| 贵州水城青山铅锌矿床地球化学研究 |
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| 引用本文： | 张启厚,顾尚义,毛健全. 贵州水城青山铅锌矿床地球化学研究[J]. 地球与环境, 1999, 0(1) |
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| 作者姓名： | 张启厚 顾尚义 毛健全 |
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| 作者单位： | 贵州工业大学资源工程系!贵阳，550003，贵州工业大学资源工程系!贵阳，550003，贵州工业大学资源工程系!贵阳，550003 |
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| 基金项目： | 贵州省“八五”攻关项目!黔科计字（1992）1017号 |
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| 摘 要： | 通过对青山铅锌矿床矿石矿物、蚀变围岩、含矿层、辉绿岩的稀土元素、硫、碳、氧同位素及黔西北岩石地层中铅锌含量的研究，笔者认为，成矿金属并非源于岩浆岩，而源于深部的沉积岩，碳、硫分别源于碳酸盐岩和含矿地层的硫酸盐硫；大气降水经深循环再上升形成成矿介质水。
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| 关 键 词： | 青山 铅锌矿 地球化学 |
GEOCHEMICAL STUDY ON QINGSHAN LEAD-ZINC DEPOSIT IN SHUICHENG,GUIZHOU PROVINCE |
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| Zhang Qihou, Gu Shangyi, Mao Jiaequan. GEOCHEMICAL STUDY ON QINGSHAN LEAD-ZINC DEPOSIT IN SHUICHENG,GUIZHOU PROVINCE[J]. Earth and Environment, 1999, 0(1) |
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| Authors: | Zhang Qihou Gu Shangyi Mao Jiaequan |
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| Abstract: | On the basis of the average contents of Pb and Zn in the strata of Northwest Guizhou Province andthe REE contents, isotopic compositions of sulfur, carbon and oxygen for minerals and host rocks anddiabase in the Qingshan lead-zinc deposit, the authors pointed out that the minerognic metals werederived from the Cambrian Niutitang Formation; sulfur and carbon from sulfate and carbonate, respec-tively; and the water from meteoric water circulating at the depth. |
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| Keywords: | Qingshan Pb-Zn deposit geochemistry |
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