913101513181511131219

23393328331R4242272536462017232543

THH TCH263A

4142

565460b5

7177

1428

TCt) VC TK TA TRA KMC) KMA KM KP tiCS

20222722232323191531172.376

4251

3034

45

4333

R0

24 5

416937362927

2526

33

6 4

77383740

49 5255

3429

30 17

44 41 25

53 2456 76

CU XGR XS XH( XCS XPC XWC Xw XPD PCGR PCG PCV INrK

67

107869689

979294

92 72

6991 88 87 74

44 6677

86 60104 60

74 7163

Geologic Unit Average Value as a Function of Map Linefor eTh (PPM Times 10)

IV-3

42

29384039403835793118293468

354772

84763

233344

ML

MLM LI

123

64

ML 4ML 5ML 6M4 7ML 8ML 9MLI0ML11ML12TL 1TG 2Ti 3TL 4Ti 5TL 6

99107

9483 69

7166

50

677071

Table IV.1

OMA OR S . QCM8 3 116 6 145 5 115 7 10

10 14 12 127 12 12 63 3 14 135 5 125 4 107 8 108 3 169 196 4 74 6 55 64 76 1?

11

OPR QUP12121216

9 1512 17

ML 1ML 2M1, 3ML 4ML 5M[, 6ML 7ML 8ML 9M1L10ML1 IML12TL ITL 2TL 3TL 4TL 5TL 6

161917

TEU TCH TCO TC TK TA TRA KMr KMA KM KP OCS7

510

1113

131311

b 158 999R9998

1057

118

219 1h

102015161615

t012

1727161020

12 11 7

11to 14

CU XGR XS XHG XCS XPC XWC XW XPD PCGR PC( PCV LiNK

1921 20

1 y

1720 1 21

Table IV.2 Geologic Unit Average Value as a Function of Map Linefor eU (PPM Times 10)

IV-4

12121313171510

69

1018

171517

15 1915

16 1116 13

2412 11

51 316

18

220

ML IMl.. 2ML 3ML 4M I[ 5ML 6ML 7ML 8ML 9ML10ML11ML12

TI, 1TI. 2TL 3TL 4T I 5TL 6

16 18

2321

1429

161917

15212019

19 17

1I11 16

1714

14 1029 14

1714 14

23

ORS244036394231178141b13

1749

()P OLIP91

109104106

28 11143 10642 10044 11147 93

ML 1

ML 2ML 3ML 4ML 5ML 6ML 7ML 8ML 9ML10ML1IML12T L ITb 2TL 3TG 4TL STb 6

TBH TCH

67QNA

5334382545

322424122311152016202838

TCO TC TK TA TRA KMO K MA K KP OCSQL 0CM74

775139

63 4971 2551 55

61383942741625333376

60132

95

10297

118115

11 041 93

499263541519

3130

12784

U3

1116773

124

P7 A2 34

8062 87

CU XGR XS XHG XCS XPC XWC XW XPf PCGR PCG

94106101

158188 182

190

8775

145130150

156 140

62

135118

94161 134 129

105

PCV IP'K

45 59

96124

90

10R

Table IV.3 Geologic Unit Average Value as a Function of Map Linefor K (PC Times 100)

IV-5

49554622145240

107

1119

20232R22241R8201315

21111633

7696

116

91 7054

63 50

64 6180

81 64

124873

M[,MbML

123

1 28

32100 68 155

ML 4ML 5ML 6ML 7ML 8ML 9ML10MbI 1ML12TL 1TL 2TI, 3TL 4Ti 5TL 6

10398

I 10109 85

134

QPB (tiP34333030

31 2832 3()32 2530 2734 23

Mil 1ML 2I, 3

ML 4Ml 5

ML 6M , 7ML 8ML 9ML 10Mi,11Mt 12TL 1TL 2TL 3TL 4TL 5Tt 6

QMA5751385534514754635771533546483733

TBH TCH31

GAS73574453

1131325170539358

2729

T'Cf TC TK tA TRA KV KMA KM KP oCSOL QC +56394040

36 4636 3929 35

34

434448433527272729

29

4R

333121

2732 30

2942465459

4449

2527

31 39 3925 27 3335 2443 4943 57

524250

45 64

27 32 31

2125

392R

CU XGR XS XHC, XCS XPC XWC XW XP() PCGR PCG PCV IUIiK

2219 21

22

2522 19 24

Geologic Unit Average Value as a Function of Map Linefor eU/eTh (Times 100)

IV-6

3652523245323226

4135

2627

35394o45424242526537393733

1013026

2R

MLMLML

123

24 22

ML 4ML 5ML 6ML 7L B

ML 9ML1OMi11ML12TL 1TL 2TL 3TL 4TL 5TL 6

2425

3030

26

242925

222121

21 24

74

1728

27

27 2474

1723

2521 24

19 2136

Table IV.4

QBS19821718129721763901447028157098285560202341

27211393

OPH QUP146612271258

15883786 14533299 17923497 19313064 17993427 1923

MML 1ML 2ML 3ML 4ML 5ML 6ML 7ML 8ML 9MLI10ML 114[,12

TL 1T16 2

TG 3TL 4TL 5TL 6

TBH TCH1162

OMA18612014175827172251261226503787650661878732735435354535471314561620

TCO TC1515

OL (ACM

2498250629733199

2128 34191730 32762667 2883

3493382636675070286750842510222621621720

19848731489

TK TA TRA KMO K'iA KM KP [CS

143312081353

854

R75992

19851993

18632455250072371 R37

257722022842317211394

9560

45024282

130

1694 2765 18522803 1633

1482591 22902655 2275

32241670 1747

624030972404

1414

13A5 1606 2356

1316 26781644 2065 2429 1162

CU XGR XS XHG XCS XPC XwC Xw XPI PCGR PCG PCV UNK

180619171755

12401202 1152

1061

20781990

152015581350

1298 1242

18291267 1262 1671

24647754

7684 2755

1103 11042540 1155

21 311409 1658

2224

Table IV.5 Geologic Unit Average Value as a Function of Map Linefor eU/K (Times 1000)

IV-7

31055731455350575714255128951702

54095461

3397440140744982489761695904771264555377633655492713

MG

MLM 1,td U

1234

ML 5ML 6ML 7ML 8ML 9ML10ML11M(,12TL 1T t, 2TL 3TL 4TL 5TL 6

22962164

16702672

2695

1376

QBS1525301229604460415139545111

12570563564225260

72754761

1111

QPH QOlP4322389641975370

1667 51520307 57070715 69620174 6630(9668 8725

ML 1

ML 2M[. 3ML 4ML 5ML 6ML 7Ml 8ML 9ML10

ML11ML12TL 1TL 2TL 3TL 4TL 5TL 6

TRH TCH3847

(MA36174297440854126711538946366927

11317129281315313851

847010275920040034949

QL 0CM421464317149816R

6214 81314801 79748445 8317

1019396278487106996598

131918634812976715963

7076

TCO TC422279993564

10138 450011355 3916

1052111744123911525214834156841202714875]733115051

811934243723

TK TA TWA Kr.O KMA KM KP OCS

72967649

4125758469677016

2056016337

103948929

4743

729169366037519H3775

5443 7293 502910263 5049

624R5567 48734R35 5565

63283692 2727

5113 5034 7379

6075 74306394 7509

55331n320

9706

5166

9890 5308

CU XGR XS XHG XCS XPC XWC XW XPD PCGR PCG PCV ITAK

99119385

91788542

6292

746R68246740

54706000 5290

4692

815994975090

680971806399

5995 5194

73635667 6606 6958

10091 9918 111629241

6404 63108889 4984

89567279 8045

6019

Geologic Unit Average Value as a Function of Map Linefor eTh/K (Times 1000)

IV-8

98211016

93191466814911

799188686409

1275315376

33035505

ML 1Mb 2ML 3ML 4ML 5ML 6ML 7ML 8M, 9ML10ML1 IML12TI 1TL 2Tb 3TL 4Tb 5TL 6

Table IV.6

eTh eU K eU/eTh eU/K eTh/K MAX. GEOL.x E N O .I ax zx 0 x Qx a X EVENTS UNIT

1.2117!'.92501.75321.96301.SC61

1.73480.78860.75381.08341.15511.54732.52391.70461.16122.03462.15811.68411.17082.36543.63611.58371.46031.49141 .03411.13351.53171 .44202.k0391.63100 .5606

1.54.13.23..r,5.')2.77.6

2.14.13.65.44.73.k

4.44.65.76.99.39.4R.17. *

1".70.3U..24.17.19.16.64.4

01.40410.46750.4860.61220.71P90.44740.21930 30333

0.3x+58( .377 90.53A10.57630.55790.48050.60600.61520.49600.33360.72450.45970.41150. 46P0.47560.3409U. 34250.43700.371 11.01 38n. 51 026.1710

f1.6

1.21.11.71.4

() .N

0.9

1.71.51.51.91.51.71.51.5

1.82.53.0

2.11.82.17.02.02.11.72.11.5

1.2

0.21750.17850.( 147

0.36610.778 80.7773

0.05940. 17120.14420.73500.)R64

0.77100. 15940. 19960.23360.3439

0.26200.20390.1675

0.21240.14010.19260.4390

0.1967

0.26710. 5020.19700.27070.22760.0714

('.3n.30 .

1.1

0.41.0'.7

0.70.q1.10.40.Q

1.00.71.7

0.9

1.11.21.1

1. *1.91.91.51.40.81.2

1.10.4

0.307?0.571t30.13430.19460.17890.0$390.12550.15A5

0.27990.10490.17020.19540.13940.21500.15701.11670.123I0.07040.07A60.1 3030.05100.07290 . 0 06

".04730.04150.048)

0.04360.07560. 06920.0466

0.5'1 40'.72170.*3190

('.344M. 3'+71 .367 30. 3015S

0.39710.31390.4765().31590.4520

0.34570.43080.4386

0.41740.34000.2920.27040.2704'). 30670.2580.26130.1Q700.22160.71530.22650.24230 .22520.73190.2704

3.50301 .8540.77351 .Q684

7.5299

0.53117.24Q10.41453.3019

039465. 702 (2

0.34670.75160. P9210.79960.*66711.00430. 2523(.92470.60 13

3.43 890.5603

n.4039

0.23650.7550.3799n.51Q30. 86140.61140.6205

3.7717

3.0107?. (Q772.9333.69011.43485.43791.16725.726',1.1 9795.6720

1.94162.14142.14512.58931.6'.P2.73361. 3S892.77642.67247.17531.90361.70261.15961.29501.53277.22021.74761.47572.6"44

5.6994

2.35892. 1967

4.12534.8875

1.75714I"5010. 5$046.5454}.4 3557.24471.77012.03861 .0940

1.91251.77552.37011.07532.77671.84371.50091 .55861 .60663.56440.72301.2914

1.k4082.0957

7.25101.2937

7.59524.79966. 597.77R

10.25454.91R6

14.20073.9479

12.97534.A563

11.65606.28625.35745.234P6.5714S.1323

.6225.19799.19739.39559.32447.40706.0004

5.24576.04926.87599.25777.60366.4649

9.91k3o.7296 6.6 0.3351 1.6 0.0693 0.6 0.0460 0 .445 0.6936 2.7555 1.0931 11.1677

4730

24A'24976q

409737064958

7923

6455299

84790

194310255704763

72457389

59843

242215

1798196486401

5222

09

0 I,

011 P

TRH

TCHTKrTr

TN

TPA

Ri( P

K M

KM

Kp1CS

C.9YGR

xsxHG

x PCxpCxwxPr)PCC.RPC GPCV[INK

Table IV.7 Mean (X) and Standard Deviation (a) for Each Geologic Type.

IV-9

Geologic Units with Significant Variations from UnimodalDistributions, Based on the Analysis of the eTh Histograms

208TL ReconendedGeologic Unit No. Events Split (c/s)

TABLE IV.8

QmaQbsQlQcmQpbQupTcTkKmoKmaKmKpXpcPGgrPGg

4709224266409732064954288847310255204259242486403

nonenone46;nonenonenonenone51;47;51;52;47;none103;none

IV-10

TABLE IV.9 Sunmary of AnomaliesTABLE IV.10 Radioactivity Anomalies per Geologic Map Unit

20O8TI 214Bi 208T.

ML1WML 1E

Qma,920-930;

ML2W Qcm,1150-1165;

ML3 Qcm,2715-2735,2760-2775

M4E Qcm,5905-5965;

ML4W Qup,460-470;

ML5 Qma,1530-1540,1470,1450-1455,1200-1250;Qcm,l170-1185;

ML6 Qpb,4165-4185,4200-4210,4230-4250;Tco,4250-4265,4280-4285;Qma,4665-4670;Km,5120-5125;

ML7 Kmo,3100-3105,3150;Qcm,3320;Qpb,3615-3690;

ML8 Qpb,1430-1450;Tco,1460-1500;Qma ,1525-1535;Qpb,1580-1610;Tk,1640-1660;Qma,1 790-1825;Qup,2040-2055,2345;

ML9 Tco,3340,3390;

ML10 Tco,3635-3640,3655-3680,3875;Kma,4960-4965,4980;

ML11E

ML11WML12E Qpb,1160-1175;

ML12W PGgr,160-180;

Qma,2770-2775;

Qup,025-040,065-070;

Qma,1205-1240;Qcm,1175-1180;

Tco,4255-4260;Qma,4670;Km,5120-5125;

Kmo,3105-3110;Qcm,3305-3310;Tk,3620;Tco ,3700-3705;Tco,1450,1470-1500;Qcm,1640-1660,1790-1795,1810-1815;Qup,2035-2065,2260;

Qma ,2460 ;Tco ,3380-3390;

Tco ,3660-3675 ;Kma ,4510,4660-4670 ;Xw ,5335-5340;

Qpb,1430 ,1530 ,1545;Qcm,1750-1760;Tk,1850-1870;Qma,l 840;Tk,1880-1885;Tco,1910-1920;

Qma,1050;Qcm,1135-1175;

PGgr ,170-180;

Qup,310,460,695-700;Qma,4045-4055;Qcm,4100-4115,4150

Qup,1335-1340,1360,1585,1605-1610;

Qup,2065,2310-2315;Qcm,3780-3800;

Qcm,5155

Qcm,2385;Qma,2730-2740;

Qbs,2850;Qma,2990;3000;Qcm,3030;Tco,3725-3730,3870;

Qpb,4240-4245,4265,Tco,4550;

Qma,475,540,610;Tco,625,670;

Xw,1980 ;Qcm,2475 ,2490,2500 ;Tco ,3220 ;Qma ,3550 ;Tco,3615-3620;Qpb,3720;

Kmo,4465;Qma,2960,3280-3290,3315;

Qpb ,1835-1840 ;Tco ,1880-1895,2160-2170;

PGg,930;Tco,510,550,570,580,650,690,700,725;Qpb,840-845,1210;Xpc,485;

TL 1

TL2

TL3 Kma,050;

TL4 Tco,4795-4800;

TL5 Qcm,3165-3170;Qma,3120;. Qcm,3680-3690;Qcm,3665-3670;

TL6 Qup,1345-1360,1200-12201235-1245;

Tco,2990;Qpb,3065-3070,3090;

Qma,440;

Qma,2960;

PGg,2265;

Geologic Unit 208Tt 2 14Bi 214Bi/2 o 8

QmaQbsQcmQpbQup

TcoTk

KmoKma

XpcXwPGgrPGg

90876

8

23

00

0

50834

63

2

0

10

IV-llbIV-llaIV-12

1521089

130

00

02

20812, 214Bi 214Bi/208T2,

60 .f 9 Ao

(TABLE IV.9 Cont'd.)

TABLE IV.11 Statistical Summary of Radioactivity Anomalies by Geologic Unit

Geologic Unit 208T 214Bi 2 14Bi/ 208 TL

QuaternaryNo. of Units w/AnomaliesNo. of Anomalies

TertiaryNo.- of Units w/AnomaliesNo. of Anomalies

MesozoicNo. of Units w/AnomaliesNo. of Anomalies

Paleozoic/Precambrian

No. of Units w/AnomaliesNo. of Anomalies

Total SampleNo. of Units w/AnomaliesNo. of Anomalies

4 430 20

29

36

1

29

34

22

10 1146 35

544

13

1

34

1062

Relationship between Radioactivity Anomalies and the GeologicMap Units

Quaternary Geologic Units: Qma,Qbs,Qcm,Qpb,Qup208TH Anomalies

Sixty-five percent of the 2 o8 TR anomalies occur in fourQuaternary units, these units occupy some fifty percent of the

surveyed area. The radiometric anomalies are evenlyddistri-buted amongst the four units (Qma,9; Qcm,8; Qpb,7 and Qup,6).Great variety in type and lithology of the sediments occurs inall four units. This, coupled with considerable variation innear-surface drainage and water-table conditions, probablyaccounts for most of the anomalous readings. However, placerdeposits with minerals derived from the Piedmont may occur.There are no incidences of

2 08T9 anomalies coinciding withratio anomalies.

214Bi and 214Bi/ 208TL Anomalies

Fifty-seven percent of the "4Bi anomalies, and seventypercent of the "

4Bi/2 0 T9 anomalies, occur in four and five,respectively, of the Quaternary units. These units occupysome fifty percent of the surveyed area. None of the 214Bi

anomalies coincide geographically with the ratio anomalies.Most of the anomalies are thought to be the result of eitherintra-unit changes in lithology or intra-unit changes in near-surface hydrology. In some cases, there may be placer depositswith material derived from the crystalline Piedmont rocks.

Tertiary Geologic Units: Tco,Tk

208Tt Anomalies

Almost twenty percent of the 208 TZ anomalies occur in two

Tertiary units, Tco and Tk. Most of the anomalies are in theTco unit (8), which occupies over nineteen percent of thesurveyed area. None of the anomalies coincide with ratioanomalies. Unless some of the deposits are placer, most ofthe anomalies are due to intra-unit changes in lithology andvariations in lithofacies.

214Bi and 214 Bi/ 208 TL Anomalies

Twenty-five percent of the 214Bi anomalies, and almost twenty-

one percent of the 214Bi/20 8 TZ anomalies, occur in two andone, respectively, of the geologic units. All of the ratioanomalies and two-thirds of the 214Bi anomalies in the Tertiaryunits occur in unit Tco. Tco occupies some nineteen percentof the surveyed area. None of the the 214Bi anomalies coin-

cide with ratio anomalies. Unless some of the anomalies areplacer deposits, which are also rich in thorium minerals, itseems unlikely that any of the 214Bi anomalies are associatedwith significant uranium ore concentrations.

Mesozoic Geologic Units: Kmo,Kma,Km

2OIT Anomalies

Some thirteen percent of the 208Tz anomalies occur in threeMesozoic units, which occupy two to three percent of thesurveyed area. None of the 208TH anomalies coincide withratio anomalies. Placer deposits are the most likely sourceof thorium-rich minerals within the Mesozoic units.

214Bi and 214Bi/ 20 8Ti Anomalies

Greater than eleven percent of the 214Bi, but less than twopercent of the 214Bi/ 2 08TE anomalies, occur in Mesozoic units.The units occupy less than three percent of the surveyed area.None of the 214Bi anomalies coincide geographically with theratio anomalies. Most of the 21 4Bi anomalies are thought tobe associated with either intra-unit changes in lithology orwith lithofacies changes. Some may be associated with uraniumand thorium-rich minerals in placer deposits.

Paleozoic and Precambrian Geologic Units: Xpc,Xw,PGgr,PGg

208T Anomalies

One 2 08T9 anomaly occurs in the PGgr unit. It may be associ-ated with a vein deposit, a pegmatite, or a change in lith-ology within the granite gneiss. It does not coincide geo-graphically with a ratio anomaly.

214Bi and 214Bi/ 208TL Anomalies

Greater than five percent of the 214Bi anomalies, and sixpercent of the ratio anomalies, occur in two and three,respectively, of the Paleozoic/Precambrian geologic units.These units occupy greater than six and seven percent,respectively, of the surveyed area. None of the 214Bi anoma-lies coincide with ratio anomalies. Most of the anomalies arethought to be associated with intra-unit changes in lithology;some, however, may be associated with either vein or pegmatiteunits.

(...) denotes negative anomalyIV-14 IV-15

IV-13

Relationship between Radioactivit Anomalies and KnownOccurrences of Radioactive Minerals

There does not appear to be any coincidence between thelocation of the radioactivity anomalies, and specific sites,where radioactive minerals or anomalous radioactivity havebeen previously recorded.

Relationship between the Occurrence of Radioactivity Anomaliesand Cultural Features

208T9 Anomalies

An anomaly on ML2, station 1150-1160, is near the Dover AirForce Base in Kent County, Delaware.

214Bi Anomalies

Three 2 14Bi anomalies on ML11, between stations 1450 and 1550,are near the Marlton urban area, on the eastern side ofPhiladelphia.

214 Bi/20 8Tk Anomalies

Two ratio anomalies on ML6, stations 3725-3730 and 3870, aresoutheast and south of the town of Vereland in New Jersey.

Trends208T2 Anomalies

The eastern half of the map sheet has very few 208TQ anoma-lies. The westcentral portion of the map area, in south-western New Jersey and northern Delaware, has the greatestconcentration.

A large cluster of anomalies is noted between TL4 and TL6 andML4 and ML8. The area involved has a variety of Cretaceous,Middle and Early Tertiary, and Quaternary outcrops. It lieson either side of the Delaware River, to the south of Phila-del phia.21 Bi Anomalies

The distribution of 214 Bi anomalies is extremely uneventhroughout the surveyed area. Two major clusters are appar-ent.

East of Philadelphia, north of ML10 and west if TL2, Bianomalies occur over Quaternary, Tertiary and Cretaceousoutcrops.

South of Philadelphia, between TL4 and TL6, and north of ML5,a larger cluster occurs on both the eastern and western sidesof the Delaware River. The anomalies occur over a variety ofMesozoic and Cenozoic outcrops.214 Bi/20 8TZ Anomalies

The ratio anomalies are unevenly distributed throughout themap area. Very few ratio anomalies occur in the centralportion of the surveyed area or in the northwestern corner inPennsylvania. Two areas of anomaly concentration occur.

In the northeastern quadrant, north of ML8 and east of TL3, alarge number of anomalies are recorded over the Quaternary andTertiary units of the New Jersey Coastal Plain. Most of theseratio anomalies have very limited areal extent.

In the southwestern corner, to the west of Delaware Bay,anomalies occur on ML1, ML2 and ML3. Most of these anomaliesoccur over the Quaternary units.

3. Sunary and Recommendations

The area can be divided into two major physiographic andgeologic units; the crystalline rocks of the Piedmont and thesedimentaries of the Coastal Plain. The Piedmont area issmall, and confined to the northwestern corner of the maparea. It has very few anomalies. Most of the anomalies arein the Coastal Plain. The 214Bi and 208Th anomalies concen-trate in the central part of the map area, in western NewJersey and northern Delaware. Mainly they are to the south ofPhiladelphia. The anomalies crop-out in a variety of sedi-mentary units, which range in age from Quaternary to Creta-ceous. The 214 Bi anomalies are also concentrated in the areato the east of Philadelphia, in the Mesozoic and Cenozoicoutcrops. The 214 Bi/ 20 Th anomalies are mainly in the north-eastern corner of the surveyed area over the New JerseyCoastal Plain.

Most of the anomalies are in Quaternary units, or in theextensive Cohansey Formation. The Quaternary units and theCohansey occupy seventy percent of the surveyed area. None ofthe 214 Bi or ii anomalies coincide geographically withratio anomalies. A number of 208 Th anomalies do coincide with214 Bi anomalies. The anomalies in the Quaternary units arethought to be associated mainly with intra-unit changes inlithology or near-surface hydrology. However, placer depositsmay occur within the Quaternary units.

F. NATIONAL GAMMA RAY MAP SERIES (NGRMS)

The geologic base has been photographically screened to allowemphasis of the flight line locations and of the informationregarding data analysis. These maps are used as the base forpresenting statistical information on the six variables:

* TZ

* 214Bi* 4K

* 214Bi/2 08TE Ratio* 214Bi/ 4OK Ratio* 208T*/4oK Ratio

The six NGRMS sheets are presented in Figures IV.(1-6) of thisreport at a scale of 1:500,000 and as separate sheets at a scale of1:250,000.

The statistical information is summarized on these maps through theutilization of one, two or three dots above or below the flightline at every fifth data point. One dot above the line indicatesthat the variable value at that point is between la and 2a greaterthan the mean value for that geologic type where a values aredetermined for each geologic type based on all flight line datafrom the area, as is discussed further in Section V.B.4. Two dotsindicate values between 2a and 3a, and three dots show valuesgreater than 3Q. Dots below the line indicate the variable valueswhich are less than the mean value by 1, 2 or 3a in the samemanner.

G. LINE PRINTER CONTOURS

Printer contours have been generated at a 1:500,000 scale for sevenvariables (eTh, eU, K, eU/eTh, eU/K, eTh/K, RMag, respectively).They appear in Appendix IV. Note that every alternate contourinterval is composed of blanks to help delineate contour boundaries.Dots are used where the denominator value for a ratio is approachingzero, and to denote non-data areas.

IV-16IV-18Iy-17

40

ML 12

MLI1

L 1

ML9

ML8

ML 7

ML 6

ML 5

ML4

ML 3

ML 2

TL4

!.a45



306

N

15

5 0

75*00'

5 t0 15 20WILMINGTON, DELAWARE

25MILES

5 0 5 10 15 20 25 30KILOMETERS

Figure IV.1 National Gamma Ray Map Series

IV.19a

TL 6

.

40e5, 4515750d 4530 15

-- * * --- * -- S n *. ~

7V

2 a*s * E a, *- ..:-o . r ..---3

r t~/ ^ p A PH - CHR ; H IL . 44o ^ '<c * ,. ... IE

- **2.-. ? -0- -9

ht J o * t-. k

tot1 .. qf- _ r ors n ., L / .0

DELAWARE-- A

45'

* *a o .ers l. t r . -a m.

+. d se 1.

Tc

.. - ----

Oi V Ix ppm . G)Z .* 05 c r .

"* I )11I h

r I.+ ax t-se -Ito.

18 i

j{ /( . I'. * t i

ML I

TL3

-

2 08T1 t STANDARD DEVIATIONS

TL 5

. ar"I31sc

004000'

45'

30'

15'

39e00'74 00'

39OQ76.0 r.r

bb

TL I

TL 5

reap 'L415

TL 3

75*0d r 45'7640*00'

ML 10

45'

ML 8

ML7

30

ML 6

ML4

r ieA -

- r

of I

_______ r____ 4j+++..+

. . ..

*_ ' o-

a a -- -0aw

- - -- - ---50-0-

/ J <I,

L . a . , a J ."

00 \%~

~~V DC.V (.R.e

t

0 5 o0

.9 0. 5.

30 5

2 e00

o

f'I j7

30' 15'

L . oe jay*- RIVER

- - ei

"l / " PH A PH V"*.m

1' U

- x "t-1 n

.. *

-00 . <. <0 0 - - -A

-- u

-D 9-0C m , T / /

<'-O- -(J

() Om'..

" $0 .J0

~~Jo

... a.

r2.%>,

Y--'a2w

Y(71

}0

9-.

T 5'

:00

26300

'*~

OM \/

--------

I

Iuo /

oab

t

l

o Pbo'.

a

va.o

o AV%

ocm

Ila00

9 i j 1p i W 'AA

0. N 77- I

DELAWARE BAY

A-

o..

a..

75*00'

bb



- 5

Figure IV.2 National Gamma Ray Map SerN IV.19b

5 I0 15 20WILMINGTON, DELAWARE

25MILES

5 0 5 10 15____ 20 25 30KILOMETERS 214 Bi STANDARD DEVIATIONS

'0TL 6

,, .! 45

7,.

a.6

oa

a .

o3 0 L1 1

I .,

T< I.

T[ 0 .91

15

ML3

ML2

MLI

390 00Q

H " o

\

Y0 O w

1r.7t"

"% O

-~

760d

0 y

l""", 45

39*00

T4 00'7

1301

-

V. : 1 -. "..,..

I i

?r"/?

o<

a.

o ,:.

oON

o.. "+r...r-..-..

TJLLLB- JL

74*00'40 00'

45'

30

15

"

4y -y 6c c-. aw.._

I

. _______.til. l "r-Te-

rsoo o",.

" q t0

o.. o, VO~d-G+.Aw-.... ,

4"___""_..4L-T - "'- ' - " - "- .__ - " I;

_ . rl . 1 . -.. -

t-T..- 4 _

v----... " -. ""-c---" T , " , , , 5% - 9 , 09 - - -&- - A;;D - - , t lb -0 - 11 C1.0 .1 -!o OWY A-.--. -.-. . -- -------------R - 4--.. - - P.-*... .

.o. IOU..L.i

.L.

o+-v. Ic"-i --

A-7 . . I I i , I I I . -I

I--_-

i -

Lt

TL I

TL 5

4

ML I

ML I

'dL9

wIL 8

L 7

IL 6

L5

1L4

L 3

L2

39

TL3

6 .ellkTL4

76-00' fro, 45 15'5 '45'30' 15' ao 74

1*0 -- T LL 1

0 . -* - --/-

45O I* ?O < i\ *

NNS A x- . :.+ CEN

." . .. . . - - - - - -.5- . .

t", DOV e-RI(_L*

DELAWARE BAYv

.9

-- . 5 *z

10%

*6 i s_ -*.

00 IWI LM I ON

45 5

to -n

3 . .. /(1 9x_

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slie110.

" IO r ({_ ,{ ^nw 11

76 45 3dbb

GEODATA INTERNATIONAL, INC.7035 JOHN W. CARPENTER FRWY DALLAS, TEXAS 75247


5

Figure IV.3 National Gamma RayN TV.19c

0 5 I0 15 20WILMINGTON. DELAWARE

25MILES

5 O 5 _10 _ I5 20 25 3OKILOMETERS

Map Series

? 31st

45'

30

15'

39 00'74 00'

40K t STANDARD DEVIATIONS

-.4 i . - . - - k , a - t I 111 - 6- -A---.

TI R

*00'

7Dd

I. 75*00

TL I

TL 5

TL 67600' 45

TL 3

5 45 30

40

ML 12

45 15 75.00.

15'

oo= I~t'9-

RIVE

0o us 1

ML IC

ML9

ML 8

ML 7

ML 6

ML 5

ML4

ML 3

ML 2

)"00 -- - - -k TL

at .. P A " PH CHERY HL .. ,r o. 1 1

.t-t -.- - - 1101T

45 --t eo t -- - - _ -

, " NNSY V IA x - n -- " *- * " $ , 1:: eo

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e rr 1 - _ .-" T J- , .o .

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r

" a4 "C

s l r _ O ,rfs- - -l - -sN

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*o /) - o, ,oso 1

O~i O7000

+a- -J

385

a.,

\ aa1

5

+c b

)ca . .

bib



1 5

Figure IV.4 National Gamma Ray Map SerieT V 19 d

5 10 15 20 25MILES

5 0 5 10 15 20 25 30KILOMETERS

WILMINGTON, DELAWARE2 14

Zi/i2ceTR STANDARD DEVIATIONS

3101

y< ,"

ro

c

oa

a T, ,o'

4, ,+

. . -.

ML I

39

.. s - i-- .r r '

30

15'

39*00'

-00'74

-f75*00

IL

:-3 i ...- I Ilk_

74*00

45'

7

76od 300e

30

TL I

TL 5

::usTL 6.0 &?l 45

TL 3

TL47500d

.2

p Vt f . . . . .- "p ' 0>p-p0 0 / S 0

.--ow l -y m !--

I .7th0

76 0

4000

ML 12 0

M L 10

45

ML9 *

ML 8

ML 7

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V

A

VI I II

. . . .. .. . .

1 t 1 I f S 7

I LONG 75.750

~-u 00

** liiiI 1 11111111 I

MLII

ii 11i 11 1 1 1 I N III1111111 1

ML11


BMAG10 GAMMA/DIVBASE = 5I10



ALT100 FT/DIV

0 I sI 5 7 ! 19It 1 1. 71 5i

LONG 74.500

s

h S... ML 11E WILMINGTON.ML 11W WILMINGTON

CHER K,..L . a . oCHE Y ILL am eT ,RIVER n I

r e4 2 . . .r

ML 12

I I I

11 I'l 1A 1 1 11)1 1 11

III 11 1

TL/K1.0 /DIV

BI/K.5 /DIV

BI/TL.07 /DIV

GC2E0 C/S/DIV


BIAIR2.5 C/S/CIV

K.15 PC/DIV

BI.25 PPM/DIV

- _7_s -I

+ ____ ________

76.000

ML 12W WILMINGTON

2 " 2

11I i1l 111 I Ii I I III1111

L_ fV -V-

II 1

S 6 74 500?

I1H ill III 1 11

I

I -- -

D 1 TE

Y W~

TL.75 PPM/DIV

ALT100O FT/DIV

lj

__ _

- ,-. i if-

-:

I

! 11 v le-'so o I N _ ', 'I I

V j v-

TTS 1

T

V

Ll I I I

Ski

rt- - -r ---- sr -- r - -r -- rr -T-r-

- -- - - 11--J11 1 1 4 I 811 1

v

R'M VA i t 9 1

ML 12

PMIAIPI

L I I I II -

S 1t 3 1 $ 1 3

I LONG 76.000

ML 12W WILMINGTON

c ee M L I2

CHER Y H IL L o <.t ,e o .. IVER

Qc.o.. ,.-.

*%lb

U II I I II I 1 1111 II II II III I I I I I

9

SI ! 3 1 S !10 It It 1 i

LONG 74.500

ML 12E WILMINGTON

RMAG10 GAMMA!DIVBASE = -1000


BP3 I1 HG/DIYBASE = 700


ALT100 FT/DIV

_ __ _ __i

A

:

e -e c i e w~o

II I I 1 I I 1 I 1 1 I 11 1 I

I-

TL/ K1.0 /DIV

BI/K.5 /DIV

BI/TL.07 /DIV

GC250 C/S/DIV


BIAIR2.5 C/S/DIV

K.15 PC/DIV

BE.25 PPM/DIV

0 4 0 T40 000 9

TL 1 WILMINGTON

II I 111Hil 11

L.?8 PPM/DIV

ALT10~0 FT/DIV

r0

1 Q

5 0

7

'IK

"( 0

1/ '->

II

4LA 4 .. C 48

r4


BMAG10 GAMMRA/DIVBASE = 54180



ALT100 FT/DIV

so s ,o y. .u.

I I I I I 1 1 1 1 1 1 1 1

TL 1 WILMINGTON

/1 /1 -,

3 - I -ta

I I 1 i i 111 1 11 111I I III IN 1 I i i 1 I1 1 1 1 1 1 1

TL/K1.0 /DIV

BI/K.5 /DIV

BI/TL.0? /DIV

GC250 C/S/DIV


BLAIR2.5 C/S/DIV

K.15 PC/DIV

.25 PPM/DIV

T t Gt

TL 2 WILMINGTON

t S39.7 S0

U I I1 !I' It

P11I I~ l ll l I1111 J 1110 ___1__,_1,____

IPAAA _

TL.75 PPM/DIV

ALT100 FT/O1'

-

-I

n \ ' ~\ /( >7

1' r 1 =

- -\ eO , eN -. 1 K e

o 0I eI r ilI S2e

I I III 111111 1I I I111II1I1 1II 1 I I 1111

TL 2 WILMINGTON ,0,

r --

LAT 33 750


BMAG - -10 GAMMA/DIVBASE = 54180

BP3 MM MG/DIVBASE = 700


ALT100 FT/DIV

V'

.r0

0YO

\ w

'(-l

- -- . S

*Y 1e I

,.1 '

L Lo' ~ %

0 \4*0 _ = f

l I 1 I 1 1 1 III II II 11111 i I 11 1 1 1 I I I I till t II 1 i11111111111

TL/ K1 .1 /0./

BI/K.5 /DIY

BI/TL.0 /DIV

GC250 C/S/DIV


BLAIR2.5 C/S/DIV

K.15 PC/DIV

BI.25 PPM/DIV

T o 5o2

17 400tJ1'

I -

(N

1 I I Io f Ial lIITL.75 PPM/DIV

ALT100 FT/DIV

r >i

q

:

1.& . 6, 1 9-40"Z - - -1_ --I[ -, ' _ _ ' \ I _ t

G t t " s c t c s u it It t' 14 1" 19 2)1

TL 3 WILMINGTON

33.

"9a

: ' C->o

s' 4.' (j

* 5/J

A. ," . . " '

'2

' w 3

7t! jj

r l ii I 1 1I 1I 1I1 I I I II II 1111 1111 I 11 1 1 1 1 1 1 I lIII 1 1I 11111 11111

0 t vsc 7 I 12 3]Ivs II 1? 13..

LHT 40.000

-rw-


BMRG10 GRMMA/DIVBASE = 54180



AL T1)3 FT 'DIV

' U - ;, -,r ,,o

TL 3 WILMINGTON

f- ua- F n p r '_'U. .. .1.

rr.,-" -L". - rl ~t

I I 1 I I I 1 1 11 1 1 I 1 1 I 1111 1 1 1 11111 111 111 1

a o s1 n s n

q

s

i

: , .

< <0)

a

o

I'I

eC1 1

-

Q - n3 r ,

0

L

1111 I I I I I 1 III I 111

o t t s c r t s ii iti

TL 4 WILIINGTON

f"'

.A

%0.

+4:

0N

I 1 11 1

IA1 ,

rIv-

m

TL!K1.0 /DIV

BI/KBS /DT

BI/TL.?/011

GC250 C'S/DIV

RMAG

BASE = -1000

BIAIR2.5 C/S/DIV

K.15 PC/DIV

.25 PPM/DIV

TLPPM.DIV

ALT100 FT/DIV,

4w 4j-t

s o .o

.,

1

l

e S

O

e O 1

l f o,( e o , f

pm. r,4 It , , .0. ..- u-. a..""..".-4-.o~

3 \-.

e9

"P

e , ,

/ j Sti

G "2_j

1 '

1 1 1 1 1 1 I I I I 111 111111

-4;v

I2

A'7

m

i 1 1

00

r J PJOl O r 1'u

e ! l ,

Jo q

.'i ee o y


BMAG10 GAMMA/D[VBASE = 54180



AL T100 Ft/DIV

- -v

a ! ] 1 2s c ,211 10 IX t2 12

LT 3 G NTL 4 WILMINGTON

lp- 0 q A , 1 -r---+IF11---- T

I I 1 11 I I I I I I I I I I I I 11 11 111 1

C !

O

clJ

I \

0 '

)

, - n

.

LR.

1,

00

3 =

1% DAII III I I 1 11111 1 1 1 1 I 11 1 1 1 111 1 11i 1 1 11 1I

ek-I) Al "

Ih - p -P A ArV l ~I r IA'A~ h iI 11 1 ' 11"111 111 11K111'k11Il II ,I 11 mMi'VIA IIIIIII

v u11191 IIIU II IIi

t t G t " ! t TS!10 11 It i1 N4 1S 14 IT It 40.Coc#'

TL 5 W Ilt'JNGTON o___________________

j0"

1 i

t n

- ;

e 0

e!,.,

TL/K1.0 /DIV

-I-

I

I 1

BI/K.5 /DIV

BI/TL.0T /DIV

GC250 C/S/DIV


BIAIR2.5 C/S/DIV

K.15 PC/DI/

.25 PPM/DIV

TL.75 PPM/DIV

ALT100 FT/DIV

I

A1

40T0

o 0 1 0

eo reeo DELA RE( J

00 ' 1

( e

I III II II 11111 1 1 1 1 I 11 I II 1 1i L I Ill II I 1

A

X R II II I I I

I I

0 I1t 5 G7 1

TL 5 WILMINGTON

07 It t'. 1 t itt7LAT 40.

I LAT 40 .OJC




TEA)1'1 PEG C/DIVBASE = 15

ALT100 FT/DIV

111 1 11 1 1 1 11 1 1 1 1 1 1 I 1 1

------- --

-j

i

_ 1T- - - -

100I,

106. 1100 , DELA RE {

Ile, f

,IRS

m Fell //LL e e e

I ee U 3A 3 \ M

V7

Y 111II I1111111 iii II N I ImI

" O

PllIi,

0oo 39000e0r7 t e1 1 10 0u 0u Oq 0 Iu 07 u8 II

TL/ K1.0 /DIV

BI/K.5 /DIV

BI/TL.07 /DIV

GC250 C/S/DIV


BLAIR2.5 C/S/DIV

K.15 PC/DIV

BI.25 PPM/DIV

TL.75 PPM/DIV

ALT100 FT/DIY

O ! - '0 ' r--TL 6 WILlMINGTON

16.

I 1 111111I 11 1 11 11111 I1 I 1

u I t rs c Sts

LAT 39 .006 WIi1INGTON

11 1111 11 1 11 1 1 LIII.1_


BMAG10 GAMMA;DIVBALE = 54180


L MP0 CEG C/DIVBASE = 15

ALT100 FT/DIV

: o

.-- -

-

---

I

JI

I

T1 - r T - - - - -- - -- r --3

150

125

10

360

300

240

180

C X 100 TOTAL EVENTS 4730 MEAN 07.45 ST DEV 21.75

275

220

165

110

55

B O Mf11 10V TOT VN 1363 .MEY 6. ST .i i

BI PPM X 10 TOTAL EVENTS 4363 M1E 1 .44 ST DEV 4.04120

100

so

60

L

Oz2

20

30

25

20 4.

.1 . ,ei~ar -.-

15

10

5

KOOOOOOOOOOO O O O O

TL/K X 100 TOTAL EVENTS 4470 MEAN 753.52 ST 0EV 568.84

330 .

20

15

10

5

O K 1O O O O O O O O O O O O O O O O O

BI/K X 100 TOTAL EVENTS 4031 MEAN 379.It ST DEV 35!.30

25

20

15

10

Z

O

J

30

30

25

20

15

10

PC X 100 TOTAL EVENTS 248 MEAN 32.27 ST DEV 17.85

30

25

20

15

10

5

BI PPM X 10 TOTAL EVENTS 209

30 ,

MEAN 8.35 ST DEV 4.87

30

25

C. N i T

N O O O

O O O O

O

TL/K X 100

s + r ro ro ro ro n r u u m u0 o w a e o ro a m o ro a n s0 0 0 0 0 0 o e o 0 0 0 0 0 0 0

0 0 0 0 0 0 0 0 0 0 0 0 o e o

TOTRL EVENTS 2 2 1 MERN 4?0.38 ST DEV 135.08

Sli i .m

BI/K X 100 TOTAL EVENTS 209

T

MEAN 301.0? ST DEV 138.54

0 4

15

LL-o 10

z

4. CE .Iau.T O O O O O O O O O

TOTAL EVENTS 4 14 1 MEAN 50.14 ST DEV 30.??

