| 湘中锑矿深源流体的地幔柱成矿演化 |
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| 引用本文： | 黎盛斯. 湘中锑矿深源流体的地幔柱成矿演化[J]. 湖南地质, 1996, 15(3): 137-142 |
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| 作者姓名： | 黎盛斯 |
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| 作者单位： | 湖南省地质矿产厅 |
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| 摘 要： | 深源流体在地幔柱热驱动下，历经长期壳幔循环，形成高浓度古水热成矿流体，为湘中锑的成矿蓄积丰沛的矿源。
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| 关 键 词： | 深源流体 湘中地幔柱 壳幔循环 锑矿床 成矿演化 |
Evolution of Antimony Mineralization by the Mantle Plume of Deep Fluid in Central Hunan |
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| Li Shengsi Hunan Bureau of Geology and Mineral Resources. Evolution of Antimony Mineralization by the Mantle Plume of Deep Fluid in Central Hunan[J]. Land & Resources Herald, 1996, 15(3): 137-142 |
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| Authors: | Li Shengsi Hunan Bureau of Geology and Mineral Resources |
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| Affiliation: | Li Shengsi Hunan Bureau of Geology and Mineral Resources |
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| Abstract: | Driven by the heat of the mantle plume and undergone a long period of circulation in the region between mantle and crust,the deep fluid itself evolves progressively into the paleo-and-mineralized thermal liquid with high concentration,from which antimony mines in Central Hunan obtain their abundant sources of ore materials. |
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| Keywords: | deep fluid antimony with multi sources mantle plume in Central Hunan circulation between mantle and crust paleo-and-mineralized thermal liquid |
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