贵州习水县谢家坝铅锌矿矿床地质特征及成因浅析 |
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引用本文: | 石治均. 贵州习水县谢家坝铅锌矿矿床地质特征及成因浅析[J]. 西南科技大学学报, 2014, 0(1): 29-33,44 |
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作者姓名: | 石治均 |
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作者单位: | 贵州省地矿局102地质大队,贵州遵义563003 |
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摘 要: | 通过对谢家坝铅锌矿床的矿体特征、矿物组分、矿石结构构造、围岩蚀变、找矿标志等的分析与研究,得出了该区铅锌矿床与灯影组白云岩、构造裂隙、围岩蚀变等的关系密切,通过与其他扬子地台型碳酸盐铅锌矿特征的对比研究,认为该矿床为密西西比河谷型(MVT)矿床。
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关 键 词: | 铅锌矿 矿床成因 找矿标志 |
Geological Characteristics and Formation Analysis of the Xie Jiaba Pb -Zn Deposit in the Xishui County of Guizhou Province |
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Affiliation: | SHI Zhi - jun (Brigade 102, Guizhou Bureau of Geology and Mineral Exploration & Development, Zunyi 563003, Guizhou, China) |
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Abstract: | Analysis and research of the ore body characteristics, mineral components, ore structures, wallrock alteration,indicators for deposit in the Xie Jiaba lead -zinc deposits indicate that the deposits in thestudy area are closely related to DENG YING dolomite ,fissures, wall rock alteration, etc. A comparative a-nalysis of the carbonate lead - zinc ore characteristics of Yangtze platform displays that the deposit in thestudy area is of Mississippi valley - type. |
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Keywords: | Plumbic zinc mine the Genesis of the deposit Indicator for deposit |
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