N 4! O m NTIL. PPM X 10 TOTAL EVENTS 224 MEAN 15.1? ST DEV 5.25

3F.)LOGIC UNIT QBSBI/ TL X 100 TOTAL EVENTS 198 MEAN 72.17

A A2

75

120

20

K

240

200

160

120

8s

40

PC

240

200

160

120

80

Z0

-

J

O m N fJ tJ iJ T T 'V " m V r

TL PPM X 10 TOTAL EVENTS 4709 MEAN 15.65 ST 0EV 12.12

GEOLOGIC UNIT QMA

BI/TL X 100 ST DEV 57.13

1-2 -a-1- 0 1'X1' r- i a 1 I 1 0 1 1 1 I I-- I I I I I I I I I I

I 1

6-.4 - - - 6 4. 1. aJz Ira A I i « 0 i 0-14- r" .11 q-,,- IlM-ar, M', It-+-

50

25

1

"E "

5

R2

j . 1 q o

30

K PC X 100 TOTAL EVENTS 263 MEAN 60.66 ST DEV 25.4230

25

20

15

10

5

4 WtVIlN !Uiij~i~[1 m................

30

25

20

15

10

25

20

15

t0

5

-L.1 O N i q q + + N N N N N Y Y Y Y Y

N O O O O O N i It q O N i q q O N a T q

O O O O O O O O O O O O O O O O O O O O

O O O O O O O O O O O O O O

TL/ K X 100 TOTAL EVENTS 263 MEAN 688.53 ST DEV 219.67 K PC

120 T

100 I

60

O

f. I.1

150

125

100

75

50

25

X 100 TOTAL EVENTS 4034 MEAN 51.49 ST DEV 36.61

120

100

s0

60

40

20

.41j 4A

TL/K X 100 TOTAL EVENTS '4070 MEAN 777.18 ST DEV 012.53

PPM X 10 TOTAL EVENTS 265 MEAN 11.34 ST 0EV 4.5030

25

20

Z 15

10

6z

5

BOK 10 O O O O O O O O O O O O O O O

B I/ K X 10 0 TOTAL EVENTS 262 MEA 20! .72 ST DEV ?7.35 BI PPM X 10120 .

100

90

60

40

Z0H-03Z

3:I i . ai I . a A i -

TOTAL EVENTS 3931 MEAN 11.30 ST DEV 6.12O O O O O

Bil/K X 1001t0


TOTAL EVENTS 3964 MEAN 133.33 ST DEV 136.0%

150 .1

120

U,Z 30

o 60

zZ 0

BI/TL 100 OTAOEVENO 20 MEA 31.0 ST EV 1

BI/TL X 100 TOTAL EVENTS 260 MEAN 31.30 ST DEV 13.43 TL PPM X 10GEOLOGIC UNIT QCM

TTLA 3 T E

TOTAL EVENTS 9?3 MEAN 32.36 ST DEV 13.63 BI/TL X 100O O O O O O O O O O

TOTAL EVENTS 3969 MEAN 3 8.84 ST DEV 13.46

A4

I. T,30

25

to

15

10

5

BI

30

25

20

15

10

z0

Z-

JO3

a t W O m<JTL PPM X 10 TOTAL EVENTS 266 MEAN 40.7 ST DEV 17.53

GEOLOGIC UNIT QL

10

150

120

30

60

30

I I I I I I I- I I

i+i i t t i a 0 F 0 F r -I.l q, -11 0 { i a

4-;

- II

. 4 1 d a i -l r ,:r-rr t R 4 1 :m - 4 -: 1 a

I I I I I I

R I ft a -

A 3

L- - - - - - - -

120

100

80

60

40

20

30

75

$0

453

30

15

120

100

30

120

100

0 .

60

40

t0

X 100 TOTAL EVENTS 3172 MEAN 43.0$ ST 0EV 27.88

150

125

100

75

50

25

10 TOTAL EVENTS 3198 MEAN 12.41 ST DEV7.1S

120

100

0

60

TL/K X 100

e r ro ro ro ro ro w w w w0 o ro s s o ro + w e o ro + %0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0

0 0 0 0 0 0 0 0 0 0 0 0 0 0 0

TOTAL EVENTS 3 16 5 MEAN 1025.45 ST DEV 432.25

150

125

100

50

25

0 0 0

BI/K X 100

150

125

100

UZ75

LL,

o 50

O

25

0 0 0OL EVENS 315 MEAN 36.01 S

TOTAL EVENTS 3 15 2 MEAN 368.01 ST DEV 252.39

Fl-

K

BI PPM X 10

120

I1 I I U I I I I I I I I I

240

200

160

120

so

40

TOTAL EVENTS 4957 MEAN 14.30 ST DEV 4.63

300

100

30

60

Z0F-

J

I On n n-ll..... _ n _ _

40

00

250

200

U-o100

O

50

-L

TL/F

i i i i i i i i

BI/K

X 100

X 100 TO

OOOOOO O O O O O O O OTOTAL EVENts 4 35 4 MEAN 491.19 ST DEV 1?5.41

TAL EVENTS 4957 MEAN 143.48 ST DEV 53.31

T 10VE O O O O O O O O.

BI/ TL X 100 TOTAL EVENTS 3185 MEAN 36.73 ST DEV 17.89 TL. PPM X 10 TOTAL EVENTS 4954 MEAN 43.73 ST DEV 17.35

GEOLOGC UNIT QUPBI/TL X 100 TOTAL EVENTS 4953 MEAN 30.05 ST DEV 9.33

A6

K PC

PPM XBI

40

t0

Z0H-(7Z

J

3E

W 41 O " 41 4

TL PPM X 10 TOTAL EVENTS 3206 MEAN 35.35 ST DEV 15.00

GEOLOGIC UNIT QPB

PCu 10nTy v V NS 958 MEA ST0. 07.73

PC X 10 0 TOTAL EVENTS 4 95 8 MEAN 105.04 ST DEV 7?.?3 K

F a i 0 9 2 -0 -1 9 1- q I I it L4 0 1 1 1 4

i + F' P. " " a d a i 0 - I . .I I I I F F f F I 6 I__w

300

250

200

150

100

50

11

. . . . .... ..

tJRJL

. . . . . . . . ..

A5

3030

25

20

15

to

5


Y MX1O Td T ENTS 23 EN T0EVY. i i i i

PPM X 10 TOTAL EVENTS 29 MEAN 8.10 ST DEV 2.88

30

25

20

15

10

5

30

05

20

15

10

nRLA

30

25

20

15

10

5

25

20

15

10

5

N O O O O O N a p " O N i " O Ni pO O O O O O O O O O O O O O O O

TL/ K X 100 TOTAL EVENTS 29 MEAN 1420.04 ST DEV 405.31

30

25

15

10

5

fl.f Ii ftmfflf lfl pI I. AI. .ft

O O O O O O O O O O O O O O O O O O O

BI/K X 100 TOTAL EVENTS 29 MEAN 543.73 ST 0EV 24.31

30

25

20

BI/TL

30

25

20

15

10

5

At R I I

K PC X 100 TOTAL EVENTS 23 MEAN 64.61 ST 0EV 14.72

30

25

20

15

10

5

BI

30

25

20

15

10

Z

On

-J

O O O O O O O O O 0.

X 10 0 TOTAL EVENTS 2 3 MEAN 38.21 ST DEV i2.ss5

30

25

20

15

10

5


30

25

20

UZ 15z

LL10

z

w W O m wTL PPM X 10 TOTAL EVENTS 23 MEAN 26.00 ST DEV 7.54

GEULOGIC UNIT TCH

2nO O OO O OO O O O O O O O O O

TL/K X 100 TOTfAL EVENTS 23 MEAN 384.7$ ST DEV 58.04

BIK X 100H TOTAL EVENTS 23d 11.22 ST 0V 41.5O O O O O O O O O O O O O O O O O

B I/ K X 10 0 TOTAL EVENTS 23 MEAN 116.4! ST DEV 41.45

0 . .0

BI/TL X 100 TOTAL EVENTS 23 MEAN 31.39 ST DEV 15.85

A 8

AL

U)15

Uo 10

z

5ZOI-L7Z

J

3

BI

I O m N W 1 i i 0 Of 'V O .t N .m tA 4J O m N

TL PPM X 10 TOTAL EVENTS 23 MEAN 22.31 ST DEV ?.83

GEOLOGIC UNIT TBH

i / 1 1 F 4 H -F -1 0 "H 0 H 1' I F I i - i--------*-

5

R8

150

I I I


630

525

420

O O O O O O O O O O O O O OTL/K X 100 TOTAL EVENTS 6203 MEAN 123?.53 ST DEV 654.50 K

30

25 4

"20

315

210

BI PPM X 10 TOTAL EVENTS 6416 MEAN 0.2! ST DEV 3.81

105

BI/K X 100 TOTALNEVNTS6158 MEAN52.0ST0V330.1

B I/ K X 10 0 TOTRL EVENTS 6 15 8 tEi 520.60 ST DEV 330.16

200

10O

U)Z 120

z .

O

Z

0

30

25 1

20 I

15

10

BI

...

30

25

20

15

10

5

350

200

210

1.0

70

30

25

20

PPM X 10 TOTAL EVENTS 2 88 MEAN 12.31 ST 0EV 3.7$

15

10

5

30

25

020 4.

15

10

5z0

(1

J

3IL 100 OTiAL EVENS ME .

O ~O O O O O O O O O .BI/ TL X 100 TOTAL EVENTS 6369 MEHN 42.68 ST DEV 22. 9

Inzi

0106z

5

nrlfld Ill : IN 41O m N 4

TL PPM X 10 TOTAL EVENTS 288 MEAN 40.83 ST 0EV 11.55GEOLOGIC UNIT TC

60

so

40

30

20

10

O O O O O O O O O O O O O O O OTL/ K X 10 0 TOTAL EVENTS 28 9 MEAN 365.63 ST DEV 33.55

I.

BI/K X 100 TOTAL EVENTS 288 MEAN 118.7$ ST DEV 38.40

BIL 100 TOTAL E S 28 A 1. S 0E 1.O O O O O O O O O O O

BI/ TL X 100 TOTAL EVENTS 28 8 MEAN 31.59 ST DEV 10.49

A9

its

100

75

50

25

K270

225

10

135

50

45

210

200

160

120

0

40ZF-.O0Z

.E /1L 4 1 M 1 11 1 i 1 K I '

TL PPM X 10 TOTAL EVENTS 6455 MEAN 23.13 ST 0EV 10.83

GEOLOGIC UNIT TCO

a...-JL

I I I 4 4" I I I 1 ' 'I I I i I

" "'" ^'c

I .. SR.J if\


5

. .

0

810

60

50

40

PC X 100 TOTAL EVENTS 837 MEAN 43.14 ST DEV S$.6%

30

t5

to

15

10

5 .

TL/K X 100 TOTAL EVENTS 837 MEAN 1185.60 ST 0EV 721.1?

10 ,

30

150

10

30

25

00

15

10

5

6o 4.

30

I PPM X 10 TOTAL EVENTS 8q7 MEAN 15.06 ST DEV 5.36

30

t5

to

30

Y5

!0

15

10

5

co

50

40

30

00

O O O O BI/K X 100

OT 3O O O O O O O O O O O O

TOTAL EVENTS 8 37 MEAN 562.!0 ST DEV 505.02

30

25

20

15

10

Z

I

J01

3030

25

20

15

10

5

1ALfh1 1

30

i5

to

15

1o

5

I PPM X 10 TOTAL EVENTS 80 MEAN 15.53 ST DEV 5.?6

30

95

0

Z 15W

0 10

O

5

Rinuk m kr~L

B

TL/K X 100 TOTAL EVENTS 80 MEAN 628.62 ST DEV 144.03

BI/K X 100 TOTAL EVENTS 80 MEAN 134.16 ST DEV 34.67

f1d11I 0

T O O O O OTLET 8 MEN 5.2 T E Co

TOTAL EVENTS 847 MEAN 45.20 ST DEV t7.et

Q 4l O O UTL PPM X 10 TOTAL EVENTS 80 MEAN 54.11 ST DEV 25.24

EOLOG1C UNIT TABI/TL X 100 TOTAL EVENTS 80 MEAN 34.58 ST DEV 18.54

A 11

:5

to

15

10

30 4.

to

to

K

15

1L

010

5

BI

10Z0C-

J

TL PPM XGEOLOGIC UNIT T

N Y O m m10 TOTAL EVENTS 8$47 MEAN 36.25 ST DEV 15.1?

KBI/TL X 100

I I I lINh JI rro l ,I I

- I I I I I R .IIpI . .-

i -. I "1 """ "" """ " I + a i . I . ;-I


s

T

5

A812

ne

3030

25

20

15

10

5

30

25

20

15

10

5

30

25

20

15

10

5

X 100 TOTAL EVENTS 134 MEAN 37.48 ST DEV 35.54

30

25

20

15

10

5

A l bi 0 Jp


30

U)15i

w

w

U.

D 10

z

P.J b kw~Rmin.

BI/K

30

25

20

15

25

20

15

10

TL/K X 100 TOTAL EVENTS 194 MEAN 535.70 ST DEV 203.$$ K30

25

20

15

10

5

10 1 4 AD

O O O O O O O O O O O O O O O O O O

X 10 0 TOTAL EVENTS 194 MEAN !14.14 ST DEV 45.16

5

10

BI

30

25

60

50

40

30

20

10

N.

PC X 100T O ENTS 310 74.34 ST E 15.

TOTNL EVENTS 3 10 PEIN ?4.34 ST DEV 13.36

30

25

20

15

10

5


20 1

15

10

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SECTION Y

GEODATA DATA AQUISITION AND PROCESSING

SECTION V.

GEODATA DATA ACQUISITION AND PROCESSING

A. DATA ACQUISITION SYSTEM

A brief description of the computer-linked Geodata Data Acquisition

System (GDAS), used in the present survey, is presented here. Thefive primary components of the GDAS, which are mounted aboard aDouglas Super DC-3 aircraft, Figure V.1, are:

1) An array of nine (9) 11z" dia. by 4" thick NaI(Ti) detectors;

2) a NOVA mini-computer system

3) a Collins ALT-50 radar altimeter system;

4) a proton precession magnetometer; and

5) a Bendix DRA-12C doppler navigation system.

The nine-crystal detector array has been calibrated to measure the

gamma radiation spectrum between 0-6 MeV. The contents of the 3 to6 MeV interval is monitored in order to reduce the contributions of

the cosmic events in the 0-3 MeV interval, which is of primaryinterest in this survey. Eight of the nine detectors are mounted

to measure the 4ir solid angle gamma radiation spectrum emanatingfrom the earth's surface. The ninth detector, which is partiallyshielded underneath by a 3.5-inch lead plate, is situated tomeasure the

21 Bi radiation incoming from the upper 2n solid angle.

Each crystal detector has an estimated volume of 415.5 cubic

inches, resulting in a total volume for the entire 4ir system of

3324 cubic inches. The estimated volume to velocity ratio for this

sytem is 23.7, where the average speed for the DC3-S is approxi-mately 140 mph.

The energy resolution of the GDAS as calculated from the 137Cs 662

keV photopeak was 10.7%, where each individual crystal was 9.0% or

better. Automatic digital gain calibration for the eight detectorarray and the single detector system was accomplished by stabili-

zing on the 4 0K photopeak data.

The NOVA computer, shown in the system block diagram of Figure V.2.

is the control center of the GDAS. The data is gathered by thecomputer for every one-second period in a manner giving no dead

time when readout to the magnetic tapes for storage. Two magnetic

tape recorders are used; one to record the total spectral data and

the computer tabulated results (LDT), and the other to record onlythe computer tabulated results (CDT).

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Digital-to-analog conversion of the resultant intensities, theirratios and the magnetic field data are plotted on multi-trackpaper, allowing immediate examination for anomalous data.

The spectral data from the single detector system gathers andrecords the 2rr spectral data every nine seconds. This 2rr data isnecessary to determine the amount of atmospheric 21"Bi radiation inthe 4n spectral data. A third segment of the computer's coregathers and sums the total 2rr and 4ir gamma radiation spectra foreach flight line, which can then be plotted as shown in Figure V.3(EOFL spectrum).

Due to the dependence of the gamma ray data on altitude, a highlyaccurate radar altimeter is used. The Collins ALT-50 system isdesigned to make a series of 8 measurements per second, where theresulting altitude is the average.

Since the gathered data are dependent on the current ambienttemperature and pressure readings, a Senso-Tek barometric pressuresensor and a Hy-Col thermocouple sensor were used to monitorconditions outside the aircraft.

A proton precession magnetometer sensor, having a 0.25 gammareadout resolution and less than a 1.0 gamma noise envelope, issampled every second to yield a measurement of the total intensityof the earth's magnetic field below the aircraft. The sensor iscarried as a "bird" on a 100-foot cable in order to minimize themagnetic effects of the aircraft.

A Bendix DRA-12C navigation system with a 100th/nautical mileaccuracy provides a doppler navigation cross-track and along-trackanalog signal to be recorded each second onto magnetic tape. Twoother methods are used to properly locate the aircraft's track:visual sightings and photography. The first method is employed bythe navigator who marks flight map location reference points withcomputer-displayed record numbers. The second method is a 35mmfilm that records a continuous, recoverable track which has a 20%overlap/frame at an elevation of 400 feet.

There are three basic operating modes of the GDAS that the operatorcan manipulate:

1) CALIBRATE, which allows proper gain calibration for thedetectors;

2) OPERATE, which allows data to be collected, summed and recorded;and

3) PLAYBACK, which allows the operator to examine the newlyacquired data.

10-

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-- - - - - - --- - + -- x - --+ -------40.00 80.00 120.00 160.00

CHANNEL

B. DATA PROCESSING

1. Data Reduction

The field data tapes produced by the data acquisition system(Section V.A) contain the 4ir and 27 gamma radiation spectra,measured between 0 to 6 MeV. The resulting gamma ray spectraare composite spectra of the several different isotopes thatemit gamma rays within the detectors' energy range. Themethod used in this work to determine the concentrations ofthe different isotopes monitored is discussed in this section.

In this work, there are four different isotopes which contri-buted to the resultant composite spectra under consideration.In order of the highest to lowest energy emitter, they are:cosmic, eTh, eU and K counting rates.

x x xx x x x

PHA-2

Energy Interval (MeV)

3.0 to 6.02.410 to 2.7961.661 to 1.8601.357 to 1.556

Due to the occurrence of Compton scatter at all gamma rayenergy intervals, a 4 x 4 matrix method approach is used to"spectrally strip" the group summed counting rates into theirindividual counting rates attributed only to the isotopeassociated with that energy interval.

This matrix method approach is theoretically applicable to aspectrum containing any number of isotopic gamma rays. Forconvenience, the four isotopes will be denoted as: COS, TL,BI and K. The channel group sum for each energy interval canbe considered to consist of fractional components of each ofits constituents. For instance, one can write for the TLchannel group sum:

aCOS + 1.0TL + fBI + 0.0K = MTL

where MTL is the channel group sum count;

and the coefficients, which are known as Compton coefficients,for each variable represent the responses of the data gather,system to each isotope over the entire energy spectrum.

Similarly, equations can be written for the energy intervalgroup sums for MCOS, MBI and MK, as shown below in matrixnotation by

200.00 240.00 280.00

L I 1I - ---0.0 0.5 1.0 1.5 2 0 2 5 3.0 (MeV)

ENERGY LEVEL

Figure V.3 Typical End-of-Flight-Line Spectral Plot

V-5V-4V-6

r7.w -sw-

Isotope

Cosmic

4 K

10 1r

I

1.0 0.0 0.0 0.0 COS MCOS

a 1.0 f 0.0 TL MTL

b 1.0 g BI MBI

c Y 1.0 K MK Lwhere each element of the 4 x 4 matrix is a Compton coeffi-cient. By inverting the 4 x 4 matrix and multiplying on theleft by the channel group sum matrix, the resulting columnmatrix, whose elements are COS, TL, BI, and K, represents thecounts in each energy interval attributed only to the indi-cated isotope source.

Table V.1 contains the data reduction parameters, coefficientsand backgrounds used in this survey. The listed Comptoncoefficients were determined from data acquired during highaltitude flights and from "known" test pad data concentrationsin Grand Junction, Colorado.

The resulting reduced counting rates for COS, TL, BI and Kmust then be normalized with respect to the measured live timecounting rate of the data acquisition system. This is necessaryin order to restore the linear relationship between the photo-peak counts and the source's intensity. This procedure isaccomplished by dividing the reduced counts by the live time,LTC1:

thus,

costTL1BI 1K1

COS/LTCiTL/LTC1BI/LTC1K/LTC1

The next step in the data processing involves the subtractionof the background counts present onboard the aircraft. Thebackground counts, which exist in the aircraft and its equip-ment, are determined from high altitude data where the dataacquisition is free from all ground sources and atmospheric21"Bi contamination. The background counts. denoted as BT,B and B , used in this work are listed in Table V.1. DOingth processing, the backgrounds are checked by observing theresulting counting rates over large bodies of water, where therates would have near zero intensities. The gross count'sbackground counting rate, BGC, over channels 35-239, is alsogiven in Table V.1.

After the backgrounds have been subtracted from the live timecorrected photopeak counts, thus

TL1 = TL1 - BTt

BIl = BIl -

K1 = K1 -

BBi

BK

The resulting counting rates for TL1 and K1 represent thecounts contributed only by the sources below the aircraft onthe earth's surface. In the case of BIT, an additional sourceof 2 14Bi radiation, which is caused by atmospheric 214Bi,BIAIR, is still eminent.

The 27 detector system data is used to determine the magnitudeof the BIAIR to be subtracted. Since the predominate variablesource affecting the 2

.r detector is the atmospheric 2 1'Bi, itis possible to utilize most of the 271 spectrum in the BIAIRdetermination, and thereby produce some improvement in thestatistical error. The energy interval used for the 27crystal is between 1.05 to 2.79 MeV. Within this interval,the aircraft's background, B , and its Compton coefficient,C , have been determined frbN the high altitude data. (SeeTale V.1).

The BIAIR associated with the unshielded detector array isdetermined, using the shielded detector by the relation:

G(x)BIAIR = (1 - k2.Gx)) [Vc - C2 .cOS1 -

where k,, k2 , k3 are constant factors that correct for thepenetration/spill of the emanated surface radiation. Thesepenetration/spill constants are dependent on the amount oflead shielding used on the 27 crystal. The values used inthis work are listed in Table V.1.

T[I, BTT and XT have already been defined as the 4Tr

reduced data counting rates, c/s.

Finally, the '2Bi counting rate caused only by the surfacesources is given by

BISUR = BTT - BIAIR

Briefly summarizing, Tl, BISUR and KT are the counting ratesas measured at the height of the aircraft. All interferingcounts from cosmic, backgrounds and atmospheric 214Bi havebeen removed.

Since the various counting rates are dependent upon the heightof the aircraft above the surface terrain, it is necessary tocorrect the associated isotope's counting rate to an altitudeof 400 feet above the surface terrain. This is accomplishedthrough the equations indicated below:

TLS = TLT .e- 400-

BIS = BISUR - e-02(00 - I x)

KS = KT-e113(400-

and

GC(gross count) = (GC - BGC - S-BIAIR)-e '"' -- x

where

:ALMl

where

G(x) is the relationship between the 4i and 2isolid angles, the channel group sums andthe number of detectors in the detector arrays;

VC is the 2n total count group sum of channels91-239, c/s:

COS1 is the r cosmic count, greater than 3.0 MeV,c/s;

and,

RVALM = kTl-T + k2 WTT + k 3 KT

GC

S

BGC

is the live time corrected gross count.channels 35-239,

is the ratio of the BI data, channels 35-239 to channels 143-159,

is the gross count background,

V-8V-7 V-9

TLS,BIS,KS are the respective photopeak's countingrates at 400 feet;

p is the air density at standard temperatureand pressure; 0.001293 gm/cc

p is the air density at the time the surveydata was flown;

SI ,9u2 ,91 3 ,1, are the respective linear attenuationcoefficients;

x is the aircraft's height above the surfaceterrain in feet.

The attenuation coefficients and other constants used in thealtitude normalization are listed in Table V.1.

After each flight line of data has undergone the above datareduction, the average values for each radiation variable andvariable ratios for each of the flight lines were plotted todemonstrate the consistency of the average values and that asmooth flow continues from day to day, and from the start tothe finish of each day.

Diurnal variations of the magnetic field base station inten-sity were measured and applied to the field data. (SeeSection II.D and Appendix I.C). The magnetic heading correc-tions for the aircraft and its equipment used in this surveywere determined by flying a predetermined path at a surveyaltitude in first an east to west direction, then in a west toeast direction. The same procedure is used on a north tosouth path. Based on the data obtained in this fashion, seeTable V.1, the heading corrections were removed from all thedata. The magnetic field data were then IGRF corrected togive the residual magnetic field. The International Geomag-netic Reference Field subtracted was provided by the U.S.Geological Survey with reference to the IAGA Bulletin #38,"Grid Values and Charts by the IGRF 1975.0", National Tech-nical Information Service Report #PB265483.

The system sensitivities at 400 feet used :. this survey areshown in Table V.1.

2. Description of the Data Processing

The processing flow chart representative of the work performedin this survey is shown in Figure V.4.

As stated in Section V.A., the original field data tapes wererecorded to contain the various tag words, 4n and 2ir spectral

V-10

TABLE V.1: DATA REDUCTION PARAMETERS AND CONSTANTS

AIRCRAFT BACKGROUNDS

- N540S 1979

COSMIC CORRECTIONRATIOS

ValueDetector Parameter Window (CPS) Parameter Value

BK Potassium 25.82 c 0.2028Terrestrial K

(4n) BBi Uranium 9.42 b 0.1546

BT Thorium 7.60 a 0.1897

BGC Gross 337.0 -

Atmospheric B Uranium 8.19 C 0.2169(2 ) B2 1 2ir

DERIVED STRIPPING COEFFICIENTS AND RATIOS

SYSTEM SENSITIVITIESRADIOELEMENT AT 400 FEET

Potassium(cps/%K) 105.00

Uranium(cps/ppm eU) 13.85

Thorium(cps/ppm eTh) 7.24

V-11

ILD

DATA FLOWDIAGRAM

REFORM

ORIG.FIELD

DATA CDT PLOT DATATAPES PLOTS

FIXMOD

REDUCED REDUCEDDATA CDT PLOT DATA

TASPLOTSKE

LOCATION REE- (DIGITIZER)RENCE POINTS = TAPES

FLIGHT BASESTACK LOCATION PLOTS

= PROGRAMS

O TAPES FOR CUSTOMER

= INPUT/OUTPUT

DPTAP L'AT'' L"NGINFO

STATION

(AG)

GRDMRG

REECODEGEOLOGYLDATA

SINGLE REC. (OGT E)

MAGETICE RAIOMETRIC

PLOTS

VARPLT

GEODOT HISTO

STD. DEV.DOT PLOTS_,

HISTO -+ MERGE

FICHE IT

CUSTOMER

/GEOLOGYSTATISTICAL HI SPLT SORT I

MIC"EOFICHE INFORMATION

TO MICROFICHE VENDOR

GGICAPLOTS

Figure V.4 Data Reduction Flow Chart

V-12

Coefficient Value Coefficient Value

a 0.2889 k 0.053

0.3896 k2 0.0

y 0.8669 k3 0.0

f 0.0 S 17.5

90.0

LINEAR ABSORPTION COEFFICIENTS

ValueRadio Element Parameter (x10-per ft.)Potassium y112.795Uranium 112 2.212

Thorium yu32.129Gross 1142.160

MAGNETIC H );rNG CORRECTION

CorrectionFlight Direction (garmmas)

West to East +3.56

East to West -3.56

North to South -1.0

South to North +1.0

--I

data and the trailer record sums for each flight line. Thepurpose of the REFORM program is to sum the raw spectral data(LDT) into the proper group sum energy intervals for eachsecond for each line. The CDTPLT program is a data certifi-cation program that produces the EOFL spectral plots, FigureV.3, and profiles of each of the channel group sums, which areplotted as a function of each line's record numbers.

A brief sunnary of each program and its uses is given below:

FUNCTION

Produces energy group sums and EOFL spectra.

Primary processing for "spectral stripping"matrix reduction, live time normalization,background and BIAIR subtraction, and altitudecorrections.

Flight path recovery to produce record locationmap at a scale of 1:250,000.

Single record processing with latitude/longitude positioning, IGRF and single pointstatistical adequacy computations, and magneticheading corrections.

Merges aircraft magnetometer and ground magne-tometer in proper time sequence and appliesdiurnal corrections to the field data.

Produces radiometric and magnetic stackedprofile plot tapes.

Preliminary programs to prepare/sort data asa function of geologic type for the entirearea.

Produces geological histograms,mean andstandard deviation tables,and plot tape forthe entire area.

Produces plot tape for standard deviation"dot plots" related to geologic type.

Produces average record and single recordreduced data listings and microfiche tapes,which are sent to microfiche vendor.

Produces all customer required tapes.

3. Data Presentation

The surveyed area was positioned geographically to completelycover the specific National Topographic Map. Each topographicmap has been used as the flight base and sufficient geograph-ical and 15' location information has been shown. The flightline pattern has been superpositioned onto these created basemaps, where the standard deviation levels for each independentvariable and each ratio of these variables have been plotted(NGRMS), based on the data contained within the total maparea. Every fifth data point along each :ap line has itsstandard deviation value shown at the location of that value.Therefore, there are six NGRMS sheets which indicate thelocation and magnitude of anomalous data.

The multivariable map line profile, which represents 10variables as a function of their latitude and longitudelocation for each line, is presented at a scale of 1:500,000.Each profile presents:

1. Aircraft altitude above the surface2. eTh (208T9. from '32 Th decay series)3. eU (214Bi from 238U decay series)4. K (40K from natural potassium)5. BIAIR (atmospheric 2ABi)6. Residual magnetic field7. Gross count (greater than 400 keV)8. eU/eTh ('2 4Bi/208TZ) ratio9. eU/K ( 21"Bi/**K) ratio

10. eTh/K (2 08Tt/4 0K) ratio11. Geologic data, including aircraft flight pcth

The residual magnetic field map line profile, which representsfive variables as a function of their latitude and longitudelocation for each line, plus geologic data at a scale of1:500,000 is presented as:

1. Aircraft altitude2. Atmospheric temperature3. Atmospheric pressure4. Residual magnetic field data5. Magnetic field base line station data6. Geological data, including aircraft flight path

The output of these various computations supplies, beyond twoprofile sets, the following data:

* Histograms of the radiation data distribution withineach geologic unit.

* Histograms of the average velocity distribution foreach one-second record for each map and tie line.

Histograms of the average altitude distribution foreach one-second record for each map and tie line.

* Tables giving the average radiation concentration ofeach geologic unit for each flight line.

* Average radiation concentration for each variable asa function of flight line, including the atmospheric214Bi.

* Set of maps showing the standard deviation data as afunction of location and radiation variable.

* Printer plot contour maps of eTh, eU, K, eU/K, eU/eTh,eTh/K and the magnetics at a scale of 1:500,000.

4. Statistical Analysis Procedures

It is necessary to exclude from the statistical analysis allvariables which have too low a counting rate to be statisti-cally valid, and data which were obtained at altitudes above1,000 feet. To this end, a statistical adequacy test was runon all data for each data record. If a given value of TV., Bior K failed the test, that variable value, and any ratio valueassociated with it, were not used in the statistical deter-minations of mean and standard deviation values. In addition,such values are indicated on the radiometric profiles by avertical (tick) mark along the base line for the variable, andare flagged in the single record and averaged record listings(microfiche). The ratio values are set to zero in the Radio-metric Profile Plots, The flags in the listings appear underthe heading ANJT for altitude, 4

0K, ?4Bi and 08T, respec-

tively. The flags are zero for statistically valid data, andone for rejected data in the case of K, U and T. For altitude(A), a zero indicates altitudes to 700 feet, a one (1) indi-cates altitudes between 700 and 1,000 feet, and a two (2)indicates altitudes above 1,000 feet.

The tests used to reject data were as follows:

PROGRAM

RE FORM

FIXMOD

STACK

DOPTAP

GNDMRG

VARPLT

HISTO,MERGE,and SORT1

HISPLT

GEODOT

FICHE

CUSTOMER

Tfw - TiT =

Biw - BISUR =

/Kw -KT

1.5cT

1.5,B

1.5iK

V-14

(1) TT < 1.5

(2) BISUR < 1.5

(3) KY < 1.5

V-13V-15

where the "w" subscript refers to the respective windowcounting rates from the raw data and T1, BISUR and K1 havepreviously been defined. If any of the above inequalitieswere true, the associated variable was flagged, and that valuewas rejected in all statistical determinations.

The values of the radicals in the above equations, which areindicated as aT, aB, aK and the barred values, were calculatedon the basis of a single record value for determining flags inthe single record listings and the 7-point weighted values fordetermining flags in the averaged records listings.

The mean value and standard deviations were calculated assumingthe data to have a normal distribution within a geologic type.The equation used in determining the variance is:

a2 = x?- Ni2

where N is the number of statistically valid samples for agiven geologic type, x. is the value of the variable forsample number i, and x is the mean value of the variable forthe geologic type. Values from the entire survey of the areaare used in these computations.

V-16

APPENDICES

I PRODUCTION SUMMARY

II TAPE FORMAT STATEMENTS

HE COMPUTER LISTINGS

JZ LINE PRINTER CONTOURS

AI.C DTIJRNA, CRRECTTINS Tn TNE )ATAAI.A PRODUCTION SUMMARY - SURVEY TIME PERIOD

DATE FLOWN

7-22-79

7-29-79

7-30-79

Total Mileage

*Note: The survey

11 (23.5 m

prohibited

Terminal C

Philadelph

Also, ML-1

area

nort

ML-1

Inte

arou

SURVEYLINE MILES

315.6

403.0

535.6

1254.2

AVERAGESPEED/DAY

135

136

135

over the center cif maplrines

Miles) and 12 (23.

due to the preser

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?E detoured south

designated: R5001i around Greater I

detoured south

national TCA. TL

id Dove Air Force

miles) wasce of the

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around restrict

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443

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AI. AVERA(F SPFrF) AN[) ALTITIOf E DATA SUMMARY

AI.D EXPLANATORY NOTESLItI.

The correspondence between the map/tie line numbering systems of the

base maps and profiles of this report to those listed on the customer

magnetic tapes is given below:

Customer Tapes

20

21

40

41

60

80

81

100

120

140

160

180200

220

221

240

241

Report

TL 1

2

3

4

5

6

Customer Tapes

5020

5040

5060

50805100

5120

AVFRAGFALTITL'rF. FT

447477

4344354?H45345F%

457460

48548t

487

526499

49P512536

410413381373403385

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AI-5

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Line Character NumberNumber 123456789012345678961234567890123456789012345678901234567890123456789012

A. DESCRIPTION OF DATA TAPES

Al. General

All data tapes are 9-track, 800 BPI (NRZI), odd parity, EBCDICcode. Each tape contains a gum label giving the survey projectname, month and year of survey, tape type, subcontractor name,date tape created, tape reel count, tape recording character-istics, block size in Bytes and location of tape format informa-tion.

APPENDIX II

TAPE FORMAT STATEMENTS

The general description for each of the tape types is asfollows:

Block Number Description

1234

LineNumb(

12345678910

Format DescriptionTape IdentificationFirst Data BlockSecond Data Block

Last Data BlockEOF

A2. Raw Spectral Data Tapes

Block Size (Physical Record): 6600 charactersLogical Record, Data : 1100 characters

1. Format Description Block (Block 1)

The Format Description utilizes 4248 characters. Theremaining 2352 characters of this block are blanks.

Character Numberer 123456789012345678901234567890123456789012345678901234567890123456789012

01 0978 (DATA TAPE TYPE AND FORMAT SPECIFICATION DATE CODES)

RAW SPECTRAL DATA TAPE

FORMAT FOR TAPE IDENTIFICATION BLOCK (SECOND BLOCK ON TAPE)

ITEM FORMAT DESCRIPTION1 A40 QUADRANGLE NAME AS PROJECT IDENTIFICATION2 A20 NAME OF SUBCONTRACTOR3 14 APPROXIMATE DATE OF SURVEY (MONTH, YEAR)

11121314151617181920212223242526272829303132333435363738394041424344454647484950515253545556575859

4567

8

91011121314

15-17

*

**

306-308

FORMAT

ITEM12345678

91011

1213

14

1516*

*

*

270

I1A2013F6.3

F6.3

131313141613

14,16,13

*

**

I4,I6,13

FOR RAW

FORMATIi141616F8.4F8.4F6.1F7.1

A814F4.1

F5.1F5.3

14

1414*

*

*

14

AII-1

AERIAL SYSTEM IDENTIFICATION CODEAIRCRAFT IDENTIFICATION BY TYPE AND FAA NUMBERBFEC CALIBRATION REPORT NUMBER4PI SYSTEM DATA COLLECTION INTERVAL TO THREE DECIMALPLACES IN SECONDS2PI SYSTEM DATA COLLECTION INTERVAL TO THREE DECIMALPLACES IN SECONDSNUMBER OF CHANNELS (0-3 MEV) FOR 4PI SYSTEMNUMBER OF CHANNELS (0-3 MEV) FOR 2PI SYSTEMNUMBER OF FLIGHT LINES ON THIS TAPEFIRST FLIGHT LINE NUMBER ON THIS TAPEFIRST RECORD NUMBER OF FIRST FLIGHT LINEJULIAN DATE (DAY OF YEAR) FIRST FLIGHT LINE WASCOLLECTEDREPEAT OF ITEMS 12-14 FOR SECOND FLIGHT LINE ON THISTAPE

*

**

REPEAT OF ITEMS 12-14 FOR 99TH FLIGHT LINE ON THISTAPE

SPECTRAL DATA RECORD (THIRD THRU LAST BLOCK ON TAPE)

DESCRIPTIONAERIAL SYSTEM IDENTIFICATION CODEFLIGHT LINE NUMBERRECORD IDENTIFICATION NUMBERGMT TIME OF DAY (HHMMSS)LATITUDE TO FOUR DECIMAL PLACES IN DEGREESLONGITUDE TO FOUR DECIMAL PLACES IN DEGREESTERRAIN CLEARANCE TO ONE DECIMAL PLACE IN METERSTOTAL MAGNETIC FIELD INTENSITY TO ONE DECIMAL PLACEIN GAMMASSURFACE GEOLOGIC MAP UNIT CODEQUALITY FLAG CODESOUTSIDE AIR TEMPERATURE TO ONE DECIMAL PLACE INDEGREES CELSIUSOUTSIDE AIR PRESSURE TO ONE DECIMAL PLACE IN MMHGLIVE TIME COUNTING PERIOD TO THREE DECIMAL PLACES INSECONDSSUMMED RAW OUTPUT FROM COSMIC CHANNELS (3-6 MEV) INCOUNTSRAW OUTPUT FROM CHANNEL 1 IN COUNTSRAW OUTPUT FROM CHANNEL 2 IN COUNTS

**

*

RAW OUTPUT FROM CHANNEL 2;6 IN COUNTS2352 BLANK CHARACTERS

AII-2

2. Tape Identification Block (Block 2)

The information and format for this block are indicatedin lines 8 through 30 of the Format Description BlockA2.1, and 1396 characters are produced. The remaining5204 characters in this block are blanks.

If fewer than 99 flight lines exist, the unused flightline information, 13 characters per flight line, isfilled with 9's through the 99th flight line.

3. Raw Spectral Data Blocks

The information and format for the logical records inthese blocks are indicated in lines 36 through 59 of theFormat Description Block A2.1. One logical record con-tains 1100 characters. There are six such logical recordsper 6600 character physical record or block.

The 27r data logical record is recorded after the corres-ponding 4ir data collection intervals at a frequencydependent on the 2ir system data collection interval. Forexample, if the 47 data collection interval is 1 secondand the 2ir data collection interval is 10 seconds, then10 records of 4ir data are recorded followed by 1 recordof the 2ir data which was collected during the preceding10 seconds. The format for the 2ir data is identical tothat of the 4ir data, except for lines 40 through 49 ofthe Format Description Block given above. These vari-ables are expressed in the 27r record as all nines in theformat specified for I and F fields, and all zeros for Afields.

A3. Single Record Reduced Data Tapes



The Format Description utilizes 6768 characters. Theremaining 132 characters of this block are blanks.

Line Character NumberNumber 12345678901234567890123456789012345678901234567890123456789C123456789012

02 0978 (DATA TAPE TYPE AND FORMAT SPECIFICATION DATE CODES)23 SINGLE RECORD REDUCED DATA TAPE45 FORMAT FOR TAPE IDENTIFICATION BLOCK (SECOND BLOCK)6

Line Ciaracter NumberNumber 1234 56789 01234567890123467390123456789012345678901234567890123456789012

7891011121314151617181920212223242526272829303132333435363738394041424344454647484950515253545556575859

ITEM FORMAT DESCRIPTION1 A40 QUADRANGLE NAME AS PROJECT IDENTIFICATION2 A20 NAME OF SUBCONTRACTOR3 14 APPROXIMATE DATE OF SURVEY (MONTH, YEAR)4 Il NUMBER OF AERIAL SYSTEMS USED TO COLLECT DATA FOR

THIS QUADRANGLE.5 Il AERIAL SYSTEM IDENTIFICATION CODE FOR FIRST SYSTEM6 A20 AIRCRAFT IDENTIFICATION BY TYPE AND FAA NUMBER FOR

FIRST SYSTEM7 F6.1 NOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TO

TERRESTRIAL POTASSIUM (K-40) TO ONE DECIMAL PLACEIN CPS PER PERCENT K FOR FIRST SYSTEM

8 F6.1 NOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TOTERRESTRIAL URANIUM (BI-214) TO ONE DECIMAL PLACEIN CPS PER PPM EQUIVALENT U

9 F6.1 NOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TOTERRESTRIAL THORIUM (TL-208) TO ONE DECIMAL PLACEIN CPS PER PPM EQUIVALENT TH

10 16 BLANK FIELD (999999)11 F6.3 4PI-SYSTEM DATA COLLECTION INTERVAL TO THREE DECIMAL

PLACES IN SECONDS FOR FIRST SYSTEM12 F6.3 2PI-SYSTEM DATA COLLECTION INTERVAL TO THREE DECIMAL

PLACES IN SECONDS FOR FIRST SYSTEM13 13 NUMBER OF CHANNELS (0-3 MEV) IN 4PI SYSTEM FOR FIRST

AERIAL SYSTEM14 13 NUMBER OF CHANNELS (0-3 MEV) IN 2PI SYSTEM FOR FIRST

AERIAL SYSTEM15-24 (SAME) REPEAT OF ITEMS 5-14 FOR SECOND AERIAL SYSTEM* * **

*

85-9495969798

99-10]

*

*

*

390-392

FORMAT

ITEM12345

*

*

(SAME)13141613

1 I4,16,13

*

*

*

I4,16,13

FOR SINGLE

FORMATIl141616F8.4

*

REPEAT OF ITEMS 5-14 FOR NINTH AERIAL SYSTEMNUMBER OF FLIGHT LINES ON THIS TAPEFIRST FLIGHT LINE NUMBER ON THIS TAPEFIRST RECORD NUMBER OF FIRS] FLIG;lT LINEJULIAN DATE (DAY OF YEAR) FIRST FLIGHT-LINE DATA WASCOLLECTEDREPEAT OF ITEMS 96-98 FOR SECOND FLIGHT LINE ON THISTAPE

*

*

*

REPEAT OF ITEMS 96-98 -OR 99TH FLIGHT LINE ON THISTAPE

RECORD REDUCED DATA RECORD (ThIRD THPH Li T CK)

DESCRIPTIONAERIAL SYSTEM IDENTIFICATIGN CODEFLIGHT LINE NUMBERRECORD IDENTIFICATION NUMBEiIGMT TIME OF DAY (WHMMSS)LATITUDE TO FOUR O.CIMAL 'LACES IN DEGRiES


6061626364656667686970717273747576777879808182838485868788899091929394

678

91011

12

13

14

15

16

17

18

19

20

21

22

23

24

25

2.

