| 桂西古侵蚀沉积断面型金矿床 |
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| 引用本文： | 陈开礼.桂西古侵蚀沉积断面型金矿床[J].南方国土资源,2000,13(4):19-22. |
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| 作者姓名： | 陈开礼 |
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| 作者单位： | 广西地质矿产勘查开发局,广西,南宁,530023 |
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| 摘 要： | 古侵蚀沉积间断面型金矿是桂西的主要金矿床类型.文章着重分析该类型金矿成矿地质条件,论述矿床成因及成矿机理,认为此类型金矿易采易冶,经济效益显著,建议加大开发力度.
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| 关 键 词： | 古侵蚀 间断面型 矿床 成因 机理 |
| 修稿时间： | 〕 |
PALAEOEROSION SEDIMENTARY DISCONTINUITY TYPE GOLD DEPOSIT OF WESTERN GUANGXI |
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| Authors: | CHEN Kai-li |
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| Abstract: | Palaeoerosion sedimentary discontinuity type gold deposit is major type gold deposit of western Guangxi. The metallogenic geological condition of this type gold deposit are analyzed, the genesis and metallogenic mechanism are also discussed, the author thinks this type gold ore mining and semlt easy, there are remarkable economic results, and the authors propose that the devolop capability should build up. |
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| Keywords: | palaeoerosion discontinuity type mineral deposit genesis mechanism |
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