| 海底热液成矿作用 |
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| 引用本文： | 真允庆. 海底热液成矿作用[J]. 矿产与地质, 1991, 5(3): 157-162,172 |
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| 作者姓名： | 真允庆 |
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| 作者单位： | 冶金工业部第三地质勘查局 |
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| 摘 要： | 根据近二三十年海底地质考察结果,海底热液成矿作用非常普遍,可以形成铜、铅、锌、金、银、铁、硫、重晶石、萤石、锑、汞和硼等海底热液矿床.按容矿岩石不同,可分为与火山岩系有关的及与沉积岩有关的两大类矿床类型.
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| 关 键 词： | 海底 热液成矿 成矿作用 |
HYDROTHERMAL MATALLOGENESIS ON MARINE BED |
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| Zhen Yunqing. HYDROTHERMAL MATALLOGENESIS ON MARINE BED[J]. Mineral Resources and Geology, 1991, 5(3): 157-162,172 |
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| Authors: | Zhen Yunqing |
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| Affiliation: | The Third Geological Exploration Bureau of the Ministry of Metallurgical Industry |
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| Abstract: | According to nearly thirty years survey on the marine geology, it has been realized that seafloor hydrothermal metallogenesis are widespread on the marine bed, and resulted in seafloor hydrothermal deposits of Cu, Pb, Zn, Au, Ag, Fe, S, B, Hg, Sb, barite and fluorite etc. Based on the difference of ore mineral bearing rocks, two types of deposit can be classified, one related to volcanic rock system and the other associated with sedimentary rocks. |
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| Keywords: | Hydrothermol met allogenesis on marine bed deposit classification |
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