F8.4F6.1F7.1

A814F6.1

F4. 1

F6.1

F4.1

F6.1

F4.1

F6.1

F6.1

F6.1

F8.1

F6.1

F5.1

F4.1

F4. 1

F5.1

Tape

The information and format for this block are indicatedin lines 8 through 49 of the Format Description BlockA3.1, and 1922 characters are produced. The remaining4978 characters of this block are blanks.

If less than nine aerial systems are used, the spaceallocated for additional systems is filled with 9's inthe format specified for each item using I and F fields,and with zeros for A fields.

Similarly, if fewer than 99 flight lines exist, theunused flight line information, 13 characters per flightline, is filled with 9's through the 99th flight line.

LONGITUDE TO FOUR DECIMAL PLACES IN DEGREESTERRAIN CLEARANCE TO ONE DECIMAL PLACE IN METERSRESIDUAL (IGRF REMOVED) MAGNETIC FIELD INTENSITYTO ONE DECIMAL PLACE IN GAMMASSURFACE GEOLOGIC MAP UNIT CODEQUALITY FLAG CODESAPPARENT CONCENTRATION OF TERRESTRIAL POTASSIUM(K-40) TO ONE DECIMAL PLACE IN PERCENT KUNCERTAINTY IN TERRESTRIAL POTASSIUM TO ONE DECIMALPLACE IN PERCENT KAPPARENT CONCENTRATION OF TERRESTRIAL URANIUM(BI-214) TO ONE DECIMAL PLACE IN PPM EQUIVALENT UUNCERTAINTY IN TERRESTRIAL URANIUM TO ONE DECIMALPLACE IN PPM EQUIVALENT UAPPARENT CONCENTRATION OF TERRESTRIAL THORIUM(TL-208) TO ONE DECIMAL PLACE IN PPM EQUIVALENT THUNCERTAINTY IN TERRESTRIAL THORIUM TO ONE DECIMALPLACE IN PPM EQUIVALENT THURANIUM-TO-THORIUM RATIO TO ONE DECIMAL PLACE INPPM EQUIVALENT U PER PPM EQUIVALENT THURANIUM-TO-POTASSIUM RATIO TO ONE DECIMAL PLACE INPPM EQUIVALENT U PER PERCENT KTHORIUM-TO-POTASSIUM RATIO TO ONE DECIMAL PLACE INPPM EQUIVALENT TH PER PERCENT KGROSS GAMMA (0.4-3.0 MEV) COUNT RATE TO ONE DECIMALPLACE IN COUNTS PER SECONDUNCERTAINTY IN GROSS GAMMA COUNT RATE TO ONE DECIMALPLACE IN COUNTS PER SECONDATMOSPHERIC BI-214 4PI CORRECTION TO ONE DECIMALPLACE IN PPM EQUIVALENT UUNCERTAINTY IN ATMOSPHERIC BI-214 4PI CORRECTIONTO ONE DECIMAL PLACE IN PPM EQUIVALENT UOUTSIDE AIR TEMPERATURE TO ONE DECIMAL PLACE INDEGREES CELSIUSOUTSIDE AIR PRESSURE TO ONE DECIMAL PLACE IN MMHG

Identification Block (Block 2)

AII-3 All-4All-5

3. Single Record Reduced Data Blocks

The information and format for the logical records inthese blocks are indicated in lines 55 through 94 of theFormat Description Block A3.1. One logical record con-tains 138 characters. There are 50 such logical recordsper 6900 character physical record or block.

The data appearing in locations specified by lines 68,72, 76, 86 and 90 of the Format Description Block A3.1are 9's in the format specified in each case.

A4. Statistical Analysis Tapes (Data and Sumnary)File 1: Statistical Analysis Data



The Format Description utilizes 7560 characters. Theremaining 440 characters are blanks.

Character Numberer 123456789012345678901234567890123456789012345678901234567890123456789012


STATISTICAL ANALYSIS DATA TAPE

LineNumber

30313233343536373839404142434445464748495051525354555657585960616263646566676869707172737475767778798081

FORMAT FOR TAPE IDENTIFICATION BLOCK (SECOND BLOCK)

ITEM FORMAT DESCRIPTION1 A40 QUADRANGLE NAME AS PROJECT IDENTIFICATION2 A20 NAME OF SUBCONTRACTOR3 14 APPROXIMATE DATE OF SURVEY (MONTH, YEAR)4 Il NUMBER OF AERIAL SYSTEMS USED TO COLLECT DATA FOR

THIS QUADRANGLE5 Il AERIAL SYSTEM IDENTIFICATION CODE FOR FIRST SYSTEM6 A20 AIRCRAFT IDENTIFICATION BY TYPE AND FAA NUMBER FOR

FIRST SYSTEM7 F6.1 NOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TO

TERRESTRIAL POTASSIUM (K-40) TO ONE DECIMAL PLACEIN CPS PER PERCENT K

8 F6.1 NOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TOTERRESTRIAL URANIUM (BI-214) TO ONE DECIMAL PLACEIN CPS PER PPM EQUIVALENT U

9 F6.1 NOMINAL ALTITUDE SYSTEM SENSITIVITY RELATIVE TOTERRESTRIAL THORIUM (TL-208) TO ONE DECIMAL PLACEIN CPS PER PPM EQUIVALENT TH

10 16 BLANK FIELD (999999)11 F6.3 4PI-SYSTEM DATA COLLECTION INTERVAL TO THREE DECIMAL

PLACES IN SECONDS FOR FIRST SYSTEM12 F6.3 2PI-SYSTEM DATA COLLECTION INTERVAL TO THREE DECIMAL

PLACES IN SECONDS FOR FIRST SYSTEM

Character Number123456789012345678901234 5678901234 567890)1234 56 18901234567890123456789012

13

14

15-24*

*

*

85-9495969798

99-101

*

*

390-392

FORMAT

ITEM12345678

91011

12

13

14

15

16

17

18

13

13

(SAME)*

*

*

(SAME)13141613

14,I6,I3

*

*

*

NUMBER OF CHANNELS (0-3 MEV) IN 4PI SYSTEM FOR FIRSTAERIAL SYSTEMNUMBER OF CHANNELS (0-3 MEV) IN 2PI SYSTEM FOR FIRSTAERIAL SYSTEMREPEAT OF ITEMS 5-14 FOR SECOND AERIAL SYSTEM

*

*

REPEAT OF ITEMS 5-14 FOR NINTH AERIAL SYSTEMNUMBER OF FLIGHT LINES ON THIS TAPEFIRST FLIGHT LINE NUMBER ON THIS TAPEFIRST RECORD NUMBER OF FIRST FLIGHT LINEJULIAN DATE (DAY OF YEAR) FIRST FLIGHT LINE DATA WASCOLLECTEDREPEAT OF ITEMS 96-98 FOR SECOND FLIGHT LINE ON THISTAPE

14,16,13 REPEAT OF ITEMS 96-98 FOR 99TH FLIGHT LINE ON THISTAPE

FOR STATISTICAL ANALYSIS DATA RECORD (THIRD THRU LAST BLOCK)

FORMAT DESCRIPTIONI1 AERIAL SYSTEM IDENTIFICATION CODE14 FLIGHT LINE NUMBER16 RECORD IDENTIFICATION NUMBER16 GMT TIME OF DAY (HHMMSS)F8.4 LATITUDE TO FOUR DECIMAL PLACES IN DEGREESF8.4 LONGITUDE TO FOUR DECIMAL PLACES IN DEGREESF6.1 TERRAIN CLEARANCE TO ONE DECIMAL PLACE IN METERSF7.1 RESIDUAL (IGRF REMOVED) MAGNETIC FIELD INTENSITY

TO ONE DECIMAL PLACE. IN GAMMASA8 SURFACE GEOLOGIC MAP UNIT CODE15 QUALITY FLAG CODESF6.1 AVERAGED CONCENTRATION OF TERRESTRIAL POTASSIUM

(K-40) TO ONE DECIMAL PLACE IN PERCENT KF4.1 UNCERTAINTY IN TERRESTRIAL POTASSIUM TO ONE DECIMA

PLACE IN PERCENT KF5.1 POTASSIUM STANDARD DEIIAT10N FROM THE MEAN TO ONE

DECIMAL PLACE AND ALGEBR4ICALLY SIGNEDF6.1 AVERAGED CONCENTRATION Or TERRESTRIAL URANIUM

(BI-214) TO ONE DECIMAL PiACE IN PPM EQliJVALENT UF4.1 UNCERTAINTY IN TERPFSTRiAL URANIUM TO 0,E DECIMAL

PLACE IN PPM EOUIJ'ALLNI UF5.1 URANIUM STANDARD DEV i N FROM ThE MEAN TO ONE

DECIMAL PLACE AND ALGEERAiCALLY SIGNEDF6.1 AVERAGED CONCENTRATION OF TERRESTRIAL THORIUM

(TL-208) TO ONE DECIMAL PLACE IN PPM EQUIVALENT THF4.1 UNCERTAINTY IN TERRESTRIAL THORIUM TO ONF DETMAL

PLACE IN PPM EQUIVALENT TH

LineNumber

828384858687888990919293949596979899100101102103104105

L

Character Number123456789012345678901?34667890123456789012345678901234567890123456789012

19 F5.1 THORIUM STANDARD DEVIATION FROM THE MEAN TO ONEDECIMAL PLACE AND ALGEBRAICALLY SIGNED

20 F8.1 GROSS GAMMA (0.4-3.0 MEV) COUNT RATE TO ONE DECIMALPLACE IN COUNTS PER SECOND

21 F6.1 UNCERTAINTY IN GROSS GAMMA COUNT RATE TO ONE DECIMALPLACE IN COUNTS PER SECOND

22 F5.1 ATMOSPHERIC BI-214 4PI CORRECTION TO ONE DECIMALPLACE IN PPM EQUIVALENT U

23 F4.1 UNCERTAINTY IN ATMOSPHERIC BI-214 4PI CORRECTIONTO ONE DECIMAL PLACE IN PPM EQUIVALENT U

24 F6.1 AVERAGED URANIUM-TO-THORIUM RATIO TO ONE DECIMALPLACE IN PPM EQUIVALENT U PER PPM EQUIVALENT TH

25 F5.1 URANIUM-TO-THORIUM RATIO STANDARD DEVIATION FROM THEMEAN TO ONE DECIMAL PLACE AND ALGEBRAICALLY SIGNED

26 F6.1 AVERAGED URANIUM-TO-POTASSIUM RATIO TOKONE DECIMALPLACE IN PPM EQUIVALENT U PER PERCENT K

27 F5.1 URANIUM-TO-POTASSIUM RATIO STANDARD DEVIATION FROMTHE MEAN TO ONE DECIMAL PLACE AND ALGEBRAICALLY SIGNEDSIGNED

28 F6.1 AVERAGED THORIUM-TO-POTASSIUM RATIO TO ONE DECIMALPLACE IN PPM EQUIVALENT TH PER PERCENT K

29 F5.1 THORIUM-TO-POTASSIUM RATIO STANDARD DEVIATION FROMTHE MEAN TO ONE DECIMAL PLACE AND ALGEBRAICALLYSIGNED


The information and format for this block are indicatedin lines 8 through 49 of the Forniat Description BlockA4.1, and 1922 characters are produced. The remaining6078 characters of this block are blanks.

If less than nine aerial systems are used, the spaceallocated for additional systems is filled with 9's inthe format specified for each item using I and F fields,and with zeros for A fields.

Similarly, if fewer than 99 flight lines exist, theunused flight line information, 13 characters per flightline, is filled with 9's through the 99th flight line.

3. Statistical Analysis Data Blocks

The information and format for the logical records inthese blocks are indicated in lines 55 through 103 of theFormat Description Block A'4.1. One logical record contains160 characters. There are 50 such logical records per8000 character physical record or block.

The data appearing in locations specified by lines 68,74, 80, 86 and 90 of the Format Description Block A4.1are 9's in the format s e _.fied in each case.

AII-8

LineNumb

12345

67891011121314151617181920212223242526272829

All-7AIl-6

File 2: Statistical Analysis Summary

Block Size (Physical Record): 7000 characters

Logical Record (Data) : 140 characters




1 05 0978 (DATA TAPE TYPE AND FORMAT SPECIFICATION DATE CODE)23 STATISTICAL ANALYSIS SUMMARY TAPE (OR FILE)45 FORMAT FOR TAPE IDENTIFICATION BLOCK (SECOND BLOCK)67 ITEM FORMAT DESCRIPTION8 1 A40 QUADRANGLE NAME AS PROJECT IDENTIFICATION9 2 A20 NAME OF SUBCONTRACTOR10 3 14 APPROXIMATE DATE OF SURVEY (MONTH, YEAR)11 4 16 NUMBER OF GEOLOGIC MAP UNITS USED FOR THIS

12 QUADRANGLE1314 FORMAT FOR STATISTICAL ANALYSIS SUMMARY DATA RECORD (THIRD THRU LAST15 BLOCK)1617 ITEM FORMAT DESCRIPTION

123

4

5

678

9

101112

13

A81616

F6.1

F6.1

A316F6.1

F6.1

A316F6.1

F6.1

SURFACE GEOLOGIC MAP UNIT IDENTIFYING CODETOTAL RECORDS FOR GEOLOGIC MAP UNITNUMBER OF POTASSIUM RECORDS COMPUTED FOR GEOLOGICUNITPOTASSIUM CONCENTRATION MEAN TO ONE DECIMALPLACE IN PERCENT KPOTASSIUM CONCENTRATION STANDARD DEVIATION TO ONEDECIMAL PLACE IN PERCENT KPOTASSIUM CONCENTRATION DISTRIBUTION CODENUMBER OF URANIUM RECORDS COMPUTED FOR GEOLOGIC UNITURANIUM CONCENTRATION MEAN TO ONE DECIMAL PLACEIN PPM EQUIVALENT UURANIUM CONCENTRATION STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT UURANIUM CONCENTRATION DISTRIBUTION CODENUMBER OF THORIUM RECORDS COMPUTED FOR GEOLOGIC UNITTHORIUM CONCENTRATION MEAN TO ONE DECIMAL PLACE INPPM EQUIVALENT THTHORIUM CONCENTRATION STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT TH

Line character r NumberNumber 123456789012345678901234567890123456789012345678901234567890123456789012

3839404142434445464748495051525354555657585960

14 A3

1415

16

17

A3

16

F6.1

F6.1

18 A319 1620 F6.1

21 F6.1

22 A323 16

24 F6.1

25 F6.1

26 A3

2. Tape

THORIUM CONCENTRATION DISTRIBUTION CODENUMBER OF URANIUM-TO-THORIUM RATIO RECORDS COMPUTEDFOR GEOLOGIC UNITURANIUM-TO-THORIUM RATIO MEAN TO ONE DECIMAL PLACEIN PPM EQUIVALENT U PER PPM EQUIVALENT THURANIUM-TO-THORIUM RATIO STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT U PER PPM EQUIVALENTTHURANIUM-TO-THORIUM RATIO DISTRIBUTION CODENUMBER OF URANIUM-TO-POTASSIUM RATIO RECORDSCOMPUTED FOR GEOLOGIC UNITURANIUM-TO-POTASSIUM RATIO MEAN TO ONE DECIMAL PLACEIN PPM EQUIVALENT U PER PERCENT KURANIUM-TO-POTASSIUM RATIO STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT U PER PERCENT KURANIUM-TO-POTASSIUM RATIO DISTRIBUTION CODENUMBER OF THORIUM-TO-POTASSIUM RATIO RECORDSCOMPUTED FOR GEOLOGIC UNITTHORIUM-TO-POTASSIUM RATIO MEAN TO ONE DECIMAL PLACEIN PPM EQUIVALENT TH PFNR PERCENT KTHORIUM-TO-POTASSIUM RATIO STANDARD DEVIATION TO ONEDECIMAL PLACE IN PPM EQUIVALENT TH PER PERCENT vTHORIUM-TO-POTASSIUM RATIO DISTRIBUTION CODE

Identification Block (Block 2)


1234567891011121314151617181920212223242526272829303132333435363738394041424344454647

The information and format for this block are indicatedin lines 8 through 11 of the Format Description BlockA6.1, and 70 characters are produced. The remaining 6930characters of this block are blanks.

3. Statistical Analysis Summary Data Blocks

The information and format for the logical records inthese blocks are indicated in lines 18 through 60 of theFormat Description Block A6.1. One logical record con-tains 140 characters. There are 50 such logical recordsper 7000 character physical record or block.

A5. Magnetic Data Tapes

Block Size (Physical Record): 8000 charactersLogical Record (Data) : 80 characters




MAGNETIC DATA TAPE

FORMAT

ITEM1234567

8

9

10-14

*

*

*

495-499

FORMAT

ITEM12345678910

11

12

13

FOR TAPE

FORMATA40A201413141613

F8.4

F8.4

(SAME)

*

*

*

IDENTIFICATION BLOCK (SECOND BLOCK)

DESCRIPTIONQUADRANGLE NAME AS PROJECT IDENTIFICATIONNAME OF SUBCONTRACTORAPPROXIMATE DATE OF SURVEY (MONTH, YEAR)NUMBER OF FLIGHT LINES ON THIS TAPEFIRST FLIGHT LINE ON THIS TAPEFIRST RECORD NUMBER OF FIRST FLIGHT LINEJULIAN DATE (DAY OF YEAR) FIRST FLIGHT LINE DATA WASCOLLECTEDLATITUDE OF GROUND BASE STATION TO FOUR DECIMALPLACES IN DEGREES FOR FIRST FLIGHT LINELONGITUDE OF GROUND BASE STATION TO FOUR DECIMALPLACES IN DEGREES FOR FIRST FLIGHT LINEREPEAT OF ITEMS 5-9 FOR SECOND FLIGHT LINE ON THISTAPE

(SAME) REPEAT OF ITEMS 5-9 FOR 99TH FLIGHT LINE ON THISTAPE

FOR MAGNETIC DATA RECORD (THIRD THRU LAST BLOCK)

FORMAT DESCRIPTIONI1 AERIAL SYSTEM IDENTIFICATION CODE14 FLIGHT LINE NUMBER16 RECORD IDENTIFICATION NUMBER16 GMT TIME OF DAY (HHMMSS)F8.4 LATITUDE TO FOUR DECIMAL PLACES IN DEGREESF8.4 LONGITUDE TO FOUR DECIMAL PLACES IN DEGREESF6.1 TERRAIN CLEARANCE TO ONE DECIMAL PLACE IN METERSF5.1 OUTSIDE AIR PRESSURE TO ONE DECIMAL PLACE IN MMHGA8 SURFACE GEOLOGIC MAP UNIT CODEF7.1 TOTAL MAGNETIC FIELD INTENSITY TO ONE DECIMAL PLACE

IN GAMMASF7.1 RESIDUAL (IGRF REMOVED) MAGNETIC FIELD INTENSITY

TO ONE DECIMAL PLACE IN GAMMASF7.1 DIURNAL MAGNETIC INTENSITY VARIATION TO ONE DECIMAL

PLACE IN GAMMASF7.1 MAGNETIC DEPTH-TO-BASEMENT TO ONE DECIMAL PLACE

IN METERS (IF REQUIRED)

All-9 All-11

1819202122232425262728293031323334353637

AII-10


The information and format for this block are indicatedin lines 8 through 25 of the Format Description BlockA5.1, and 2938 characters are produced. The remaining5062 characters of this block are blanks.

If fewer than 99 flight lines exist, the unused flightline information, 29 characters per flight line, isfilled with 9's through the 99th flight line in theformat indicated.

3. Magnetic Data Blocks

The information and format for the logical records inthese blocks are indicated in lines 31 through 46 of theFormat Description Block A5.1. One logical record contains80 characters. There are 100 such logical records per8000 character physical record or block.

If the magnetic depth-to-basement is not required, thisitem is expressed as 99999.9.

B. DESCRIPTION OF LISTINGS

Bl. Single record reduced data listings: include the followinginformation on Microfiche:

ITEM DESCRIPTION

REC Sequential record numberLat Location Y in latitudeLong Location X in longitudeRMag Residual magnetic field,Alt Surface altitudeGEO UNIT Geologic TypeAKUT A=Altitude; K=Potassium:

cosBiAirGCTiBiKBI:TiBI:kT&:KTEMPBP

B2.. Averaged record data listings:information on Microfiche:

ITEM

RECGEO UNITAKUT

Long

Lat

RMagCOSBiAirGC

gammas

U=UraniumT=Thorium - Results of statisticaladequacy testCosmic c/Airborne Bi, 4i dataGross count, .4 MeV - 2.8 MeV208Ti c/s214 Bi c/s40K c/sRatioRatioRatioOutside Air Temperature ( C)Atmospheric Pressure (In. Hg)

include the following

DESCRIPTION

Sequential Record numberGeologic typeA=Altitude; K=Potassium; U=Uranium;T=Thorium - Results of statisticaladequacy testLongitude of X location of geologictypelatitude of Y location of geologictypeResidual magnetic field, gammasCosmic, 47Atmospheric Bi, 4TrGross count, c/s

ITEM

TiRankBiRankKRankBi/TiRankBi/KRankTi/KRank

DESCRIPTION

Ti value, c/sTi standard deviation rankBi value, c/sBi standard deviation rankK value, c/sK standard deviation rankRatio valueBi/Ti standard deviation rankRatio valueBi/K standard deviation rankRatio valueTi/K standard deviation rank

AII-13 All-14All-12

GFJDATA INT. I1c.w1 ,INGT0)' N.1 19..07 MAPlINE I

WI MINOTONONG RMAG COS

76.0169 -563.6 31

76.0364 -579.5 576.0360 -576.0 3276.0355 -579.7 30

76.0146 -576.5 3976.0342 -576.7 2876.0337 -577.7 29

76.0333 -579.4 4576.0329 -580.1 4476.0374 -590.5 25

76.0320 -581.7 3576.0316 -581.7 30

76.0311 -597.7 4276.0307 -594.1 28

76.0303 -584.8 3376.0299 -585.5 3876.0294 -596.2 31

76.0790 -598.0 29

76.0295 -588.5 30

76.0291 -590.7 3276.0277 -599.3 31

76.0277 -588.9 36

76.0268 -591.1 25

76.0264 -591.7 2376.0759 -597.9 3976.0255 -593.6 3776.0251 -591.3 3576.0246 -593.4 3376.0742 -594.9 40

76.0239 -505.5 3176.0233 -595.5 4376.0229 -597.2 3776.0225 -597.4 3476.0220 -596.9 32

76.0216 -597.3 36

76.0217 -597.5 3576.0207 -597.2 30

76.0203 -599.9 3476.0199 -599.7 29

76.0194 -600.3 3876.0190 -600.2 29

76.0196 -599.1 30

76.0191 -599.5 32

76.0177 -599.4 4476.0173 -600.0 4376.0169 -600.9 3976.0164 -601.6 30

76.0160 -602.0 23

76.0155 -607.0 21

76.0151 -603.1 20

76.0147 -602.6 40

76.0147 -601.0 3476.0139 -604.4 30

76.0134 -604.9 23

76.0129 -605.6 41

76.0175 -607.3 3776.0121 -609.5 32

MAP1,TNE

GC RTATR1975 3.A

107 3.91504 3.81602 3.91736 3.91596 3.91792 3.81930 3.91876 3.91663 3.81950 3.91879 3.81765 3.9

1699 1.81531 3.81413 3.91396 3.91636 3.81877 3.91961 3.91945 3.91855 3.91875 3.91796 3.91910 3.91940 3.91943 3.91768 7.51699 7.51791 7.51710 7.51604 7.51549 7.51546 7.51435 7.51215 7.51192 9.7

1233 9.71303 8.71449 9.2

1463 9.71407 9.7

1545 9.2

1453 8.21605 8.21516 9.7

1470 9.7

1490 9.2

1397 9.21515 9.2

1457 9.21538 9.2

1611 9.2

1569 9.2

1479 10.4

1637 10.4

1515 10.4

1wALT

4410

419

417416414411408

408407

407400394393399394394374390

395401409

412414413413

414419

417

41741 3412

406

401

400

407

395392

396399393401406

409413

413410413414416

414

416414

416414411

406

TFMP24.424.524.424.524.424.524.624.524.424.574.474.524.474.574.474.324.424.574.624.524.624.524.624.724.624.574.474.324.224.324.224.124.024.124.023.974.023.924.023.924.024.174.224.124.0

23.974.024.174.224.374.224.174.224.324.274.124.2

PP

740.9

747.4743.4747.4742.4742.4747.9742.9742.9743.4742.9743.4743.4743.4744.5743.4744.5744.0744.0743.4741 .4742.9743.4747.4747.4740.9742.4740.9742.9742.4743.4742.4745.0744.5742.9744.5743.4743.4744.5742.9741.4744.0747.4747.4742.9747.4747.4747.4747.4742.4741.9742.9747.4747.9747.4743.4743.4

TL AT K RT/TL NT/K TL/K

R.00.31.73.95.R4.16.16.25.R3.36.26.15.46.46.54.45.56.25.84.46.56.R5.16.57,0

7.66.65.75.16.65.05.14.35.54.83.21.54.42.55.R

3.93.94.13.65.0

4.34.05.14.17.23.65.04.83.75.14.45.7

2.40.11.21.72.52.71.92.07.93.17.2

2.47.31.71.81.60.6

1.51.93.27.02.42.82.41.61.71.82.52.41.51.72.57.57.67.20.90.9

0.51.30.91.41.21.11.21.77.62.50.60.9

1.21.02.31.43.60.41.51.0

1.30.1

1.21.21.21.11.51.31.21.21.41.51.31.20.91.0

1.10.91.31.21.21.21.21.11.31.31.31.11.41.61.31.10.91.10.R0.90.R0.91.10.91.21.11.31.21.40.91.11.21.21.31.31.11.31.01.21.41.1

0.30

0.360.330.430.420.640.310.310.490.940.360.390.430.270.790.360.110.240.340.740.310.35

0.550.37

0.730.770.270.45

0.470.230.330.4110.570.470.450.270.270.110.570.160.350.300.260.340.350.610.610.110.230.160.7910.460.790.970.090.340.111

1.791.751.051.361 .977.491.29

1.597.272.651.661.601.911.501.911.590.541.621.452.621.637.057.777.09

1.241 .741 .442.731.710.931.37

2.372.667.447.610.911.750.581.191.00

1.111.060.941.04

1.742.R42.260.550.76

0.870.797.071 .073.790.361.110.93

6.01

4.943.193.174.653.954.144.874.697.834.604.094.725.516.894.475.136.664.37

3.575.245.874.135.695.485.665.775.003.694.053.964.834.635.195.933.404.595.107.256.153.123.563.223.043.554.693.694.793.355.437.774.353.763.924.763.775.77

Z"A

76A

7.A

7-aA,1A

7'IA

70A

76A7r. A

7 A71A7tA

7. A

7.r.9

71A7119A7'A

7..17.66

7',A

7%A

7^^A

7.'A

7.A769A

719

7"A

7,1.

79A

7 I A7. )A

79A

79 A7"A7:j AI

7A7.'i1A

79A

74A

7 A

7"A6

7^ A

7.;+ A

7.9A

7"'A7.".A9

'/.9A

(10

00(4)00111

00(001(110

11(100

00011nn0(

onnn

nu(1

100

4004)

0001,

0110(

0noon

0000

0011

(00,1

00(0f

0100

(0on

nnnn(

00(0(

000

000 1

000

040110

00041

0)1(1(1

onnn11

100001

(00(+11

1A 9

39.171449.071413.07143.021339.021339.021339.021 3319.0213

39.0(21730.071234.121213.021?39.021239.021 139.071139.021110.071134.071139.021139.0710319.021039.1210

39.021019.071034.0210

34.020939.020939.020939.02119

19.020934.021439.020R39.020439.070439.0704

34.0204

31.0217

39.1120739.0207

3Q. 02117

34.021)739.027 1139.02116

(9.706

31.0206

39.217))643.0709

3.0710534.07)S13.070534,.)705(4.02115

3.'12(143.020334.01704(4.1214

f0flGr RMaG cos76.11366 -563.6 3176.0364 -579.5 576.060 -576.0 3276.0355 -579.2 3076.0346 -576.5 3976.0142 -576.7 29

76.0337 -577.7 29

76.0333 -579.4 4576.1329 -590.1 4476.0374 -540.5 2576.0370 -581.7 3576.0316 -581.7 3076.0311 -547.7 4276.0307 -594.1 2976.0303 -54.9 3376.0299 -585.5 39

76.0794 -596.2 3176.079( -9A.0 21

76.0?95 -588.5 3076.0291 -591.7 3276.0777 -599.3 3176.0772 -588.9 3676.0769 -591.1 2576.0264 -591.7 2376.0759 -597.9 3976.0755 -593.6 3776.0751 -593.3 35

71.0246 -593.4 3376.0747 -594.8 4016.0?39 -595.5 3176.0233 -595.5 4376.0729 -597.7 3776.0725 -597.4 3476.0720 -596.9 3276.0716 -597.3 3676.0712 -597.5 35

76.707 -597.7 3076.0203 -5Q6.9 34

76.0199 -590.7 2976.0194 -600.3 3876.0190 -600.7 2976.0196 -59. 3 3076.0181 -599.5 3276.0177 -S99.4 44

76.0173 -600.0 4376.016 -600.9 3976.0164 -601.6 1076.n1161 -607.0 23

76.0155 -607.0 2176.0151 -60.1 2076.0147 -b07.6 40

76.0142 -6013.0 3476.0139 -604.4 3076.0134 -604.9 7376.0170 -605.6 41

76.' 175 -607.1 1776.0171 -650.5 .47

c1975107

1504160717361596179219301976166319501979

176516991531141313961646197714611445195519751796191014401943176816981791171016041549154614351715119212331303144914631407154514531605151614701490

1397

15151457153816311569147916371915

8API. IFHIAT4

3.93.83.93.R

3.R3.43.93.93.91 3.93.R3.9S 3.93.81 3.A

3.93.R3.R

l 3.93.R3.83.R

3.93.R3.5S 7.57.57.57.57.57.57.57.57.5

..29.21 .78.29.7

1 .79.29.2A.7H.2

9.29.79.79.79.7

9.79.79.79.210.4

10.410.4

IwT1, (ANK 7R RANK K RANK RI/T1 RANK

9.0+ 1 2.4+ 1 1.3+ 1 0.30- 0

0.3- 2 0.1- 2 0.1- 2 0.36+ 03.7- 1 1.2- 1 1.2+ 1 0.33+ 04.2- 1 1.7+ 0 1.1+ 1 0.41+ 14.6- 0 1.9+ 0 1.7+ 1 0.42+ 15.1- 0 2.2+ 1 1.2+ 1 0.43+ 15.4- 0 2.3+ 1 1.3+ 1 0.43+ 1

5.5+ 0 2.4+ 1 1.3+ 1 0.44+ 15.4+ 0 2.5+ 1 1.3+ 1 0.46+ 15.3- 0 2.5+ 1 1.3+ 1 0.49+ 2

5.5+ 0 2.5+ 1 1.3+ 1 0.45+ 15.7+ 0 2.3+ 1 1.3+ 1 0.41+ 15.7+ 0 2.1+ 1 1.7+ 1 0.37+ 15.9+ 0 1.9+ 0 1.7+ 1 0.32+ 05.R+ 0 1.7- 0 1.1+ 1 0.29- 0

5.6+ 0 1.5- 0 1.1+ 1 0.27- 05.6+ 0 1.5- 0 1.1+ 1 0.27- 05.6+ 0 1.7- 0 1.1+ 1 0.30- 05.6+ 0 2.0+ 0 1.7+ 1 0.35+ 0

5.7+ 0 ?.3+ 1 1.2+ 1 0.40+ 15.9+ 0 2.4+ 1 1.7+ 1 0.41+ 1

6.0+ 0 2.4+ 1 1.7+ 1 0.40+ 16.,7+ 0 2.4+ 1 1.2+ 1 0.3R+ 16.5+ 0 2.2+ 1 1.7+ 1 0.33+ 06.6+ 1 2.0+ 0 1.7+ 1 0.31- 0

6.6+ 1 2.0+ 0 1.3+ 1 0.30- 06.5+ 0 2.0+ 0 1.3+ 1 0.30- 06.1+ 0 2.0+ 0 1.3+ 1 0.33+ 05.R+ 0 2.0+ 0 1.3+ 1 0.35+ 05.6+ 0 2.0+ 0 1.3+ 1 0.36+ 05.3- 0 2.1+ 1 1.7+ 1 0.39+ 1

5.2- 0 2.2+ 1 1.1+ 1 0.42+ 14.9- 0 2.7+ 1 1.1+ 1 0.45+ 14.7- 0 2.1+ 1 1.0+ 0 0.45+ 14.4- 0 1.R+ 0 0.9+ 0 0.41+ 1

4.0- 1 1.4- 0 0.9+ 0 0.35+ 03.9- 1 1.1- 1 0.9+ 0 0.29- 03.9- 1 1.0- 1 0.9+ 0 0.26- 13.9- 1 1.0- 1 1.0+ 0 0.26- 14.2- 1 1.1- 1 1.0+ t 0.26- 14.1- 1 1.1- 1 1.1+ 1 0.29- 0

4.1- 1 1.7- 1 1.7+ 1 0.29- 04.7- 1 1.3- 1 1.7+ 1 0.32- 0

4.1- 1 1.5- 0 1.7+ 1 0.37+ 14.1- 0 1.7+ 0 1.7+ 1 0.40+ 14.4- 0 1.9+ 0 1.1+ I 0.41+ 14.6- 0 1.7+ 0 1.7+ 1 0.37+ 14.9- 0 1.4- 0 1.7+ 1 0.30- ()4.9- 0 1.3- 1 1.7+ 1 0.27- 05.1- 0 1.1- 1 1.7+ 1 0.25- 14.9- 0 1.5- 0 1,7+ 1 0.30- 04.8- 0 1.7+ 0 1.7+.1 0.36+ 04.7- 0 1.8+ 0 1.2+ 1 0.39+ 14.5- 0 1.9+ 0 1.7+ 1 0.41+ 14.6- 0 1.6- 0 1.7+ 1 0.35+ 04.7- 0 1.6- 0 1.7+ 1 0.33+ 05.1- 0 1.5- 0 1.2+ 1 0.31- 0

RT/K RANK TL/K RANK1.79-1.75-1,05-1.60-1.69-1.77-1 .92-1.99-1.95-I.96-1.99-1.81-1.74-I1.61-1.55-

1.44-1.41-1.54-1.67-

1.99-I1.99-2.00-1.93-1.76-1 .64-'1.59-11 .54- .1.54-1.54-'1.54-'1.67-'1.90-2.09-I2.16-1.97-1 .59-1.29-1 .07-'1 .02-1.02-1 .07-1.04-1.11-1.79-1.44-1.56-1.49-1.77-1.09-1.01-1.18-1.41-1.51-1.59-1.40-1.33-1.37-

6.01- 04.84- 13.18- 13.89- 13.97- 14.13- 14.23- 14.30- 14.73- 14.12- 14.22- 14.39- 14.65- 15.02- 15.33- 15.35- 15.24- 15.07- 14.94- 14.75- 14.85- 14.96- 15.09- 15.31- 15.35- 15.25- 15.04- 14.69- 14.39- 14.24- 14.27- 14.49- 14.67- 14.90- 14.83- 14.47- 14.3R- 14.19- 13.93- 13.97- 13.69- 13.52- 13.50- 13.45- 13.64- 13.79- 13.97- 14.04- 14.03- 14.06- 13.93- 13.95- 13.99- 13.90- 13.96- 1.4.03-.14.30- 1

A1AIII

1l ,rA I"T. I " .1.1 14-07

1v79

rApf 1 F 1 w

HCN

29

303132333435363738394041424344454647411495051525354555657585960616?63

6465

666761669707172737475767778

79s0

91(828384

G06I IT

79A97NAZNAZNA7NA

7,NA

7^A7NA76A

ZNA76A7NA7NA

7NA

71A7NA7NA

ZNAZNA

7N A

ZNAZNA7 A

7NA

Z6A79NA7A

ZNA7NA7.roA7NAZtiAZNA79NA

7NA

7NA7NA7NA7NA

7NAZNARNA7A79A

ZNA7NA

7NA

Z'A7MA769

79NA

7NA

7NA

7NA

AKIT

1000(0011

00000000000000(0)1000000000000000000010000000(000(10000000000000004000001(0000000000000000000000000000000000000000000000000(100000000000000000(0000100000000000000000

0 100000000000000000000000000000

0000000(

00(0o0000

001001(0

0000

LAT39.021439.021439.021439.021339.021339.021339.021339.021339.021239.021239.021239.021239.021239.021139.021039.021139.021139.021139.021139.021039.0210'39.021039.021039.021039.021039.070939.020939.020939.020939.020939.0209

39.020839.020839.020939.020939.020839.020739.070739.020739.020739.020739.020739.0206

39.0206

39.020639.020639.020639.020639.0705

39.070539.020539.020539.020539.020539.020419.020439.0204

SINGLE. WFC LISTI'iG 14794

kC>, CF0!ir.1T A k f

AIII-2 '

.. .... .. .. JJ ............... GGG 1N HHH................F FF FF T ............................................................................ ,+n,>.... . . ......... ...... HH . ... .. . ., .... ... ,,,.............. ..4 ... .... .. .............. H H NHHH................ F FF F FF ...... P..................................... ............. .............. ...... ,..... .. .... ,,,............ .. . ........... .. . .. .....

... .. HHH . . PFFF F PF ... . ............................... . ...... ... ... ... .. ...FF. .. ... ... ..

.. . . . .. ". . .. . ..... ."...HHHNH HH.... .. .......... FFFFFFFFFFFF."...... ................................ .................................. 0) ...............,."............ .. . . 8 ............... .... . ... 8 8... " " ..... ". . . .. HHH - N H... FFFFFFFFFFt .. .. .. .. FPB........... .1 . .. .

... . . . . .. . . . . .. . . .... .. ...... .. .. FHF..." ............. .. .. .. .. . .. .. .. .. . .. .. .. .................. ......... .. . .. . . , ,,. ..... ARB........ ... ...... AR BA . . . . . . ..... 4" .4. . . . . .F. . . ... ....... 4 1 1.

.. .44H... ..FPFP.. ..1. 141 4141 141..

........... . ............ i. ..HHF GGG F 'F G. . . . . . . ..." F ....F." FF" F . " D C 1..I II 1I TI II H4HH4H11 GG G FFF G... FF'FFFFFF' eFF rp E.F F E'E'I FF, F: Et IrI CCCCc 141414144B14 R 141R4 114B FFF1111 PRR1141 H14 4 AR...

.. IIIIIIIITIIII 111111111 HHHHHHH GGGC PFFFF GGG H.CCCC4.............................4414F1411441F41F41414h E144CC1414 1414141414 4 ....

........... .. 11 I I IIII II I III 1 HH HHHHHHH1 GCG FFFFF G;vG ... FFF F_~FF. F. r. r . E- noonE CCCCCC 1414RB PR1R1144 BadR8RRR ARb........................ "" .IiIIIIIIIIIIlI II I I i H H A H HGG FFFFFF GG H.............................. FF FfFFF Fr h FEF FI,. KF, FF'F:FE r',F ""Ill CCCCCCCHRRRARPRH H AR5RPR N yH RARRPAB 8bPH .............. . ........ IIIIIIIIIIIItIIIIIIII TIll HHX HN H G FFFFFF GGG H!,,GGGG,,,,, PE4,,,,. "",,,",,,IFF F FFF EIFIEE fl D CCCCCCCC 414R1AR4114ARtlH4 1414Rq NHRA 9A1BH...... . . 1I111I1IIIIIIIIII1 TIH HHH1H GG FFFFFFC .G ... . GGG...... ..... FFFFFF&FF PFFt41.F. EtFF. O,0 1o,,nlvO"I LCCOOCCCCC 44141414,4R414IR)C1CC 144 14NHNH5 4H14R1RHb1 4 ..

