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ZHANG Hong-wei, KANG Lei, ZHAO Chun-huan, et al. Geochemical Evidence of Magma Mingling of Xiaerpu Granite in West Junggar, Xinjiang[J]. Northwestern Geology, 2011, 44(2): 41-50.
Citation: ZHANG Hong-wei, KANG Lei, ZHAO Chun-huan, et al. Geochemical Evidence of Magma Mingling of Xiaerpu Granite in West Junggar, Xinjiang[J]. Northwestern Geology, 2011, 44(2): 41-50.
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Geochemical Evidence of Magma Mingling of Xiaerpu Granite in West Junggar, Xinjiang

  • 1.

    No. 7 Geological party, BGMERD of Xinjiang, Wusu 833000, China

  • 2.

    Earth Science & Resources College of Chang'an University, Xi'an 710054, China;Xi'an Center of Geological Survey, GGS, Xi'an 710054, China

  • 3.

    No. 1 Geological party, BGMERD of Xinjiang, Changji 831100, China

  • 4.

    Earth Science & Resources College of Chang'an University, Xi'an 710054, China

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  • Received Date: May 12, 2011
  • Revised Date: May 23, 2011
  • Published Date: June 04, 2011
    Graphical Abstract
    • Abstract
  • Xiaerpu granite is one of the typical magma mixing granites in West Junggar,which is composed of the host rock,mafic microgranular enclave,and basic dyke swarm.The double diffusion and relativity of geochemistry are one of the most effective means of differentiating magma mixing.Petrochemistry features are difference between the host rock and basic dyke swarm which have distinct evolution.There was strong double diffusion between the host rock and mafic microgranular enclave,and affinity between mafic microgranular enclave and basic dyke swarm.Xiaerpu granite is the mixture between mantle magma represented by mafic microgranular enclave and basic dyke swarm and crust magma represented by the host rock.Magma mixing information from geochemistry is in conformity with petrographical feature,which support magma mixing,providing an important proof for solving the difference of Xiaerpu granite's origin from petrographical field.
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