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| 湘中锑矿深源流体的地幔柱成矿演化 | |
| 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. |
| 作者姓名： | 黎盛斯 |
| 作者单位： | 湖南省地质矿产厅 |
| 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。 |
| 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].Hunan Geology,1996,15(3):137-142. | |
| Authors: | Li Shengsi Hunan Bureau of Geology and Mineral Resources |
| Institution: | Li Shengsi Hunan Bureau of Geology and Mineral Resources |
| 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. |
| 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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