................ uI ITII1111 III II I 1 HHH GG II Ti4HHNH FFFFF GG 1HH 14 GGGGG FFFFFFF ' 4Frh 6FF 441<4.1 1<I4 rooror0 oo ccC cccccCC 1441144444114411 14114 1444411441144F.......... 11 1.11 IIIIII.I.II.I. .. III. HHH.H GG PF.F GG 14 1 OGCGG pFF F PF F PP F FF PFIFJ I''I0000004011 C C C.CCCCCCCC C I+ PPAHNRdN RAN8 t 1 A44 4A14 141R44114144114................ 111111111II1IIIIIIIIII[I IIII NHHHH1GGFFFFF GG NH110nH141414 GO fGFH F GGG F iFFFFFF P 1<4.14:1 4'4F. FF 4k: Fn'nn[ CCCl CC CCCCCCCC.CC 4'.44 R4 A 4R41A4R14H1RRBRRRA................ 11111 IIII 111 HHH GG PFF GG H 4114HHH 17.1G.1; PFF 'FTITTHN GG FF.F4FFPfNH4;CtGGGGIFFF'F F F EI'FlF n CC CCCCCCCCCCCCCCC 1414144H1D),4RN1)nnnnn4 4AAIAN 4B14RP8AR14 R R

.......... III I IIlI1TIIlIIII ITI III II HUH GG FFFFF GG A GG, H GGG 1F'F F FFFF e FFF FFFF fl14F:FIFF EO 1 CCC.CCCCCCCCCCCCCCCC 110)1)141414 14414148141414 141414F1F14H141Ph4141 4H14R6IIIIIIIIIIII JIIII llHFI III! IIH G PF F FGGGFFFFFFF E(E rffF1F'c 41.Un.4,-nr PDF 11 0 CCCCCC CCCCCCC 1114RnHR4R1 RHR1 BaP4 1 4R1HR41R4 RR1BRBHB

h.... .......... I IIIIITIIII IIIII TI 11IT 14HHH GG FFFFFFF FFFFF FFFFPP P -FFF. F tFF t F1) 1) CCCCCCI CCCCCCC CC4144aRa 148PH HRNR 1R4RBH14 RPRF1

....... IITI II11 HHH GG FFFF EE ET HF CFF F E P:1<FFFF,".eFF: . r 1, 4t11II"t CCCCCCC (CCCCC CCCCC 14141414141414141 14RHO1HA 4BRH 14411 1RR11R4114.......... 11 1 III11 HUH GG FFF EEE C lf) EE PPFEEFE P FE.EF F h00 F 0 1h0. CCCCCC CCCC CCCCC 141FB1414CCCCCCHCC 1411H1P144M1B 4 1 R14BhRH AAA

........ .. HHHH HHH4 IIII1 HHH GG FF' PEE I) C 144 C ) FEEFFEF EP FFFPP14 1 II0 t C .C)"C. 1413 c CC CCCCCCCC C R44 hn1 4 % .AA 1b44141 C 4R 1H1B AA1 A. . ..... 1HHHHHHHIHHH1THHHHI 1111111 HHH GG PPII')FF F CC 1414 C DI) PFFF4FFFDFFFF1.r CcCtC( 1410 cCC C1CC4C1 1R4R1BH4R 1 C 141414141414 AAAA1R14

....... .. H" HHHIIHHHI HHUHHHHHHHH FF FH PP PEF D CC 814 C 00 r))FOII 1E001 t0 I r0FF, CCCCC CC 144141 CCCCCCCCCCCCC 14114114, Br4 H AR 14441114441 C 1411441441 AAA

............ HHHHHH1HHH HHHHHH1 1 111111 HH GG FF F EE DD CC 4 CC 00001l1004 000 )1 I F FF00I,0hn001,00000IIW CCCCCC 1444 C CC C CCCCCCCCCC' 4R 141414114 111RRA11441B414b C 444111 AAA.. HHHHHHHHHHHH H44HH1 HHHH 41414141441414 1FF. C HHH GG PC PP DI.) CCC N CC onnoopo D0I:r)0h,001OOlfli.F?14)0 1 CCCCCCC 4 '1 (CCCCCCCCCCC 111444411441 14484BN 4B1841 C 14R4141 AA

........... ".. HH HHHHHHHHHHN14 114H1 4 N11 t1II 141 HGG FF EE D) CCC CCC CCC 1U F010000[ O11'. CC.CCCCCC RNN1 R CCCCC CCCCC 4441444114 lRl 1 1RH 144441414 C. HPH4NHA A A

................ 1hHHHHHHHH H HHHHHHHHH IIII1 HH GG FF EE D CH141 GP Do CCCC CCC.CCCCCCCCCCCCCCCCCCC i)DD C.CCCC;CCCCC 1AR AB C CCCCCC.CC CCCC A B H 144411BH 14RM1 C. RRH RB A.14. ..... .HHHHHHH1 H HHHHHHH141414141411 IIIIIIIII1 141H GG F F EE DD C CCCC CCCCCCCCCCC.CCCCCCCCCCCC 0I0 400t,0 ) E CCCCCCCCCChC. 1H41414141414141 1 4311r, 48N1 1414114441R4R11414 11C11HPR4... .411HHH4HHHHHHH 4HHHHHHH + IIIIIIIIIF 1414 GG PP EE+ 0D CCCCC CCCCOCCCCCCCCCCCCCC+CCCC 1401)01 )0 i' L CCCCCCCCCC 1414841414 + 11A44H 4B4RHB 4 H1 +nARUHP1 C1R +R A

... .1.... 4HHHHHHHHHH MHH HHHH TI IIIIIII 1 1HH GG FF EE 0 CCCCC C(CCC CCCCC IoL, rO r '" 1 ' + CCCCCCCCCCCC H, 144144441 114 41B4141414RH 1 444 144R1 4441aa44RR1144RR414

....... 4......H 1HHHHHHHH 1 1I I III 4 P0H GG FF E D 0 .CCCC CCCCCCCCCCCCCCCCCCCCCC JDIoD DD uI l1 CCCCCCCCCCCCC 14141414CCCCCCCC4HRPAB P 11141R441141aR 414RN4 1 AAA,.14.4414.14 44 11HHHHHHIIIIIIII III 1H GG PFF EE D0 CCCCCCCCC C 00000001II.OCICl141 04U001,0 C.CC.CCCCCCCCCCCCCCCC 4rR 4HAR1. BA RHR NHAH4 4 R1R4R14 1 1444RU AAAA

1.............HHHHHHHH IIII I III H1 GG FF PE 1D0 CC CCCCCC 1)1)I)ICfn )1)i 7)tl'0D 0ICtl: CCCCCCCCCCCCRCCCCCCCCCC 141A)4141H4 .F414 4141 RRH441 1HH4H144 AAA

......... ..... HHHHHHHHPIIIIIIIIIII HH GG FF EFE1441)P CCCCC CCCC0000CCCCCC41,too 4 I00. I I ) CCCCCCCCCCCCCCCCHC. CCC 1 R1 R AHH1 4114B4R 1 14 44BBA4AAAA.. . . .... 4HHHHHH H IIIIIIII II HH GG FF E EE 0D00 C 0000400mD000000000 D) nn0000 , (CCCCCCCCCCCCCCHCC. CCC 14141 14B41a4R11 R1AORR NR R1H 4 AAA

1............. HHHHHH411 1111111 II 1H GG FF EPE )DD CCCCC00000 D0o 0 000I)0000000 4000400IIUL CCCCCCCCCCCCCCCC CCCC 144144411411PR R4HR1R4RPP RB1B4AAAA............. HH 414 4141414H14 Il! II HH GG F EEE E DDTD) CCC CCCC UD U0000040000(00I ) l 0": . CCCCCCCCCCCCCCC CCC 4H4H141 4114R1 1144 1 14141441 14PAAAA

....... 1...1.... H HH IH11H1H H III II 4H GG FF EEE DF, 0 D0) CC 0C 000 I I)Du01)) )4100141)140 00111,01N 1)140 CCCCCCCCCCCCCC. CCC 1414 14 R14 1414R 141141 H AAAAA.. HHHHHHHHH L IIII I I HH GG FrF EEE 1) D DD DD1) C U1nD1111111 0 P En 01000n0001 OU1 D L tLn 01 CCCCCCCCCCCCCC CCC 141144 1 14141H414 81411414RHRR AAAA

.......... GGGGGGGG HH TIIII1 HHH H II HH GGG FF EFDDDDDD~D EE D UDUDD 10PUD n n Dn D UVDrDUD Dn~nD CCCCCCCCCCCCCCCC CC C ARP HHA1, A ANRd PA RBARHB A...... . . . G HH HHHHHHH III I HH GG FF EEE DD ) .E10 PFEPEPEEE 0UDDD D nDI4IE1 00 )0C0140 CCCCCCCCCCCCCCCC CCC 441H14 144 14141R4H14 1 B414.......

. . . .. F GG G G 41414H41414141 114HGG FF EEE 1DD )EEEEE FFFE PE FE:EE 000000 II" 4441)I 4I) CCC CCCCCCCCCCCC. 4 RI BB HHBH b144414 414B1 H .........PP GOOG 0 HHHHHH 11114 HTGGFPP EF. 0 D F:EPPPnnnFDPP t EP DD)UDD 1 1) UU [UL 'I)CCC CCCC CCCC CCCCCC. R1441441444144141H41RHH1141P4R4A141444A

................ FFPF GGGG GGGGGGGGGG GGG Pp EEEE 0000 EE1EEEP EEEE L.)01 CCC CCCC.CCCCCCC 1CC4 414141414 14144144R HAH A.......

............. HH GG GGGG G G G FF EE D1FE00 EEE FFF FpFPFFPi, E 100 C CCCCC CCCCCCRCCCCC 4BB14H1 1R 1 4 B44 AA......... . EEE PGG GG G G H PPG F FF EPE 01FE0 PEP FPPFFF FP PP FF00F0 Df CCC C CCCCCCCC C 4414414 CCCCCCCCCCCC' 4B1H 4 1414B14 HBBBR1. AA...

......... EEE F GGGGGCGGGGGG GFFFFEF FFFFFF E E 001)0 )00 FF EE PFFP F" FF UOD 00 CCCCCCC CCCC CCC 14C44C1111 CCCCCCCCCCCC HH 14 414R414 1448141 1A........EEE FFP GGGGGG GGGGG FPFPFFP PFFFF E EDODDDDDDEEE F FF)' FF DF FF 000 CCCCCCCCCCCCC CCCC 1414141441 CC.CCCCCCCCCCCC 4144141 8144 14BR14AAAA......

. EEEE FF GGG GG G FG FFF FFFF EE P 0 0)00 PEF FFFF F PFFFFPFF F D C.CCCCC CCCCCCCCCC 1441H4H1 R CCCCCCCCCCCCC 141411 1141 B41141C 1AAAF........ ... EEEEE FF GGGGGGGG FF F F F FFF E E CCCC 1)D EEEP FFFF F PFFFFF PFFP CCCCCCCCCCCCCCC C' A 1h..hR C CCCCCCCCCCCC 1414H14 14414A 44R AAAA........

.EEEE FFF PPFFF FF G FFF E D C CCC D00 EEE FPFFFFPP FFFFFF FP CC.CCCCC1CCCC.C114CCC1B 44H11 CCCCCCCCCCCCC 4U R 1RB1RB41UBH4AAAA............ .. EEEE FFp P POFFFGFF GG 0 C 114 CCC 0FFDDDD E FFFFFF PFFF E CCCCCCCCCD1CCCCC) 1CCCCCC1414CC PH 1R R 14114 CCCCCCCCCCCC 41414144448144 118R AAAAA........

.. 0 PEE F FP P F GG PP0FF E D C C CC 000 EDO E PFFFF FFFFF FP 0) CCCCCCCCCCCCCCCC 4H RH4BHA41 1 CCCCCCCC 4HRRA144 11414144 148141 .. 4....14... .. 0 EEE FFF FFF E FF G FFF E D C 41 CC D0 EPPE FFFFPPFFFPFF P FFFFF .F. 11 CCCCCCCCCCCCCCCC . A 1414HBMP41 141414CCCC1414 141C1BRUR RB 4B14AAAA............

. DDDD EEE FFF F PE FF GG PFF P 0 C 1BB4 CC DD EPE FF P1FFF)FF IE ICCCCCCCCCCCCCCCCC RC 14. 1 4141414C14 8141414141414141414BH141414.............. EEE F F FFP PP FFP FFP P 0 1 BB CC DD PFP EFFFF E FFFF F U100 CCCCCCCCCCCCCCCCCHCC ABRMN1RNRN4NHHH1CC CCCBRR1 1 1 B4BR41...............

.. . DD EEP FFFFF PP PFFF PFFF E D C 1 HB CC DD P FE FFPEFFE4 P .EPPFF PF FFF FTP DD0 CCC CCCCCCCCCCCCCCCCCC C HBAHHRH14114H4Bb141414 14414H 4HBRRHHH4 . . ......... C.C. . 0.. DD EEE FFFF PFF EEP FFFFF E D C H B CC DD EE EEEEE EEE FFP F CCC CCCCCCCCCCCCCDCFCFCCCCCCCCC 14C D444FF141414 14 141414 ...............

.. CC DDD EEE F FFFFFF EEP P F EP D C 1414 CC DD E FEEEE 00001) PE P EIFF 011 CCC C CCCCC CCCCC C CCCCC 1RR 1414141 414R41R41 1 14 R4...............CCC 0 PDD EEEP pFFFFF PEEE EE D C 1B CC 00 F E E PFE 01 1 FEE FFD1 ,E 00 CC CCC.CCC CCCCCCCCCCCCCCCCRC 1414H14 14144R1 4R 44 A ................ -

.. 0..0... .CCC DD EEPEE F PFFFF EEEEEEEEEEE EE 0 CC CCC D PP PE EIEEEE DDD0 EPE E 00 CC CCCCCCCCCCCCCCCCCCCCCCCC 14R1 48 148 111R44 AA AA................

.. CC DD E F EEP PFF EEEEEEE EEE E D C CCCCC PP EEEEEE 0DDDDDDDD EEE PEP D0 CC CCCCCCCCCCCCCCCCCCCCCCC 144H1 R BB C 14HR14 A A 1.................. .. .C DODD EE PFFP EEEEEEE 0EEEEEE CCCCCCC 0 EFPEE E 100 0DD1 PP FE D0 CC CCCCCCCCCCCCCCCCCCCCCCCCC R4R4 HH1414 CCCC 4BBRRAAA.............

.. D0D EEE PF EEEEE EEEP D CCC CC DD EEEEFPEEE DDD D D0 ) PEF EP )DO CC CCCCCCCCCCCCCCCCCCCCCCCCC 11414 4RB CCCCCC H 4R141141 AAA414 11AA .................... DDD EEE E +EEEE 0 EEE DD CCCCCCCCC+ DD 1 PEP 0D D1)0 01)0 PF+ FE 1F) Cl CCCCCC+4CCCCCCCCCCCCCCCC R 1 + 4AMB CCCCCCCCC R+HA A.......+..........

0000..... DD0 E EP EEEE EE 0 CCCCCCC CC D0 0000I )0001DDDDDD EE EEF DD CCC CCCCCCCCCCCCCCCCCCCCCCCC 4H44 1R 4 CCCCCCCCCCCCC '41R4A. ............................... 00+EE EEE EEEE D CC CC DODD 1)00001)000 EP0EEPFEE 01 CCC CCCCCCCCCCCCC CCCCCCC CC 4141 4w1)1H4 CCCCCCCCCCCCCCCC 414R 4 AB. ....... .........

0.. DDD0EE PEEP PEE DD CC C BCCCC 1 CCCC 00 0 pDO00EEE0FEFE DO CCCCC CCCCCCCCCCCCCCCCCCCCCC H BRR H41

1 ABBR ' CCCCCCCCCCCCCCCCCCCCC B.. . . . .

......... DDDDDD EEEEE P EEE D CC 1444B 1 CCCCCCC 1)0 FEPEEDEEPoFFEF. 00 CCCC CCCCCCCCCCCCCCCCCCCCC C41RH 14 A HHH 1 CCCCCCC CCCCCCCCC CC B41414...... .... . . ,-

0DDDDD EEE FFPP EE 0D CC 1BB 4AAAA B411 CC 00 EEEEE PEEEFFP.E 0ED CCCC CCCCCCCCCCCCCCCCCCCCCC H 14414144411 C.CCCCCC CCCCCCCCCC 4R.. ............. E1 EE 14PP PEEP DD CCC BB AAAAAA144 C C CC D FEEE EEPP 0DD CCCC CCCCCCCCCCCCCC CCCCCC 4A4R1B4RAB4 CCCCC CCCCCCCCC 1. . . . . . .

.00000 EEEEEE FFFFF EE D0 CC 11 AAAAABA14 81 C PDEEEEE EEFPE 00100 CCCCC CCCCCCCCCCCCC CCCCCC 41HhRR bU4 CCCCCCC CCCCCC1CC 14H... ..............

... DDDD E.EEEE FFFFF EEE DD CC BB AAAAAAAAA 4B 1 CC DDF EFF' EEEF 0 f)D CCCCC CCCCC.CCCCCCC 1CCCC7CC 1 HA HHHR1 CCCCCC CCCCCCCCCC 1PR. . .

.EDEEEE FFFF EE DD CC 1BB AAAAAAAAAAAA1 14 C D EEEEE EEEE DDU) CCCC C CCCCCCCCCCC CCCCCCC 1 11BRHHH4144 .CCCCCC CCCCCCCCCCC 14. .. . . . ..

. . . .EEEEEEE FFFF EEE 000 CCC BB AAAAAAAAAAAAA 1 B C D EE: P PPEF. EE 01)141)0 1CCCCC C CCCCCCC CCCCCC -R 114 B14 CCCCCC CCCCCCCCCCCCC RR. . . . . .EEEEEEE FFF PE DD CCC BB AAAAAAAAAAAAAA4 1 CC 00 EFFEE..EE 10D00 CCCC CC.CCC CCCCCCC 114RRR14 4 CCCCCC CCCCCCCCCCCCCC BB14. .. . . ........... .. EEEEEEEEEEEE FF EEE DDD CCC B AAAAAAAAAAAAAAA B C D EEF.EEEEE DDDDD CCCC h('CCCC (CCCCCCCC NhHARB CdB CCCCCC CCCCCCCCCCCCCCC RHCAP ... ....................... .

EE EEPP EEEE E P EPEE 00DD CCCC 141 N AAAAAAAAAAAAAe BB CC DO1 C 0 0 PF;FPEPE 00000 CC CCCC C CCCC.CCCCC 444BR 41 CCCCCCCCCCCCCCCCCCCCCCC 18888 ...................

. ... .. ... EEEEEEEEEEEEEE E E E EEE ODD DCDC C B A AA AAAAAAA A 0 C D1)1D01DI) 1)04 0 CCCCCC CCCCCCCCCCCCCC HARBH 1d 4 CCCCC CCCCCCCCCCCC CH4 ................ . .

.......... D PEEE EEEEEEE EEE E E DEEE C 14 1414AA4A14A 1441 CCC DDDD CCCC CC1CCC CCCCCCC 14RRRCCCCCC88............................. 0..D0 PEEPEE PEP EE EEEE EEEEEE C BB C A 4AAAA4AAA B 4 CCC C00 0 CCCC CCCCCCCCCCCCC.C 841 4 C1 CCCCCCC CC B ................

... 0 PEEE EEEEE EE PPV P 0 C 14 1CAAAAAAA BB CCCCCCCCCCCCCCCCCCCCCCC CCCCC 1 CCCCCCCCCCCCCCC 4CCC1CC4 14114 1 CCC 414......... ................ .C 0 EE E F F EEEEE EEEE P P P C 4144AAA1AAAA 1BB4 CCCCCCCCCCCCCCCCCCCCCCCC CCCC 14444 444 CCCCCCCC CCCCCCC 4CC4 141414141414 CC..................................

......... .C 0 PP F EEE EEEE EP G P PE 0 C 4AAAAAAA 14 CCCCCCCCCCCC CCCCCCC CCCC 1 4,4.b 4) CCCCCCCCCCCCCC 4RA1BC44C1 C ..................................................... PC D EE FPEEEEE PEEEEE FFF GF E D C 4A4AAAAA BA CCCCCC CCCCCCCC CCCCC FNNHSH48 P18 CCCCCCCCCCCCCC.C 144814441414 14141414................................ C 00 P E FFFF EEEEE PEEE FF G F P C AAAAAAACC14C 1C CCCCCC CCCCC R "h hD1hRM 4 CCCCCCCCCCCCCC 4411414R14411441 RHAH 4AB CC...................................... C D EE PFFFF EPEEE EEEPEE FF GG F EE D C R 4AAAAAA BR4 CCCCCCC CCC(C CCCC4141414144181414414 17CCC.CCCCCCCCC.C H814814R1R8144414144 144)4141414141,14 1411481414. ...........

.. ......... E E FFFFFF EEEEE EEE PFF G G FF E D C B AAAAAAA1414CCCC 41 1 1 CC tC CC CCCCCC 4 44H1 4444AD1 CCCCCCCCCCC17C 141B.44PR BHRP 1 RB 4BB. .. . . .. . .. . ..

D P PVPPPPPD EEEF EEEE PP GG G 1 E D C 1AAAAAAAHCC 1 4 14414414111 CCCCCCCCCCCCC ,11nHU4 MHB4C CCCCCCCCCCCC 11RU b PUH10B14R1PH4H ......................................... "......C EE FFFFFFF EEEEE EEEEEE FF GGG FF.F. ED C AAAAAA A RA CCCRBBRB~sRP CCCCC CCC CCC Bs98H8 A."O I CCCCCCCCCCCCC RR Ab R6b A H RB He R B P B ..... R........................................

..... . EE FFFFFFFF EEEEE EEEEE FF G FF E P C A AA1AAAA141414 144R1R RCCCCCCCCCCC 1 4r n NU 4.144 CCCCCCCCC H14441441B4141BH44hFBI H 4 R1H4148 ,, , ...............

................ E FFFFFFFF E EE EEPEEEE FF PPFF P 0 C 14 1AAAA 14411 CC 41414)U1414141CCCCC CCCCCC 1444444114444441811111111 1A.....1.............................

.............. 0.41EFFFFFFFFFFF E.EE EF EEEEEEFE FF 1 41FFF E D C R AAAA AAA4 41AAAAAPR41H41RNRN1nNPRh1 1 141AAA................... ......... GG FFF FF EEEE E E PE 0 CC 414 A1FF4D4CA A A AAAAAAAR 4AAA ACC 1481C DCC CC448CC 1 H4R1HP1 A141414A4..............................................

000.......GG PPF PEEPE EPEE PP 0 CC 8148 AAAAAAAAAAAAAAAAAAAAAAA 4141414141414 1414481414141414141414e4 14P141414141 1..4"4.4 1 AAAAAA.." ..... . . . . . ......................... . F GG PFF EE 000 EEEP PP FTP D CC 84 AAAAAAAAAAAAAAAAAAAAAAAA111 FAA4A 4 b1 1R41R44 P4 4 1 4444AAAAAA.................... ........ .......... 1.".... G G FFF EEE 0 0. EE PE F FFF EE 00 CC 14 AAAAAAAAAAAAAAAAAAAA44 A AA A HHBHHNU1 1 4P 4 41 ) 41 4 H4F. 8 N4 1 AAAAAAA................................ .........

. P ..... P.........GGGGPFFF E 0 0 EEPFPPEE 0 CC 1 AAAAHAAAAHAA AAAAAAAAAAA 1 A NA Rbb 1, 4.1948'1-4414441 .H" 4 1{1411 SH41AAAAAAA,,A..................................................... .HGGG FFF EEE DDD EEEEEEE D CC RA AAAAAA AA AAAAA AAAAAAAAAAAAAA PH BE1RBN IH nvNHH)3l abbAUhBAHHHSRHRR hA AAAAAAAA.." ...... ".....................

....... P EEP 00000000 EPE EPPPEPEEE PPEPE +p )ED C R 1 AAAAAAAAA4AAAAAAAAAAAA141441441411A114114144 1 )P+H14H H+AAAAAAAAAA..................................+..........P................H G FF EEE EE00 01E E E EE E EE EP CAAAAAAAAA148 1414141414141414rA1441441 1r4FSO4A+.............................................................

.......... .. GGG FFF EEEE DDDDD D .EEEEEEEEEEE EFE EPE 1D A CC 1414 1411AAA AAA AA4AAAAAAAAAA4 AA 814141444141444)1414 61 8 ... 1.4...........,........14.................................. ".... FF EEEEE DDDDDDE E+ 00 EEEEE P OiD CC 14 AA AAAA AA AAAAA4 AAAAAAAAAAAA A 141414144141414141 1AAA14h4 8141.4 4H1h4h1wH 4A A A 141 A......................................

.0...............H.0 0F0EEEEE ODDD0DD IEEE EPE EE )0 CC B4 141414141411CC1A: AAAAAAAAAAAAAA4AAAAAAAAAAAA~HAn Nr 411414R1)HH4wRHUR4ah1X1HHRNH."418 4, AA144....................P........... .. EEEEEEEEE DDDD000.." ." ..D..PEEEE.. C 1 4 AA A AA A AA A AA A A AA41 1 14141414A41A .. . . ....................................................

................. EEEEEEEE EEE DDDDDDDDD D D 0 EEE PEE ) 0 C 1144 1CRA AAAAPAAAAAAAAUAAAAAA AAAAAA AAAAA AAA1AA4A A................................"...........................

.... P.EEEE DDFODDDDDO DD D01)1)00DDDD PP PEE 0 C 1414 14AAAAAAAAAA441411AAAAAAAAAAAAAAA44141141AAAAAA44141814A14AAA1 1411 C F8H a . .. ... ... .. .... .. .. . .... . ..... .. .....PEEE 1)0"."" "...DF0FDE0ED000DD 0D PP EEPE 0 C 1414 14141414141C R1AA AAAAAAAAAAAAAAAA AAAAAAAAAAAAAAAA AAAnC AP1).. ..... .................. ,, .... ...... ... ..... ................. EE 00000)01)0 0 00000EEPEEEDDDDDD0D0D C 14EEAEEEDC C AA A AAAAAAAAAAAAAAAAA AAAAHAAAAAAAAAAAAAAAAAA414411441144NA 4 4 1.. ............................

.......... EEE . DOD..DDD0 D0 10 PP EEFE D0CC 1414 AAAAAAAAA AAAAAAAAAAAACAAAAAAAAAAA A AAA Arh,....................... ....... ...... 1.....................,.....

... ... EEE 0140DD DDD 0DD0D0 000 EEI EEPE 00 CC 141 AAAAAAAAA41441141AAAAAAAAAAAAAAAAAA4141 AAAAAAAAA441 AAA.44 4148b C 41414 .... .... ... .... ... .... .... ....... ... .,.. .... ... .... ...

. . . ". ...... FFFFFFFDDDDDDDD DDDDDODDDD DDD D DD E FE EEEFD C b A AAAAA AAAAAAA AAH AA4 AA AAAA HAAAAAA, AAAAA NHH SPB h PN+H AAA.... ....... . . . . . . . . . . . . . . . . . . . . . . . . . . .

... EEP 14000DD 01)1) EE EEEEE 00CC EC R AAA AAA AAAHAAAAAA HAA AAAAAAAAAAAAAAAAAAAA........C......,.............................................. ....... .EEE 1 00DD0440 PE 0F D CC H4 AA4 AAAAAAAAAAA44 AA OA A 0A AAAA1AAA AAAAA HH1414114C411411 AI+H1M. .. ,. .. . . . .. . . . . . . . ., . . ..

.... . EPPPEEE PEDDDDD 0 DD0)EEEEEEE0D00CC H1414 AAAAAAAAAAA A AA A A AAAAAAAAAAAAA1AAAAAApAA A) h C HPRAH . . .... .. .

.. . . .EEEEEE DpppDDDp~p~pP 000 D000004) D4D D E411)1)00(40000 CC 14 AAAAAAAAAAAAAAAA AAAAAAAAAAAAA4AA1AAAAA1.A..AA.A.AA..88.A...... .. ............ ... .... .....................

......... EE.FE EEEEEE EEE EEE 0110 0 )D D0 DD F 014004D1 CC 14 AAAAAAAAAAAAAAAAAAA AA AAAAAAAAAAAAAAAAAAA AA AAA AAA AAA..............4....................................... """"4."... ...... .......

......... EEEEEEEEE EEEEE 000 CCDDD) DD FE EF0C 0001DAAA H A CC 4AAA A AAAAAAAAAAAAA AAAAA AAAAAAAAAA4 A A AAAAAAA H.{ A A1A . ........................................................................ P... F EE E PEPEEE 000 CCCCCDD0001D 044)4)0 44D CC 1 AA AAAA AAAAAAAAAAAAAAAAAAAAAAAAAA1AAAAAAAAAAAAAAAAHAAAAAAA 4 ) .. ."..............."... ....... ,....... . .............................. "

.... EEEF EDD EEEFE 0D CCCCDD D0Df4D 00000 . D CC 1NR A4 A AA AAAAAAAAAAAAAAAAAA AAAAA)AAAAHAAAHAAA4 A0AAAAAAAA AAAAA8 4aAPAHH.................................................................................... EEFFEEEEEP EEE E 000 CCCCCC1D)DDDUOUDF)0) DDO CC)A44AAAAAAAAAAAA4A)AA1AA0ACAAA AAAAAAAA& AA A44AAA1H>001<:0.I,"4 ", ,"1AA AA,,AA ,A1 4 4),, 4. , . . . . . . . . . .. ............................ ,,.....

......... FEF EEEEEEE EEEE D CCCCCCCC DDDDD0D)D0000DED 0001 D00 CC 14 AAA AA AAAAA AAAAAA AAAAAAAAAAAAAAAAAA AAA0AAA44440AAAAAAAAA1AAAAAAA1 A 414 1AiAA ea... E PE :E EEPEEE EE PE DDn CCCCCCCC 0040DDD0)040N0 000)4 C AAAAAACAAACAAAAAAAAA0AAAAAAAAAA A OA AA4H1)AAAAAA AAA0AAAA 4 1AAAAF1 H1 1 . 1...... . . . . . . . . . ........... ..... .... ........

........ EE EEEE E EEPE E DD0)DD CCCCCCC 4) DDD014 DD14000 ) DD) 01 l CC F AAAAAAAAAAApAAA00 )A0A AAAAAAAAAAA A1AAAAAAAAA AAAAAAAAAAAA NAHH1441k ............................................................................

........ EEEEEEFEEEFE EEEEE 00 CCCCCC 0 ' DDD0 0 D0 DD0 0 4)0D D CC 1. C 4AAAA4A A A AAAAA AAA AAAAAAAAAAAAAAAAAAAAAAAA)AAADAAAA AAAA4 1AAA Nn H................. .. . .................. " " . ",.......... .,"......... .. ........,." "FEE EEE 0000EEE DD CCCCC 04000400041lDl000 C.1)))1) f1 CC A 14144' 144A 414 81.AAAAA0AA0A .4AA~~ p 4414148) AH4"w0),,, , ..,.,,,,.,.,.,,, ,..,.,, ..

.. . . . EEEFEEEE E EE E E DD CCCCCCC 1 DDD D DD O CCD CC AA0AAAAAAHAA4AA AAA AAA1AAAAAAAA AAAAAAAAAAAA AAAA AA44AAAA 4...,...............,....................... . . . . . . . . . . .,

........ FEEEEFEE EE1)0 C CCCCCC C C D.00DDD4 DD14 DD40D0 CCC17CCCCDCCCC CAAAAAAAAAAA4AAAAAOAAAAPACAAC4AAAAAAAAAA. 1H A AAAAAAAAAAA AAAAAA1)a4)81 84 ....... . . ... .. . . .. . ...........................

.... E.... . . . .. E. .EEE)))EF ). . . . CCDDCCCCCC. . . . . . . .. DD. .D..CCC.AAAAAAAAA.AAA.AAAAA AAA A.AAAA AA 0A AAAAAAAAAAAAAAAA. .'.r Hr+H .................................. ................. ................................ HE "{,1C.C. . . .)0,CCI <CC. . . .A.. . ...... . . . ............ ... . .... ............ ...............

........ ..EE .... CC.CCCC . 00 . . C CC.......A...A...AAsAAA,...A ...pA............................... ,....

........ EE. . . .. CCCCCCCCCCa.. . . . . . CCCCCCCCC. C. .C C......... ..................................... ..................

........ .. ...... ...... ... . ...... .... C . . 000 0 ........ ........ ..... CRC CA00.... ......... ........ ........ ........ ........ .............................. HN . ....................................... .............. . .......................... ........................... E:E ........-.. CCCCC .................................................................................................

."".. . . . . . . . . . . . . . . . . . . . .. "0 0 . . . . . . . . ..... FEF DD CCC0CCDD O D0 U nCC C.. .. .. .. .. .. .. ... .. .. .. .. .. .. ... .. .. .. .. .. .. ... .. .. .. .. .. .. .............................. .....................................................

. .... . . . ..... . .0......................C.................... . . . . . . .... ............................... +.................................+.. 000101)0....................... C+CCCCCr..... .......................+................... ...................................... ..........................................+...........................................

............................................ nn00000.............-.........CCCCCCCC........................ .........-.-..-..................................................................................................................................

. . . . . ................................ ....n Dn n n ....................... CCCCCCCC.....................-... ".-.....* - . - .- - . - -... .. . ........ ..-... .. .... ..... .--.................................---...... "- ."...-....................... .. -

GF )1'IA I0NT ) 4 AIIAI.. I 1 .,A)L,1 IF 1AS

i r.- I, I' I. v.;I =- . I- I, I - (.I , I'I Ia l A" . , i I II -7h6 .0 l

7.jo <:;< 7.80 '1 . '<I< 1 :, ), I1%. r1< < ]%2.0

, '. le II I F . 1 si1.1 I .1 "r . , 1 .. II ; ,

.......... *......K L L ............. .GGGGGG GGGG................ FF FE ........................................................................... * GGG * C...................................... ........................ n ................

................................... .GGGGGC. GGGG................FFF f:EEEEEEE ........................................................................... GG(, r ...................................... CC ....................... n .................. G... ...... ... GGGG GGG ............ . .FFF FE EE E F .. ........... (",,."... .(, ........ CC....... ........ ). ...

....... F............................F . GGGG...............FFF F FF.F.................................. .................. ".............. ..... GG,4 C ...... ,.............. . , . .. .0 C ....,.................. ...... ..... ...... . . .... GG ... FFF F .......... ..... ........................ .GG ...,,.....*.........,............C..... b 0 C ...... . . . . . ..

.. . ....... GG ........ FFF ... ...... ...no.. ... . .... LC............. ...... . .GGGG.FF .... ........................... G................... C...... ........

."..".. ................ ISHfI HH" GGGGH , H . 4 H , HH h1F F FiFF HGH..............................1HHHdFMHHMH«HHHHHrMw HHHHHHHHHHH'- .GG 4i h A 1 J l " 1HHH G FF F 0') ClECCCC DC1CLC .-CCC........... 1111III HHH GGGGGGG FFFF FE FFF G HH........................ ' ,HF H HHiHI 'HHOIH GG l I J' H G F CCCCCCCCC 1DD CCCCCCCCCC........

"....l.................11 HHHH GGGGGG FFFF EFE FF G H ........................ ,..... NHHHH GG H I I NH (GG FF F 01 CCCCCCCCC DDDDC CCCCCCCCCC......... .. ... .. HHHH CGGGGG FFFF EEEEEE FF G H I0............................. iHHn Gt H 11 1 HH GG.GGGG F FF O CCCCCCCC DO CCCCCCCCCCC.....

..... HHHH GGGGG FFF E EE EEE FG H I ........................... III1 Ill H H{ ll HH GGGGG FF F EF CCCCCCCCCC U CCCCCCCCCCC........................ HHHXHHHNHH GGGGG FFF EF EEE FG H J........................... 1111l1 I1T11TI HP rHH HHH GGGG FF FF 0 CCCCCCCCCC CCCCCCCCCCCC........

. . HHHHHHHHHHHHHHHH OGG GGGGG FFF EEE FF G H J JJJ 117IIIIIT[TITIIII1111TI 1111 N IHHH 0GGG , HH HHH GGG FF FE D CCCCCCCCCC CCCCCCCCHHH HHHHHHHHHHH GGGGG GGGGG FF1 EFF FF. G HI J JJJJ I1lJIJTT111IIIIT T111111 11! HHHNH GGGGGG G 4HH HH GG F 1FF 0 ) CCCCCCCCCC CCCCHHNHHHHHHHHHH GGGGGGGGGG GGGGG FF E EFF1' F f HI J JJJJJ 11111111T1111111111111 1 4 H GSGGr(. GG HHHHHHNH GG F FFF D)) CCCCCCCCCCCC CCCCHHHHHHHHHHHHH GGGGGGGGGG GGGGG FF FFE EFF F G HI J JJJJ IITIIIIITIIIIT1 1111 HHH Hi, GG~G r;(.GGNGo HHH G FF F lDDD CCCCCCCCCCCCC CCCC

..... .. HHHHHHHHHHHH GGCGGGGG GGGGGGG FFF GGT FF EFEEEEE F G HIH J JJJ II "I'l" 11T "l"1 HHHHHH" nNHAGI:^, C.C.GGC(; NH 1; F E OD CCCCCCCCCCCCCC CCC

HHHHHH GGGGGGGGGGGG GGGGGG FFF FEFEEF F G 1 J JJ TIIHIII IIIIuII:I T UHHHHH HH GGG (,GCGGGGG ccGG G F F D0l ('CCCCCCCCCCCCCCCCCC CCC CCHHHHHHHHHH GGGGGGGGGGGCGGG GGGGGGGGGG FFF EFF GF fiG HI 1 J 7JJJJJ 1T[LIIlTIITf11t1TI HFHHHH 4HHHHH GGGGG OGGGGGGGGGGGG FF F DD CCCCCCCCCCCCCCCCCCC CCCCC

....... HHHHHHHHHHHHHH GGGGGGGGGGGGGGGGGGGGGGGG FFFF FFFF G HH III 1111114I111111IIII H4uI'lH GIGGG FFFFFFFFFFFFFF GG F lF 1TO (CCCCCCCCCCCCCCCCCCC CCCCCHHHNHHHHHHHHH HH GGGGCGGGGGGGGGGGGI;CGGGGG FFFFFFFFFFFFFFF G HI 11 HMHr'r' GGGGGGGCG FFFF F FFFFF FFFFF F 01 CCCCCCCCCCCCCCCCCCCCCCC CCCCCCCC A

HHHHHIIHHHHHHHHH GGGGGGGG GGGGGGGGGGGGGGG FFFFFFFFFFF F G HHH. HHHFHHn GGGGCC, FFFF F.FFFE F FFFFFFFF EFE lD'T) CCCCCCCCCC CCCCCCCCCCCCCC CCCCCCCCCCCC BBB................ HHHH HHHHHHHHH GGGGGGGG GGGGGGGGGGGGGGGC FFFF FE DO F F G HHHHHHHHHHHHHH HHHH HHHN H G GGGGGG FFFFF FFFE 0000 EF EEEE DDDD CCCC('CCC CCCCCCC(CCCCCCCCCCCCCCCCCCCCCCCCCCCCC BARB

HHH HHHHH GGGGGGGG GGGGGGGG GGGGCGC. FF D C Cu F F G HHHHHHHHHHHHHHUHHH HII G(,GGGG OFF EFF P 0004 10 ? FFF FFFF F i)4D; CCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC C H......... HHHH HHHHHH GGGGGGG GGGGGGGGGCGGGGGGGGG FFF F U CC C DO F CGGG HHHHHH4HHHHHHHn GGG( FF FF E1. bDD C 1)C EEEE:F. 1 ) CCCCCCCC CCCCCCCCCCCCCCCCCCCC B14

.. HHHH HHHHHHCH GGGGGGGGG GGGGGGGGGGGGG FFFF F. n CC F F GGGG HHHHHIHHH*, GGG 'FFF EFFr D10 CCC 0114 E On CCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC 1.B... . HHHH HHHHHHHH GGGGGGGGGG GGGGGGGGGGGGGGGGGG FFFF F CC TF F FF1 GGGGGCGGG HM HHHHHH EGG FFF FEFFl F 10nDn CC CCC UDUC CCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC 11B4

HHHNH HHHHHHHHHH GGGGGGGGGGGCG GGGGGCGGGG G FFFF EF. 01) E FFFFFF CCG HH HHHHHH GG EFF F D)00D CCC CCC ) TDDD CCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC BB.1HH14HHHHHHHHHHH GGGGGG GGGGGG GGGGGGGIIIGGG FFF FE 0 DD FF FFFFFFFF GG HH HHHFH GGF Fl FD 0000DD00 H CCC CC DtB)B)'FF CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC APB

............... GHHHHHHHHHHHHHH GGGGG GGGGGGGGGGGGGGGGGG FFF FE DD)) FFFF FFFFF GMG H H1H4.4 GG F EF Do 0400r)) 1 (CCC CC W00)0"4o CCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC KB. HH HHHH HHHHHHH H GGGGGGGGGG GGGGGG FFFFF EFF DODO1 FFF FFFFF GG HHHHHH GG FE FF n u nn I00ulnouoof CCCC CCCC D'0DDn11) CCC CCCCCCCCCCCCCCCCCCCCCCCCCC 144

............. HHHHHHHHHNHIH + GGGGGGGGGGGGG FFFFFFFFF+ EF F 001)) F F: FFF+FFF GG GG FCG FF rI) 011)I)4n1)01W CCCC + CCCCC + CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC+ BB

HHHHH)HHHHHHHH4 GGGGGGGG FFFFFFF EFELE DD0 EFF FFFFFFFFFF: I GGGGGoG Fr F; lr0I,)0t)I 000DI CCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC . FIBA.B........ . HHHHHHHHHHHHHHHH HHHH GGGG FFFF EEFEEFE. I) E FFFFFFFFFFFFF GGG FF E EI D00D1D4I,0DD),D'D)1l)0Du04 ' CCCCCCCCCCCCCCCC CCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCC RBBRB

.. .. HHHHHHHHHHHH.HHHHHHHHHHHHHHH GGGG FFF FEEEEFEFE 1)0 EF FFFFFFFFFFFFFFFF FFFF FF1 Ir nl)I;4)DDDI I D 01)0DonDO,0)0D CCCCCCCCCCCCCCCCCCCC CCCCCCC CCCCCCCCCCCCCCCCCCC BBRBRB.... HHHHHHHHHHHHHHHHHHHHHHHHHHHHHHHH GGG FF EEEFE D FFFF 01)FEF FFFFF FFFFFFFFFFFFFFFFFFFFFFF FF DI,'.0D0))1)D "OD CCC CCCCCCCCCCCCCCCC CCCCCCCC CCCCCCCCCCCCCCCC BRB.H

.......... HH4HHHHHHHHHHHHHHHHHHHHHHHHHHH GGGG FFF EEEEEE EFEFFEFE D FE FFFF FFFFFFFFFFFFFF FFFFFF IUl000) 0) ID CCCC CCCCCCCCCCCCC CCCCCCC CCCCCCCCCCCCCCC B1RBBBHHHHHHHHHHHHHHHHHHHHH.H GGG FFF EE F D) FEF FFFF FFFFFFFF EEFFL LEEEFFE )InDnDDl 41Dnn CCCC CCCCCCCCCCCCC CCCCCCC CCCCCCCCCCCCCCCC HBB

......... .... HHHHHHHHHHHHHHHHHHH GGGG FFF EEEEFFDDFDF) E FFF G FFFFF EFF F F. FE FE EFFFF.Ff EE . C DnbIDU 1D0 CCCC CCCCCCCCCC CCCCCCC CCCCCCCCCCCCCCCCC PBBBB. ........... G HHHHHHHHHIHHHHHHHHH GGG FFF FEF DDn1 FEE FF GGGG FF1 EEFLEFL LIEE EFEEFFFE )1:1 DDDU00D DDDD CCCC CCCCCCC CCCCCC CCCCCCCCCCCCCCCCC BBBB A

............... GG HHHHHHHHHHH GGG FFF EFEEEE DDODDDD EE FFF GGGGG FFF FF EE FFF P FE FE)Eb F 1nD)1) CCCC CCCC H CCCCCC CCCCCCCCCCCCCCCCC BBBB AA... GGG GGG FFF EFEEE E DIDfDlDDDD F FF GG GGG FFF EFF DDDU EFF : n I I) 0) I. DDD CCCC C B CCCCCC CCCCCCCCCCCCCCCCCC bB AA

... .. GGGGGGGGGG GGGG FFFF EEEEEE DDO EF FF GGG GGG FF FF1 DOD T.n0L FFFFF EF 011DDD1DI)D '11)D) CCCC CCCCCCCCC B8B CCCCCC CCCCCCCCCCCCCCCCCCCC 44.......GGGGGGGG GGGG FFFF EEEFEE FF EFE FF CGG GG GGG FlF IE 0ODp1uD FEFFEF l1D00D141)0DDD1DD04 1DD)0 CCCCCCCCCCCCCC B4B1 CCCCCCCCCCCCCCCCCCCCCCCCCC s........

