东天山土屋-延东斑岩铜矿围岩的同位素年代和地球化学研究

侯广顺 唐红峰 刘丛强 王彦斌. 东天山土屋-延东斑岩铜矿围岩的同位素年代和地球化学研究[J]. 岩石学报, 2005, 21(6): 1729-1736.
引用本文: 侯广顺 唐红峰 刘丛强 王彦斌. 东天山土屋-延东斑岩铜矿围岩的同位素年代和地球化学研究[J]. 岩石学报, 2005, 21(6): 1729-1736.
HOU GuangShun TANG HongFeng LIU CongQiang WANG YanBin 1.Laboratory for Study of Earth''s Interior and Geofluids,Institute of Geochemistry,CAS,Guiyang 550002,China2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China3.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China. Geochronological and geochemical study on the wallrock of Tuwu-Yandong porphyry copper deposits, eastern Tianshan mountains[J]. Acta Petrologica Sinica, 2005, 21(6): 1729-1736.
Citation: HOU GuangShun TANG HongFeng LIU CongQiang WANG YanBin 1.Laboratory for Study of Earth''s Interior and Geofluids,Institute of Geochemistry,CAS,Guiyang 550002,China2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China3.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China. Geochronological and geochemical study on the wallrock of Tuwu-Yandong porphyry copper deposits, eastern Tianshan mountains[J]. Acta Petrologica Sinica, 2005, 21(6): 1729-1736.

东天山土屋-延东斑岩铜矿围岩的同位素年代和地球化学研究

  • 基金项目:

    国家重点基础研究发展规划项目(2001CB409805)和2002年度中国科学院西部之光项目资助.致谢 本工作受国家重点基础研究发展规划项目(2001CB409805)和2002年度中国科学院西部之光项目的资助.野外工作得到李文铅和张连昌博士的热情帮助.

  • 东天山土屋-延东大型斑岩铜矿的成岩成矿时代及其构造背景还存在很大争议。本文报道了铜矿远矿围岩—企鹅山群的同位素年代和地球化学研究结果。研究表明,企鹅山群安山岩中锆石 SHRIMP U-Pb 谐和年龄值336.5±6.6Ma,玄武岩的透辉石、斜长石和全岩 Sm-Nd 内部等时线年龄值334±36Ma,两个结果一致地表明企鹅山群形成于早石炭世。元素地球化学研究表明,企鹅山群玄武岩样品属于岛弧拉斑玄武岩系列,其稀土元素配分模式显示轻稀土相对富集,重稀土相对亏损的右倾模式,与洋中脊玄武岩相比,具有大离子亲石元素相对富集、高场强元素相对亏损的特征,具有俯冲带岛弧火山岩的典型特征。构造环境判别图解也指示企鹅山群形成于俯冲带环境。本研究对土屋-延东大型斑岩铜矿的成岩成矿作用时代及其构造背景问题提供了重要制约。
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出版历程
收稿日期:  2005-03-03
刊出日期:  2005-11-30

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