ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
新疆谢米斯台地区首次发现自然铜矿化
  
关键词:native copper  Xiemisitai  Xinjiang
基金项目:国家科技支撑计划项目(编号: 2011BAB06B01-03)
作者单位E-mail
王居里 大陆动力学国家重点实验室, 西北大学地质学系 jlwang@nwu.edu.cn 
王建其 大陆动力学国家重点实验室, 西北大学地质学系  
安芳 大陆动力学国家重点实验室, 西北大学地质学系  
杨猛 大陆动力学国家重点实验室, 西北大学地质学系  
宋子升 大陆动力学国家重点实验室, 西北大学地质学系  
令伟伟 大陆动力学国家重点实验室, 西北大学地质学系  
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摘要:
The First Discovery of Native Copper in Xiemisitai Area, Xinjiang
      The native copper mineralization associated with native silver was found for the first time in basalts of Xiemisitai area, Xinjiang, and chalcopyrite and bornite mineralization was found in acidic subvolcanic rocks in the same area. The native copper mineralization occurs mainly in the altered basalts and the late hydrothermal veins in the basalts. The mineralization is closely related to epidotization, carbonation, prehnitization, zeolitization and silicification. Preliminary studies suggest that the native copper and silver mineralization is related to volcanic hydrothermal activity and belongs to volcanic rock type, while the chalcopyrite and bornite mineralization belongs to porphyry type. There may be a variety of copper mineralization types in Xiemisitai area, and it is expected that new breakthrough can be made in further copper prospecting.
WANG Ju-li,WANG Jian-qi,AN Fang,YANG Meng,SONG Zi-sheng,LING Wei-wei.2013.The First Discovery of Native Copper in Xiemisitai Area, Xinjiang[J].Acta Geoscientica Sinica,34(3):371-374.
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