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  1. Carbonate-hosted lead-zinc ore deposits are important and highly valuable concentrations of lead and zinc sulfide ores hosted within carbonate (limestone, marl, dolomite) formations and which share...
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    Carbonate-hosted lead-zinc ore deposits are important and highly valuable concentrations of lead and zinc sulfide ores hosted within carbonate (limestone, marl, dolomite) formations and which share...
    en.wikipedia.org/wiki/Carbonate-hosted_lead-zinc_…
    They are a diverse group of ore deposits hosted by a wide variety of carbonate andsiliciclastic rocks that have no obvious genetic association with igneous activity.
    pubs.usgs.gov/publication/70146125
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    Carbonate-hosted lead-zinc ore deposits - Wikipedia

    Carbonate-hosted lead-zinc ore deposits are important and highly valuable concentrations of lead and zinc sulfide ores hosted within carbonate (limestone, marl, dolomite) formations and which share a common genetic origin. These ore bodies range from 0.5 million tonnes of contained ore, to 20 million tonnes or … 展开

    The ultimate source of the mineralizing fluid(s) in MVT deposits is unknown. The ore fluids of MVT deposits are typically low temperature (100 °C–150 °C) and have the composition of basinal … 展开

    The trap for carbonate-hosted lead-zinc sulfides is a chemical reaction which occurs as a consequence of concentration of sulfur, often hydrocarbons, and zinc and lead which are absorbed … 展开

    The importance and synergies between hydrocarbon source-transport-trap 'fairways' and MVT and Irish Type lead-zinc deposits has been known for several decades. Often the … 展开

    Similar deposit styles may be encountered in sheared and deformed carbonate belts where zinc-lead sulfides are hosted at the sheared contact of carbonates with siliciclastic sequences. … 展开

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    Two potential transportation mechanisms for the metal-bearing ore fluid have been proposed. The first involves compaction of sediments in basins with … 展开

    Ore minerals in carbonate replacement deposits are typically lead sulfide, galena, and zinc sulfide sphalerite. Weathered equivalents form anglesite, cerussite, smithsonite, 展开

    Exploration for MVT deposits is relatively complex in theory and straightforward in practise. During the area selection phase, attention must be paid to the nature of the carbonate sequences, especially if there is a 'dolomite front' alteration identified within oil exploration 展开

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  4. Carbonate-Hosted Lead-Zinc Deposits: 75 - GeoScienceWorld

  5. Carbonate hosted lead zinc ore deposits - chemeurope.com

  6. (PDF) Sediment-Hosted Lead-Zinc DepositsA Global …

    2005年1月1日 · S EDIMENT-HOSTED Pb-Zn deposits are a diverse group of ore deposits hosted by a wide variety of carbonate and siliciclastic rocks that have no obvious genetic association with igneous

  7. Genesis of the carbonate-hosted zinc–lead deposits in the …

  8. Genesis of the carbonate-hosted Pb–Zn deposits in western …

  9. Hydrogeologic modelling of the genesis of carbonate …

    1999年2月18日 · Numerical simulations of basin-scale hydrodynamics and of deposit-scale reactive flow are presented to demonstrate the processes controlling low-temperature Pb–Zn ore genesis in two world-class ore...

  10. Anatomy and genesis of the world’s largest carbonate-hosted Zn …

  11. Paleoproterozoic Mississippi Valley-type mineralization at

  12. Hydrogeologic modeling of the genesis of carbonate-hosted lead …

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