......... FF GGGGGG GGGGGGGGGGGC FFF FEEFEFF EEEE FFF GGGGGGGG FF FF OtJ0)0vV4;t 11DUD D00DD4)I0DD 000)4) CCCCCCCCCC B1 CCCCCCCCCCCCCCCCCCCCCCCC B84B...FFFF GGGG GGGGGGGGGGGG FFFF EEEEEEE EFEFEE FFFF GGG GCGGG(G(GG FF El 0

4D01)0D b0DDD1UD)D1)0 D)r' O Dn LFDDD CCCC HHHBB CCCCCCCCCCCCCCCCCCCCC BBB.".."..

........ EFFF GGG GGGGGGGGGGGG FFFF EEEEEEEE EEE EEE FFF GGGG GGGGGG FF EE Un4 ID )OD'D0UDDD DDUDUD D 0140 CCC PBITBBHAA1 CCCCCCCCCCCCCCCCCCC BBBHBB.........E FFF GGG GGGG FFFFF FEFEEE EFE FF GG HHHH GGGGGG FF E 1)0DU): DD nt4unD )1DDDI1DI CCCC BNHRHBHRBB CCCCCCCCCCCCCCCCC R1d1BBB......

.EEE FF G GGG FFFF EE EFE FF GC G HHHH4 1.,GG G FF F )D1D1 1DD0DD pD CCC BBBHRRBBB CCCCCCCCCCCCCC 4BBBBBBB,........FEE.., ... IGEEE FFF GG GGG FFF EE DDDD FEE FF GG HHHHHHHH GGGGGG FF FE L DD1 CC DD) flDnn CCC RNHnRnHHB CCCCCCCCCCCC MB.BB .".......

........ EEE FF GGG GGGG GGG FF E D DDDD D F EE F GG HHHHHHHH GGGGGG F FE DD0 CCCCCC DDDDDDD0D CCC 1RRHHnRHA CCCCCCCC BBBB ........F...EE FFF C GGG FF GGGGG F F 0 C DDD EF.E FF G HHHHHHHH GGGGGGG F FE DIFU) CCCCCCCCCCC ODD0D1)DD0D CCC H BABBRBRBB 14BBRB A........

EEE FF GG GGG FFFF GGGGGG F F D CCCC DDD FEE FF GG HhHHHHHH 1GGGGGG F FE 100 CC('CCCCCCCCC 0D)D1D)D0DD1 CCC HRPH1BBBRBB4HRBR A11BR AAA........ F........ EEE FF GG GGGGG FFFFF GGGGGGG F E D C CCC DD0 EF FF GG HHHHHH GGGGGGGC FF FE 1)11Off CCCCCCCCCCCCCCC CCCCCCCCCCC DDDDDODDDDD CC 1bHRABARHHdRR4 BBB AAAA........

................ 0 FEE FF GGGGGGGGGG FF FFF GGGGGG F F D CB CCC D FE FF GG HHH 41 GGGGGc FF KF 01) CCCCCCCCCCCCC CCCCCCCCC D)0DOUD00DD0D CCC Rb1414 RRH B H H R H1BB 1 4H)1 .B4B1B.4.......... ...... .0 EEE FFF GGGGGGGG FFF FF GGGGG F E D CB CCC DD EE FF GGGGGGGG GGGGG GG F F rE 40n CCCCCCCCCC DD CCCC 4HHBR4H1 BB41BRR1 RBRRR ..........

. 00 E FFF FFF FFF GGG FF F 0 C CCC DO EF FFFF G G FF EFF 4) CCCCCCCCCCC CCCCCC HBR14 1R4 BBBBBBBAH11B4 BHBR1BR11 .... .......... -.000 FEE FFF FFF FF GG FFF F D C CCC DD FE FFFFFF FFFFFFFFFFFF G FFF FL 44D) CCCCCCCCCCCCCCC CCCCCCC 14BB1R414144 BBBH4b1BBBB41BB1........

.. . FDD EEE FFFFF FFF FFF G FFF E DD C CC DD F FFFFFFFFFFFFF FFFFFFFF G FF LFE DDD DnD CCCCC CCCCCCC CCCCCC 14S14HB4R14 yBB1B ....... 0.......... DDD EEE FFFFFFF FF1 F FF FFFF F 0 C CC DD FE FFFFFFF EFFE FFFF G FI EF 00 1)I11)),0D00I)1D000 CCCC CCCC CCCCCC 144141141 1141...1.....

. 0 DDD EEEE FFFFFFFFFFF E FFF FFFFFF E DD C CCC D FE FFFFFF 1FFFFFEE FIF C F F FE 0DF F F CD F FTGD,)1 I,.0100I000 'CCC CCC CCCCCC HRRRHA 0........................ 000 EEEE FFFFFFFFFFF F FFFFFFFFFFF E D C CCC DD L FFFFF EFFF FE FFF FF FE 0D t00C'0000 0000C00 CCC CCC CCCCCC .4AR1 B .............. '

.0...0......DD EFEEE FFFFFFFFFF FFFFFFFFF FE D CCC DD EE FFFFF FEEEt FFFE FFF FF EF DU DDDUDnD D IDD 1) D, (CCCC CCC CCCC(C C nRBB41 .. ...

... . .D EEEEE FFFFFFFFFF FF E D C D EE FFFFF EEEFE EEF FFF FF EF D ' 00))010)1))001004 CCCC CCC (CCCCC AR ................F.EEEEEF FFFFFFFF EEEE F F DO 00 EFFFFFF EEF EFFF FF FFF FDODDDOD U O CCCCCCC C"E FFFFFFFFF EC1EE1E F E.DD4DDDDEEFFFFF EEEE EEFE FFF FFF RECC ...............

......... EEEE FFFFFFFF EEEEEEFEE F FE 0 DDDDOD FE FFFF FEFEE EEF FF1' FFF FEE 01)0 l)01DD000I)D)1)41001)DD01, CCCC CCC 00 C(CCCCr 14141144 1, .... ,....,

......... +......nEEEEEE FFFFFFF F F + 0E EEE FE 00000 D+ E F F F1' EFE FF1+ FF EEF 000 0g+ )000010l10I)))) CCCC + CCC DDDD)CCCCC+ B.1 B418.................. '................ EEFEEE FFFFFFFFFFFF EEEFEE EE D0 D EEEEEE EEE FFFFFF FFFF F 00D 000010oL0o0000004000 CCCC CCCC DDDDDO CCCCCC 18 14RBBBB11.......................

.... EEEEEE FFFFFFFFFFFFFFFF EFEEE EE DD CCCCCCC ODD DDDD F.E FFFFFFF FFF E D 00D0D D )DD)DDD)D CCCCCC CCCC 0D0UD0n0 CCCC 4R1B4B0B ...................

... EEEE FFFFFFFFFFFFFFFFFFFF EEEEEEE DD CCCC CCC D0DDDDDU 04 O FIE FFFFFFFFFFFFF EE 000 C bDDDD IDD)0TD CCCCCCC CCCC U0n010000)100) CCCCC 41414CCC.................................... EEE FFFFFFFFFFFFFFFFFFFFFFFFF EEEEEE DD CCC RAB CCCCCC D FE FFFF FFFFF FEE 1DD1 C DDDDI1)0) 1 CCCCCCCCCCCCCCCCCC D DDODDUDDDU D0D0D0 CCCC CCC........

.EE FFFFFFFFFFFFFFFF FFFF EEE DD CCC 11 RRB CCCC DD1FF FFF FFFFF FE 01) CCC D DD1)0)D0'CCCCCCCCCCCCCCCC DDDDDDD1 00D0DDDDD CCCC CCC............ EE FFFFFFFFFFFFFFFF FFFF EEEE DO CC 1B 1411 C E FFFF G FFFF EEF1 DD CCCC D1)T001DLD CCCCCCCCCCCCCC 1DDDD) O1 0DD0)D CCCC CCC 0...................

. . E FFFFFFFFFFFFFFFF FFFFF EEEE E 0 CCC 1B A 4BB C D E FFF FFFF FE E )1n CCCC 0D0Dt).UDD CCCCCCCCCCCCCCC P1)0000 01)000 CCCC CCC 0................... FFFFFFFFFFFFFFFFFF FFFFF EFEE DD CC BB A 111 C D E FFFFFFF EFF )DDDD CCCCC D DDII1L CCCCCCCCCCCCCCCC.................CCCCCCC

... .. FFFFFFFFFFFFFFFFF FFFFF EEEE DDD CC 8A4AA RB1C18. C 0 F FFF FFFF EFF DDDD CCCCCC DD1)CCCC.F CCCCCCCCCCCCCC DD0D0 0 D CCCC ........................FFFFFFFIFFFFFFFFFFFFFFFF FFFF EEEE 000 C 41 AAAAAAAAA BB8 C ) FE FFF FFFF EEL DDOD CCCCCCC DDIIDDD) CCCCCCCCCCCCC DUDDDD D0DDD CCC ........

............ FFFFFFFFFFFFFFFFFFFFFFFFF FFFF EEEE DD CC B4 AAAAAAAAAAA b C D FF FFF EF 1DP10D CCCCCCCC CCCCCCCCCCCCC D1DDD DDD .......... FFFFFFFFFFFFFFFFFFFFFFFFFF FFFFF EEEFEE DD CC BB AAAAAAAAA 4 C D EF FF FFF EEL 1)D1D CCCCCCCC CCCCCCCCCCC DDD 1D)DD .. . . . .

FFFFFFFFFFFFFFFFFFFFFFFFFFFFFFF F:EEEEE D C B A1AAAAA4 B C D FEE FFF EFEE 10DnUIDi1 CCCCCCC CCCCCCCCCCCCC [1DD)4)01)1) 0 ...................

.E . FFFFFFFFFFFFFFFFFFFFFFFFFF EFEEEEEEEEEEEEEEE 0 C 841 1AAAAA4 B C FEF EFFFE )0

T '0I)001 CCCCCCCCCCCC DD CCCCCCCCCCCCC )DDDDUD EEEEF 00..................................... ,....EE FFFFFFFFFFFFFFFFFFFFFFF EEEEEFEE FF E DD C 11 8AAAA 11 CC D11 EEE Io)4,0000lb 0 CCCCCCCCCCCCCCCCCCCC D0DD D CCCCCCCCCCCCC 000A0IDDF EE EE ..... ..........F...... .. EE FFFFF FFFFFFFFFFF EFEFEEEEEF E FFF F E D CC 4 8AAA 1N CC DD)01 0 1D)DDDF)0FiDF l'1D 0 (CCCCCCCCCCCCC CCCCCCC 4)lD)D0D4) CCCCCCCCCCCCCC DDDD0DE E FF EEE..............................

.00 FE FFFF FTFFFFFFFF EFEEE EEEE FF GG G F F D CC 1 A81A 14 CCC DDDD4)DD0 DDDl400 )DD CCCCCCC CCCC )D))0D0DDD0)D CCCCCCCCCCCCC 4D0DDDD0 O EE FF FF E.................D EE FFFF FFFFFFFF EFEE FEE F GG H G F E C B AAA CCCCCCC D DUDD1) D D( CCCCC CCC D)nm)D D 1)DE0 CCCCCCCCC CCCC DDUDDDU U F. FF............

.0. . FE FFFF FFFFFFFF FEEFE EEE F G H G F F T C 1 AAA B4 CCCCCCCCCC 01nD0)D) 1C U CCC C'( CCC D) 4DDDDn0 CCCCCCCC CCCC ODDDODDDOODPU FE FF............ ...............

S . ........... DD E FFFF FFFFFFFF EEEEE EEEE FF G H 0 F FD C 1 AAAB R CCCCCCCCCCCCCCC DfoDU)4r DC CCCC CCCCC D0000001fF CCCCCCCC CCCC CC0DUDDDDD F FE F.............. 00 FE FFFF FFFFFFF EEEFE EEEE FF GG M G F E D C A AAR 4 CCCCCCCCCCCCCCCCC ")o0I0D1 4 1;01' CCCCC CCC DTfDn)D1)DD)0) CCCCCCC CCCC DDnnDpDnnOD EF .... ....... ...............

D. . FE IFFF FFFFFFFF EFEE EEE FF G H H G F F D C A81AA B CCCCCCCCCCCCCCCCCCC lUDPOFnDDU) CCCCC CCC nnnD001)D1)1 CCCCCCC (CCCC DDODD10D D FE"......... D EE FFFFF FFFFFFFF EEEEE EEE FF G H H G F ED C R AA BBB CCCCCCCCCCCCCCCCCCC DDD1DD 0 CCCCC CCC 040D0D1lDD CCCCCC rCCC )DDDDD)41)1")1 EE'.............................

....... ,....D EEE FFFFF FFFFFFFF EEEEEE EEEE F G H H G F FO CR AA q1B4 CCCCC 4))11'Of0 CCCCC CCCC ) 10 0000F CCCCC CCCC D0U0D0D............................................. .. EEE FFFFFFF FFFFFFFFF FEEEEFEEE FF GG HH G F E D C B 4PHB CCCCC 1DUO) CCCCCC CCCC ,DIII)04) CCCCC CCCCC 0D ............ ......

... ,FFFFFFFFFFFFFFFFFFF EEE FFF GG H G FF F D C RRBBA AB RB)H 1C1 CCCC D CCCCC (CCCC UDn1 CCCC CCCCC 0)401..............:............................... FFFFFFFFFFFFFFFFFFFFFFF FFFFF GGG GG FF F D C 4R14R1R4141 FHHP1M4RR4HHH14 CCCCC CCCCC C( CCCCC (DDCCCC 4 CCCCCC 4)n0n............. ... .... .....

.,,.............FFFFFFFFFFF FFFFFFFF GGGGGGG FF F D C RR.RB14R1R4)111H1R4 RHB 4RRR CCCCCC CCCCCCCC CCCCC CCCCC HN CCCCCC 1)11)............................................................ GGGGG FFFFFFFFF FFFFFFFF GGGGG F FE CCC 4bBH4'1AB11 B44 4R41R. CCCCCCCC CCCCCCCCCCC CCCCCC CCCC B4B1 CCCCCC 00)............................................

..... . GGG FFFFFFF FFFFF F F DD CCC NHNR4 8H414. CCCCCCCCCCCC CCCCCCCCCCCCCCCCCC C CCCCC RRAH1 CCCCCC 400............................... .......... GG FFFFFF FFFF F F. 0 CC 4RBRA 1 RC CCCCCCCCCCCC CCC CCCCCCCCCC CCCCCCC CCCCC444144A CCCCCC no,..............................................

............... . GG FFFFFF FFFF F EE D CC BBR4 4B4 CCCCCCCCCCCCCCC ('CCCCC CCCCCCC CCCCC R4RBBH CCCCCC 0....... ............................. ... ,..H CG FFFFF FFFFFF F LE D CC B414 A 1414 1 CCCCCCCCC('CCCC (CCCCCCCC CCCCCCCC 14H 4HB H 4 CCCCC 00............................................

......... H G FFFFF FFFFFFF F E EI CC 1B AAAA H CCCC4CCCCCCCC CCCCCCC CCCCCCCCC (.RRIR4R1 CCCCCC 1D"............... ............... ........ " .. .... HH GGG IFF + FFFFFFFF + F 0) CC .44 1AAAAA + 84144 CCCCICCCCC + CCCCCCCCC CCCCCCCfC + MHBFO. BO CCCCC 0".+................+...."..."

............. "..HR GG FFFF FE FFFFFFFFFFFFFF FFFF D CC 88AAAAAA 0)" CC CCCCCCCC CC.......IGG FFF EEEEE FFFFFFcFFFFFFFFFFFFc FF FL CC CCCCCC C CCCCCCC C 4 ........... ............................................

............... GGFFFFFF EEEFEFEEF FFFFFF FF F D CC BO14 AAAAA 41 1A n4aw 1C 11 CCCCCC CCCC c CC .....................

................ FFFFFFF EEEEEEEE FF FF Fl 0 CC 1414F1FFFFFF1FF1BBBAA BNHbHB 1CCCCCCC ."""......... ............ .CCCC.CCC' 41141414.......................... FFF FFFF EEEE EFE EEEFEE EEEEEEEEFF FFF FF EF D C 11BA B4B A R14..R41M4R144141441.4lCCCCCCCCCCCCCCCCCC ...............

........ (....EEEE EE EEEEEEEEEEEEEEEEEECEEE FF FFF EE 0C CC 1141414 1. .. 41F1b. .CCC CCCCCCCCCCC ............................. ....F....FfEEEEEEEEFEEEEEEFEEEEEEE FI FT F 0 C 114141 41H144I4411141 14 144,1144114W) (CCC CCCCCC(CCCCC 1.................................................... .... FFEFFFFEFEEEEEEEEEEEFEFFFEFEE F E FF FFF FE 4 C 4114b4 R 4141nB14 AA1.A 1rn1CCC CCCCCCCCCCCC ................ C...................................................

. FFF EEEEFEEEEEEEEEEEEFEEEEEEEEEEEE E F FFF EE 00 CC 14414 1484)4.4414 88AAAA1 4141FFEnDC BAgH.4nbFh ('CC CCCCCCCCCCC BbC ... F.......FF E EEEEEEE EEEEEEE EEEEEEEFE EF F FFF F 4)F) CC 14141414 .64144114401.. 1.0AAAAA84 144,'4'11'"41"" (CCC (C"CCCC(CCCCCC.................................

FF E EEE EEEE EEEE EEE FE FF FFFF E D CC H CCC CCCCCCCCCCCCCCC .....................................................................F........T EEEEEEE EEEEEEEEE EEFEE FE F F FF 'FF .D CCC 1HB14 AR 330H 8AAAA A AA 4CC hnn-n14... CCC CCCCC('CCCCCCCCCCCC,....... ., .... ...............................................

. FT EE EFEEEFFEEEEEEEEEEEELEEE F FF FFFF F 1) CC R1411F1 41F)EEnUlC4H 8H1na01HaA p nAgA H«AA 41n 4 4HH4 C CCC CCCCCCCCCC............................,,,......................................... FFT EEEEEEEEFEEFEEEEFEFEEEE EE FF' FFFF L 11 CCC....1..........................4.......ACCC.C.........................

.... FFF EEEEEELEEEEEEEEEEEEEEEE E FF FFFFFR EF F CC F E nO CC4 4" h41AAAAntA AAAA1881 4oR14 CCC CCC CCCCCCC .................................. ................................ FFF EEEEEEEEE:E EEEEEEEEE FFFFFFFFF E 0C CC P1 41AAA1 ,FAA4 1411- 4AA .44.4 CCC CCCCCCCCCC..........

.. FF...... F",F EE000 EEEEEEEEEEEEEF FFFFFF 4DC C N I H4 RF {, 44114R41Aa1

1M 4 CCC CCC'CCCCCC............................. FFF FIFEEE EEE FF F EEL EFFFFFF E DC CC B, , 14 HMnRRNPAH PHw41)0 H1)4[FE1Mn t CCC CCCCCCCCC........................

.... C... FFFFFFFFF FEEF 000OF LE CCH )111D EEl FFFIFFEa 0 CC 14 8R411AP1AA4.4.14144411N CCC CCCCCCCCC...440."..."14".14....4..1,...'C............................ . FFFFF1F E EEF D1)DDD4DD00 D EEF F FFFFFF FE 0 CC L ' 41N14114l4)44 4H hn4NHHP4u4,1AP1CCC CCCCCCCC....................""......14......('(.C.C .

........ G FFFFFFF EEEE D Onn4)DDDDt'1DDDD EEEF FL FFFF FE D CC 14 N HRNH 4 .4141 44R4B HH-+wFMA ,+4

o CCC CCCCCICC. ............................... GG FFFFFFF'FF EIEFE 0000D 0 FLEE FEE FFFF EEF I; CC 14 P..A"..r"...: " 144444 (CC (CC'.C(O...

.... .GG FFFFFF FFF FEFFE 1)0DDODDD1)1I EFE IE FFF FF.D CC n 14Hl4

4 4PH4A1

1H 14)11A) .N0H..,,oo. l nhrg . 4 CC CCCCCCCCC.

... .. G FFFFFFFFF HEEFE D DOOD D D D EEECL E FFFFF EE u CC A R"ARRNHH4Hd1NRAHHHM~eM .+Rnn ('seoM RNB ~ a CCC('CCCCCCCC........: ..... ................ .............. ".. "... ......... ".....

........ G FFFFFFFFF EEEE DDD10 4DID DD EFF FEE FF FE 0 CC H 44PF1RA411lRH..)3 1l)4H4N.rF1R.+hP 31")) 41CCC C8l4. 1.... .. CC ,.

........ G FFIFFF E E EE 0 DD O EEEE 1EE FEE 1 C 1 4 441441 1Pa41. 1....... ...'... t. .. .CCC... ...............I.... FF'FF EEEE DDOOODD0D EEEEE FFEFEEE14:FEEE 4)1 CC CCC . 4''1k' ((CCCC........ " F... F F EEEEE DDDDDODT4 EEEEE EEFEF F.R EFFFFEFF 4)D CCCCCCCCCCC'CCCCCCCCCCCCCCCCC C IC CCCC 0..0 .......

...... FFFF FEEEEE 0DDD EEEEEE FEEFEEFE EEE 1)1)01D' 4HCCCCCCCCCCCCCCCCCcCCCC (CCCC. 11 CC(CC 0)4014' C.............. FEFF EEEF )F00E EEEEEEEEE FFFFFFEEEFE EFF 4)nF1001'0 l))H ('('CCCII F CCC( CI'C(CH "C C('C ) "0l C........

...... FF EEEE D DDDD EEEE.EEEFERE EFEEFF FEF F FEI n fr H 00 RCC0I1'C00I000 "0" C(CCCCCCCCCCCC IIO 1 n1 1)......... ......... . EEF........FEF 0.....................................................

...... GFFFF EY FE UDG~UDOEEEL_ EFF.......R..tr N ~nrFCCr(.... .. G.............................. FE'EE ......... lF

F FF.........................................................

. . . . . . . . . . .... EE............... EEEF ............... ........................... ....................... ...................................................... " . ..............................................

Gh1IA )P VILV, T IT :>.A1, '

U:, I 1. 1 I h v [, ' .10 " 1,.I .1. ,,. sn 4', il .O,,, I L ': -7 , 1 r

..... F*..HHFIH 1II1.GGGGGGGGGCGGG. ............... ................... PI .".".."""..... .GG.... . .... "............... . . . . . . . . . . . . . . ..... HHHHH if II ................ GGGGGGG GGGGGG.... ........................... ......................,.,............... We ..................................... MM 11H H ..... ................ ..... ........ .

... .......... II.. .GGC.G;GCrG( ....... ................ .. F. ........ HHR. . .. . . . .. . .......... ......... ... HHH HH HN H il . . . .. . .. .GGGGGGGGGG .......... ......... . . . . . .............................. ..........rr Fr, .. .. ............................... NHnHas H .......... .......... ................. . ..... ..... .. .......... . .. .HNNN I1................GGGGGGGGG . .. . .. . .. . .. . ..... ."..... .................................... r.yr FF .......................................8R' ."......"..,.............. .........,... .

.. . . . . . . . . . ........ .. .. e HHH - . ... ...... ..GGGGGCGG ""... .. .. .. .... ...... """. ....- ".-......................................... . K SF F ......................................NF . . .. . . . .. , . . ........ . . ... .. .. .. . .. .. .. .. . .. .. .. ... .. .. .. . .. GG 0G.. . .. .. ...... ....."" " " . " .. ".............................................. / Er . .. . . ... . .. . .. . ........... . . . . . . . . . ... . . . .. . .......................... .H....... .GGG(GG..

....... HHHHHA GGGG FFFF FF.....:..................... , FEF:"""V" I) C kBHA .. ,..,,.. ....... AHHHH GGGG FFFFFFF FF FFF Ell . F IOI F D C C u. . .

....... .. ..... ,....I I I HHH GG. FFFFFFFFFFFF ... .. ... .. ............ . FFFF F . PI11011Th1 CC C HlC l............ 1Il III INTHHNA GGG FFFFFFFFFFFF ..... .......... FFFFFF 0 C CC

.... "............ . . II IH H G F F F F F E .......................... F F F F G F F D D C C 8 6 8A A A A . .... . . ..... " IIII IIIIII HNNH GG FFFFFFFFFFFF F $FFF FF FF F I)O CCCCCCCC MO' AAAAA....AAA

............... 1TIIIi HHHH GG F F FFFFF F. E . FGGFFF 1 F1 f1 (0 CICC C If AAAAAAAA.,, ~JJJJJ 1111IHHHH G FF FFFFF F:FEF'hAFF FF 0 G Fl F o) CC ,iKlH4hA AAAAAA44 AAAAA

............. JJJJ 111111T HHHHHHHHHH HHHHHHHHH GG FF EEEFFFIFFFFFE F FFF FF F F D CC ,, M4 AAAAAAAAAAA AAAAAAAAAAAA

............. JJJJ IiIIIIII HHHHHHHNHHHHHHIHHHHHH HH GG FF ENNFEFFFFEFrEEFFFEE1EF1E:EI FFF F F l 1 CC 4H AAAAAAAAAAA AAAAAAAAAAAAA

................ JJJJ IIIIIII HHHHHHHHHHHn HHHHHHHHHH GG FF FFEE FE EEFFEF l AF: :FFF;E EE F .FFF :?Fh AEFFFFF EF F F FF nU CC K AAAAA AAAAAAAAAAAA AAAAAAAAAAAAA........... JJJJ TIIIII HHHHHHHHHHHHHHHHHHHHHH GG FF EEEE FE EFF EFE EEEEFEEEFEEFFEEEFF F'F' ',F FFe.F tr EFE EFEEE EE FFFF F E ii .CC Ab AAAAAAAA AAAAAAAAAAAA AAAAAAAA AAAAA

..... ......... II1111 HHNHHDHHH HHHH HHHHHHHHNHHI GC.G IF FEEEF FIFEE:1.:FI::FF:FFF FFt. k. E E AEEFF FkFE At E FF F FEEFE F IOU CCC HOAR AAAAAAAA AAAAAAAAAAAAAA AAAAAAAAAAAAA.J Ill HHHHHHHHXHH GGGG IF FFF UDDDIIIF EFF::FFFF AEAEEE EEFF :EE "F. E eF F I F F EEEEr E:EF. 00 CCCC AI+H" .l AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA AAAAAAAAAAAA

. . 11 1 NHHHHHHHHHHH GGGGG FFF EFFE D 000 EEEFF FEEEEEEEEIF.AED 0Dl CCCCC MyMMHM AAAAAAAAAAAAAAAAAAAAAAA4 AAAAAAA AAAAAAAAAAAA. .1. . . ANN1HHHHHHM GGGGGG FFF FEFE E DD UDDD 1 FEEFEF.FF EE FFIIEF 1)IlI,00111 CCC MMNM AAAAAAAAAAAAAAAAAAAAAAAAAAAA AAA AAAAAAAAAAA

.11 HHHNH GGGGGGGGG GCGGCGG FFF EFEEE D CCCC D)DDD DDDDDDU1 CCCCC K nHKn h14F AAAAAAAAAAAAAAAAAAAAAAAAAA AAAAAA AAAAAAAAAA. HHHH GGGGGGGGGGGGGGGGGOGGGGGGGGGGGGGG FFFF EEEe DD C CCC 0DD1DD) 1CDDDOD CCCC HRPA H AR 4A HH AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA . AAAAAAAAA

............. , H GGGGGGG GGGGGGGGG GGGGGGGGGGGGG FFFF EEEE D CC CCC D0DDoDD ODuliCl0DIA'00 CCCCC nMRH4RA MA H v0.O AAAAAAAAAAAAAAAAAAAAAAA AAAAAAAA AAAAAAAA....... .. NI GGG GG GGGGGGGGGGGGGGGGGGGGG FFFFF EEFE D CC CCCC UD(DUD UU D0001 a I.LU CCCCC 1IH8 8k .11 H PlNHI A AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA AAAAAAA... HHHk GGGGGGGGGGGGGGGGGGGGGGGGGGGG FFFF EEE ODD CCCCC(C D 0D0)DD011 LIU)0ir

01)IrU CCCCCC MHPR4P AAA P Fl"y lM1IlAe AAAAAAAAAAAAAAIAAAAAAAAAAAAAAAAAAA AAAAAA

.HHHH GGGGGGGGCGGGGGGGGGGGGOGGG FFFFF FEE DDDD CCCCCCC UOUO o jr0 10 CCCCCC H'RnHI AAAAA n SHRHIIH AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA AAA...... . .NHH GGGGGGGGGGGG GGGG FFFFFF FEEE ODDD CCCCCCC IO00 00000 C1 D CCCC 'bbblIHI AAAAAAAA NRhARPRIADH AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA

.......H G GGGGGGGGGGGG GGGG FFFFFF EFFE DDD CCCCCCC DO0 DUD CCCCC IEBlIRFA AI1 AAAAAAAAA RIy HI+HRl AAAAAAAAAAAAAAAAAAAA4AAAAAAAAAAAAAA...... ,. . . G.GGGG GGGGGG GGG FFFFF EEEE DDD CCCCC DDD DDn1 CCCCCC dMBHRHRIy AAAAAAAAA AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA

.+..... GGGG G + GGG FFFFF EFEEE + ODD CCCCC 00+00 00) CCCCCCCCC AAHIRMoHHA AAAAAA + AAAAAAAAAAAAAAAAAAAAAAA+AAAAAAAA +...............GGGGGGGG HH AHHHHHH GG 1FFF EEEEEE 001) CCCC ID1)000000000111 CCCCCCCCCCC +RI.1I A AA AAAAAAAAAAAAAAAAAAA AAAAAAAAAAAA

........ GGGGGGGGG H HHHHHHHHHHH GG FF EEEEEEE DOD1 CCC D oDDD D )f LD CCCCCCCCCCCC +' IbMBOH A AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA.. .......... GGGGG HH HHHHHHHHHHHHHHH GG F EEEEE D n CC DD0I)DD)l I)Dl)D I)D DD CCCCCCCCCCCCC RARM1H1ARIRI AAAAAAA AAAAAAAAAAAAAAAAAAAAAAAAA

.. F CGG HHHHHHHHHHHH HHHH GG FF EFFE DOOD CC 00lDD OD OD D D)D 0.1D CCCCCCCCCCCCCCC AlRR lPIlRRMR'AAl AAA AAAAAAAAA A AAAAAAAAAAAAAAAAAAA.FF GGGG HHHHHHHHHHHHH HHHHN GG FF ElE DDDDD C 0D0I)D ODO I10nDODOOU DDn CCCCCCCCCLCCCCCC Ml,,IIMHnDRI"MR ,AI AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA

........... FFF1 GGGG HHHHHHHHHH H HHHHH GG FF EFE 00D0D1 CC DD OOOUODUillD)ODD I01 CCCCCCCCCCCCCCCC'CCCC bARl lRllbHlA iRARp l AAAAAAA0

AAAApAAAAApA AAgAAAAAAAAAAA.FF GGGG A ANHHHHHHHHHHHHHHHHHHNIFANODON I GG FF EEE 00000 CCCCCCC D0D0D0 OlDoIlDD D CCCCC CCCCCCCCCCCCCCC AH hRF HM1IHFRRHR AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA AAAAAAA

........ . f FF11 GGGG HHH HHHH GG FF EEE DUD00D CCCCCCCC 1)D00 oD)D1D)1n CCCCC CCCCCCCCCCCCCC RMRlRI lRl, RR&BH R A AAAAAAAAAAAA AAAAAAAAAAAAAAAAAAAAAA. ... E FFF GGGG GG FF FEEE 00UO0 CCCCCCCCC 01100 100D)D CCCCC CCCCCCCCCCCCCC AMRHIAFMDHyA8gq.H1RR AAAAAAAAAAAAAAAAAA AAAAAAAAAAAAAAAAA BBBB

... ,..... EEE FF1 GGG G GG FF FEEE DDDU CCCCCCCCC 0DD rCOOU CCCCC CCQCCCCCCCC CCFC BBRyRlRAB ARR~yHPH9AMRHM AAAA 0AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA ABBB BB

............ EEEE FFF GGGGG GGGGGG GG FFF EEE DD00 C0 CCC CC DDD 00000 CCCC CCCCCCCCCCCCC I M1sIHNlgAB R HAPl AAAAAAA AAAAAAAAAAAAAAAAAAAAAAAAAA.. . . . EEE FFF G GGGG GG GG GO FFF FE 00DDD D DDDCD C UFEDUEFA 00U CCCCC CCCCCCCCCC NHlnRHIhAb y BtRNHDMA AAAAAAAAAAAAAAIAAAAAAAAAAAAAAAA.....

. .. 000 EEEE F1FF OGGGGGGGGGGG GGG FF EEE DDUDD 0 0DDDDDU EFEFFEFFE 0Dom CCCCC PCCCCAHM b IAiFBAM AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA. .. DDD EEE FFFFF G GGGGG GGG FF EEE DDDUDD nDODDD EEEEFEEEEFEE(FE D11 CCCC NARHMtl bBlDIA AAAAAAAAAAAAAAAAAAAAAAAAAAAA........

.... ....... DDD E EE FF FFF GGGGG GG FF E G F FE DDD DDDD 0DDDDDD EEE EE 1EEEEFEFEF 0 CCCC RK1 Hh AAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA,......C 0 0 EEE FFFF GFF GGGG GG0 FF EEE DDDDDDD DDDD0DD0EEEEE00 F EFF FFF 1F u CCCC ) MPR hNHHHH n AARlA AAAA AAAAAAAAAAAAAAAAAAAAAAA ........

.... CCCC DDD EEE F FFF GCGGG GG FF1 FE 0DDDDD 0D EE FFF FF 010 CCCC f FhPHRlBRhH HFR8AR6 AAAAAAAAAAAAAAAAAAAAAAAAAAAAAA dRRB. ....... ... CCCC DDD EFEE FFFFF GGGG GG FFF E DD DODD EEEFk .EFFFF ' )0 CCCC h HFHAND RbRFH IlBlwH AAAAAAAAAAAAAAAAAAAAAAAA A AIBBBMRB ........

..... CCCCCCC DDDD EEEE FFFFF GGGG GG FFF FE DD DD FEF EErEFFEE n0 CCCC nRNRRI BNbARPMA deh RMPM AAAAAAAAAAAAAAAAAAAAAAAA BBBBBB ....... CCCCCCC DDDD EEE FFF GGGGC GO FFFEE D CCCCCCC ODD FEFE F.EEEEEEEEE D CCC A AoA((ABb tlldl B IbRR4 AAAAAAAAAAAAI*AA AAAAA BBBR NR,........

............... CCCCCC D DD FEE FFFF GGGG G FFF E D C CCCCC D00 EEE FFEEEFFFE 110 CCC AHlrrl th BP Pb MR bRAlNB IMRRAn AAAAAAAAAAAAAAAAAAAAA BRBMBAdB R..... CCCCC DDDD EEE FFF GGGG FF E D C B CCCC DD EEEE EEFFEFEFE D CCC b(KReMbHbA HRI R AAAAAAAAAAAAAAAAAA IRAHBB ABBRR........

............... CCCCC DDD EEE FFFF GGGGGG FF1 E D C B CCC 0 n EEEEEEE FEEEEE EFE D1 CCC ANBFlA'IlbAFblollAyihR ARAAAAAAA AAAM A ARB1BA H ............. CCCC 00 EEE FFF GGGGG FF E D C B CCC D0 EEEEEEE EEE EEEEE FEEEEEEE 111 CCC AbFIlAA1Ahb8lH 8lMh.A A AAAAAAAAAA BBR BMB BRIBI.......... ..

.. CCCC DD EEE FFFFr GG FF1 E 0 C BB CCCC DoD 00EEEEE 1D CCC AALMbIIbAARhAblHIRRAM HI.AM AR ABBBBRBBB ............................. B CCC ODD EEE FFFF G FFF E D C BB CCC 0DD0 0D D A:EAF DO CCC RRbIM bbbHHNNAhAHR hybMFH AARH FRBII B BRBIBIBBB B .........

.85M CCC DD0 E FFFFF FFF E D C BR CCC D0 00D DDD0 0 1D)0 ) E F D) CC RDbAhAEMbHH IBM Ib 6H« tHHHH H IBBBIBBB BeNBD . ... ......... .BBB CCC DD EE FFFFFFF AFF E D CCA88ACCC DHARDD OD DDO DDII CC RIdd HnItRHIMyB nh~d hHMB8 bH BBdR RBBR9 61469 ...........

... ...... BB CCC D EEE FFFFFFFF FFF EE D C FB CCC D0 00000 CCC CCCC DD F D)0 CC IlAAhbRnh lb0N HIHhbn MYbHBlHelb$lB AAA MHAAAMBMBBA MBPN RD ... ... A. R8A CCC 00 EEE FFFFFFFFFFFFFF EE 00 C CCCC DD DDD CCCCCCCCC DD 00 CC II8DIIRRAIFHhbdHMHARNR HAI1R DPRA A AAAA AR 1 SNHRIBBAI RFlI M HRM .. ... . ...

.... .... B CCC DD EEE FFFFFFFFFFFFFF EE DD CC CCCCC D D DDDOD CCCCCCCCCC DDn )n CC RAM hK Bb h h P R PFPHP lM1IAylDlRlF DRAM AAA)A HRHIRyHAHRIBA D BI9RIA AHA................. " . .. B...B CCC DD FEE FFFFFFFFFFFFFF EEE DD CC CCCCCCCC ODD DDDD CCCC CCCCCC DD DDD CC AR ABNEiPRPAPORnHAR bIHHl'lHllARIB AA IAHIIRBBB PN BBHBBRABBRI .B............

...... N.B......F CCC DD EEE FFFFFFFFFF EEEE D CCCCCCCCCC 0DD0 DD CCCCC CCCCC DUI 11110 CCC lI1l bMHlMRP do bhl MHFARR R8bRBR AAAAAH RB ARABPABRARRABB RB................... .... B. CCC DD EE FFFFFFFF EEFEE 0 CCCCCCCCCCC DD0D0 CCCCC CCCCC DD1 0I1) CCC Hy Hb ylAIhboAD 8888988 HlI lAA" AAAAA ARIHBR BBBDBB D R RR ................

..... +...... CCC DDD EE FF+FFFFFF EEEEE DD CCCCCCCCC + D0D0 CCCCCC CCCCC DU+ D CCC BBRBA lRNlbFgdi RA6l+R BRFDDHR1A BAIRIR AAAAA bRRB+RDMIDRRHBPR . . .. ................... CCCCC DDD EE FFFFFFFFFF EEEE DO CCCCC CCCC CCCCCCCCCCCCC 000 DDD CCC RIHHRbHFl(IIAAAkHRHAHABBAAI MHAR A RHB RDRRABBRNRbDBBB R.H. .H. . .

................ CCCCCCC DD EE FFFF FFFFF EEE DD CC H CCCCCCCCCCCCCCCCCCCC ODDn UDD U DU1 CCC BRRRbiHAA1BMHRAHIR MhnAhIOIN L' r'i HHMRRbR RR H AHHPb BHObyuyhIHRHNMBR RRBHHHRIbRH ........................CCCCCC DDDD FEE FFFF FFFF EEE D CC IBBIABB CCCCCC CCCCC OD ODDODDODDODD CCC PRN lRMAAdn IblHR FDRARI PH8H hliNIUIIPI RPDF H BMBRRRFHHRHNRFHPRRMHeRHIMHRBHR .......................

.... CCCC DDD EEE FFF FFFFE D CC BABRM BBA CCC DDD0 DDDDD CCCC IlBIINIIbR AHHHas RI +A1AnnnRAsRMH R RR BDDIRHAIRRIIIA ARRBDRHRABRHABRBBB........................ ... DDDDD EEE FFF G FFF EE DD CC BB A BBRABAB CCC 010D 0)DD000 CCCC A3 Ait DFFBbHHRP RR lIIHDNNHHHMR RIRH HIBINHRMRMHHR RRFRNPBIBBRMB4AN HBRBPRBIBHRN ..................

........... DDDDD EEE FFF GGG FFF EE DD CC RBB AAAAA INBB ABA CC 000 DDDD CCCC DHObF FbR F HD KAbAsHdNNHM RR4RAIRARNHanH HMRB MHA RBHARRBBHR HPRBRPRHRBB.......................DD0D FEE FFF GGGG FF EE DD CC BB AAAAA AABBBB CC po pDDUD CCCCC MsAh 'M RPMFAIR4 HIH R N d Kb hA AMR H RRMBR RAIRRHMBBAARP8BA HHRDRR ARM .......................

. . . . D0000 EEE FFF GCGG FFF EE DD CC BB AAAAAA DAMN CC 0011 DD110 CCCC RRRA-hE-l lPkAA Rh lAsl l,.IlHAs l,, Ell 5HMN4MRRR MRIRAHA 4A RPR R P SRAMAB.......... . DODDODDD O EEE 1FF GGGG FFF FE ED CC BBS AAAAAAAA BBB C 0000 1DD CCCC DRnROnNM RhrHRNAMAHY1hHHDhNHI n HRAMn HRA . DIRARMIRMHBRHRRMAM9 HRM H...,.... .............

... 000000FDDDDEEE FFF GGGGG FFF EE DD CC BS AAAAAAAAA Al CC DD0 DD0 CCCC R0IHAIAAFb0A8088H1,11RMD HARRIMHRMRIHAIIA MAAHMRADBAMRIIFH IRA ANB RAIB.................... . .DDDD0DD0 EEE FFF GGGGG FF FE DD CC BB8 AAAAAAAAAAAA R CC 0 I)DDDD 0 CCCC RHIBlbln4lll)M1MlAHP HNHnAtl AA hHHAHRRAAAM AARRhDARRNHIABRR B I ARK..................

