| 西藏满总金铅银多金属矿床地质与成因 |
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| 引用本文： | 侯世云, 尹光侯. 1997. 西藏满总金铅银多金属矿床地质与成因. 地质通报, 16(4). |
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| 作者姓名： | 侯世云 尹光侯 |
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| 作者单位： | 云南地勘局第三地质大 |
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| 摘 要： | 满总金铅银多金属矿床产于三缅村岩浆弧内，与满总单元中细粒角闪黑云二长花岗岩、谢巴组火山岩关系密切，围岩岩石化学、地球化学特征对成矿较为有利。据围岩特征及矿体中黄铁矿的热声测试和硫、铅稳定同位素测试成果分析，该矿床为花岗岩浆中温热液成因类型。
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| 关 键 词： | ; ; |
GEOLOGY AND GENESIS OF THE MANZONG GOLD LEAD SILVER POLYMETALLIC DEPOSIT IN TIBET |
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| 1997. GEOLOGY AND GENESIS OF THE MANZONG GOLD LEAD SILVER POLYMETALLIC DEPOSIT IN TIBET. Geological Bulletin of China, 16(4). |
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| Authors: | Hou Shiyun and Yin Guanghou |
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| Affiliation: | No. 3 Geological Party,Yunnan Bureau of Geology and Mineral Resources,Dali,Yunnan |
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| Abstract: | The Manzong gold lead silver polymetallic deposit occurs in the Sanmiancun magma arc in Tibet and is closely related to medium and fine grained hornblende biotite monzogranite of the Manzong unit and volcanic rocks of the Xieba Formation.The chemical and geochemical characteristics of the host rocks are favorable to mineralization.According to the characteristics of host rocks and thermosonimetric analysis of pyrite from orebodies with the BRC 1 type thermosonimeter,coupled with sulfur lead stable isotopic study,it is considered that this deposit is a mesothermal deposit associated with granitic magma. |
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| Keywords: | Manzong gold lead silver geology of the deposit genesis |
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