| 个旧东区基性火山岩型铜矿床地质特征和成因探讨 |
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| 引用本文： | 路红记. 个旧东区基性火山岩型铜矿床地质特征和成因探讨[J]. 有色金属(矿山部分), 2008, 60(1): 21-24,33 |
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| 作者姓名： | 路红记 |
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| 作者单位： | 云南锡业集团(控股)有限责任公司总公办,云南,个旧,661000 |
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| 摘 要： | 通过对个旧东区基性火山岩型铜矿的矿床地质、微量元素、稀土元素、硫同位素、铅同位素及矿物包裹体等的分析表明,区内铜矿床的产出与地层产状一致,其形成与印支期基性火山岩活动可能有着直接的成因关系。
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| 关 键 词： | 玄武岩成矿 印支期 铜矿床 基性火山岩 |
| 文章编号： | 1671-4172（2008）01-0021-04 |
An Approach to Geologic Features and Genesis of Basic Volcanic Rock-type Copper Deposit in Eastern Gejiu Zone |
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| LU Hongji. An Approach to Geologic Features and Genesis of Basic Volcanic Rock-type Copper Deposit in Eastern Gejiu Zone[J]. , 2008, 60(1): 21-24,33 |
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| Authors: | LU Hongji |
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| Abstract: | The geological features,trace elements,REE,sulphur isotope,lead isotope,and mineral inclusions of basic volcanic rock-type copper deposits in eastern Gejiu zone are studied.It's proved that the location of copper ore bodies is consistent with the attitude of strata,and their formation is directly related with basic volcanism of the Indo-Chinese epoch in Gejiu. |
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| Keywords: | basalt mineralization Indo-Chinese epoch copper deposit basic volcanic rock |
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