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斑岩铜矿的源岩或源区探讨

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文章导航 > 岩石学报 > 2004 > 20(2): 229-238

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芮宗瑶 张立生 陈振宇 王龙生 刘玉琳 王义天. 斑岩铜矿的源岩或源区探讨[J]. 岩石学报, 2004, 20(2): 229-238.
引用本文: 芮宗瑶 张立生 陈振宇 王龙生 刘玉琳 王义天. 斑岩铜矿的源岩或源区探讨[J]. 岩石学报, 2004, 20(2): 229-238.
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RUI ZongYao,ZHANG LiSheng,CHEN ZhenYu,WANG LongSheng,LIU YuLin and WANG YiTian Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China Chendu Institute of Geology and Mineral Resources,Chinese Academy of Geological Sciences,Chengdu 610082,China Department of Geology,Beijing University,Beijing 100871,China. Approach on source rock or source region of porphyry copper deposits[J]. Acta Petrologica Sinica, 2004, 20(2): 229-238.
Citation: RUI ZongYao,ZHANG LiSheng,CHEN ZhenYu,WANG LongSheng,LIU YuLin and WANG YiTian Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China Chendu Institute of Geology and Mineral Resources,Chinese Academy of Geological Sciences,Chengdu 610082,China Department of Geology,Beijing University,Beijing 100871,China. Approach on source rock or source region of porphyry copper deposits[J]. Acta Petrologica Sinica, 2004, 20(2): 229-238.
shu

斑岩铜矿的源岩或源区探讨

    • [1]中国地质科学矿产资源研究所，北京100037 [2]成都地质矿产研究所，四川成都610082 [3]北京大学地质系，北京100871

  • 基金项目:

    国土资源大调查项目199910200246的资助

Approach on source rock or source region of porphyry copper deposits

    摘要
  • 世界斑岩铜矿主要产于中亚-蒙古带，环太平洋带和特提斯带，上述三个地带分别为古生代、中新生代和新生代聚合板块最活跃的地区。还有少数斑岩铜矿产于前寒武纪造山带，推测类似的板块聚合的地质环境可能从前寒武纪就开始了。作者结合斑岩铜矿产出的地质环境分析，利用大量锶初始值、εNd(t)，εSr(t)和REE等资料，说明成矿斑岩的源岩或源区与大洋玄武岩(或亏损上地幔)比较接近。由此推测成矿斑岩主要是洋壳或上地幔部分熔融的产物，但也有部分下地壳混合的证据。斑岩铜矿带在空间上与活动大陆边缘相吻合，与板块缝合带相伴生(产于板块缝合带的上盘)；在时间上从洋壳俯冲(Subduction)到陆陆碰撞造山过程(Continent-continent collision orogeny)都有斑岩铜矿产生，因此，它们贯穿活动大陆边缘增生到岩石圈折沉整个过程。
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    • 参考文献(42)
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修回日期:  2003-10-02
刊出日期:  2004-03-31

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