| 四川大梁子铅锌矿床的成因分析 |
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| 引用本文： | 王小春. 四川大梁子铅锌矿床的成因分析[J]. 矿产与地质, 1991, 5(3): 151-156 |
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| 作者姓名： | 王小春 |
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| 作者单位： | 西南冶金地质科学研究所 |
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| 摘 要： | 四川大梁子铅锌矿床赋存于震旦系上统灯影组白云岩中.受断裂控制明显.成矿物质主要来自“地层源”、经地下热水循环富集.沿断裂充填、交代、形成热水溶滤层控铅锌矿床.
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| 关 键 词： | 铅锌矿床 成因 地层源 四川 |
GENESIS ANALYSIS OF DALIANGZI Pb-Zn DEPOSIT IN SICHUAN PROVINCE |
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| Wang Xiaochun. GENESIS ANALYSIS OF DALIANGZI Pb-Zn DEPOSIT IN SICHUAN PROVINCE[J]. Mineral Resources and Geology, 1991, 5(3): 151-156 |
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| Authors: | Wang Xiaochun |
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| Affiliation: | Research Institute of Metallurgical Geoscience in the Southwestern China |
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| Abstract: | The Daliangzi Pb-Zn deposit occurs as veins controlled clearly by fractures in the dolostone of Dengying Formation of Upper Sinian System. It belongs to a stratabound hydrothermal percolating lead-zinc deposit. Ore-forming material is originated mainly from strata, which was leached and concentrated by the circulation of underground hydrothermal water, and filled and replaced in the fractures. |
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| Keywords: | Dalingzi Sichuan Pb-Zn deposit Genesis of deposit |
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