.0..DDD 0D EEEE FFF GGGGGG FF EE DD CC BB AAAAAAAAAAAA 9M CC 01)DD0 1DUD) CCCCC MRHM(,RDRA RFhRIIhNHMIRRI1Hn AR.A Sbd AdRBNRIH yPMHANBRBbB............. ................... ...... DDDDDD EEE FFF CGGGGGGG FF EE DD CCC BB AAAAAAAAAAA BB CC DD0I)000l)I CCCCCC RbIIAAbAI 1ANDNBRhtIFI HHRI RA bKMAI AA AFDRMHBNRHN RRA R CC ... .. .. .. .. ..

00FDD E EE FFF GGGCGGGG4 FFF EEE D0D CC BB AAAAAAAA 8BR CC 0DD CCCCCCCC AinAhrMMnRAMMPFNRHBARABlRDAR L1RMRMAI AMAAAIAARR IHRI HRHR CCCCC......... DDDD EE FFF GGGGGGG FFF EEE DD CC BB AAAAAAA BRB CC CCCCCCCCCCCC MAHEPBHRPHP NRB8AHDHFPHAHRPMw IRDRE.HMAABRRRBH CCCCCCC

.. CC D0 FEEE FF GGGGGGGGGG FFF EEFE D C AR AAdAAA BB CCCCCCCCCCCCCCCCCCCCCCCCCCCC HEbMbNAMA 8h R1 R AMRRRMAHM Rl)MARIBA RNHMIR CCCCCCCC ................................... CCC DDD EEE FFFF CGGGGGGGGGGG FFFF EEE 0 C PM AAAAAA AR CCCCCCCCCCCCCC CCCCCCC oPJAMF I lHR lMl 9 RNHwRA P RRH R ARHBIRAH CCC CCCC ...............................

.... CC 0DD EEE FFF1 GGGG GGGGG FFFFFF E D C RB AAAA INN CCCCCC CCCCCC (lIFhhHK AH4eI $FAAIn RBHRAMIRBAIIMBR CCC.............CCC DD EEE FFFF GGGG GGGGG G FFFFFF EE DD CC bH AADA AID CCCC C hnMAK HRA.A' RHKADM BRBAlMHMMAbRMbH CCC................................ .

.............. :CC 00 EEE FFFF GGGGG GGGGGG FFFFFFFF E 0 CC B AAAAA b B CC An6R M MMARi)BAIRRilR RAAIIRRBnBICCR..........A..CC..... ........ ... CC00D0 EEE FFFF G G G GGGGGG FFFFFFF EE D C B AAAAA BD DAB AHARrb AnBRARAA RnRIF AFP R HbR Hd P..BR .. .....

... CC DD EEEE FFFF GGGG GGGGGGG FFFFFFF E D CC H AAAAA BRM IRIDAADARI PbAA R MI)IMAIDIAAM'3 lBPB RIMDRD BAH ...

............... C DD EEE FF0F GGGG GGGGGG FFFF E D C RB AAAAA BAH R MR BO.IAR IMAN rHAHIB4R' A NMBd BA RBBR .. HI.R .....................................OD4EOFF000 COCGG E0 NMMA MAI DAMI~II1IAA AIRRI9Ny'NHDHDHAO R BB yP ,,,,M,,.. . . . . . ... "....... ....... D.......DDD EEE FFFF GGGGG GGGGGGGG F EE DD C B AAAAA BRBR Mdn IRDRDDIH8BAIlRb "BR1II 1,HARIAIDAHHD RRNA. .................

. .. DDD EEFE FFFFFF GGGGGGGGGGGGGGGGCAF FE 00 CC BB AAA BHBBB HBIAIR RMIRAHRR BnF AIHI AD S IRHRB AIBNRBRBBhRhB8.............. . .............. EEFEEE FFFFFFF GGGGGGGGGGGGGGGGG FF E 0D CC H AHIlBBIAMRGBR98RBMAH H PnbbE1H1P1IH N P.RA b R b M ARIlRR AHA .....................

..... .... EEEEEEFFFFFFFF GCGGGGGGGGGGGGGG FF EE 0 C R MHeA HHDRBR PRRyHHnhrHRRNR D RA A D IH4 BRB O........................................................ GGGGG FF GGGGGGGGGGGGGG FF EE D CC MAR AbbRAHIPbP6RHyH HPnH nEr1l HlrN.1 HAAOOBB MAHMR nHAHn enM HAI1BH RMIRRAR..

........ ,.....FFFFF FFFFF GGG GGGG FFF EEE on CC RBBR AAAAAAAAAAAAAA BBBRAHB NHHBRBRh nrnnhabcBRMNBhMRM ABHRHRMMRR MP H AR AMB RR BBRE'HBB..... .....................................

... . . . FFFFFFF FF GG GGG FFF EE D CC RHB AAAAAAAAAAAAAAAAM RBdRHdAHb AD NRiFdbonEdPHMHHHARAARRIAI DMADRAID I AI HRRbRNRHFMRA.. A.. .... .... .......... ..

,.... .. FFFFFFF FFF GG GG FFF FEE 00 CC DA AAA AAAAAAAAAAAAAAA RPAAI1HAAIPMP IlMM111FIAIBORDRAAHIRAAARAAAOHDAeRI MDARIRI IRDBAD A..........................

........ FFFFFF FFF GGG GGG FFFF FE D C B AAAAAAA AAAADAAAAADMA HNDFFAAAIA RAbeHMI)MAMHRIIII1RIIRA HADHRMIRADAR IAIHHBRHPHRR AA...................

"............G FFFFFF FFF 0000 GGG FI F 00 C C AN ADAAMAAAAAAAAAA AIYIHhR uIAIDH ME6lAOFII84H9HK680HAHl{l8lM9IAAA A0HMHAHHARR 8HR. . . AA........................ +..GGG FFFFFFF + FF 0GGGG GGG 1FF E+ III CC AM AMDDADMAMAA HlNR ~OR~1AAAAAAAAAAAAAA+AAADAIIHBMMB~dnhSRAIAIHIRNR.,1FRAI1 F AHIDFIAFIIAIRDARARHIAA AAD.+....................+.....

................ G FFFFFF FF G GGGG GGG FFFF EFE CC RB AAAAAAAAAAAAAAADAAAAA M!nMHit n HHH n H H H 1b H AMA Ma AAHAA I Mp RARAA.H dH9H H40... . . . ..................................................FFFF"1 FFFFFF FFF GGGGGGGGGGGC FFFF E D CC B AAA AAAAAAAAAAAMAAAA 'IHdN .MEbHHAoA Ahebl(Il8lllAHAHlRHl8lMRR9CARRHR ARAHAMHHA..........................

+ ... FF FFFFFFFFFFFFF + FFFFFFFFF GGGGGGGGG FFFF F+ FE 00 CC AAAAAAAAAAAAAAAAAAAA IIIMFA jAEAR RRMMRRDD88AE BlIRI AD MDD DMI h AP+............................ FFFF FFFFFFFFFFFFFFFFFFFFF GGGGGGG FFFFF CF D CC MA AAAAAAAAA AAAAAAAAAA H HAIR A84800488888RRA HN« H68888888 8.................I..A..A.....................................

.FFFFFFFFFFFFFFFFFF GF FFFF FEE CC ARM AAAAAAAAAAAAAAAA FAI HAHIIRARAHAI A8bIR....................... ,........

AEEE E FFFFFFF F FFFF FEE 0 C M AAAA AAAAAAAAAAAA A AM CCCCCCCCC k AR NHM RHnHHH R HNHIRH AMNN.. ...... .....................................FEEFFFEFEE FFFF FFF EEEE 00 CC AlA AAAAAAAAAAAA AD CCCCCCCCCCC RAA R .......................................................

.F EEEE FE FF1F FFFFF EFE 0 C MAD AAAAAAAAAMAA MID CCCCCCCCCC A MA ...............................................FF I.FFFEEEEE FFFFF FFFFF F. F1 1) C B A AAA AAA AAAAA AAAAMDDMA ADA lR CCCCCCCCCC IF I sR 8 8....,.........,... ... ........ .............. ...

... , EEFFEEEEEE FFFFF FFFFF FFF Eh; I C iA MAAAAAAAAADAAAAAAA A AA Nl CCCCCCCCCCC MAAINH H nR B ... ,.,,................. .............................. ........FF EEEEE E FFFFF FFFFF FFF FE 0 C MAR A AAA AAA A AAAA t CCCCCCCCCCC 1 ARMB 1I H......... ..................................................... ..

.FF FEEE.E,, EEE FFFFFFFFFF FFFIF FE 1D CC I AMAAAAAAAAAAAAAAAA AAM IA CCCCCCCCCC 1 AAII'IA DIR............................ FF FEFFF EEEEE FFFFF FFFF F FFA' FE D CC HR AAAAAAA MAAAAAAAAA AAAMAHC CCCCCCCCCCCC FKR........FF1 CEFEEEFEEE FFFFFFFF FFFFFFFFFFFrF FFFFFFF F1FFFF F D" CC MA A AAAA A.A..A AA AA F .. .. ........ ".........................

.FF EFEIEELF FFFFFFFFFFFFFFCFFFFFAFFFFFFFFF FFFFFF E I CC RI AAAAAAAAAAAAAAAA A A DA IA C 1 'I FR A . . . ..................................... . ..................... "..FFF FFFFFFFFFFFFFFFFFFFFFFF FFF FF 0000 FFFF E D) CC I AAAAAAAAAA AAAAB+AAAA AA404AA MICCRFFCAClI'HAIHhDRRAR, ,,AI. . ... ... .. .. .. .. ..........................

F.... FF FFFFFFFFFFF FFF GGGGG 0000 FFIF F 0CC AMDAAAA AAAAAAAAAAAAAAAAAAAAAAAAAAAAAA AMFA DIDANNRD I'MAHAI. .. ... . .. ............................

.... F FFFFF FFFFFFFFF' 1FF GGG F GF FFF F D C A AMA4A AAAAAA AAAAAAMMMAAMrnADA'CAAAAID AA AIDIF1M'AICAM HP A NI'..... .............................. ....................... ........0... FFFFFFF FFFFFFFF FF GGG HNHHH GG FFF F 0 C AAA A AAAAAAA A AAA AAAA AAAA AAA .1AA AAA 4A1 I AA AAAAAAw as AlN Dl'H............................................................................

...... G FFFFFFF FFFFFFF 1FF GGG II RH GGG FFF F 0 C AAIAAAAAAAAAAAAAAAAAAAAAAAAAAAAAA ADAAAAA , A ,............................,. ...........................

....... G FFFF FF FFFFFFF FEE EEE FFF1 CG H NH G FFF E 1CC AAAAAA AAAAAAAAAAAAAA AAAAAAAAAnA0AAAIAAADA AAAAMAAAAMHAAA A l AAI 1..,... . ... ...................... .............. FFFF F FFFFF FEEEEEF EEFEE FFF GG IA NH GG FFF F D CC AAAAA AAAA AAAAAAAA4 A A. AAA AAAA AH.. ... .. . .. ...................... ..............

.l....G FFFFF FFFF EFFFF AFFFFA FFF GG HHA HH G G FFr E ICC H AdOAAA AAAAAAAIA4ADAAAAAA AAAAAAA AAA AAAAA AAAAAAAAAAA lAMslIDA. . . . . . . . . . . . . . . ....... F F F FF EEEEFEEFFEFEEEE FF GO M HN ,0G FF :E ICC Il AAAAAAAAAA AA4AA AAAAAA AA AAADAAAAAAAAAAA AADAAM AAAAAAA DIFAAD..

.G FFFF F EEFFFFEFEEFFFEEE FF C NHH HH 1 CGG FFF.E 0CC 1 AAAAAAAAAAA A AAAAAg4AAAAA pM AAAAAR4A. . . . . .. .. . . . . .. AA...IA. . .. .. . .. .. .. .

..... FFFFFF EEEFEFFAEErEFFEFF FF OGG H H GG FrFEE 0 C nA AAAAAAAAAAAAAAAAAAAAAAAAA +MAAAAA AAA . AAA) 4 AAAAl AlAAAA AA.I'wMARM+"........ ........................... ..................................... FFFF EE F FF FEFFDEFF.EEFFFE FFF GG NH N H GG ' F AE 00 C A AADAAMA A AAAAAA AAA MAAA AAAAAAAADAAAD lAM A A A ... ............................ . . . . ................ ........... .

...... FFF F EEEEEEFEEEhEF EEEFEFEF I FFFF GG lAHH GGG FF FE D C C HAA A Al44AARM 110HIkAA 1A4 AA AAAAA RnAM'+AIII.HI,,..........................

..... FFFFF FEF EEEEFEEE-. FF FFFFFF GG HHHH GGG FF AF I 111 CCC C C1," l 1, 8'."1RI1 hH 1 A .9'.. r.'rFH D .............................. "........................................................... FFF EEEEE 00 EIFE : FFEFFFFFF GG I GGGG FF E D00) CCCCCCCCCCCCCC CMr Ir ID" F.r IM IF4H ,.) AM1IM .... "................... .... ...................................... ......

... F EEEEEE DDDDDDD EEEEFE FFFFFF FF GG H GGG FF FEE 010 DU 0001' CCCCCCCCCCCCCC lrru1' 1b9, 0 yI,1H. n4AI, ... ..................... ".................................................................................... ... ........ EF, ... ".."..... ............ G FF ............................................................................................................ .................................................................

"...FE '."...................FF.......

...... +..... . ........................ .. 1.FFEE ....... ............ 0.+ FFFF...........................+................... . . ...... .. +........ ....... ............ +. .... ........ .. ......... +.......... +.. ............ ... .FEEEE ........ .. G .FF....................................... ................. ..................

,.".... ......... .. .. ... .... ........ EEFFEF'"...... ... ........ G . .... .................. ............................. . . .................... ...... . . . . . . ...... . ...."""""."".... . .. ..

EIO)ATM IFNTFNATI110A, I * C.MIDIAA, 1FX M

1.21<GC 1.1'. 1. A'<n< I.0 1.h)<I 1. 7" 1.n .<r< 1.-I

C_'(-IT B P RAH PHBa1= 1 11 APP.Ar. 1 A. Ib-er c '/c c . - . .h.01

.. . . B .RBRRRRR RRB . . . . .. RRR RRR . . . . . . . . . . . . . . . . . . . ............................. .......... C cc ..........................

.............. . ............... . . . . . . . . . . . . . ..... CCC C...... __......CCCf._..Cc.................c. . . . . . . ...... . ... .. . . . . . . . . . . . . . . . ........................................ 0C0 .....NP. .H.H......_C.CCC. ......... C c

.. . . _ . ." - " . .. . . . . .. . . . . C - cr . ...c c . ." " .. . .. " '- " "" . C r CC(C[..C .................................. "................R RRRBRRRHgBP ................ RRRRHRRRRRRRRC.... ........................................ .............. .. CCCCCC............. . ....... c c..cc rc.......................cCC c. ....................................... . .BR B A A RRR...............RR BRRRRR RRR ............. .. . ..................................................... CC CCCCC..... ..... . ... CCCCC....C.... C........ CCC

.. . . ................,.............. BBARRBRRRRRBRtl................PAFPRRRPRRRRRR .._..................._... ...................................,...............000CCC 00...._.._... ........................... r00c ................-......-.. C... ..C.. .

.B.......BR. ..B. PR R RR RBB.._ .B-RBRRRRRR R .... . . . . . . . . . . .CTC. CCC(.............................. CCC.CCCCCCCCCCc. CCCcCCCCCCCCCCCc CCCCC.......BBA RRRBR BBBR8 IRRRF~BBBBRRBRR RRR RR RR . ................................ CCCCCC CC......CCCCC.

... . . . . . B B B BBR BRRBR BRBRRRRRBBBR R R R B R R C CCCcCCCCCCCCCCCCCCcCCCCCCCCCCCCCCCCCcCC DDf DDDDD Wnnnlllff fDCCCCCCCCCC C CCCCCCCCCCCCCCCcCCC CC ...,,,,,,,,,, R~rHRBH..............Be RR BR RC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCcC flI.D )DDpnrCCCnn C CCCCCC C CCCCCCCCCCCCCCCCCCC. . . .. B.BBB BAAABRRRRR R. ..rRBABRRRR HB B;rRRR DR CCC CCC CCCCC C CCCCCCCCCCCCCCCCCCC DlflI)D Cnl DDr nDOnn C C CC r CCC CCCCOCC CCc C CCCC

."B ;BBBBRRABRBAR BABBRRABRB ARRRRRRRRRARBB CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC DVDffDDDCfCClCCCCCCCC C CCCCCCCCCcCC C.... BBBBBBBBBBRBRB RB BaBBABBBRRRA BARBARRRRRR.. . .CC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC nDD I Df nnnn CCC CCCCCCC ccCC Cc CCCCCCC CCC c c......

. BBB BBBBRBAAA ABBABB ARBRBARRRRRBRR ABCA CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC DD DD CCCCCCCCCCCCCC ccccc ........

C~rrccccC~r. (1) D DO D ) CCC CCCnn CCCCCC rCCCCr c c CCCCrcccrCCc

.. BBBBRBBBBRBB BRHAR RBRAABRBARABRRBRHRRABACCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC flC f DDDDlflD C C C CCCc c c r rC.......BBBBBBBBBBBRRBBABBBAARAB ARABAACCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC C nnCDConnonoCCC CCCCCCCCCC CCCCCC CCcCCC ...

.BBBBBBBBBBBBBRBBAB RRR B BRARABA RCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC DO 10 C C ODDCCCC CCCCCCCCCCC CCCCCCC C C CCC CCC.............. BABBBReBBABR q BBBRAPBR RRPRRBARCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CC flClCCCCC CCCCCCCCCCCCCCCC CCCCC CCC BCCC ... CCCCC............... B:8 B 1BABRRBABB R PRBBRBA RCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCC CCCCCCC CCCC.

... BBBBABBBABAB B BBBRRBBBB RR BRBBACCCCCCCCRAC CCCCCC CCCC CCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCDCCCCC CCCCCCCCC CCCC CCCCCcCB CCCCC...

................. BBBBARBB RBR ABA BABRHR BR ABRRBAgBAR6 C CC C CCCCC C CC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCC C CC CCCCC rCC C CCCCCCCCCCCCCC CCCC ........

... .. BAB BABBRBABARBBBBBAABBAA ARBRABBARRR A R CCCBRCCCCCCCCCCCccC D C CCC(CCCCCCCCC C CCCCCCCCCCCCCCCCC CCCC CCCCCCCCCCCCCCCCCCCCCCC CCC CCCC ... ....... . ..ABBBBBBBBBBBBAA ABARRRBAB BR RAABB PARRPRBRABBBRRA CCC Ce CCCCCC CCCCCCCCCCCDCDDCCCCDCCCCCCCCCC R CCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCC CCCCC cCCCCCCCCCCCCC CCCCCCC BRB. CCCCC.

............. BBBBBBBBBBBRBARBBBBBB+B BB PRRR BPRR + CCCCCCCCCCCCCCCCCCC CC CCCCCCCCCC r CCCCCCC CCCCCCCCCCCCC +CCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCC B CCCC

...... B.......BBBB BBBB BBARR BBRBRBPABR AB B ARRRPBRRRRARAR CCCCCCCCCCCCCCCCCCCCC r CCCCCCCC + CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC C CCCCCC CCCCCCCC BcCCcC ............ ..... BB ABB BBBBBRRBB BBBRR BBRRRRBBRR CCCCCCCCCCCCCCCCCCCCCC0 CCCCCCC CCCCCc CCCCC CCCCCCCCCCCC CCC CCCCCCCCCCCCCC CCCCCC CCCCCCCCCCCC CCCCDE H

............. BBBRBBRBBBABRAAR RBBBAB RBBR BARR BBBARBRBA BR RR CCC CCC0CC ccccccCCCCCCCCCCCCCrrCCCCCCCCCCC CCCCCC ACCCCCCCCC CCCCCC CCCCC CCCCCC Cr CCCCCCCCCCCCCCCCC RRBA CCCJ................ BBBBBRB BBBR BBAABBBP RRR AAAARR ARB BBRRRB C C C C CCCCCCCCCCCC DODO CC CCCCCCCCCC CCCCCCCCCCCCCCCCCCCCC CC CCCCCD CCCCCCCCCCCCCCCC........... BBrBBrBB' rrrcBBBccBcr CCCBCBBBBRRRRBBRRrr BRBBCC CCCCCCCCCCCCC ..C .""DD CC CCC

........ .BBBBRBBBRBBBBBR RBABR8RRRBBARA A B BBRPARRRRABB RRC CCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCC Cf[+CCCCCCCCCCCCCCCCC CCCCCCCC C CCCCCCCCCPBCC CCCC DE F ............. BABBABBRA BBBAAAPBRABRBAAP BR B BARRRRRRBRAAR A CCCCC CCCCCCCCCCCCC CCCCCCCC 'CCCCCCCCCCC CCCCCC D CCCCCCCC CCCCCCCCCBCCCCCCCCCCACC CCC D G

................ BBBRBBAABA BBBBRRRBAB R BRB R ABBA BABBA ARRBBRRPRR [CC CCCCCCCCCCCCCCCCCCCCC CcCCCCCCCCCCCCCCCCCCCCCCCC D DDCccc CCC C C C CCCCC cccCCC CCCC DF EE

. .. ... BBBBRBBBBABARABBRABRBARBABR ABBBRBB ARRA RRRRAABB R RrBA rR RCCCCCCCC CCC CC CCCC CCCCCCCCCCCCC CCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCC CCCCCCCCC.... BBBBBBBBBBB RBB BBBARABBRBB BBAP RBABBBBRHBBRBRR AAAARBR RPRB BRBBRR CCCRRRCCCCcCccCCCC rcDcD cc CcCCBBCCCCCC f0')0 DCCCCCCC CC CCCCRC

............... BBBBBBABBBABR HRBBRBB B ARRR RARBABBBBABBRBRPRRRBAAAARRBPCRRCCCCCCCCCCCCCCCCCCCCCCCCCC BCC CCCCCCC +DDDDD DDDDDDD CCCCC B c+0C0 ........

.. BBBBABBBBRBARABAAARBBBPBB BB BRBRRBBBA RSaRaBRARABAARBR CCCCCCC CCCCCCCCCCCCCCCCCCCB RBC+CCCCCC CCCCCC flf 0 CDCCCC CCC CCC CD .....

.BBBBBBBRPABARA BRBRBP9BRPRPARBABRBBBRABRRBBBRRRABRBRRRRRARA RBRccc rCCCCCCC CCCCCCCCBCCCCCCCCCCCC00CCCCC 0 CC CCC CCCC CC0 FC CE .. ..... BBBBBABRBRASAA BBg RAARRBRBRR BBBBA RA BBBPABAAI3BABA RRB ARAARRR RRA B RCCBCCCCCCCCCC CCCrRRcrr CCCCCCCCCCCCCCCCCCC0CCCCCC 0. ..

............. BBBBBABB BBBAAABARBBB BRABARRRRBBBBBBABRRAB RR RBBRRRR B R RBARCCCCCCCCCCCCCCCC(CCCBACCCB C CCCCCCC C0CCC0 C0(CCCCCG............. .. BBBBBBBBBBB BB B ABRBBBBRRB AARBBRBABBABRABBRBRRaRRBBRBSBRARRRARAA CCCCCCCCCCCCCCC BCCP ACC HCCCCCCCCC000 CCCC CC CCC . .

....... BBBBBBBRBSBBBBAB RRAB RRBBRB BR RABAARBA BBBBBBRRBABARRBRARAB R CARBRA BBArBBBBA CC CCCCCCC CCCCCCCCCC CC00000RCRCCCC.. . .

... .... BBBRB BBBBABABBPAAARBSBBSBBABAAAARBBAAPBABAB AABAAARRABAARBBRRAARArcrRrACBA AB CCCCCCCCCCCC CCCCCC CCCCC0ccc R ... CCC...C0 ..

.............BBBBBBRBBBBBBBABRRBBBRABRBBPRRBBBBBABRRAABRPB0BRA RRBAPRBeC CCC CARAABbiaR CCCCCCCCCCCCC CCCCCCCCCCCCC .. .......

.... ... BBBBB AB BBBBBABB ABAPRBARBBRABBABBARBBRAABPARAABBBRRAARR BARBBRB BBCCCCCCCR RR ABRA B CCCCCCCCCCCCCCCC C CCC CCCCCCCCCCCC cBBBB... F.................... BBBBBBBB B BBBBAAAAARABBABBBRBBABRBBBBBRBBRBRR RABBRRARRABRRBR R BABBARRRR HCBBC CCCCCCCCCDCDDDCCCC CCC CCC .... ........

A.. .... BBAB BBABBBARRBARABBBBRBR RBRAAAR ABBRBABAAPRBAA ARBRB R RRBBRBARRABRRRR A CCpCCCC CC CCCCCCCCCCCCCCCCCCCCCCCCC.CC.............

................ BBABBBB ABBBAARBBRRAABB RARBBRRBABBBRBBARBB ABABB RABRRBBB B PRAR bbS CCCCCCCCCCCCCCCCC C CCCCCCC CCC RBA. ............ .,BBBBB BBBRRAaRBBRBBC CRRCBCRRCCCCCBBBCBBBRBBRBCCRBC SPBCCCBBBBCCBRCCARPRABAARAB ABCCCCCCCCCCCCCCCCCCCCCCCCCCC ARRABS.......

............... BBBBBBBBBAABARBBRBABBBBRPBRRRBRBBBBABRABAB B PBABB BBRAPBRA BBERABPRBRRRB9 BCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCC APRBB. .

................ .BBBBSBBRABRBBBBRBBRBBBBABBBSB BBBBB RA S BRA BBAB RRRBRRABRARC C C CCCCBCCCCCCCCCCCCCCCCCCCCCCCCCC CCC RBRRRB.. ........

................. BBB BBBBBBBBBARBBBARRAARAABABBRBBAB AAA BBBABRA RRABBRBBBBBB RBRRBCC C CCC C CCBACCCCCCCCCCCCCCCCCCCCCCCC ACCCCCC A BAB B ....... .....

............... BBB BABBRAAARBBBRBBBBBRABRAAABAA BRA BBA C ARBBARR ARABAA R ABRAR BARA ARP AB CCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCC C RC RR BBR .................. B BB.BB. .B BB ABBRARBBBBABABBRRBRABBBRBBABB BB AR RBBRARARBARBRBBBRRRBRRRABAPCCCCCCCCCCCCCCCCCCC CCCCC C C CCCC C ARARABBR ................

.... BB..B.....B.BB RRBRBBBRBRBBARBBRMBBBBBABRBRBAARR A RBRRARB RRA HARRAA ARpPA CCCCCCCCCCCCCCCCCCCC 4 [CCCCCCCC CCCCC ABRRBBBRB............... . BBBB BABBBBBRB ARRBAABRBRRABBBBARBRBB AABgRB BBABAABARBABBABBRBBRRR R ACCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCC ARBBCCC................

......B.B....BARSRBRBRBABBRBBBRBRBB BBARRBBAR RAPRRBRBR BBRS B Be ABRASRARAB CCCCCCCCCCCCCCCCCCC CC CCCCC CCCCCCCCCCC C RRR AB..B...................... BBBBBBRABBRBBBRRAABRRRABRBBBBBPBA CCCBABARAB BBARRABARRCCCCCCCCCCC C CCC CCCCCCCCCCCCCCCCCCC CCRCC.BAB..........

.. B....BBBBBBBBBBRRBBBRRABBBARRBABBPA C SCCCCCCCRRRBBBCBBRB CCCCCCCCC 00 C C CCCCCCCCCCC RCCBB.R. ........

A.A....+..A.BB AAARBARA+ABBRBBRRBRABB C...BBRR.AR.B.AR+RBAR RCARSR BC D +CC CC C0CCCCC....00CCCCCCCCC RRRBRAB ... . .. ... AR....RRBRRBBARAABRBAABRABBRSSBBB. .RAR.RR. RRRBARRRRAR CCCC CCCC 00000 CCC CCCCCCCC ARCCRCC. ... .. ... IL

............... RBRBSBBBB BR HRB ............... RBBBRABBBHRBCCCCCC 000 0 CCCC CCCCCCCCCC CCC.... ................. s.. A.BBABAR BPR BPBRRRBBRBBCRC .B C A.AR .RB BRRBBBBRCC....... .BDDBCBBRBRBRRRBBBBABR CC............. RARSRBRAAB CCCCCCCCCCCCCCCCCCCCCCCC DCDE C.. ..................

............ R.R.BR RRPBR RRRBBAB ABSBB CS C.............B RRRBARS CCC CCCCC CCCr, C C CCCCCCCCD EE ... ................. .B..B.BBRBABABRA RRBBBBABB . . . . . .RCCCCCRARRCCCCCCCCCCC CCCC E ... r..

..... AB....R.RRB.BBBBBR BCBRA BCBRACCCCCCCC CCCCCCCCCCCDDCCCCCCC. .. . . ....... "C

.... R.BR.BB BBRARBRRBB SC............ARABBRRBA CnCC CC CCCCCCCCCCCC CC E................ .............. B BRRA BRAaBBBB B RABB B C . . . . . . ABRRBB BC CCC000C CCCCC CCCCCCCCCCDC ED.. .................

... . .. RABRRBR RRBBR BBBRB CCCC. ................ A.A BBBRABg C CC n CC CCCCCCC CCC EE ... ..................... .. ."... R RBABRRABAR RBB B C0g........i..,.......A.BBB.... RAB R CCCCCCCCCCC CCCCCCCCC0E ...... ...........

...... ... BBaRRBRRABBHBA CCCC.. ..... BAARR AAB CC CCCCCCCCCCCCCCCCCCC CCCC 00. .... ......................BRRBPBPRRRAARBS C C. .. .............. BRR B CCCCCCCCCCC C CCCCCCCD 0 ............................. . .B.BRR BBRRABARBBBB CC............ . .BRRBRRCACCCCCCCCCCCC CCCCCCC 0.0.............................

. .. . . BB BRBBRRABRB BR B. ....... SRRR BCBCCCCCCCCCCC CCCCCCCE E . ......................... . ."B AR M RRRBRRRRSRCR B CCCC......................SARRFIBR0FB.CCCCCCCCCCCCCCCCCC 0DECE E . ........................

B BBBRA RBRABABB B CCCC ................"....BABARR AABACCCCCCCCCCC CCCCC(D D no .E F.......................RBBRRRBBBBRRAA BBCCCC...... ......... .RARRRRRBBBBCCCCCCCCCCCCC C CCCCcc 0. .. EE ........................

.BBBBBRARABBBBBB R CCCB.B ................ A R ABA CCCCCCCCCC CCC C CCCCCC 0DD.... ........................ .B BBBRABRRB RB BB CB...... .. PaBR AAeCCCCCCCCCC C CCCCCCCCCCC 00E.. . ........... ".........

.. . . .. BBB ABR RBARRR B BR . . ...B..............B R RBAB R BBBCCCCCCCCCCC CCCCC - 0.0...................._..... .......... ... B B BBBRAMRABBAB RABRBBRARB.. . ........... RAR RRRPRRB CCCCCCCCC CCCCCC EEE00DFF..F..... . . .....

...... ........ AABBBRBAB BBB RABB B RBRBRRRBBBBBRB. . . .....C . BRRARB CCCCCcCCCCC CCCC C EECCCCC G. ........................ .......... B BBABBBBBBRBBBBBRBAARRABBRBBBBBAAr................ .A... CCCCCCCCCC CCCCC C 0 ..........

.. . . RB BBB BBBR BBRBBR BRRRRRBA B BBBRRR R R . .BBR............... .RP....... CCACABCCCCCCCCCCCC CCCCC D ...... ....................... .......RASBSBBBRBBBRBBARARBAARBRABBRBBBR RBRBR...............DRA CBABCCCCCCCCCC CCCCC 0000DE..............

BBBB ARBRRABNARPBB AABBAARABRRRBARRRBABPBB .. ....... ... R . D CA CCCCCCCCC C CCCc 0 r..... . . ..............................BRABBBRBBBARBBBR RR R RRB BBRBRR BBRAR...................... ECCCCCCCCCCCCCCCC 0 F F... ..............................

. .BB.BB BSABR BB B R BRRRARPBBBBR BAAAR ...... ............ .. . R.... BE CCCCBCCCCCCCCCC C CCCC C 00.............. .............................................. ABRBBAB ASSBBBa BBBAR A BBBABAARBCBA..BRR....AP..R...............CCRCCBBA OBARR CCCCCCCCCCC 000 FE . . . . ............

..... ... BAaBBB SRBBBBARABAARBRB BRRABBBAABB....AA. .. RB..R.............C CCCCCBC CCCCCCCCCCCC C 0 ....................................... ....-- BSBBBBAARBASB RRBBB9PB B ARRBRBR BBSAB ACRBRRACBA R . . ....... . . . .... . .CCCAB CCCCCCCCCCCC ECC F O .... D....... ............................BBBBBRBB""BBB",,,, BBBAAARSABAB A RARBRARBA C. .... AR.. ... PB-B..... .. ... .. C C CCCCCCCCCC CCCCCCCC CCC O D. ..... .....................................

....AA..B BRBB RBRBBARRR AS RABRRBBBB RRRSSRRRR ...... .. . .. F.... . C CCCCCCCCCCCCCCCCCC CCCCCCCADI F ..... .......................................... ........ BBARBBRBBBBRBBRR BBRR BB+CARA....BA... ............ ... +F00CCCCC CC CCCCCCCCCCCCC CCCCCC 0 FE .... ......................................

/ ................ B BBBBB BBBB B BRB pP R BBf BBB B R RP B R P.. .. . ...................... ... .. . .. C C CC . .. ... . .. CccCCCCCCCCCC CC0 rr............. ...................................-.... .... .

SBBBRAAARRARBASAP BBABB BRRBABABBAB....RRPBBP ............ F F 0 CCCC CC[CCCC CCCCC.CCC CC CCC C 00 F

B A................ BBBSBB ARBR.C ....----.-..................... CC.............CCCCC CCCCCCCCCCCCCC CCC CC 0 .E..................................................................... SBBBBRBBBBBBRRRB RRBBBBBRA CC..............--... .. 0- C-C CCCCCCCCCCCCCCCCCCCCC 0 -n-.... .....- . ...--..-... ....... --..........

SS........BHBBSBBRRA RRBAB C. . . . . . . . 0 CC CCCC CCCCCC CCCCCCCcCCCCCC OO nFF.....-,,........... .. .

. . . .. .. . .. ..ccc.. . . . . . .." BBRBOR BBR BBBB BRR ....---- BBR B B....-.-....--. --.. ... .. n (CC.. .. ... .. CCCC rR R CC rrC c c CC nn FF.. .......................................................,B.........BBBBBBBBBBBBB R BBCC......... .............. .....ECDf[...............BF CCCCcCC CCCCCCCCCC CCFCCC0 . E... ...... ................................................. ... BBBRRBBHSRB ABRBRA......-......--. -.-.........F F---0- C E C . . - -CCCCCCCCCCCCCCCCCD 000FF.. N...................................... .........

..... . BBBABBHBARBBASRA R ARBAC.... ......................... . . ... C CC ........ CCCCCCC DCCCCCCCC0.F.. .............................................. ....... BBBBA RBRB ARARA.... .................................................... CCCCCCC CCCCCC..CCCCCCCCC 0.0. ........... ...... . ....

......... . BRBABBRRBRBRB A. . . . . . ... ..................... . ... . . .. CCCC. .. CC CCCCCCCCCCCC 00...F.... ..................... ...... ...........B........f......P A BRBBRBA R A BAR 00CBC CCCB0 FEC. ..C. .................... -..---. ..-... ..---- ... ... .CCCC CCCCC C ... ---.----..... .........-- .........-. -............ .......

B........SBA BB 0BBBR0.BRAPB 0R..C C0F......... ... -.................. .............. .CCCCC C CC ..... ............... .. ..........................................A........ABRB RBBRB C. . . . . . . . . . . . ................ .. .. .. .. .. CCC C..CC.............................................................

. ... B BBR R BAR . C.............................. .... ............. ........ . CCCC 000 ............................. RBBBB RABRBARC.... ....... C.................................. CCCCC 00F.......................

... B BB BABBR . .............................. ............................. H CCCCCC 0 0 ............. ......................BBBBRBRBABR..B.BRR CC --..................... CCCC 00..0.................................

.......... 0BRA BR ARBB BBRBAB.AR C..................... ..A0BP CCCC 0D00.0-................................................................

........ B BBH BBP BBBBSRBBAB R AR C ........................................................ ... R... . CCCC 000 D ... . ...................................................................

........ BBBA BBOHB BBAB AC ..................................................... . . . BCCCCCC 00D0 F............................................................................

........ B BRBRBH AgRgAB CA. .. . . . . .. . . . ... . . . . .. . . . .. . . . . .. . . . . .. 04C C CC C 3. . . . . . . .. . . . . . . .. . . . . . . .. . .. 3..0. . . . . . . .

R CC ...................................... . .. . . . R CCCCC 0 F..................................................... .......

BBBABSRABRRABARB CC. . . . . . . . ............ .CCCCC....F

........ BBBBBRABBBB CCC.......................... CC(CCCC 0 F F........................,....... A BS BBB BBA BR RCC CCCC. ........................... ........................ . .. . . CCCCC 0 .... . ...................................................................

........ BB BSBBBBB AB RCACCCC ......................... ........................................ CCCCCC C CCCCC . ............... ..........................................................

B .BR RBCRARACCCC ................................................................ . C CCCCCC C . F.............. ...................................................................... CCCBBCBA B R RACCC .. ........ ....................... ................................. C C CCCCCCC 0.... ............... ................................ ..........................

..... CCBBCBRRCCC 0C.................................................................... CC CCCCCCC. . F..........................................................................J ........ B RCRHCA BC9BB R C C ..................................................................... CCCCCCF n 0.... . . ..... ...... ............"..... ............................"... .... . .

.... BBBRAARRIABBBR B CCC CCCf .. ................... I) CCC(CCCC.. .. .. .. F.. .. .. . ..

........ CCCCCc ..... ............................................. . . . .... ................. .. ......A.. . . . . .. RB . .B. . . . .C C .C. . .............. :. ............ -. .... ................................ C .. . - -. F.---- ....... -------- ..-. -. --- .------ .... - .. ...........

.C...... .. .. .. --..... .-- .CCCCCCC .C.... . .... - .e .-.......... 0...... .. .....

jBP CCCCCCCC RRR 9CCC ..... C.. ......... CCrr(CCC0FFF..............__..))0)........_._.. ............... _..........

..... CCCCC CC. . .- ..... .. .. .. . ....... --- C .--------.--- n..-. ..--- ...----.- . ... ................... . ..

... ... .................. +ACCCCC.. ............................................... .................. ............ +..........._................................. .............. .. ........

...... .................... CC rC........ . ......... . .... ... ... ... .... ... ... ...

. . .. . . A B B E R R R A R. .B P . ..RB A R .R.- -C 0. .. .. ... .. ... ... .... .. . .. . ...-. .. .. . .. ...- .. .-. ... ... . . ...... .. . . .. .. ....... .. . . . C - . ece. . e *reD.- . .F- e. .*. ..*. .*. *..* *. _.* *. .*. ._-. * * * * . * -.* *.. * .* _* .* * * * * -* -. .... .* **_ _* * * *. ... .. .

.. . .... . . . . . . . . . CCCCCCC CCCC . . . . . ... .. .. ... ...... ... .. ..... ... ... .... . .. ..... . . . . . . . .. .. ... ... _.. .......... .. .. .. ...... .... .. ...... . .... ..

................................................... C...... ........................-.-- .... *.*. .o...

........BBB CC ~ CCC C. ............................................. .. . . .. . . .. . . .. . . ..... "............____......... .. _..C.. . .. _."_CCC. . ...... . . . . ............ .. . . . . . . . . . . . . .

GFDOATA INTFNATIONAI,. INC.DALLAS. TXAS

A< 0.10 0.20<R< 0.3 0.4<C< 0.50 0.1<0< 0.70 ).RO<F< 1.90 1.O<F< 1.10

1.20<C.< 1.30 1.40<H 1.50 1.0<1< 1.70 1.0<,1< 1.9 2.00<K 2.102.20<< 2.30 2.40<0< 2.50 7.0<< 7.70 7.Il<0s< 7.90 3.00<P< 3.10

3.20(< 3.30 3.40<1( 3.50 .5)40<< .70 1.BO<T< 1.90 4.000< 4.10

4.20<V< 4.30 4.40<(4< 4.50 4.f<l< 4.70 4.B0<Y< 4.90 5.00<7< 5.10

5.20<1< 5.30

1AT 39.0''i ING -7f,.flO

................ ...............

......................................

.................

......... ........ ..-

................ R

...BABRBRA

............... BB 8R B B

................ R RB R....... RB A UBHRB....... 9BAB AH RBRBB...... ARAHBAAH BRRB H A... . .RBB A BBR BB R B RRRB R BRB

.... BBBBB8BBBRRBBB

...A,. BNP B BRBRRH B BBBRBBB

BRBBBHHABBH...... ABRABRAB

.,............... R8 R B

............... RRR B R,................ B 8 R

. ........... ABBR R

...4............ B BR............ ,,... RB RR

.C BBABAB B

..... .... . CC RRBBRBB

.. . .. BBRB

.... .. A.A

....... BB B..... ..... .BB BR

............ BBBBBBBB BBB

.... .. ."B BBB BBBBBB B.:::::::: Bc BBBBBBBB R

.CCBB ABBBBBRBBBBR

.C.. . BBBBBBRBRBRBB

........... BBBBBBBBBBBBBBBBRBBBBB

SCCC BBBBBBARBRRBBB.. CC RRURABRBBB

........ ....BBBBBBBBBBBBBBBBBB

.. BABBBR AB

B BBBBBBRBAR

."".."...::BBBBBBBBBBR BB BB

BRBBRABRRBBHBH..... BBBBRBA RBBBARRAAB

... .BBBBRBRBBBBRBRBBR.RA.. ABABBAAABRBB

, ., . BBBRBBB BBBRH.... A. BBRBRBBA R

.. .RBCCC B BBBBB BBBB

... .... CCCRRBBBR BBBBRR...... CCCC . B ABABBBB BR

. .. BBRR RBBBBB BR

.AA.R... .CCC RAHAUB........ CCC ABBBBBARU

...CCC AHBRNBBB

....... ... CC RB BBBB BBBB +......... . BBR BB BBBB

..... .BABRBBRHAAB

. ..................... B...BBBBBB

..B.H BBBBB. .B

.BBBRABBBBB BB B. BBRABBBBBABB

.. RBBBBBBHRABBBB.BBBRB'BBBBBB B

.BRANNABRABBBB.. BRABRBB R

.......... B...... 9.RBBBBABNA B

.RBABBBBA B

.BBBBA BBB

................

