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    岩浆Cu-Ni-PGE矿床和Fe-Ti-V矿床的关键控矿因素评述:兼论与峨眉山玄武岩的关系

    骆文娟

    骆文娟, 2014. 岩浆Cu-Ni-PGE矿床和Fe-Ti-V矿床的关键控矿因素评述:兼论与峨眉山玄武岩的关系. 地球科学, 39(10): 1343-1354. doi: 10.3799/dqkx.2014.126
    引用本文: 骆文娟, 2014. 岩浆Cu-Ni-PGE矿床和Fe-Ti-V矿床的关键控矿因素评述:兼论与峨眉山玄武岩的关系. 地球科学, 39(10): 1343-1354. doi: 10.3799/dqkx.2014.126
    Luo Wenjuan, 2014. Magmatic Cu-Ni-PGE Sulfide and Fe-Ti-V Oxide Deposits and Their Relationship to Emeishan Basalt in Permian Emeishan Large IgneousProvince, SW China: A Review. Earth Science, 39(10): 1343-1354. doi: 10.3799/dqkx.2014.126
    Citation: Luo Wenjuan, 2014. Magmatic Cu-Ni-PGE Sulfide and Fe-Ti-V Oxide Deposits and Their Relationship to Emeishan Basalt in Permian Emeishan Large IgneousProvince, SW China: A Review. Earth Science, 39(10): 1343-1354. doi: 10.3799/dqkx.2014.126

    岩浆Cu-Ni-PGE矿床和Fe-Ti-V矿床的关键控矿因素评述:兼论与峨眉山玄武岩的关系

    doi: 10.3799/dqkx.2014.126
    基金项目: 

    中央级公益性科研院所基本科研业务专项资金 K1412

    中央级公益性科研院所基本科研业务专项资金 K1202

    中国地质调查局地质调查工作项目 12120113090300

    中国地质调查局地质调查工作项目 1212011220894-2

    详细信息
      作者简介:

      骆文娟(1986-),女,助理研究员,主要从事岩浆岩及相关矿产研究.E-mail: luowenjuan05@126.com

    • 中图分类号: P611.1

    Magmatic Cu-Ni-PGE Sulfide and Fe-Ti-V Oxide Deposits and Their Relationship to Emeishan Basalt in Permian Emeishan Large IgneousProvince, SW China: A Review

    • 摘要: 峨眉山大火成岩省中广泛分布着赋存Fe-Ti-V氧化物矿的层状辉长岩体和赋存Cu-Ni-PGE硫化物矿的镁铁超镁铁岩体,系统归纳并分析了这两类成矿岩浆在控矿因素、岩浆性质、岩浆过程等方面存在的差异.对比Cu-Ni-PGE硫化物矿床和Fe-Ti-V氧化物矿床差异,认为岩浆分异程度、部分熔融程度、挥发分(S和P)以及是否存在地壳混染是造成这两类矿床成矿差异的原因.一系列的矿床实例分析表明高Ti或低Ti性质并不是玄武质岩浆成矿专属性的决定性因素,Fe-Ti-V氧化物矿床和Cu-Ni-PGE硫化物矿床的形成与各自的控矿因素有关.

       

    • 图  1  峨眉山大火成岩省中Fe-Ti-V氧化物矿床与Cu-Ni-PGE硫化物矿床成矿模式简图

      Fig.  1.  The metallogenic model of the Fe-Ti-V oxide and Cu-Ni-PGE sulfide deposits in Emeishan large igneous province, SW China

      表  1  2类成矿岩体地质特征对比

      Table  1.   Comparisons between Cu-Ni-PGE sulfide-bearing intrusions and Fe-Ti-V oxide-bearing intrusions on geological features

      Fe-Ti-V氧化物矿岩体 Cu-Ni-PGE硫化物矿岩体
      侵位地层 大多数前寒武系,少数志留系 大多数泥盆系、奥陶系,少数前震旦系
      岩体出露面积 攀枝花约30 km2,白马约50 km2 金宝山约5 km2,力马河约0.12~0.16 km2,杨柳坪约0.5 km2
      辉石种类 单斜辉石 斜方辉石
      围岩特征 白云质灰岩、玄武岩 含少量黄铁矿的硅质岩
      磷灰石 攀枝花岩体中间带的岩石含5%磷灰石
      伴生岩体 中酸性岩
      下载: 导出CSV
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