| 绿春大马尖山铜砷矿矿床成因 |
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| 引用本文： | 郑世红.绿春大马尖山铜砷矿矿床成因[J].云南地质,2010,29(4):420-423. |
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| 作者姓名： | 郑世红 |
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| 作者单位： | 云南省地勘局第二地质大队,云南文山663000 |
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| 摘 要： | 矿体赋存于下志留统变质砂板岩及侵入其中的石英斑岩中,与燕山晚期构造运动及岩浆活动有关。水平及垂直分带明显。属低温热液硫化物充填—交代型铜砷矿。
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| 关 键 词： | 铜砷铅银矿 充填一交代 石英斑岩型 下志留统砂板岩 云南绿春大马关 |
THE GENESIS OF DAMAJIANSHAN CU-AS DEPOSIT IN LUCHUN |
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| ZHENG Shi-hong.THE GENESIS OF DAMAJIANSHAN CU-AS DEPOSIT IN LUCHUN[J].Yunnan Geology,2010,29(4):420-423. |
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| Authors: | ZHENG Shi-hong |
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| Institution: | ZHENG Shi-hong ( Geological Team 2, Geoexploration Bureau of Yunnan, Wenshan 663000 ) |
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| Abstract: | The ore deposit is in the S1 metamorphic sandy slate and the quartz porphyry intrusion in it, which is in relation to the Late Yanshanian structure and magmatism. The horizontal and vertical belongs to the Cu - As deposit of low T hydrothermal sulfide filling--metasomatie type. |
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| Keywords: | Cu - As - Pb - Ag Deposit Filling - Metasomatism Quartz Porphyry Damajian Luehun Yunnan zonation is evident It Type S1 Sandy Slate |
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