.. .. .. .. .. .A."..... ..... ... . . . .. . . .........."......... ....... , . " ." "... .. .. ....RRRRMRa4............... ....... ..............RRRRRB."...". ... .. .... ... "DDD ."."... .. "...................... ... ".". .. ..- . .... "". .. "". .. - .........-...... "...." .. . ... *.-* 4498888-*- -. *- - . . . . - . - - . - - . . - . . e . ....... * D .^ . . . . . .

.. .. .. ... . ..........- .- e ....... . . -. - ...........-...... e.. ..-... ... ..,.- ... - .HNNPR H N .e."....-.."..,.,... ". ... "... .... "... c e.... ........--.... "DDn ............. e.... - . . . .. - . - -- . . . - -- . - . . .. . - . . . ........--.........-- ...--- -- .-- 88RHRNR ".------------- "...."".,--""-C-C C----..-..-..... -- - .- - - . ..----- DD .... "....".......

.... .. .".. ... .................--...............-.........-------. . -- - - .* -- ---.. * .A H -- -- - -- -- -. .- -.. H- -- .- - . CCCC.-- .- - . ..----- .- DDDDD . . ..........

.RR....................................... .B . . ......... . . . .RRRARR RRARRR. . .. C.C.C.. . .. .. G.H...... . .:nn DDDDDDDD DDDDD DDDDDDDDDDD...... ....... .... . . . . .... .CGG.. . . . . ..C..CE G.G E. . .D Dn.

.. A ...... ....................... ......... .. ... R R N R RR .... E.F.GG nHnH f "..". ."DDDDDD. .....

..RRE ---..--. --------------8RRRRRRB RRBBbBRPRbRRRRRRRRRBRR4 NHR RRRRRRRRRRA CCC DD EE F G G HHHHH GG FFF O ED D D 66DDDDDDD bDDDD DDDDDDDDDDDDD.......BRP ..... * RH.UUHH...P..(H1. .. .RRMBAH.HBkRRiABkRRBR PR R BMHHRRR HRRRRRH C CCCCCC 00 GF H IT H CGF FFF f nflpfllflf f D lD flnD DDiDfDnf n DnD . .

RARRA BA.A ARARRRAARRAAAR0RRARHHRUB UFURAI.UUUMNHAB RM4 RU URUR CCCC 0E GFE F H IT H G FF1F , fl DDODDDDDfnn DnDDnDT DDDDOO DDDn .D"nn

APR * HAURRRRRBRRRBRRRRRUIHUHPPHRPPRNUB UUPBRRRHUUUUHB CCC 000 F F CGJ N HNGGC FF FFF' flfinnflflflnflnDnnfDnnnnflnDDnnnnDnDnnnnnARAB . . .B.R.B R.NH..R B .P...RUUBUPU.NU..UH..H..RH 0 CCC O FKE F GG HHNHGC FFF FFFF nnDDfDoDDnnnDDnDDDDTnD nnDDDnnnn nDD.DBRR C. . URBARR BMHBURRUBPRBRU RUMRHHRR RRRNHRHR CCC on FF F C JHH F C FF 'FFEF DOnDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDD. D

RRR CU"UU"U"UURRRRBURRRBURFHBRRRRHARRR CCC 0 FE F G THI HH C EEC FFFF FF nDDDDDD DCDfnfDDnnDODD onnDDnnODDDDDDD'*BRRR RCRCCBARRRRBRA BBBRHPH FRHHBPRHURBUHRRARRHH4RR CCC o EFF FG H I JJ I HK G EFFFFFFFF FFE DDnnnDDDnnDDDDDD O O nnDDnnnDDDDDDDDBAR ABUBRUUARHRNBHEB BR6PRNMMRMIBIUHUMUHNRK "HU CCC n F F G UH K K JI H GC FF .FFFFF FF . . nn... . DDnNDDDOOOnnOOnnlOnODDODDDD

BUH BRR CUA BHHUP fBARPHPABP U URR UH RH I UR U CCC D F FFG HIJ JTNC FF FFF FF DDDFnn.O............ DD DODnn nDOfD DDODDBBRR CC A eRRAUBBUUUU AUBUUURHH RR H H4HRHHHMUCCC on I FE G.IJ K H FFF EFF .FFF.F. ODnnDDnnnDDDDD DDDDDDDDDDDDDDDBRUB CCCCCC ARMB BHHUBBRHBHRFR 4HHHRRRHR UHCMH CPRCCACCCC C F F C FGOP LF FFFFFF F.F FFFF FE ODD DDDnPfnDOnfnffDDDnnDRBRR BUURRBBH BRPRRUUUH HEHAHN CCHHCHU C CCC nC F G N JHCFF FFF.................IODD 0f nDDDDDDDDDDDDDCBRRA BRBHSbBPRRFR HRHAH CUB CRRUII CCCCCCCC F FFC LL CFF F..............EE DD CCC DDDDDD DDD CC

BRBARUBRRBBCC.P.R......RRRR....R..CCCCCCCCCCFE F, IJ K J H FFFF . ...... DnnDD CC DDDDDoDDoDDDA BBRRRRBBRRBB CCHRCCHCRC....RH .. CCCCCCCCCCCC CCCFFC C I FFII NC FFFFF............... DD CnnCCDDDDDoD

BRARBBRRBRARRR B UCPCRC.R. . CCCCC CCCCCCCCCC0C F E F FFFCCC FFFFF....... .E f nCn DnDDODDD CCRRRRRRRBBRUR RARRC HR .CCCCC CCCCCCCCCCC D E FFFFF. . .......... F.F Do CCC nnnDD D CCPRRRR RARBRR ORRRRCCC ............... C0CC0CCC D F FFFF FFF.......... .F , On CCCC nnnnnnnnnn CCC

RHRRRRRRBRPRBR RRRRBBRR CCCCCCC......CCCCCCCC D F FFFFFFFFFFFFFF..........FE DD CCCC nnDCC DDoDo CCCHBRHRRARR RRRARRRRH BBRRRRRR CCCCC. . . . .CCCCCCCC n . .FFFFFFFFFFFFF...... .... EF n CCCC CnDD CCCC

RBBBRB HA BUBHRRRBRRHRRRRAUR ARRBRRR CCCCC. ............... +CCCCCCCC 0 F FFFFFFFF E... . .. +CCCCCCCCO CCCCBURHBRRRARRRAUUURAHURHBBRRAHAU URRRRRRARRR CCCCC 0........... CCCCCCCC F 0 FFF Dn CCCCCCCRBARR RRRURN RRRRBRRRRHRBRRRU R RRARRRRAR CCCCCCCCCC .o.......EEECCCCc.... . F' n CCCCCC C CCCCCBBUBURAURRBBBRUUURRRRRRU RRRRBBURRBBBRRRRRRRR CCCCCCCCCC n ... ...... F E FFF F .......... EF. ODT!CCCCCC CCCCCCC

BUHARRR+URRURBHRRR RBBRRRBRRRRR RRRN+AARRRPRR CCCCCCC n .n....... .. on E+nno FE EFFEFF...............FF. DOW D+CCCCCCCC

BABHARBRR RBRRUBBRURRRRBRBRBUURRRRRBBRRBRHRBRR CCRRRCCCCCC D 0"............nnnF.F FFFEF..... 0DDDDDCCCCCCBBBBBRRURBBBARRRRRRRBRABRRBRRRRRRRRHRBBRRARRRRRBRRRRCCCCCCC .. EE .......FF . F..FF.FFFFFFFF......DDDDDDD CCCC

BABRURRRR RRRRBRRRRRRRRRRRRRRRBRBRBRHRRURRRRRRCCCCCCC .. . F.... .FFFFFFF.F.EF.. FFFFFFFFFF...... D DnflDDD CCC BRABBBRRBURRUBHB B RRR U HRRRRBBHRBRBR RURRBRRBARRRRRHRRR BCCCCCCC. . . . . F.. FE .FFFFFFFFF . . .DDDODODDD CCC BARBUBBA

HABBRRBR ARRRRRHRRBBBBRBRHRBRRRRABRBRRRRRRRRRRBBRACCCCCCC Do T FF........... .. F FFFFFFFF D D DDDnnDDDnonnDDCCC RBRARBBBRR RR RRRRRBRRRRRRRRURRRRRBRR RRRR RBUBRRURBAB RCCCCCCC On FE............... FF FFFEFFFF DnDDDDDDDDDDDDDDCCCCC BBBRARA

RAB RRBRHRABRRRRRRRBBBRRRRRRRRRBRA RARRHUBBRRRHRBUARCBCCCCCC 00 FF......... . FF1' FFFFFF DDD DDDOiDrOD D CC CCC .RB

RHUBBRRUBUABBBRBBRR HARRHBRHBHBRRBARHBHABRBBRB BRB B CCCCCCC 10 FF............... FFF F.FEE .E DnIDDDDDDDDOD CC C CCC B.. .ARBRBRUARRBBRHBRBUBURRRUBRHRRRBRRHRRRRRRRRRRRBBRARBRR CCCCCCC nnDFF.....FFF FFFF oDDDDDDDDD CCCCn CCC .R A.RRBRRABBUHURAAAA UBHHRA RRABRRRRRR RBRARRABBR BCCCCCC on FF. . ...... F FEF DDDDDDCCCCCoCO.....n CCCCC BAB AAAAFBRR B BRRRRAAUBAUBRRRARURRRBBRARRRRBHRRRBHARRBRURRRRR ABRB CCCCCCC o.F. . . .. F FEFF )nDDDDDDDDDnD CCoCCCCCCCCC B........RBRBBRABRRRRBBRBRRBRRB RRBUARRABRRHRHR RRRPRBFIURHUHBAR CCCCCCC nonCF..... FF FFEFE DDDooonnDD CCCCCCCCCCCC ........ABRRHRBRRpRARBBRBRUABRRRBRRARBRHRRRRBRRHRRRRHA CHHCCCCRRCCCCCCCCnoonEE EEEE....FF1' FFFFFfODDD CCCCCCC B ......BBARRRRRBARHR RRBBBB RTRBR RRRRRRHBRRBRBRRHR HBBRUACCCCCCC CCCC .CC ...D...F E FFFFonnnDDDDDD CCCCCCB .......

B BRB RBRRRRRRRRBUBRAHHBUBRBRABRRURRRRURRRRRR BRRBUU CCCCCCC C CC CC .... EEE.... FF:FFCFFFCnnDDn CCCCCB ABAR ........RBARRRRRRURBRRRRBAURURUARRBRRBURRRRBARRRRRRRRHRBARU CCCCCCC CCCCCCCC ... .FDFFFFFFFFD0000CCCCCC BBRBR ........RUURARBRRRRRHRRRRHRRBRRABRBUABRRUBRRRRRRRRBRRRBHABRA CCCCCCC CCCCCCCCCCCC D0D EFFDFDCFFFFCCCCCCCC CCCCC BR RBR ........ABRRBURRUBBHRBRRRARARRARBRRBRRRRURRRRRRRBARRABRBBB CCCCCCC CCCCCCCCCCC Dnoon FFFFFFFF nDnn CCnnOOC oo C CCCCC ARUB RAABBAA.......RBRBBRBBHRRURHRRBRARRAARBRBR UBBRBRRRRRRRABRRAA CCCCCCC CCCCCCCCCCC D00DDDf EEECFFCCnnD nCnOBDfO.CCCCCC ABRB ... AB B........

BBRR BRAABBBRRR.ARIABBURSABRRUBBBRAARRHARAHRHRBB CCCCCCC CCCCCCCCCCC 00DDDDDDD CCCCCC UBABRUB......A BRRRRRRRBBBBURBRRBRRRARRPRRRURARARRRRRBRRPBARBRCCCCCCC CCCCCCCCCCCC nnDDoDDDDo CCCCCCCCCCCCCCCCr R .BB . . .....

RRRUBBBABBBR UBRBUBBRR HA RRRBBRR ARRRRRB CCCCCCC CCCCCDCCDCCC 00000DTDOl CCCCCCCCCCCCCCCCC BRRR BAAB.. . . ..

BBRRBRABRBBRRRUBBRRBRRBAR RBRR RRBRHRACACCBCRCBBCCCCCCCC CCCCCCCCCCCC D0D DD DD DD)D CCCCCCRB ...............BB BBRRHRRURBBRRBBA RRBBABRBUBR RHRBRBBARRUBPB CCCCCCCCC CCCCCCCCCC D CCCC0DDDDDDD 0 C CC BR BB B ................

BBBBRRRBRRRRRBRRBBURUBRRBRURBBRURABHARURRRRRARRRRUB CCCCCCCCI)C0C D CCCCDDDDDDo (CCCC RRR R A BBAAA.....RR........HRRUABBRRBBRRARRRARRRBRRRABRUABRHRBHRRURRRURRUARHBRBB CCCC CCCCCCCCCCCCODC00000000CCCCCCC RBABABBRARRR A. ..........

RRARBBBBHARRRRB RBRBARBBHRBBRRR U RHRRAHRUHBRRBRUAAR CCCCCCCCCCCCCCCCCCC OODODD00 CCC CCC RBRBABAB................RBBRABBBRHRRRB RRHBRBHRRBRHRR ARRHU BBAUT3AAABBRBB CCCCCCCCCCC CCCCCCCCCODOD CCCC ODD DD CCC ABAB AAAAAAAAA . ........

BBRRRRRBBBRBRRR BRUBRBRHBRRRBRRAR ABHRBRBRRRRRABRBRR CCCCCCCCCCC CCCCCCCCC D0DD CCCCC Ofin CC BRRAAAAAAAAABBRRRRRRBBBBBURUR B RHBURRHBBBRBRB UURBARRRABABRBA CCCCCCCCCCC CCCCCCCCCC DOnODfD CCCCC CC BARB AAAAAAAAAAA ...............RBBBAR BBRB B BBRBBRR RR ABAARRBBBRRARRRRRRBBUU CCCCCCCCCCC + CCCCCCCCC 00DDD0 CCCCCC CCC RB+RA .AAA .A . ... ........

RBBRRRBBRHBBRUBBAHHUBBAAHBBBRHRBURRRRBBRRBB CCCCCCCCCCC CCCCCCCCCC DDDDD C CCCCCCCCCC RRB AAAA ....................UBBBABRBRRBUBUB RRRBRBRBRRBBB RRR B BRRRRRRR RRUR BU B CCCCCC + CCCCCCCCCCC DDDDD +CCCCCCCCCCCCC BBRRA A .. "...................

BBBBRP99RBBBPBBBB RBBBRBRRRBRBRRBAR RBAR9BPR HRBRARRA CCCCCCCCCCCCCCCCCCCDDnCDO C CCCCCCCC CCC C C CC UR RBBB.............. ......BBBRURRUABBBBRRRBBBRARRBBRRBRARRBRUBRRRRRRRRA CCBB CCCCCCC CCCCCCC 00CCC0CCCCCCCCCCCCC CCC HBBRCC RBBR ..............

RABRBRBA AA ARU+BABHUUHRRRBR RBHUBABBRBA+UAABBRBB CCCCCCCCCCCCCCCCCCCCCCCC DDCCCCCC CCCC CCCCCCCCCCCCCCCHAB RB AB.B.C.......................BBBBRBRAA. A.BB .RB.. BH R BBRARRBRRRRRRRBRRRBRRRRPRRARBBRB CCCCCCCCCCCCCCCCCCCCC CC CCCCC OCcCC C BRRRRRR C...................

BBBRBRU UAR .B.R .BR....BBRA RBAA RRBARBBRRURARRR RBBBR CC CCCCCC 0CCC CCCCCCCCCCCCCCCCCCCCCCC CC BARBABRR C.......................BBBBBB......................BR BHRRRBRR RHARRRBRRRRRBRB BB CCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCC ARARA RRBB .......................BBBBBB ...................... BBA RARRBBRRRRRBBNH RRRBRRBRA CCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCC BBRRRR RR C.......................ABRRRBU....................U.BBUA ARU R BRBBUARHNRRR RRRRRRRBRBBB CCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCC BAURBARRBR .............BABBARB.................... .A ARRRRRR BRRRABRRRRRRBRRBBRBRAB CCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCC B ARRR RBB ......................RRRBBR......................BB RRRARHABRBBRUBRRRR B RAA RBAARB CCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCC B UABRBUB .. C ..................BARBAR...................... RRARRBRARRBRRRRBRRRABRRUBABRBR CCCCCCCCCCCCCCCCCCcccCCCCC C AB .AR .B. ....................B .ARARA .. . . . .... . .. RBRRRBR RRRRRBURBRRARRRAARRRAR C C C C CCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCC ARBA RA...............................

BBARR......................BBRRUBRRRRRRRRRRRRRRRRRRBBA RAR CCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCC ABR..............................BARBA......................RRARRRRRRAR RBBBARRA RRRRB CCCCCCCCCCCCCCC C CCCCCC CCCCCCCCCCCCCCCCCC C CCC .................... .....

UBBRRB...................BARRURRRARUBRBRRRRBBBRRBRRBB BbB CCCCCCCCCCCCCCCCCCCCCCCCC DDDD CCCCCCCCCCCCCCCCCCCCCCCCCCCCC BARBA..............AUB.RA.. ..... .. HBRBUAABRRBRRRRR RBRARRRBRRBRRR B B CCCCCCCCCCCCCCCCCCCCC CCC CCCCcCCCCC CCCCCCCCCC ...............................

BR RRRBBRB...............BR A HRBRRRBRR RR RRRRRABBR A B BABB CCCCCCCCCCCCCCCCCCCCCCC(C''D'DDDD(CCC CCCCCCCCC C CCCCCCCCCC ..................... .........BA RRBB. ............. BARU ARRRRB BRRBRRRRRUURRRU R RBRCB C CCC0CCCCCCCC DDDDD CC CCCCCCCCC CCCCCCCCCCCC........................ ......

ARBRRRBBB R...............BAR B BRRBU RR RRHA AB AAB R ABA BUBPU CCCCCCCCCCCCCCCCCCCCCCCC nD nnnDDo CCCC CCCCCCCC C CCCCCCCCCC......................................ABRR BBBR ............... AUB RBRBRRARR BRB AARRARARURRU BB APFB CCCCCCCCCCCCCCCCCCCCCCCC 0000000 CCC CCCCCCCCC CCCCCCCCCCCC............................ ....BRRBBABBA...............BR AURAHBBRRABARUABBBRA BBAHB CCCCCCCCCCCCCCCCCCCCCCCCC 0000 CCC CCCCCCCC CCCCCCCCCCC......................................

RRBBABBB.. . ..A.. ......... ... BRABRRRRRARRAA RBRARB BABUBRR CCCCCCCCCCCCCCCCCCCCCCCC CCC CCCCCCC CCCCCCCCCC......................................RBRRBBBAR..............................RR BR B RB BBB CCCCCCCCCCCCCCCCCCCCCC CCC CCCCCC C . . .. . .. ..... ... ... .. ..BRRR BRB .............................. BAR AR RRRB RRHRRU RBRBB PBCCCCCCCCCCCCCCCCCCCCCCC CCCCC R CCCCCCCC CDD .............................................RRABBRRR..............................RRRBRRRRRR RBRRRRRB BC CCCCCCCCCC CCC ccC CCCC CCCR R C CCCCCCCC.... . . ....... . . .

RRARRB .............................. RBRBR RRRRURRRAHR CCCCCCC CCCCCCCCCCCCC CCCCCCC RCR CRR CC CCCCC E C.............................................R . .. .. ............- B BABRRR RR UC C C CCCCCCCCCCCC CCCCBB ('B C C DE .................................. ..RPRRABBBB..B C..... ARB..........RRRRRRRBUR ACCCCCCCCCCCCCCCCCCCC BRRRC................R AR...........CC. ................ B..... RRRRB CCCC C C CCCCCCCCCCCCCCCCCC R BA R CRR CCC ........ ... . .......................RRRBAB R.RRBRR CCC....................... RRRBRRA CCCCCCCCCCCCCCCCC CC RBU AR RR C0F.....................................................RBARRR. .RRBR .CCC....................... RBRRR CCCCCCCCCCCCCCCC BRRR RR B BR C..................................................RRR RRR . .BR .CC....................... RRBRRBUHBARRRBHHABCCCCCCCCCCCCCBBRAB RRRRR C.....................................................RBRABRRRAB CCC....................+.. RARRRBARRRR+RRRR CCCCCCCCCCCCCC ARR B RBRAB C.........................................+..........

BRRRR RRBR CCC........................ .RRR CRRCRRCRBCRccc. . ..CCCC RBR RHUBARB................ .ARRBABRBARB CC..............................RHR BRRRRNAHACCCCC BRBC................

AA RRBBRBRR CCC..............................ARBRA B AAB BHAARBRBRCRA CCCCCCCC ABRMB" R.UB ......... . . ....RBRAAABURBR "C........................."UARARAARBBBbRHRUH RBPHA CRCCC CCC, ,ABU URR. C. .............. .RRRRRRBRBACCC..............................RRBARRBUAB BB HUAR + BRARUBRR CC.CC .. AUBR. BR. ...............RBBRR RBRRRR..............................RRAR UARRRB R HBUNUB HURURACCCC RRRRR.

BRAA BABHBC.. ......... . . .............. R.R...........AAA B RP ARRACCCCCCCC ARM ... .....ABAR ACC................... BARRA ............. AAAA B RB PRBRR CCCCCCCCBRR ............. . ... .....

RBBR CC. ...................... AR B ...............AAAAAAA RB RRRBCRUCCCCC BABA....................................................................A BARCCC ...................... AA A B...............AAAAAAAAA RR CC CC ABA AU.....................................................................

RBAR CC .................. B .R...A.U..AAAAAAAAA H PCRRA CC BRO................. .... .... .RBRA CC ...................... BURR .......... . AAAAAAAAAARR C CC C BR .....................................................................

R RAB A CC ... .......... ...... B. ............... AA. . . .. . R A RRAR . R. . ...................................................................BARC..... ......... ............... A ... ........ AARAARR CC ..... ..... .. ........ ......... ....... .RB C.................................................................... RRRHA C. ................. . . . .....

NRR RR C............................................................. ........ARBARRHARR" C...................... ..................... .. .. .. .... ......RRARA.... . . . . . AU. . . ............................................. BAAAAARR" .................................. ........

RRARB.A......"....."......... .. .. "...........".HUBAARRPA

RR R ..... ........ ............ . ......................... RPAR P. RN RAAA AA ................................. . ............ . .UARRRU ........... . "................ ....... .. .... . .... . ... A................................................................................. . ...

AA R RR ..................................................... ...............MR AAR ............. ."................... .. .........."......."""........"........... .

RAUBRUR . . . . . . . . . . . . . . . . . . U.. U 4U A R A RR . . .. . .. . . . . .. .. . .. . . . .. . . . . .. . . . . . .. . .

BAR ........ .... ...... ...... . . . . . . . . ....... PCCCC RUA.. .............................................................................

RRA . . . . . . . . . . . N A 4 A U4RH N H RA ". . . . " . . . . . . . . . . . " " . " . . . . " . . . . . . . " . . .BARR...........................R.........U...............................

A.. .-.-. ..-. *-- ... ....-....................... N C . .-.-.....- ...BARRA ............................................................. ...... . . . UAH....................................................................................

UNBAR............"................".. .. .AUHNN.......... ... ".......".....A BRARA................................. ...................................... A~ANUN..........."..............

AURRR ..................................... (CC................... ......... HU..........................A URR............................................"...CCC....................... ............... ......

A....B. ......... ........ ........................................... . . .A HA...................... ......... rCCCCC... ... .... ... ... ......

"."".""...".. ... A.......""..."..RB...""...."........"........... ....... "".... ....... CCCC............ ... "."...."...... ".".....".........."" .""."."".....A....".........".............. ".... ... CCCCCCCC ... ,..."..."......"......".......C"".""."...C...".

........ A.... .............4................. - ... +.... ........ C ...... +..C'.......'.CC......'........'."C...+.'''C

.4",.....""". .............. +"."".............,..,.....""........"".............. ....... +"....""..................

GEOnATA IRTE!ATIOAL. IC.DALLAS. TFXAS

A< 0.90 1.90<e< 2.70

10.BOC<G 11.701

19.N0<1.< 20.70 21.R0<,< 22.50 73.40<&< 74.f 27%.7n<fl< 2h.10

ft"10CJ

--

'-

l2.60<< I4.5

1.40<1< f.10O

14.40<1< 1%.30

7.70<v< .m

1b.?0<.1< 17.10

9.00<F< 9.90

IB.0l<A< IB.90

27.00<P< 27.90

rnh l i Ii-ruVAi,= . j'0 .. 90 i r:Gr Fu/tw

CI)'I7 iIIF 11 I I-:F t= 1. II' I (Ti'' I TH/ K f Al 9.0110 I(nTC -7 .000

....... .............. .............. .. CCCCCCCCCCCC .................... .. .. .. .............................. 0n .................. ..F F F. ...... ..... .... ..... ..... ..... .F F F FFF .. " . . . ... .. .. .. .. . .. .. .. .. . .. .. . . .. . .. .. .. )DCC CC .. .. . .. .. .. .. .. . .. .... .. . .. .. .. .. .. . ...... .. . ...... .- . .- .- .. .. .. . .. F... .. ... .. .. .. .. . .. ... FFF . .. .. .. .. .

........................... .. . . ........ . cCCCCCC .. .FFF .. FFF F ..... ... . . . . . . . .. . . . . . . . . .... . . . . . .. . . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . ... . . . .. . . . . . . . . . . . . FF . . . .. ..... ..... F.

.... ......... ... ................ D ......................... . . .

....................... 6DDDODDDDDD656D DIDDDDIDDD " "" " """ ."DDDn D ""..............................0nD1DnflDD)IDDDDDDOI DDDDD """" " CC CC f0frf )'M' r) EE E G HI,1""" " "FFG... .... .... .. ................. . . ...... 0 0 00 0 0 0 o... .))nn0IO~)rnP c- )I!trPI TF 1 F NH C......... . . FF.......................... DDDDDDDDDDDDODDDDADDDDDDDD[ IDDDI DD E.".............................DDDDDDDDAI nD D00 DD CCCCCC on"An F. F G HI J KK J 7 H ......... GGGG GGGCC . ...

................... ,. D............................... DDDD D DDDCCCCcC n FF FG G. .... G0000D000000000001)000 FK 0000ILDIJ1PI CCCCC ~ I T f' GNHI11JJ KK J ]I N~HGG GGC.C.CGGGGG." ..

. . DDDDD/D DDDDDDDDDDDDDDDODDD0 DDDD DDDDDP E'EE_ .. )00DDDD 1D)PfODI' P CCCCCCCC(1CC P1P 10 F'E. FF G H I JJ KKK J I ........... . CGGGGGGGGG A G ......... DDDDDDDDD DDD DDD DDDDDD DDDDDDDDDDDDDD DDDDDD FE . . . . .. DDODODDDDU CCCCCCCCCCCCC Onn ) EFF FFF G H I JJ KKKKK J I..............G GGGGGGGGGGGGG HHH.......

.................... .DDDDDDDDDDDDDDDD000 DDDDDD0D0D0DDDD E FF. .. .... ... .. 0.000.. .O.D LI CCCC CCCCC Pr cF FF 0G H T J KKKKKK K JJ .... . HHHHH GGG.G .G H .................... D D D D DDDDDDDDDIDDD DD DDDDDOnoD IIDDID DDD0 n I EE F FF F .F RFFFE IIDD DD DD UD DD C CCCCC Crr C(' D FFDFF G..............KK J ......... HH HH GGGGGGG f...............

................ DDDD0DDDDDD0 0DDD0DD DDD0 0DD DDDD0 P 'EF' F FF ' EFF¬F ' ODODOD DDDDD0ID CCCCCCC CCCCC 0P FF' FF GG ............... I, K 7 ........... 1....HHHHHHHHHH GGGGGGGGG...... . .D0DD DD 0DDDDDD DD DDODDDD0D0 DD0DD00 D DDDDnDD DDDDD 0P FE FF FFF FFEE DDD D0 D Dc CCCCCCC CCCC DD F .G................ L K J .............. HHHHHH HHH GGGGGGG................

.............. DDADDD0DDDI0D0DDDDD 00DDD DDO0DD0 D 0 ) E FF' F'OFFF).FUEIDDDD D D CCCCCCCCC CCCC ) F Fl' GGCc HH. . . . .[K . . . . . . .14114C.............. L K J 1........................ 00DD0DDDDDDDDDD DDDDDDDDDDDDDrDDrDDDDDDDDD0D0 F F G FFFF FEE DDOODODODOUDDI CCCCCCCCC CCCC F F G H ..... H G......HH GGGGGG................

.... ". ""..... .DDDODDD0DDD0DDD DDDDDDDDDDDDD00DDDDD0 DD0D F E FF GG FFFF EFE DDDDDDO OODDC CCCCCCCCC CCCC 0 FF F" H . . . . L J ............... HHH GGCC ..............."""""D""."""".000000000000000 '' ''FT'''F EF.F lPOrO000000CCCCC CCfCC n0FFT FT CGCH1414. . . . . . . . . . . . . . . JHHHH GG, ................. DDDDDDDDDODDO 00DDDDDDDDDDDD0 DD00D000D DDDDDD 000 FE FF FFFFFF FEE DDDDDDDD OOO DDDD CCCCCCCCCCCC 0 FT FF (GH H . . ................. ....................... HHHH ...........

.......... ... DDDDD ODDODODDDDD 0DDDDDD D DDDDDODDDODDDD DD P EF.'EFf nnD 000 000DDD DD 000U FF F0G H..................................... . . HHHHH.............. DODDOoDODDODODDDD DDDD DODODDDODDIDDDDD EFFECT EE EFF DFODGGD....OD.D.........O..o.F.F.F FT................. HHHHHHHHHH ........

................ DDDDDDD DDDDDDD P DDD DD 'EFFTF DOD D D FF FFF G...................................... . HHHHHHHHHHHHH....... . .............. DDDDDDOnDO 0000000D CCCC no.DD EE DOODnOODDDODOIDPDDDDD PDID)DPFF F.FF FFF'..............HHHHH

............... DDDDODD OOPD OD OD CCC CCo E DFFFDFFnDDDDODDODDDDO DD DDDD FIT F F F . .FFF F........................... .. . ... HHHHH............................... DDDDODDD FK DDDDOODDD CCCC CC Or D00000000 IDDDOD DD DD DD0 E00EE ...... F. . . . . FFFF ,,FF... . . .............................. HHHHH....................... "......, DDDDDDDDE . DDDDD0DDEECCC00 00 CCCC CC D D DDD0D CCDODDDD DD FIU EE EE FF . .............. F'FFFF. ............................................ HHH ................

... ..... ODODODDDD D EEEE DDDDDDDD CCCCCCC D 00DDDD CCC CDCDCDDDDDDDD - EEEE FFF C...............FFFFFFF............................................HH ... .................. DDDDDDDDDDE E000CCEEEEEE 00000000 CCCCCCCC DD DD D CCCCCCCCC C DDDDDDDDD EF FF. FFF ... ............ FFFF ........ . ... ............... ... .. HH........ . .............. .DDODDDDDDDDDDOD DDDD DDD EEEEEDDDDD D CCCCCCCCCC CCCCCCCCCCCCCCC DDDODD EF FF FFF FF G ............... . . ............................................ 4HHH.................. DDDDDDDDDODDDDDDDDD DDDDD EEEEEEEFE 0DDD00 CCCCCCCCCC CCCC CCCCC DDU n; FTF FFFF GG HH........................HHHHH.................................. DDDDDDDDDDDDDDDDDDDDDDDDDDE EEEEEEFF DDDDDD CCCCCCCCC CCCCC CCCCCC 0DD FFF FFFFEEGDH . . . . .D......D.DHHHHH"C..._E D. 00.

.. . .+ . DDDD0DDDDDDDDDDDDDDDDDDDDD EE EEE 0DDDDDD CCCCCC CCC+CCCCCC DDD 7F FFFF GG H. ... ........................................................ ...1HHHHH G F' E 0D C0..... DD DDDDDDDDDDD DDDDDDDD DDDEE EEEEEEEEEE DDDD0CCCC CCCCCCCCC 0DDD ET 77FFFF GGG ..... ...................H' 0............C...........................HHHH GG F E D CC

.... DDD 0DDDDDD0 DD0 DDDDDDD D EEEEE.EEE DDDDDD000 CCCCCCC 0DEDD EEF 7FFFFF GGG .. .................................................................. 1HH4 4 G F EE.D CC. DDD 0D0DDDDDDD000DD DDDDDDDD0 EEEEFEEFFE DDD0DCCC0DDDD EEEEEEF FFFF FFF FF GGGGGG............................................... ...... ..... TT1 1 HHH G F E D C B

..... DDDDD DDDDDDDDDDDDDDDDDD D O EEEEFEFF'7 D 00000D0DDC D00) F' EEFFFIFEE FFFF7 GGGGGG.................................................................. III HHH G F E D C BA,."., ..... EE DDDDDDDDDDDDDDDDD DDDDDD EEEEEEEEFEE DDDDDD0DDDDDD DDDDDD EEEEEEFEEEE FFFF GGGGG ( GG .. ...................".............."................. . .ITi TIII HHH G F E D C BB...... EEEE DDDDDDDDDDDD000D EEEEJ 000000000 00000DD0DDDDDD0D0DDDD0DD FEFFFEEFEEFF FFFF GGGG.GG .............. . . .ITIIIIITTI H141 GG F E D C B A

......... E EE DDDD 0DDDDDDDDDDD DDD E.E 0000 0 00DDDDD 0DDDDDD EE FEEEEEE E FFF GGGGGGG ................................................... 7TTIIII 41 HHH GG 7 0 C B B A....EEEEE D0DD00DD0DDD0DDD D00000 00DDDD0 DDDDDD DDD D DD EE7EEEE FFF G GGG.GG .................................................... III IT HHHH G F' K D CC B A

... EEEE ODD DDDDDDDDDDDD 00 E 0DDD0000 00000000 D EE F E FFF7 GGGGGGG. ............. . . ......... ........ 1111 HHHH GGG F 0 CC B A...... EEEE 0DDDDDDDDDDDDDD 0 FEEEDUD 0000 E000000000 E EE FF GGGGC ...................... 1444 GGGG F K 0 C BR A

. . EEEE DDDDD00 0 0 EE 000000 00000DDD0D00 EKE FFE FF' G1GGGG 4 4................. ............... . .. HHHH GGG ......... EEEEEEE D 00DD DDD D00000 E 0000000 00DDDDDDD FEEE F FFF GGGGGGGGGG HHH. . . . .......................................... . . H HH GG FGFF......

.... F F EFEEEEF DDD0DDDDD D 00000000 D DDDDDDDDD)0 EEEEE FF7F G CGGGGGGH..................................................1 4 0 GG. . .

....K.......E DEEEEEEF DDDDDDDDD DDDD0D0DD0D DDDDD00D DDDDDDD D0D00DD0 0 DDD0DDFFEE FEE FFF 0G0GGGG . ................................................. 1 GG G FF .................77F KEE0.......00FF0 E0DD DDDDD0 DD0D0 DD0 DD 0DDD0DD0DDDDDDDDDDD EEEEEE FF77 C CGGG NG ................................................... 7 H GG FF E. ..... . . . FF F F E E E E E E D D D DDD D D D D D O D n o nD D D D D D D D D D D D D D D D D D D D D DD D oF F EE E E F F F F G GGG G G . . . . . . . . . . . . .F.. . . . . . . . . . . . . . . . . . . . .. FF FGF FE E 0-. . . . . . . .........D 0 D D D D D D O D D p D D D ~ O D DF F E E .F F FG f C r...''F''...........000.0.0................0.00000000007FFHFEEC 7F' 00ee:.. . ... ... ... .IIH.:F':::0. ..

..... FFFFFFFFFF FF EEE DID 0DDD0 DD D00DD DD DD00 00 DD0 DDDD0DDDD FFEEEE E FF77 F7 EEE FFFF GGGGGGGG. H... .HHH. ..H.. ................................. F I GC F FE 0[...... .. ...... " ... F FFFFFFFFFF EEEE DD0 0DD D D0D0DDDDDDDD0 DD0DDDDDDD FEEFEEE EE 7F'FFFFFF E E FFFF CGGGGGG 41H41H1HHH4 . ............................... . 1. 1 G F EE 0 .....

.FFFFFFFFF EEE 0D 0000DDDD D DDD0000DDDDDDDDDDD 0 FFEFEEEE FFFFFFFFF EE FFFFF CGGGGG HHH4HHHHHHH......................................1H G F EE DD .......

...... FFFFFF 0E DDI00000DDDDDD DD0DDDDDD DD0DDDDDDD DO EEE E FFFFFFFFF' FE FFFFF 1GGGGG1HHHHHHHHH ...................................... H G F E DD .... .......G.G. FFFF EEE DD DDDDDD DDKDD0000 DD00000000000 EEEEEE FFFFFFFFFFF E FFFFFFF GGGG HHHHHHH ........ ............................. G FF EE DD C.. ..... ..

. ..... GGGGG FFFF EEE DD0DDDDDD CC D0DD ODODDODDoDOD FEEEFEEE FFFFFFFFFFFF E FFFFFFF 1GGG HHHHHHHHH.....................................C . F EE DD C....... .... .G GGGG FFFF EE DO C DDDDDDD CCC D00 000DD 0DD000 F'F'FFF'EE FFFFF FFFFFFFFF E FFDFFFF. . . .C.14HH14............ .. 0EFF E 00E CC . . . . ...

.GGG _FFFF EKE 0DDD C DDDDD CCC 000DDDDD EEFE FFFFFFFFFFFFFFFF FF77..........14.........00 EEE EEKE 000 C......FFF E DD CC 0000FFFFFFFFFFFFFFCC 0FFFFFFF~.............HH........................ 00000 F FF EE00O CC. .....

.."FF EKE 000 CC 0000 CC DD0 EEEEEEE 77EEE DE FCC DFFFFF FFFFFFFFF' FFFFFF FFFF . ....... 0.G ....................... .00000 D D0 CCCCCC................... F'FFFEF KEEE DD CC DDD CC 0D EE FEEEEEEEE FFFF'F FFFFFFFFFFFFFFFFF F FFFF...... .. GG.........CCCCCCC CCCCCCCCC... FFFFFF EEE DD CC D CC D00 EEEEEFEEEEFEEEEEE FEEEEF F F FFFFFFFF FFFFFFFFFFF F...............GGG.. ..... .. . ...... CCC.......,

.. FFFFFFFF EEEE DOD CCC C 0000 F'CODEE FFE EEFFEF'KE E 'EFEF FFFFFFFFFFFFFFFFFFFFFFFFFFF GG 0 . ............. 0GGG 1 HF.H.. G. 7 F E0 CC CBCCCBRC ................

.. FFFFFF'F EKE DDDD C CCC 0 D000 FEEFFFEEK FFEEFFEEEEE E EEE FFFFFFFFFFFFFFFFFFFFFF'FFF C ............. 1GGG1H1HH1 G F 0 D CC B'.RBBRB. ......... FFFFFF EEE 000000 CCCCCCC 00 0D000 7EFEEFF F 'EE E 'EEE 'EEEEE F'FF.'F.EEE FFFFFFFFFFFFFFFFFFFFFFFFFFF GGG .......... 1GGG1H G F E CC BB FB8F1BBB BB8BBBB ......

.. FFFFF F EEE 00000 CCCCCCCCC 000 DDDDD00 EFEFEE EEFEEE FEEEE FFFFFFFFFFFFFFFFFFFFFFFFFFFF GGGGGGG............... GGG HH 0 7G F E CC BB D D CC1RBR4BBBRB BB"B",BBB ........FFFFF EEE 00000 CCCCCCCCCC 0D00 DDDDDD00 FEFEFF.F FFFF E FF E FFFFFFFFFFFFFFFFFFFFFFFFFFFF GGGGGGG...............F GGG G F' K D CC BBBRBBBRBBBBRBBBBB ................

.FFFF EEE 000DD0 CCCCCCCCCCC 0DDDDDD DDDDD0DD000 EFFEEFFE EEFEEE EFEE FFFFFFFFFFFFFFFFFFFFFFFFFFFF GGGfGGGGG...............F GGG C F E D CCC BBRRBB8 BRRBBBBBBB ..... ... . .

....... FF EEEE 00000DDD + CCCCCCCCCCC 000000000. +... EEKEK.+.'EEEEE EE E + FEEE EE FFFFFFFFFFFFFF +FFFFFFFFF G GGGGG............+..F GGG GG F' F D+ CC BBRRRR RHRRB ........... +...........EEEEE 000DDDD CCCCCCCCCCC DDDDD ...... F EGEGGGGEEEGFEE 777FF'FFFG..7 0 F 00 CC FRRRB ...........

E...EEEEEE DDDDD0 CCCCCCCCCCC........... EE FF. FEEE. EEEFFF F 77777 G....C....77 0000000 GGGGGGG77 FE 00 CCC B BBB.........E.EEEE DD 0DDDDD CCCCCCCCC ......... 0 FFEEEEKEE EEEE FFFFFF CGG.. ............ F GGGGGGGGGGGGGGGGGG FF FF. DD CCC BR..........".... ......

00000 DDDDDDD CCCCCCC ............... 000 EEFEEE FFFFF GGG, ............ 7 GGGGGC 7GGGGGG7GGG FFF FE 00 CC PR ....................0..0DDDDD C .............. DDDDD FF EEFF FFEEFEE 777FFFFF GGG............G.....FF' C COCOOCOCCOCOC000 FFF'E 0DO CC 8

...... DDDD DDDDDDD .......... .. ......... FFFFFE EEF:FEEFE EE FFFF CGGGGGGG FFFFFFF GGGGGGGGGGGGGGGGG FFF EE D0 CC R ......................... D0DD DDDDDDD ...... 00. ...... ........FEEEEE FEEEEEFF EFEE FF77 00000000 F7F7777 CCCCOOOCO0000 77 EE 00 CC B..............

.0 0 0DDDDDD CCCCC.......................DD0DD EEEFEEEE EEEEEEEFFF FG:7FF CGGGGGGGG FFFFFFF GGGGGGGGGGG FFFFF E D CCC B. .. .DDDDDD CCCCCCCCCCCCC.......................DDDDDDD FFFFFFKE EEEEEEEEE F'FF'F FFFF GGGGGGGG FFFFFFF GGGGGGGGG FFFFF EE D CCC .......................

