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QIN Biao. Xinjiang ALeTunKunDuo Ophiolitic Melange of Geochemical Characteristics and Formation Environment[J]. Northwestern Geology, 2013, 46(2): 30-36.
Citation: QIN Biao. Xinjiang ALeTunKunDuo Ophiolitic Melange of Geochemical Characteristics and Formation Environment[J]. Northwestern Geology, 2013, 46(2): 30-36.
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Xinjiang ALeTunKunDuo Ophiolitic Melange of Geochemical Characteristics and Formation Environment

  • China Building Materials Industry Center of Xinjiang Geological Survey Corps, Urumqi, 830000, China

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  • Received Date: July 11, 2012
  • Revised Date: April 06, 2013
  • Published Date: June 04, 2013
    Graphical Abstract
    • Abstract
  • The ophiolitic melange is consisted of gabbro, plagiogranite and volcanic lava, lacking of metamorphic peridotite, ultramafic cumulate rock and diabase dike unit. The standardized distribution pattern of REE chondrite in gabbro and basic lava of ophiolitic melange, and trace elements of the primitive mantle is nearly flat. There is loss or slight loss in light rare earth, which is similar to the transitional tectonic settings of island arc(IAB) and spreading ridge(MORB), indicating that the ophiolites is probably formed in the fore-arc expansion environment of incipient arc at the bottom of SSZ Oceanic basin.
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    • References (22)
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