| 云南省宁蒗县树扎铜矿地质特征及矿床成因探讨 |
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| 引用本文： | 蓝海洋,王密.云南省宁蒗县树扎铜矿地质特征及矿床成因探讨[J].中国科技信息,2011(10):24-25. |
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| 作者姓名： | 蓝海洋 王密 |
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| 作者单位： | 辽宁省冶金地质勘查局地质勘查研究院,114002 |
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| 摘 要： | 树扎铜矿位于区域性构造的挖开断层北东,树劳河～中梁子断层南西相交的二迭系玄武岩组地层内。区域两个构造带应力集中交汇的地段,是造就树扎铜矿的导矿构造、容矿构造之原因。后期从华力西～燕山～喜山期的岩浆热液活动,对树扎铜矿的后期成矿和富集都起了重要作用。本文介绍了树扎铜矿矿区地质概况,阐述了树扎铜矿的地质特征,并对矿床成因进行了探讨分析,对该地区今后的地质工作具有一定的指导意义。
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| 关 键 词： | 树扎铜矿 地质特征 成因探讨 |
The Geological Characteristic And Genetic Discussion Of The SHUZHA Copper Deposit In Ninglang County, Yunnan Province |
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| Lan Haiyang,Wang Mi.The Geological Characteristic And Genetic Discussion Of The SHUZHA Copper Deposit In Ninglang County, Yunnan Province[J].CHINA SCIENCE AND TECHNOLOGY INFORMATION,2011(10):24-25. |
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| Authors: | Lan Haiyang Wang Mi |
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| Institution: | Lan Haiyang Wang Mi The Geological Exploration Institute of Liaoning Metallurgically Geological Exploration Bureau,Anshan 114002,Liaoning,China |
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| Abstract: | Shuzha copper deposit located in the northeast of Wakai fault and southwest of Shulao river – Zhongliangzi fault,it＇s located in the group of Permian system basalt.Two structural belts stress concentration converged in the region is the reason of structure as passageway for ore fluid and host structure of Shuzha copper deposit.The magmatic hydrothermalism of Variscan – Yanshan – Himalayan orogeny is important role to Shuzha copper deposit formation.This paper through the geological conditions of Shuzha copper ore area introduced,the geological characteristic and genetic discussion of the Shuzha copper deposit expounded,it＇s guidance significance to geological work in the future. |
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| Keywords: | Shuzha copper deposit geological characteristic origin discussion |
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