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Carbonatehosted Leadzinc Ore Deposits

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.

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  • Australian Sediment-Hosted Zinc-Lead-Silver Deposits

    Australian Sediment-Hosted Zinc-Lead-Silver Deposits

    of eastern australia and the carbonate-hosted zn-pb deposits of northwestern. australia. broken hill is the largest single zn-pb-ag-ag deposit known any- where, with an australian sediment-hosted lead-zinc-silver deposits. d. o. 500.

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  • Geology, Isotope Geochemistry And Ore Genesis Of The

    Geology, Isotope Geochemistry And Ore Genesis Of The

    carbonate-hosted pbzn deposit, southwest china ative to the jmc 3-0749l zinc isotope standard. stages i to iii the shanshulin pbzn deposit, hosted by dolomitic lead isotopic compositions of ores and sulfides from the shanshulin.

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  • Carbonate-Hosted Base Metal Deposits

    Carbonate-Hosted Base Metal Deposits

    three main carbonate-hosted deposit types are recognized: 1. leadville-type in addition, the ore lead is isotopically different from host-rock in: the genesis of stratiform sediment-hosted lead and zinc deposits: conference.

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  • Geology, Isotope Geochemistry And Ore Genesis Of The

    Geology, Isotope Geochemistry And Ore Genesis Of The

    carbonate-hosted pbzn deposit, southwest china ative to the jmc 3-0749l zinc isotope standard. stages i to iii the shanshulin pbzn deposit, hosted by dolomitic lead isotopic compositions of ores and sulfides from the shanshulin.

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  • Carbonate-Hosted Zinc-Lead Deposits In The Lower Cambrian

    Carbonate-Hosted Zinc-Lead Deposits In The Lower Cambrian

    both ore stages are postdated by a generation of late calcite. main-stage sulfides ( 206pb/ 204pb = 18.162-18.225) display a steep linear trend on conventional pb 

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  • Compilation Of Mineral Resource Data For Mississippi Valley

    Compilation Of Mineral Resource Data For Mississippi Valley

    sediment-hosted lead-zinc deposits are historically the most significant (sedex) deposits, and those in carbonate-dominated sequences that are idaho, because these deposits probably represent different deposit types 

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  • Compilation Of Mineral Resource Data For Mississippi Valley

    Compilation Of Mineral Resource Data For Mississippi Valley

    sediment-hosted lead-zinc deposits are historically the most significant sources of sedimentary exhalative (sedex) deposits, and those in carbonate-dominated deposits probably represent different deposit types (leach and others, 2005).

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  • Sulfate-Sulfide-Carbonate Associations In Mississippi Valley

    Sulfate-Sulfide-Carbonate Associations In Mississippi Valley

    sulfate-sulfide-carbonate associations in mississippi valley-type are of interest in the interpretation of carbonate-hosted lead-zinc deposits. to the white sparry dolomite of ore districts) if aqueous metals are not present and 

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  • Comparison Of The Cracow-Silesian Mississippi Valley-Type

    Comparison Of The Cracow-Silesian Mississippi Valley-Type

    hosted ore, can be interpreted as products of fabric-conservative sulfide replacement. (in press) described lead-zinc deposits of mississippi valley-type (mvt) 11) there is always evidence of dissolution of carbonate host rocks, expressed 

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  • Mississippi Valley-Type Lead-Zinc Deposits (Mvt)

    Mississippi Valley-Type Lead-Zinc Deposits (Mvt)

    mvt deposits are stratabound, carbonate-hosted sul- phide bodies, composed predominantly of zinc and lead, bound in sphalerite and galena. deposits and 75 ore bodies and the pine point district in the. northwest territories hosts two 

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  • Sediment Hosted LeadZinc Deposits Of The

    Sediment Hosted LeadZinc Deposits Of The

    ore grading 23 zn at vazante, and 11.7 mt of sulfide subaerial exposure of the carbonate platform. the lead zinc deposits are associated with this dolomitic 

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  • Sulfate-Sulfide-Carbonate Associations In Mississippi Valley

    Sulfate-Sulfide-Carbonate Associations In Mississippi Valley

    sulfate-sulfide-carbonate associations in mississippi valley-type are of interest in the interpretation of carbonate-hosted lead-zinc deposits. to the white sparry dolomite of ore districts) if aqueous metals are not present and 

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  • Characteristics Of High Temperature, Carbonate-Hosted

    Characteristics Of High Temperature, Carbonate-Hosted

    high temperature massive sulfide ores in carbonate rocks constitute a distinct genetic class of deposits in the characteristics of high temperature, carbonate-hosted replacement ores and some valley-type ores', carbonate-hosted lead-zinc deposits: 75th anniversary volume, d.f. sangster.

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  • Internal Sediments As A Key To Understanding The

    Internal Sediments As A Key To Understanding The

    phenomena have been proposed as important ore-forming processes in mvt deposits, the hydrothermal karst origin of the upper silesian zn-pb ore deposits zn-pb ore deposits', carbonate-hosted lead-zinc deposits: 75th in solutions capable of precipitating sulfides, barite and carbonates.

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  • Emarat Carbonate-Hosted ZnPb Deposit, Markazi Province

    Emarat Carbonate-Hosted ZnPb Deposit, Markazi Province

    (2010) come from the emarat lead-zinc deposit which seems to display a larger variability. the match with the coins from group i is not perfect, 

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  • Carbonate-Hosted Base Metal Deposits

    Carbonate-Hosted Base Metal Deposits

    three main carbonate-hosted deposit types are recognized: 1. leadville-type in addition, the ore lead is isotopically different from host-rock in: the genesis of stratiform sediment-hosted lead and zinc deposits: conference.

    more