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lead zinc deposit
    STUDY OF ISOTOPE GEOCHEMISTRY ON THE KEKETALE LEAD ZINC DEPOSIT,XINJIANG
    新疆可可塔勒铅锌矿床同位素地球化学研究
    OXIDATION ENRICHMENT REGULARITY OF QIANDONGSHAN LEAD ZINC DEPOSIT
    铅硐山铅锌矿床的氧化富集规律
    The Ore-forming Geological Condition and the Ore Prospecting Direction of Huize Lead Zinc Deposit
    会泽铅锌矿床成矿地质条件及找矿方向
    THE FLUID INCLUSION IN MVT LEAD ZINC DEPOSIT IN SOUTHWEST MARGIN OF TARIM
    塔里木西南缘MVT型铅锌矿床流体包裹体研究
    GEOLOGICAL FEATURES AND GENESIS OF HUANG GOU SHAN LEAD, ZINC DEPOSIT IN JILIN
    吉林荒沟山铅锌矿床地质特征及矿床成因探讨
    In this paper the vein lead zinc deposit modeling method by researching construction of the variogram, selection of the correct estimation method and parameters by using the search ellipsoid as well as the geological assurance of evaluated resource/reserve classification was discussed.
    本文以蔡家营铅锌矿Ⅲ矿带矿床为例 ,从变异函数模型的建立、估值方法的选择、如何利用搜索椭球体确定主要估值参数以及估值后资源 /储量分类的地质可靠程度等几个方面对脉状铅锌矿床的建模方法进行了论述。
    GEOCHEMISTRY OF THE QINGCHENGZI LEAD ZINC DEPOSIT
    青城子铅锌矿床的地球化学
    RESEARCH ON GENESIS OF LEAD ZINC DEPOSIT IN YINMUSI
    银母寺铅锌矿床成因研究
    PRELIMINARY RECOGNIZATION OF THE MAIN PHASE FOLD WITHIN ORE BEARING LITHOLOGICAL SERIES IN THE XITIESHAN LEAD ZINC DEPOSIT,QINGHAI PROVINCE
    锡铁山铅锌矿床含矿岩系主褶皱的初步厘定
    RESEARCH OF THE DAUGHTER MINERALS IN FLUID INCLUSIONS OF THE HUAYUAN LEAD ZINC DEPOSIT
    花垣铅锌矿床流体包体中的子矿物
    ASSOCIATION OF SILVER MINERALIZATION IN THE HUANGSHAPING LEAD ZINC DEPOSIT
    黄沙坪铅锌矿床中银矿化组合特征
    “DOUBLE SOURCE” SEDIMENTARY TRANSFORMATION METALLOGENIC MODEL OF THE DISU LEAD ZINC DEPOSIT
    论底苏铅锌矿床的“双源”沉积改造成矿模式
    CHARACTERISTICS OF ORE CONTROLLING STRUCTURES AND REE COMPOSITION OF FAULT ROCKS IN HUIZE LEAD ZINC DEPOSIT,YUNNAN
    云南会泽铅锌矿床构造控矿及断裂构造岩稀土元素组成特征
    It is found that the main phase fold developed within the ore bearing metamorphic rock series in the Xitieshan lead zinc deposit is an oblique fold of schistosities (S 0+S 1) green schists.
    锡铁山铅锌矿床含矿岩系主褶皱是一个由绿片岩片理(S0+S1)褶皱而成的斜卧褶皱。
    The Huayuan lead zinc deposit is a large MVT ore deposit in Hunan Province, southern China, which occurs in the algal reef limestone of Lower Cambrian.
    湖南西部花垣铅锌矿床,是近年来发现的产于下寒武统清虚洞组上部藻礁灰岩中的大型MVT矿床。
    Two different kinds of minernlization associations of silver polymetals can be classified in the Huangshaping lead zinc deposit. One is the Pb(Zn) Ag Sn Sb mineralization association which is related to the graniticporphyry 301 and granophyre 304.Silver mineralization is accompanied by lead,and charaterized by high contents of Sn,Sb,Ag and low content of Bi,Te,Mo,W. Its mineral association is featured by canfieldite hocartite pyrargyrite acanthite polybasite.
    研究黄沙坪铅锌矿床中银矿化组合表明:与301花岗斑岩和304花斑岩岩体有关铅(锌)-银-锡-锑矿化组合,银矿化伴随铅矿化出现,其微量元素富Sn、Sb、Ag,低Bi、Te、Mo、Wo、W为特征;
    Mineral assemblages show zoning characters around the granite porphyry 301 and 304 in the Huangshaping lead zinc deposit,which show a positive zoning from complex to simple series.
    黄沙坪铅锌矿床围绕301号和304号花岗斑岩体出现矿物组合分带的特点。
    The deposit zoning is from contact metasomatic skarn type of iron(tin) deposit→ pneumato hydrothermal skarn tungsten (molybdenum) deposit→ to hydrothermal mesothermal iron (tin )bearing lead zinc deposit or copper lead zinc deposit from granite porphyry outward to the strata.
    矿物组合呈正向带状分布,由复杂到简单。 从花岗斑岩体至远离岩体的地层,矿床分带表现为接触交代矽卡岩型铁(锡)矿床→气化高温热液矽卡岩型钨钼矿床→高中温热液含铁(锡)铅锌矿床或铜铅锌矿床
    It is shown through isotopic data that the lead Zinc Deposit of Keketale in Xinjiang was formed in Lower Devonian in coincidence with the time of host rock.
    同位素资料表明,可可塔勒铅锌矿床成矿时代为早泥盆世,与下泥盆统海相火山岩系年代一致;
    Based on geochemical studies,the present paper puts forward a metallogenic model for the Disu lead zinc deposit.
    本文在矿床地球化学研究基础上,提出了底苏铅锌矿床的成矿模式
 

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