| 青海锡铁山块状硫化物铅锌矿床成因探讨 |
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| 引用本文： | 王可.青海锡铁山块状硫化物铅锌矿床成因探讨[J].矿物岩石,1993,13(1):76-83. |
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| 作者姓名： | 王可 |
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| 作者单位： | 四川省地质矿产局207地质队 乐山 |
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| 摘 要： | 本文着重分析研究区成矿的构造背景、成矿物质来源、成矿机理等,提出以海水为主下渗滤形成热液,由火山地震泵驱动热液上升喷发沉积成矿的观点,并探讨后期热液对矿体的改造过程。
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| 关 键 词： | 铅锌矿床 硫化物 块状 成因 |
ON GENESIS OF LEAD-ZINC ORE DEPOSIT OF MASSIVE SULFIDE IN XTTIE SHAN,QINGHAI |
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| Wang Ke.ON GENESIS OF LEAD-ZINC ORE DEPOSIT OF MASSIVE SULFIDE IN XTTIE SHAN,QINGHAI[J].Journal of Mineralogy and Petrology,1993,13(1):76-83. |
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| Authors: | Wang Ke |
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| Abstract: | The minerogenetic tectonic background, minerogenetic material source and minerogenetic mechanism of the study area are emphatically analyzed in the paper. It is pointed out that the hydrothermal liquid formed mainly by sea water penetrating downward erupted under the volcanoseismic pumping,forming the sedimentary ore deposit. The late stage reformation of the ore body by hydrothermal liquid is also discussed. |
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| Keywords: | pararift and minerogenesis stratabound lead-zinc deposit |
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