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扬子地台北缘中段中上元古界中金、银矿床稳定同位素地球化学研究
引用本文:汪东波.扬子地台北缘中段中上元古界中金、银矿床稳定同位素地球化学研究[J].中南大学学报(自然科学版),1991(6).
作者姓名:汪东波
作者单位:中南矿冶学院地质系
摘    要:本文系统地研究了扬子地台北缘中段中上元古界中金银矿床的硫、铅、碳、氢、氧同位素组成。研究表明:银洞沟Au-Ag-Pb-Zn矿床、许家坡Au-Ag-Te矿床和白岩沟Au矿床的成矿物质具深源特征,成矿流体为混有少量大气水和岩浆水的变质流体;东沟坝Au-Ag-Pb-Zn重晶石型矿床成矿物质及成矿流体皆具多来源的特征。

关 键 词:稳定同位素地球化学  金银矿床  扬子地台北缘中段

STUDIES ON STABLE ISOTOPIC GEOCHEMISTRY OF GOLD-SILVER DEPOSITS IN THE MIDDLE-UPPER PROTEROZOIC SUBERATHEM IN THE MIDDLE SECTION OF THE NORTHERN MARGIN OF YANGTZE PLATFORM
Wang Dongbo.STUDIES ON STABLE ISOTOPIC GEOCHEMISTRY OF GOLD-SILVER DEPOSITS IN THE MIDDLE-UPPER PROTEROZOIC SUBERATHEM IN THE MIDDLE SECTION OF THE NORTHERN MARGIN OF YANGTZE PLATFORM[J].Journal of Central South University:Science and Technology,1991(6).
Authors:Wang Dongbo
Institution:Wang Dongbo Department of Geology
Abstract:Compositions of S, Pb, C, H, O of gold-silver deposits in the Middle- Upper Proterozoic Suberathem in the middle section of the northern margin of Yangtze Platform bare been systematically studied in this paper. Studies show that ore-forming materials of Yingdonggou Au-Ag-Pb-Zn deposit, Xujiapo Au-Ag-Te deposit and Beiyangou gold-bearing quartze vein deposit have cha- racteristics of deep source; ore-forming fluids of them are metamorphic fluid and a mixture of a small quantity of magmatic water and meteroic water. Ore- forming material and ore-forming fluid of Donggoubar Au-Ag-Pb-Zn-barite deposit both have characteristics of multi-source.
Keywords:stable isotopic geochemistry  gold-silver deposit  middle section of northern margin of Yangtze Platform
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