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云南金顶铅锌矿床稳定同位素地球化学研究
引用本文:赵兴元.云南金顶铅锌矿床稳定同位素地球化学研究[J].地球科学,1989,14(5):495-502.
作者姓名:赵兴元
作者单位:China University of Geosciences,Wuhan 430074
摘    要:

关 键 词:铅锌矿床  稳定同位素  地球化学

STABLE ISOTOPE GEOCHEMISTRY OF THE JINDING LEAD-ZINC ORE DEPOSIT, YUNNAN
Zhao Xingyuan.STABLE ISOTOPE GEOCHEMISTRY OF THE JINDING LEAD-ZINC ORE DEPOSIT, YUNNAN[J].Earth Science-Journal of China University of Geosciences,1989,14(5):495-502.
Authors:Zhao Xingyuan
Abstract:Based on sulfur, lead, hydrogen, oxygen, carbon and strontium isotope data of the Jinding lead-zinc deposit, this paper primarily discusses the source of mi-neralizing substances. The ore-forming metals come mainly from the earth's man-tle, while a few come from the earth's crust; the sulfur and carbon originate mainly from sulfides, sulfates and organic materials in the crust, some of them originate from deep sources. The ore-forming medium is a kind of mixed fluid which is composed mainly of atmospheric water, partly and of magmatic water and evoluted water.
Keywords:the mantle  stable isotope  mixed hydrothermal fluid  organic material  Jinding
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