ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
新疆谢米斯台地区斑岩型铜矿化的发现及其意义
  
关键词:porphyry copper mineralization  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  
胡洋 大陆动力学国家重点实验室, 西北大学地质学系  
涂一安 大陆动力学国家重点实验室, 西北大学地质学系  
王敏 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 Discovery of Porphyry Copper Mineralization in Xiemisitai Area of Xinjiang and Its Significance
      The porphyry copper mineralization with a certain scale was found in intermediate-acidic subvolcanic rocks after the discovery of native copper mineralization in basalts of Xiemisitai area, Xinjiang. The primary sulfides are mainly chalcopyrite, pyrite and bornite. The porphyry copper mineralization occurs mainly in the altered rhyolitic porphyry, dacitic porphyry and andesitic porphyrite, and intense epidotization, chloritization, carbonation and silicification and weak argillation occur in the mineralized rocks. This discovery shows that there are two types of copper mineralization in Xiemisitai area, and it is expected that new breakthrough can be made in further copper prospecting. The mineralized subvolcanic rocks and the hypabyssal intrusive bodies beneath the subvolcanic rocks may be the important targets for the further porphyry copper prospecting in Xiemisitai area.
WANG Ju-li,WANG Jian-qi,HU Yang,TU Yi-an,WANG Min,LING Wei-wei.2014.The Discovery of Porphyry Copper Mineralization in Xiemisitai Area of Xinjiang and Its Significance[J].Acta Geoscientica Sinica,35(3):395-398.
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