| 广南洒拉冲-东瓜湾金矿地质 |
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| 引用本文： | 陈书富,马绍春.广南洒拉冲-东瓜湾金矿地质[J].云南地质,2008,27(2):141-148. |
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| 作者姓名： | 陈书富 马绍春 |
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| 作者单位： | 云南省有色地质306队,昆明,650216 |
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| 摘 要： | 洒拉冲-东瓜湾金矿属于微细粒浸染型金矿及火山熔岩型金矿。金矿化受地层、构造、基性火成岩的控制。多期基性火成岩侵入，为金矿化的形成提供了热源和物源。
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| 关 键 词： | 微细粒浸染型 基性火山岩型 金矿 洒拉冲-东瓜湾 广南云南 |
Geology of Salachong - Dongguawan AU Deposit in Guangnan |
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| CHEN Shu-fu,MA Shao-chun.Geology of Salachong - Dongguawan AU Deposit in Guangnan[J].Yunnan Geology,2008,27(2):141-148. |
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| Authors: | CHEN Shu-fu MA Shao-chun |
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| Institution: | (Nonferrous Geological Team 306 of Yunnan, Kunming 650216) |
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| Abstract: | The Salachong - Dongguawan Au deposit belongs to the Au deposit type of micro- grained -fine grained dissemination and volcanic lava. The Au metallogenesis is controlled by strata, structure and basic igneous rocks. The intrusion of polyphysic basic igneous rocks provides the heat and material sources for Au metallogenesis. |
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| Keywords: | Micrograined - Fine Grained Dissemination Type Basic Volcanic Rock Type Au Deposit Salachong - Dongguawan Guangnan |
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