.. 0.0DDDDDD CCCCCCCCCCCCCCCCCC............ .. . 0DDDD0 0DD000DDD F'FEEFFFFE EEFFEEE FFF F00E FFFF GGG7GGGGGGG FFFFFFFG GGGG G FFFF' E 00 CCC.......,...............0...0DDDDDD CCCCCCCCCCCCCCCCCCCC. . ................... .. DDDODD DDD DD D EEEEFEEFEE FEEEEEFEFFFFEEEE FFF GGGGGG0 FFFFFF' GG0 G FFFF FE D CCC 888.... .........

,... 0DDDDD CCCCCCCCCCCCCCCCCCCCC D....................DDDDI DDDD 0 DD000 DD EFGFF F'FF DFCCFCC .............. FFFF............GO.....FFFF777 E KC0o CCCC:.0 .... 0DD CCCCCCCCCCCCCCCCCCCCCC DD........ .00.00.0..000.........F.

.0..0000F CCCCCCCCCCCCCCCCCCCCCCC 0....... 00 FE FE EF FFFFFFFFFFFFF GGG0 G GGGG FFFF EEEE DD CCCC .............................................. 0 DDDDD CCCCCCCCCCCCCCCCCCCCC DDD...................... 0DDD0D0DDD0 0 EEFFEEEEEEEEEFEE FFFFFFFFFFFFFFF G0GGG0G GGGG 0FFF FEE DD CCC ..................................... ... DD 00000 CCCCCCCC CCCCCC DDDD ..................... lOOnDDDD FFF FFEEEE EE FFFFF FFFFF 0GGGG GGGGGG FFFF 0077 DDDD CCCC00 C

.. ..... D0 (CC(CCCC CCCCCC 0 ..................... n000000007DDD FFF FFEEFEEEE FFFF FFFF GGGG GGGGGG FFF E 0000 (CCCCC............ 0.D0DDDD000D CC CCC CCCCC 000 EEF.............. 00000D0D00 0 F.F7FFEFEEEFF FFFF GGG FFF 7GGG H GGGGG FFF E E , C....... .....

.0..............D DDDDD CCCCCC CCCCCC D EF.... ... D00000DDDD D00000000 FFEFFEFEEEE FFFF GGG FFF GGGG H GG7G FFFFFFFFFFF E D CCC..... .......00........0.00DDD 0 'CCCCC CCCCC DD FEE............... . oDD oDo oDDDoo DDDDofoD EFF'EFFFEFFFFF FFF CCG FF7 0000 00CC 777777777777 EEE 00 CCCC..... .. .

............... D0D 00000 CCCCC (CCCC 000 F'............. 000 00 0 EEE7EEEFFFFF GGGG000 77 GGGG GGGG 77777777F777 EEE 000 CCC'C(CC..... ........

...... . ... DDD DDDDD CCCCC CCCCC DDD E............... DDDDDDDoooD DDD EEEEEEFE EE F 7 FF GGGG FFFF GGGG GGGG FFFFFF00FFFF EFEE DD0 CCCCCCC.......... DDD C7DDDDD CCCCC CCCCC DD ............... C DD000DDD0D 0 D EEFEE EE F GGG 77 G G G F 7 7 F 00 CCCC

.00000000DDD FEEEEEEEEEEE FF 0GG FFFF GGGG GG7G FFF EFEEFEE DD C 0......... ............... 0.....D0DD O (D'DDD (CCCCC CCCCCC D000....................................D D7EEEEEEE7EEE0FE FFF GG FFFF GGGG7GG FFFFF 7.. 0 .DDC..."..........

000........0D0DD0DDD CCCCCCCC CCCCCCCC DD0 ...................................... 0 000 E7EFEEEEEEEEEE F FF7F77FFFFF7F7F777.F7. C 77. EE D0 0000.".........DDDD DDDDDDD CCCCCCCCCCCCCCCCCCCCCCDCCC DDD0 ........................... CC 00 FF.E 7EEEEEFEEEFEFEF F777FFFFFFFF G FFF EEE F0 FDA.................

0........DDDDD0DDDDDDD CCCCCCCCCCCCCCCCCCCCCCCCC 0DD00................. ... 0C 00D7DD E EEEEEEFFFFF EF FFFF FFFFF F FFFFEF OE 00 ('CC('CC'CCC.('..................000.....D 00DD D0D0D CCCCCCCCCCCCCCCCCCCCCCCCCCCC .,...,... ............. .......... . .C. 0D0 EEF7 77777777FE77F77FFFFFF F FFF PEF DD CCCCCCCCCCC0.....0DDDDDDDDDDD CCCCCCCCCCCCCCCCCCCCCCCCCCCCC DDDDD0 .. ............................ CFCC D 0 FEE EEFE.77 EEFE 7FF7F77F7 FF E 00 CC

.....D000000000DDDD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCC 0DD 00 .......................... . B CCC 0DD E EEEEFF 01)000E0FFFFFFFFF 7F 01 CC..................000"."...D0000000DDD0 CCCCCCCCCCCCCCCCCCCCCCCCCCCCCC'C DOODDD........... . 8 CCC D0D EEEEFFFFF 0 F.FDD FF 77 FFFFFFFFFF DO CC 14R4..F.4818..............

0000D00DDDDDDDDDDD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC 0DDD000 .............................. 88 CCC DD V EEFFEFFFE FFFFFFFIF DD7C7..FF7,,000 CC 14H814.......B,...... 00DDDDD0 DDD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC DDDD . ..... ........ 88 CCC 00 EEEEEEEFF77 DDD00DO00 FEFF F 71FFF 0+l D CC B44 BBRB . .+. . . . . . . . .+. .+.. .. . .... .. D D DDD0 00 CCCCCCCCC+CCCCCCCCCCCCCCCCCCCCCCCC DOD + .. .........................+..89 CCC C DD E EE EEE D DD +DD D 6 FE F F 0Dn CCC OB R RR BRR ........ ..................... ........... +. . . . .

.... 0DDDDD00DD CC'CCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCC 00 .................... 0...........C777 D777 0D( 41111444~4.................DDFFFF FEEFD CRRB~s.""C0000000000 CCCCCCCCCCCCCCCCCCCCCCCCCCC CCCC CC D....................... .CC.000.......00.CCCE7F77F77 000..C........ D84E14EE.F. .E. ..CC. . . . . . .

.0000000 CCCCCCCCCCCCCCCCC ('CCC('C 0 .............. 'C010)F77F7'7 00C 8144441..................... C -...... DDEREEEF D CBARRM... CCCCCC(CC CCCCCCC 0..........C 0000 F.7FFF DD 0 CC 14B144411R41 ..................... " "..

.. CCCCCCCC ('('CCCCC 0 ......... .. B C.......CCCC 0000 7 100 CC 1414 31 ..CCC CCCCC 0n ........................... +.........0DD FC. . ... .... CCCCCC .C FF FFF AD CC B RRR .

CCC CCCCCCCCCC CC CCC D .. .............................. C B D ............... CCCCCC(C('C P F) 0000 CC 11.CCCC8 .... C C'C TCCCC8CCC D".C.......................... n. ............. CCCFF CCC. F'Dn CC 0..CCCCCCCCCC CCC C............................. ............. DCCCCCCCCC D 'C . ...............

CCCCCCCCC ('CCC CC............................. ............... CCCCCCC 0000 CC FR. ...................

CCCCCCCCCCCCCCC( (CC.............................B A A...............UCCCCCCC 0001000 1 0DDD CCCC(' . . . . . . . . ..............CCCCCC.CCCCCCC CC B CBCBCBBC CC CC.........AAAAAAAA.. .... (CCCCC 0001,01)1)0 CCCC(' .. . C C CB148884BB CC CC. . . . . . ............................... CC C. .onpopoD,.p. . ... CCC..C

....... CCCCCCCCCCCCCCCCCCCCCC CCCB8 B C CCC CC.............................. .. ............ . . . .......... 00001001(000 n CCC . ............. CC8CCCCC88C8CC. (C('C ........................................... 0C.............

....... CC C CCCCCCC C8.............. ... -.... ............ .............................

.CCCCCCCCC CCCCCC 88 CC... C'...CCC..........---.---.-----..........................0000 000Dn DDDCCC....... " CCCC CCCC CCCCCCC CCCC.84888 (CCC . ....................................... , ...000) 0DD CCC A

.CCCCCCCC CCCCCCC [.F.B..... ...CC . ........................-. 0...-.......................DD DDC ....CCCCCCCC C CCCCCCC 888888 8 C CCC. .......................................... ..... ... . .....C0CC 000 CC 144. . . . . . . . . ......

.. .CCCCCCCCC C CC CBeRBBRR CCCCC ....................... ................. ....... P) 0DDD n c( 1r14. . . . . . . . . . . . . . . . . . . . . . . ..C B8814B888BB CCC'. .................................. 000. 00 CCC ....

...... "..CCCCC [CCC CCCCCCCCCCCC 88884R148188 CCCCCCCC..................................................... . . . . . ) CC . . . . . ................. .... CCCCCCCC C(CCC CCC 8CCCCCCC88C4CC88F8 (CCCCCC.......................... ))nn P. . CCC 1414........................

........ CCCCCCC CCCCC CCC CCCCCC........................-.-.............................................................. CCCCCC CCCCCCC CCCCCC. ............................................................ 00 CC .. . .....................

.. .. CCCC C1414888 C .. .................................................................. CC............................................... CCCCCC -RRRR CCCC CC 8148 8888888 ..............--.....---.-.-- -- ............................ 0 CC.................

...... .CCCCCCCC CCCC CC . . . . ............. ........... .. - . . ......................... ........ .. n'C n"...-.... .................. ............... . ..................................... . . .. C CC CCC C CCCCC CC C81 88 81RBRR 48 CCC888 . . . ................................................................... . . CC 1 ........... . ... .. .. ......... . .. .. .. .... . .. .............. . . . . . .

....... ... .. ... CCC .CC .CC. . CCC C......... ......... ............... . . . . . . . . . . . . . . . . ... .. ..........................................................................

....... .. . . . . . . . . . . . .... CCCCCC. . . . ... ... RR..................... ...- ...........-....................... ..... ... .. ... .. ... .. ....................................................................... .

.CCCCCC".C......148148811C8......................... ....00 C HH................................................

..................... ..CCCCCCC........R. ......................................................................... ..... ............... .............................. .............................

.. . . . + . . . . . . . ................. +..CCCCCCCC.... .... ... .... ... R R CC C.............. ............. +....---...........-..............+..............-- ... n .... .... -+ . ....-....---................ ................................. ........... . . . . . . . . . . . . . . ..............CCCCCCC CCCCC.... .... ... -... ... RR cRrR C.........-............----------------.-... -----. -----.-. ............. ... .... .-.. ..- C ...........--.. ......... ..........................................................

..... .. C.. .... ..... ... C..... .. H....-. .CCCH C.. .. .C.. .. . .CC.C R B .. . ..................------- ... - -- - . ............................ ..... ...... ......................... ............................ ................ ............ ..CC('CC .. .. CCCCC114. ..................... "... ......... ".... . . . . . . . . . . . . . . ..CC..CCCCCCCCCCCC.. ... .1488848... ... ... .. ... ... ... .. ..................................................

0G001ATA INTFRNFATIPF.A., INC.0'FLAS. 170XA0

14< 1.0 2.0<14< 3.0 4.0<C< 11.1 6.0<0< 7.0 14.0<F< 9.0 10.0<7< 11.0

17.11<0< l3.0 14.0<4< FS.0 114.1<1< 17.0 114.0<.J< 10.0 20.0<7< 21.0

22.0<F0< 23.0 7h.0<"< 7%.0 )F,.0<+< 27.0

C 01 1 ))sh "T j= 1.)' .1 8,l , W o( 314.('100 1,W -76.UO0

. .......... D ......... .... D CCC C .n............... E D 0CCCCCCC ............................................................ .. ..... 0 0 0. ... . . . . . . . . . . . . . . . ....DDU CCC DD .. . . . . .... E CC0CCCCCCr.. .... ..... ............... . . . . .. . ........................... " " " . . -.n ................ .................... ....................... ................

0E00......* E:E 0U CCCC . . . ..* .,. . C u .................... .D D ...... C. . . .. .. . ...............

. E D . .- . . .. ..... .....".C ."". .."... ..E.. 0DO F.)EE ....... . . . . . . . . . . . . . . . . . . . . .......................................... . .................................... .. .. C ... .................

.. .......... EE ............................ .. )1n ,tt)) CCCCCCCCCCCCCCCCCCCCCCCCCCCCCC 1)0DII)D00D CCCCCEEEEEEEE E FF F FFE FFFFF E EEE 00)) CCC 00 (F F . . . . . . . i 'l1i01 ."-10 1CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC IIp)D U ruUD CCCCC........E.EEE FFFF FFFFF FFFFF EE 0D CCCC DD0 FE F ... 'ID'Lnn CCCCCCCCCCCCCcCCCCcCCCCCCCCCC 0'lCO0 00000 CCCCCC.

.................... EEEEE FFFFFFFFFFF F F FFF LEE DDU CCCCC DD EI F .............................. bi0nronLLU CCc cccccCCCCC CCCCCCCCCCCCCCCrCC DDDDGnDDDDD CCCCCCC........

...................... EEEE FFFF GG GG FF FE DD CC CC 00 F F ............................. . 1~+nI. II[ C(CCCCCCCCCCCCCCCCCCCCCCC CCCCC OOI) 00000.0 CC.CCCCCCCCC........EEEE EF GGGG GGGG FF FE D C CC DD F ............ 100011) I CCCCCCCCCCccCCCCCCCCC CCC 0)f)00IV00)00I I CCCCCCCCCCCCCCCC CCCCCCCCC..

..... 0....0055 EEE FF GGGGG CGGGG FEFEE 0 CC CCC 00 E F GGO. FEF EEEF: FF ((EE iCH:) 101. CCCCCCCCCCCCCCCCCCCCCC CCCC r'001)00001001)I)0D CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC ECCECECE,0 EEE FFG GGGGG FF EE D0 CC CC D F F GGUG FFFF :.EU IEEF ('I nD, l CCCCCCCCCCCCCCCCCCCCCC CCC 0')on 0DP0 0000 CCCCCCCCCCCCCCCCCCCC CCCCCCC C C C

.. E FFF GGGG GGGGG FF EE D C CCC 00 FE F GGCG FFFFE FEEFEFEF r>DOLICba CCCCCCCCC(CCCCCCC CCCCC CC nCC 000D0000 000D CCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC

DD EEEE FFF GGGGG GGGGG FF FE 00 CCCCC 0 F E F GGGG G FFF EEEFEF Oi) 0uOL CCCCCCCCCCCCCCCCCCCCC CCCC UD) D1)D CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC" .....F...) 0 EEE FFFFF GGGGG GGGGG FE FE DD CCCC DDEE F GGGGGGG FFF BEEFE EE 1000 En 11 CCCCCCCCCCCCCCCCCCCCCC C CCC 00DD 0 01)01)01 CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC

F...EE FFFFFFFF GGGG GCGGG FE EE 0 CCC 00F EF G GGGGGG FF EEEEEE 0000)U) CCCCCCCCCCC CCCCICCCC H CH CCC 00LD'o 0D0 CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC. . EEE FFFFFFFFF FFFF FE DO 0000 FE F FFF E(FEEFEE I)O flb CCCCCCCCCCCCCCCCCCCCCCCC CCC 0)00001 D0FD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC

.EnEFEE FFFFFFFFF FEE 00000 EVE FFFFFF EEEEE DDDD)0' l CCCCCCCCCCCCCCCCCCCCCCCCCCCC NtCCC C 010 D0 D1D1CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCEEEEEE EEEEEEEEFEEEEFEEEEEEE F FEE EE EEEEE CCCCCCCCCCCCCCCCCCCCCCCCCC C CCCCCC 1 ) CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCC

.... ........ EE EEEE E EEEEE 00000 EEEE FFFE EEEEEE 10)00 FEE FF F Ek DD D CCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCC CCCCCCCCC CODCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCC.EEEEEEEEEEF EEEEEE 000000 00 FE FFFFF E EEE 0 CC C 00 FFEE E FF 0000)0000U UCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC C CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCC

. .. EEEEEEEEEEEE 0000 CCCCC C 0D EE FF FF EE 0 C A CC 0 ' EF EF :flOUD)n0t bCCI CCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCC............... E E E E E EEEEEE E D DD CCCCCC CCD EE FFFFFFFFFFPEE n CC C CDEEDDODCCCCCCCCCCCCC CC CCCCCCCCC C CCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCC CCCC

............ EE EFEFEEEEEE DD0 CCCCCCC CC D EE FF FFF EE 0 CC R X C 0))DD 00000 11CCCCCCCCCCCCCCCC CCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCC CCC

...... . . . FE EEEEEE DDDD CCCCCCCCC 0 FEEF G G G FF EE 0 CC BHB CC 0)1) t)) 1)1) CCCCcC.CC CCCCC CCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCCCCCC. . E EEEF D000 CCCCCCC CDD FE FF CGGGGFEF E 0CC BH NCC 0)01)OiD CCC CCOCCCCCCCCCCC1CCCCCCCC CCCCCCCCCCC

....... .EEE 0D 00 FE FF GGGGGG G FFE F 0 C CCC 000111)00 CCCCC CCCC CCCC CCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCCC.EEE 000 D10 FE FE GGG GGGGGCG F 0 C A CCCC 11000) CCCCCCCCCCC '1 CCC C A CCCCC CCCCCCCCCC CCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCCC

E..,........ EE CCCCCCC 00 F FF CCGGGGG GG F E D CC CCCC DD CCCCCCCCCCCCC DOL CC ( $ CCCCC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCCCC... EEEE DD D0D E F GGGG GGC F FE D CC CCCC 0) CCCCCCCCCCCC ) CCC HA CCCC CCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCCCCCC

.EEEE DD C0 C + FDD E F G H GG+FF F 0D CC CCCCC I))) +CCCCCCCCCC C 00 CCC BoA (CC C +CCCCCCCCCCCCCCCCC + CCCCCCCCC +.. .... . F EEE 0 0 DD FE F G HAHHHH GG F E DD CC CCCCC Ol CCCCCCCCC C D CCC CCCC+ CCCC C

.......... 0...E EEEE DDEE G HEHHHFH HHH GG F FE D CCC CCCCCCC 0 CCCCCC CCC b CCCC CCCFE EEEEE 0DD0D D EEF GG HH HHHH GC F E D CCCC CCCCCCC CCCC C CCCC 0000000 CCCC

... .. .. FFE EEEEEEE D E FF GG FHH H1i HHH GG F FE D CCCCCCCCCCCC C CCC CCCC Cooooool o10 1)D000 CCCCC. FF EE EEE DDD EE F G H HHHH GGG F F 00 CCCCCCCCCCCCCC 1 CCC CCCC D DDDOO O DDO) 000 O DDDDI 0CCCCC

... . EEEEEEEEE D EEE FF GG HHHHHHHH GGG F FE CCCCCCCCCCCCCCC CCC CCCC D0000I)D0I )01)) 00DD0D0D D0Dl)0000 D CCCC

.. E DEEEEEEEEEFE H EE FE CC GG FE D CC CCCCCC D CCCC CCCCC 1DDO'on00000 l 0DDD DDD0D 0000ID)00D0DD CCCC..... .EEE EFEE D FEE FE GGGGGGGGG FEEF 0 C CCCCCC CCCC CCCCC 00D0DD0000 D0 D D00011D DDDODDDDDODUOODDDDDDC0DD CCC

............... EEEE EEEE 00 FE FE FE FE 0 C C CCCCC O CCCCC CCCCC (:00l)DD DDDDDM DODDDDDDDDDD000000DD0DD000D000D0I0D00D0C CC....... ...... EEEE EEE DD00000 FE FFFFFEGF FEE 00 C AHACA CCCCC 0U CCCCC CCCCCC DDIIDnDO)DDD0 000000) 0 0D0000 D DDDDDDD00000 000DD0DD DDDDD C

.. EEEEE EEEE 00 D0DD0DD FEDDDD FE F FEE D C RB BA CCCC CCCCCCC CCCCCCCCCC 00DDDDD00 DD DDDD D D 0DIDoDODDODDDDODDDDDODD DDODDDDO D.. ..

. .. .. F. EEEE D000DD0DD0E00F00F00 0 E FEEE D CC BBBBAB CCCCCC CCCCCCCCCCCCCCCCCCCCC 0DDDDn000D0 0ODDDODDDDODD ODDO .... 0...00.0... 00."E E EE DD DD E000 FEE FEEE 00 CC ANBBBB B CCCCCC CCCCCCCCCCCCCCCCCCC CC 0 0000000 )00DO 0 DDDD D.....

000000DDDD0 CCCCCCCCCCCCC DD EEEE EE E DD CC BBNAB CCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCC(C 00001 )00 )DDD 00DDD0......00000000000 CCC CCCC 000 EEEEEEE DOD CCC NBF88 CCCCCCCC CCCCCCCCCC"CC CCCCCCCCCC 00000 EEEEEEEEE lDD0DD.....

. DDD000 CCCC BC CCC D D DD CCC ABABBN CCCCCCCCC CCCCCCCCCCCCCCC CCCCCCC 0000E00D DE EEE EE DD0DDD............... D CCC B RABADB B CCC DD 0DDD CCC BBBA BA C CCCCCCCC CCCCCCCCCCCCCC CCCCCC DDDDDEEEEEEEEE EEE E DDD.. ..

. .. .. .CCCC B BB CCC DD0 DD CCC ABBBRBAB CCCCCCCC CCCCCCCCCCCCCC CCCC D1D)0D1 FEEEEFEEE EFEEF 01)0.00.

.CCCCCCCCCCC BBBBBBBB CCC D0 DD CCCC BBBBBBAB C CCCCCCCCC CCCCCCCCCCCCCC C C 000D 0 EnEEEE EEEEE 00D000 ............ CCCCCCCCCCCCCCCC BBBBBBBBB CCCC DDDD DD CCCC BBBBRBB CCCCCCCCC CCCCCCCCCCCCC C100DD01) FEEEE EFEE 0DDDDCCCB.......... CCCCCCCCCCCCCCC BBB BBB8B CC DDDDDDDD CCC BBBBBBB CCCCCCCCC CCCCCCCCCCCC 0 00000 FEFFEE EEEE DD00000 ........

.CCCC CCCCC BBBBBBBB CC DDDDD D0D CCC BNBBHBBB CCCCCCCCC CCCCCCCCCCCC 0DD 000000 hFE EEEEE U 00000.00 .......... BBBBBBBBB CC DDDDDDDD CCC BBNBBBH CCCCCCCCCCCCCCCCCC 0 ) )0DDD 0DD FEFE FEEEE 0..............

. ... BB BBB AB C CC 0DDDD DDD[0 CCCC B CCBBAB CCCCCCCC D DDD0000D) DDD ID)DI EF FEE FEEEEE 1)............... BBBBBBBBBBBC CCCC DDD DD CCCC A CCCCCCCDCOC 00)0DD 0DDD ))0000D00I)ID)00DDDD0DD D (FFFEE EEE EE 00.....

...... ..... BBB CCCCCC DDD DDD CCCC CCCCCCCC 000 0000001UDU000001)00D0D0DD 0000D0DD 1000 D OFFF)EEE.F FEEFEE 00 ... . ...... ,....... A BBS CCCCCCC 0000 0000 CCCCC CCCCCCCCC 011DDDD0D0)u IPl)00l100000000000D),IDl)101101)0D0D00) 1FE(EEFEEFF F FEFEE 01).........

.AAAAAAAAA BBB CCCCC DD0D E DDD CCCCC CCCCCCCCC D01 DD)0D)I DD) 01DD)0I)) 0l)I))DD)Dl0D0I OID)00D0DID) 0 FEEEEEFEEEEEEEEEEEEE 0DD.............. AAAAAAAAA BB CCCC DDDDD EEEF DD CCCC CCCCCCCCC DDb DP0D0nu 1 00n'0o)10) I100DD0)))D I0D 00D 0 DDD FFFFEFFFFFEEEEFEEEEE D0DD................

.... AAAAAAAA BBBB CCCC DDDDD EEEEEEEF DD0 CCCC CCCCCCCCC D UIDDDDDO DDD UUUO 0 0D0J 0 iDnDl0D)DDD )0EE000......1)0000000EFFEF EFEEFFEFFFF F 001)0 ...... ,.

BB CCCC DDDDD EEEEFEEF:EEEE DD CCC CCCCCCCC FDDDDDODDU0DD0DUD0D DDnD01000) 00)I11 )DD D D0D0DD 0 (FF(F:FEEFEFFEF.EEEEEE D000D................

... .BSS CCCCC DDDDD EEEEEEEEEEEFFE D CC CCCCCCCCC ')I)000D00I) 00000 IUD 11D)0DDJD00 :EEEEEE EEEFEEEEEEFE D00).........BBBB CCCCC DDDD EEEEEEE EEFEEE DD C CCCCCCCC 1DUODDD1011D00 00U)' U) D UUOD EEEEF:FFEEEEFFFEEFEEF 000....... ....

..... ... BBBBBBBBBBBB CCCCC DDD EEEEEE EEEEEE D C CCCCCCCCC 0001)0 10000 1'))0I)000DDD ) F(EEE FFEEEEEEFEFEEEEE DD0.. . . ............... .CCCCCCCCC +DDD EEE E EEEEEEE 0 C + CCCCCCCC +D0DDDD U 0000 + 01I) WJO DDn0 + EEFEEFEE+EFFFEEEEF EEEEEEE ... .. +.......

CCCCCCCCCCCCC DDDD EEEE D CC CCCCCCCC 1D)D DDDD )DD)D0EE EEEEEEE0E EEEEEEEEE EEEEEE...F..F..F..F..E.F.E.EFEDD CCCCCCCCCCCC 000000DDDD CC CCCCCC DDDDDDDD 00000011UU)U1)000 0 0D0J tEEEEEEEEEEEEEEEEEE EFFFFEEEEE FF.E 0................

FFF EE DD CC CC(CCCC DODODDDDDDDDDDD C C C CCCCCC DDD D)00 0UL ))100)00) 1))01DDD) Dl EFEEEEEEEEF . FEEEE FEEEEF.EEEE EEEEEEEEEEEEE DDD................... .. GGG F E D CC CCCC CCCC CCCCC D~bID)0D0 0 )I1I'00p1pn D01D1D)0D10001))D F:FEEEEEEFFEEFEFEEEEEEE EEEEEEEEE DD .......

......... G HHHH GC F E 0 C B9 BBB0 CCCCCCCCCCCCCCCCCCCCCCC CCCCC 00000000 1)UDD0t-l)OC DUr0 000 1 DD D EF(FFFFFF:FEF :EEEF EE EE EEFFEEEE DDDD.......................HH III H G F E D C BBBBBRBBBB CCCCCCCCCCCCCCCCCCCC CCCCC D D0000000L 0U1ODPU l)I 00 ) DD E0EE00EFFF FFFFEEEEEFFF EEFFEE D0DD .......................

. . . . IIIIIII H G F E DD C BBBBBBBBBBB CCCCCCCCCCCCCCCCCCC CCCCC 0D0D0DD E 0lID00DD 00DD10DU O00DDD0 FEEEEEEEEEEEEEEEEFEE;DFDFFF:D0D0 ................... .... I H G F E 0 C BBBRH B C CCCCCCCCCCCCCCCC CCCC D01)0000D FE 0DD DD00DD0 DD000D EEF (EEEEEEEEEEEEFF EFFEEE DODDD. .......

.. JJJJ I HG F EE D C BBBBBBB8 CCCCCCCCCCCCCCC CCCC DDODDD0E EEEE 1D)1 0D UU0DD0EEEEE01)FEFFFEEFFFFEEFEEE EFFFE 00)0000 .. ... . ..JJJJ I H G F E D C BBBAHAB8 CCCCCCCCCCCCC CCCC 001)0000 FEEF nOrrDDUDUUUUI )DDD0 EFEFFFEEFEFE EEEEE 00000000 .. .... . .

........... .... KKK JJ I H G FP E 0 CC BBB9B8 CCCCCCCCCCCC CC CCCC 01)000) EFEEE UnDhDpDuCD O EFFFEEEFEEEE F EEEF 0000001) ... .. . . ... ..KKK JJ I H G F E D C BBB8 CCCCCCCCCCCCCCCC CCCCCCCCCCCCCCCC )DDDD EO (F E 00D 0D0D1DD EFEFEEFEEFE FEEE 000.............................

.. . II H G F EE D CC CCCCCCCCC CCCCCCCCCCC CCCCCCCCCCCCCCCCCC npOOJU FF EE E 0101)1 EEFF:FFEFFF E EFEEFEEF 0000. .................

I CE FEE DD CCCCCCCC CCCCCC CCCCCCCC CCCCCCCCCCCCCCCCCC 001)1) ( FF FF(EEFE'E-'EFF EEFFFEEE:EEEEEE 00)000............ . H GG FF EE DD CCCCCCCCCCC DDD0DD0 0 CCCCCCCCCCCCCCCCCCCCCCCC 00000 E FFFF :FFFEFE EEEEEFEEEE EE D1D)D0.........................

FF EEE D00 D00000000 DDDD CCCCCCCCCCC D01)0 . E F:FE F. E F( FEEFFF.FF EEE ODO DDnOD ......... .. ............ EEE DD000 00000000 DDD CCCCCCCCC D0)0 E FFEEFEEFF F FEFS.00EE D D0D 0DDD0 .............................

... EEEEE 0000000000 D0DDDDDDDDDD EEE 000 CCCCCCC CC 1FO0D FE F1 FE(FEFF FF FEEFFEEFE , )0000.................. .....,.0.0.0..00.000000000000000000D D FEE 0000 CCCCCCC CC 00 EE(EIEEF F EEEEEEE 100D............ ....

.......... D oDoDDo 0000000D EEEE DDDD CCCCCCCC CC 010000 F, FF(F:EFE EF FEEFEEE .01).0 .. 1)0,..................... DDODDDD D DDDDDDODODDDDDD EEEEE DDDD CCCCCC C unDODD O Et. EEF FFEF' EEEEEEEE DQ[DDDD;;;;................... . ..... ...... .. .. . DDDD OD DD DDDD DDDDDD EEFEF D0D CCCCC C))00001)0 FEFFEEFFFF'EF EEEF:EE 0)DDnDDD ....................................

000000, ODODDDDDDDDDOOOEEEE DDD CCCCC 10DD0I)00 1000 00N))0D)0 D F F.FEEFFFEEEE FE :EEF.E 0D0D)000D D00...... ................ ..... .... DD0D0 0DDDDD EEEEEEE ODD CCCCC 00DDnD)Dl DDD00 000 DD0IDh (Er FFE E EE EEE D ........... 0000.0..0.). ..............

. . .. E D D DDDD D0D DDDD DEEEEE 0DDD CCC D DO D n 1)IDD OODIDDD0 D00 D0DDD0 1 D lFEI;F FF EE EEEEEEEED 0D00................................................ EEEE D0 DDDDODDDDDDDDDDEE 00DDDD00 CCC no00U0 t 1,0bUUL1,01101)10010001. (1 ( FEEFEEEFE F E EEEEFFFEE 00).... . . .. . . ........ ...... EEEEE DD DDOD DD DDDDODDDDDDDDD 000000 CCC iODOI'0I' 0 FEE FEFEEEEF E F. F.E EEFFFEE 000............ .,............. . .....

EEE CODDDOD0D0DDD00DDDDD00D0IDDD0DDDDDDDDC CCCCCCl)CC0)CCC)LDi)DDDEF-FF EEFEEFEEEEE 00 . . ...............

."F EEE 00001 DD0 DDDDDDDDDDDDDDDDDDD0DD00.DD C C CCCCCCCCCCCCCCCC DD. . DD: .00) . ......... ......... ., F EEFEEE DDD0D0D0DDDDDDDDDDDDDCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCDOOOOVOOOO 01)1..................

FFF EEE D 00DDDDDDDDDDD 0CDDDDDDD CC CCCCCCCCCCCCCCC CCCCCCCCCCCCCCCC 01D0)D10 1)0F))................ FF FEE D0DD0DD0DDDD0D0DD0 D (CCCC CCCCCCCCCCCC CCCCCCCCCCCCCCCCCC l0001 00000........................... . . .....

FF EEE DDDDODDODODDDDDO ODOO CCCCCC CCCCCCCCCC CCCCC(CCCCCCCCCCC 0l' UU IU I)0D0D .............................................. G FF EEE DooDDDDoDDoDDDDo CCCCCCC CCCCCCCCC CCCCCCCCCCCCCCCC 'f uFU0l01D 00)0I0000..............

.. +....G FF EEE DDDD0DDD0DDDD+DDDDD + CCCCCCCCC CCCCCCCC CCCCCCCCCCCCCCOCC )1l1 IdD000 + 1D)DD 00 )))FD..................................+..........C.......G FF EEE D0DDDDDDDDDD00DDD CCCCCCCCCC C+CCCCC C CCCCC+CCCCCCCCCCC D )0DoDCUOf' 0.........................

.......... FF EEE 0DDDDDDDDDDD0 DD0 CCCCCCCCCCCC CCCCCCCC CCCCCCCCCCCCCCCCD00000 U00000 ................................................ .FEFE.E.O.......D.D.+DDD CCCCCCCCCCC CCCCCCCCC CCCCCCCC CCCCC I0000100............... ........

FE EEEEF DDDDOODDDDO CCCCCCCCCCC CCCCCrCCCCCCCCCCCCCCCC)))) n110 .... . . ....... .........

FF IEEEE D000 DD DDDDD CCCCCCCCCCCCCC CCCCCC CCC CCCC.C. .. .... .... .. .. .... ........... E EE ODDDODODODD DD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCC '( 10DI0 .... l..)................., .......... ......

EEE (DoODDODDDDD DD CCCCCCCCCCCCCCCCCCCC 100000000000100000E.EEE.D CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC 1 I lI DDU lDD n IID DU................ . ........

E EF EEEEE DDD DDD0DDOD DDOD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCi 0 ) )00 ))) 0D I+)I D ))DD. .....................................................EEEEE DD0DD DDD0DDDDDDDDD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC 00D)))0) 000000. . . .). . . . . . . . . . ...

.EEFEF 0DDDDDD DDDDD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCC CCCCCCCCC D1) 1) 0 p)110010)0)u0),...,.".......................................................E EE DDODD D D 1D DDDI CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC I101)1,,011, " , , , , ,,0l), ,,00l" ",0. ......

.EE D1)000DD D 0DD 0DDDDD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC(FCC ) uDDDDD. . . .. . . . . . . . . . ............... .EEE DDDDDDDODDDDODDC CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC OOI))hloiu0lrbo0)D)00D D0110001f'. .............................. ........... ...................

: . EEE D D DD DDDD0D0 0 D0DD CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC I Iul n00I un I 0 l00n0l..........................................................................EE D DDDDDIODD000DDD00D CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC ' Ill00Il)))l)))I)))+I00000U0)0Dn00 1'011 ...................................EEEEE DDDD000D0DDDDDD0 CCCCCCCCCCCCCCCCCCCCCCCCCCCCCCCC CCCCCCCCCCC I 0 0l)II IOi)1)IUUOOOO')IW)ll)0000.""00............................ ............EEE D DDDDDD DDOOD CCCCCCCCCCC CCCCCCCCCCCCCCCCC CCCDCCC Ci0Il)b 01 0000 001) 11) 0101000 .) ...............................................................,,,. .EE EEEE DUDUDDDDDDDDDDD CCCCCCCCCCC CCCCfCCCCCCCCCCCr CCCC'CCCC CCCbD fDDDDD000F000UOD 11 nDpnuunU DDn.............. ... ..... ............................................... .

.E.En FDD ODODD ODDDODDODCCCCCCCCCC CCCCCCCCCCCCCCC r0 0C)Llli) 011 )10, Dnl) O ploDn)o l) .............................................................................EEEE D oDD O CCCCCCCCC C( cCCCCCC 1))l')CCl)CCCC)CuC)) )0)nlI))1D U..". . ........... ...................... ......................... .

.EE FCEF 0000D D0 00D0 CCCCCCCCC CCCCCCCCCCCCCCCC ...... ul1I'.Ol liO 1)h))0l) Ib . ... .. . . . ............... DFEFFEEFD0D0DDD00DDD CCCCCCCC CCCCCCCCCCCCCCC ) 1'11)l00 I))0lI 0 11,1. 00000 1.... . ... ... ... .. .. ... .. . .... . .. ....... . .. . . . . . . . . . .

.FEFED0000000000 CCCCCCCC CCC CCCC CCCCCCCC ll0000),0101L01P0l)0),,lI0)0100

1.................................... ...................

.FE 11000000000 CCCCCC ('(''1(('( (''C(('(C('I 1))nn").O IH)101110l)01001upn11) 1 )11) 00)11 m

00.000 00 0 0 DDD DC.......CCCCCCCC.CCCCCCCCCCCCCCC. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .00000ID000DD DD00D 0 CCCCCCC CCCCCCCCCCCCCCClIln l 0000 0 000 ................................................................... .

.EE. DODDDDCC CCCCC CCrrCCC I, ~ 11 loulIIl)nDl0 I))11' 111)llilI. . . . . . . . . . . . . . .. """""",.".

D DD D DDO -D 00D0DDD 0 0 1))))0 ) l..., ............... "..... . ...... "."..."... .. ........................ ......."":"",""000000DDOI)OD1)001) II)010001CCCCC) 1CCC. . . . . . . . . . . . . . . . . . . .

... .0. . . . . . . .0000 . . . . . . . . . . . . . . . . .. ............................................................................. ... 00.. .. . .... .. ... . .. . .. . .. . . ............................ ........... ...

000 . ..... 10 .. . . .. . . .. . . .. . . . ......................

................ 000..........0000................... .................................................................................................. .. .. .. .. .. .. .. .. .. . .. .. .. .. .. 00. .. ... . . .. .. .. .00110 .. .. .. .. . .. .. .. .. .. .. .. .. .. .. . .. .. .. .. .. .. .. .. .. .. . .. .. .. .. .. .. .. .. .. .. . .. .. .. .. .. .. .. .. .. .. . .. .. .. .. .. .. .. .. .. .. .

............................................ ...................... .................................................................................................................... .......................................... D .......................DD010D.D ...................................................,.....,....................................,...........................................,...................................

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(Bibliography Cont'd.)

Bascom, F., and Stose, G.W., 1932, Description of the Coatsville andWest Chester Quadrangles, U.S. Geological Survey Atlas, FolioN. 233.

Buckwalter, T.V., 1955, The Lithology, Stratigraphic Relations andStructure of Precambrian Rocks in Eastern Pennsylvania; inField Guidebook of Appalachian Geology Pittsburgh to New York,Pittsburgh Geological Society in conjunction with the AnnualMeeting of the American Association of Petroleum Geologist,New York, 1952, pp. 93-97.

Cooper, M., 1958, Bibliography and Index of Literature on Uranium andThorium and Radioactive Occurrences in the United States; Part5: Connecticut, Delaware, Illinois, Indiana, Maine, Maryland,Massachusetts, Michigan, New Hampshire, New Jersey, New York,Ohio, Pennsylvania, Rhode Island, Vermont, and Wisconsin;Geological Society of America, Special Paper 67, 472 pp.

Fenneman, N.M., 1938, Physiography of Eastern United States; New York,McGraw-Hill Book Co., Inc., 1938, 714 pp.

Fisher, G.W., 1970, Introduction; Section IV: The Piedmont; in Fisher,G.W., et alia, eds., 1970, Studies of Appalachian Geology,Centra'Southern; New York, John Wiley and Sons, pp. 295-298.

Fisher, G.W., 1970b, The Metamorphosed Sedimentary Rocks along thePotomac River near Washington, D.C.; in Fisher, G.W., et alia,eds., 1970, Studies of Appalachian GeoTogy, Central andSouthern; New York, John Wiley and Sons, pp. 299-316.

Fisher, G.W., Pettijohn, F.J., Reed, J.C., and Weaver, K.N., eds., 1970,Studies of Appalachian Geology, Central and Southern; NewYork, John Wiley and Sons, 460 pp.

Jordan, R.R., 1976, The Columbia Group (Pleistocene) of Delaware; inThompson, A.M., ed., Guidebook to the Stratigraphy of theAtlantic Coastal Plain in Delaware; Petroleum ExplorationSociety of New York, Third Annual Field Trip, 1976, pp. 103-110.

Kummel, H.B., 1940, The Geology of New Jersey; Department of Conserva-tion and Development, State of New Jersey; Bulletin 50,Geologic Series.

McGee, W.J., 1888, Three Formations of the Middle Atlantic Slope;American Journal of Science, 3rd Series, v. 35, pp. 120-143,328-330, 365-388, 448-466.

McKinstry, H., 1941, Structure of the Glenarm Series in Chester County,Pennsylvania, Geological Society of America, Bulletin v. 72,pp. 557-578.

Mineral Resources Development, Inc., 1979, Geology of the WilmingtonQuadrangle; Map, scale 1:250,000, by Mineral Resources Devel-opment, Inc. for U.S. Department of Energy.

N.T.B.M.S., 1972, National Topographic-Bathymetric Map Series, WilmingtonSheet, Delaware, New Jersey, Pennsylvania, Maryland; U.S.Geological Survey and National Ocean Survey, Eastern U.S.,map, scale 1:250,000, NJ18-2 series, 1972.

Pickett, T., 1976, Synopsis of Atlantic Coastal Plain Stratigraphy inDelaware; in Thompson, A.M., 1976, Guidebook to the Strati-graphy of the Atlantic Coastal Plain in Delaware; Third AnnualField Trip, Petroleum Exploration Society of New York, 1976,pp. 2-11.

Southern Interstate Nuclear Board, 1969, Uranium in the Southern UnitedStates; report prepared for the Atomic Energy Commission,Division of Raw Materials, by the Southern Interstate NuclearBoard, updated November, 1970.

Sundstrom, R.W., Pickett, T., and Varrin, R.D., 1975, Hydrology, Geologyand Mineral Resources of the Coastal Zone of Delaware: WaterResources Center, University of Delaware, 268 pp.

Vokes, H.E., 1957, Geography and Geology of Maryland; Department ofGeology Mines and Water Resources, Bulletin 19, 243 pp.

Ward, R.F., and Groot, J.J., 1957, Engineering Materials of NorthernNew Castle County; State of Delaware, Delaware GeologicalSurvey, Bulletin No. 7, 103 pp.

Wise, D.U., 1970b, Multiple Deformation, Geosynclinal Transitions, andthe Martic Problem in Pennsylvania; in Fisher, G.W., et alia,eds., 1970, Studies of Appalachian Geology, Central andSouthern; New York, John Wiley and Sons, pp.317-334.

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