Mississipi Valley Type Deposit

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    MISSISSIPPI VALLEY TYPE(MVT) DEPOSIT

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    Sejarah MVT Amerika Utara(Galena ,Sphalerite,sedikit Kalkopirit )

    Banyak ditemukan terbentuk di waktu

    PROTEROZOIKUM - CRETACEOUS

    Pertama kali ditemukan 70

    tahun yang lalu (Bastian 1939)

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    Apa sih MVT (Mississippi Valley

    Type) itu ?

    Endapan MVT terdiri dari kumpulan tubuh bijih dimana silfida Fe, Pb, dan Zn mengisi

    rongga pada termokarst atau larutan breksia pada platform karbonat kebagian

    cekungan sedimen

    Ukuran rata rata Deposit7.0 Mt

    32,5 g/t

    Ag0.23 %

    Cu

    6,0 %

    Zn

    1.9 %

    Pb

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    Source Sumber

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    Transportation

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    The Trap

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    Exploration

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    Mineralisasi

    Types of Sulfide Mineralization

    There are at least five types of sulfide mineralization present in the

    Lavrion district.

    1. Porphyry-style mineralization

    2. Skarn-style mineralization are spatially associated with the Plaka

    granodiorite

    3. Breccia-style mineralization

    4. Carbonate-replacement Pb-Zn-Ag mineralization5. Vein-style Pb-Zn-Ag mineralization is present at Adami

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    Photos of various types of mineralization and rock types in the Lavrion district. a. Multiple crosscutting quartzmolybdenite-

    pyrite (Qtz-Mlb-Py) veins in the Plaka granodiorite (PG). b. Hornfels on the margin of the Plaka granodiorite porphyry. c.

    Upper Marble (UM) and interbedded schists (S) near the southern margin of the Plaka granodiorite. Massive epidote (E)-bearing skarn is outlined. d. Massive carbonate-replacement ore along the contact of the Kaesariani schists and the Lower

    Marble (LM), Jean Baptiste mine (Kamariza area). e. Massive sphalerite (Sph) and calcite (Cal) in carbonate-replacement

    ore from Kamariza. f. Intergrown massive pyrite (Py) and sphalerite (Sph) with crosscutting calcite (Cal) veins in massive

    ore from Plaka (Villia). g. Brecciated sphalerite-galena ore with clasts of Upper Marble in Vein 80 at the Adami mine. Note

    the hornfels on the upper portion of the vein. h. Vein 80 from Adami mine showing bands of galena (Gn), siderite (Sd), and

    calcite (Cal).

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    Jenis-jenis pengisian (open-space filling)

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    A. Crackle breccia with disseminated

    sphalerite crystalsin white dolomite

    cement, Robb Lake, BC.

    B. Mosaic breccia with sphalerite crystalsin white dolomite cement, Robb Lake,

    BC.

    C. Rubble breccia consisting of variably

    altered dolostone fragments and shale

    fragments in white dolomite cement.

    Note the dolostone fragments with

    zebra texture, Robb Lake, BC.

    D. Rock-matrix breccia with dolostone,

    shale, and white sparry dolomite

    fragments in dark grey fragmental

    matrix, Robb Lake, BC.E. Aggregates of massive sphalerite

    crystals and white sparry dolomite

    along small fractures, Pine Point, NWT.

    F. Aggregates of colloform sphaleriteand

    skeletal galenacompletely replacing

    the carbonate, Polaris, Nunavut; scalebar is 1 cm.

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    Various ore textures from

    Polaris, Nunavut, NWT; scale

    bar is 1 cm.

    A. Keel ore: sphalerite andskeletal galena are

    replacing the carbonate

    clasts.

    B. Keel ore: crystalline

    sphalerite in solution

    collapse breccia.C. Ocean zone: Massive

    galenaand sparry

    dolomite in

    pseudobrecciated

    carbonate host rock.

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    Peta deposit MVT di seluruh dunia

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    .

    Distribution of Mississippi Valley-type deposits/districts plotted on a simplified geological map of Canada

    (Map D1860A). Districts shown are,Cornwallis;Nanisivik, Pine Point, Prairie Creek, Robb Lake, Monarch-

    Kicking Horse, Blende, Bear-Twit, Gayna River, Goz Creek, Gays River, Jubilee, Walton, Newfoundland Zn,Upton, and Esker

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    Pine Point

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    Summary of the characteristics of three Mississippi

    Valley-type districts

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