| 黔西南锑矿床成因探讨 |
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| 引用本文： | 廖善友.黔西南锑矿床成因探讨[J].贵州科学,1998,16(4):276-279. |
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| 作者姓名： | 廖善友 |
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| 作者单位： | 贵州教育学院地理系!550003 |
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| 摘 要： | 利用黔西南地区锑矿地质资料，各种测试数据及实际观察探讨该区锑矿床成因，研究认为：锑矿物质来源于上地幔，与玄武岩关系密切，矿床类型属层控型火山沉积后期改造矿床。矿床受构造控制明显，与石油天然气运移储集颇为相似。
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| 关 键 词： | 锑矿床 构造控矿 成因 时空分布 |
Investigation of Antimony Deposit Formation in Southwest Guizhou |
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| Liao Shanyou.Investigation of Antimony Deposit Formation in Southwest Guizhou[J].Guizhou Science,1998,16(4):276-279. |
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| Authors: | Liao Shanyou |
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| Abstract: | How the antimony deposit in Southwcst Guizhou develop will be seen through the geographical intbrmation, a lot of survey data and on-the-spot investigations. The substance came from the earth's mantle and have intimate relations with basalt. The deposit was intervened in the later stage of the sinking of volcano. Its formation lave some similarities with natural gas storage. |
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| Keywords: | Antimony deposit Formation controlled mineral Southwest Guizhou |
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