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PEI Zhong-chao, DING Li, QIN Shuang, QU Jin, ZHAO Zhi-qiang. The discovery and significance of the corsite in the southern Altun fault, Xinjiang[J]. Sedimentary Geology and Tethyan Geology, 2004, 24(1): 41-45.
Citation: PEI Zhong-chao, DING Li, QIN Shuang, QU Jin, ZHAO Zhi-qiang. The discovery and significance of the corsite in the southern Altun fault, Xinjiang[J]. Sedimentary Geology and Tethyan Geology, 2004, 24(1): 41-45.
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The discovery and significance of the corsite in the southern Altun fault, Xinjiang

  • Henan Institute of Geological Survey, Zhengzhou 450007, Henan, China

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  • Received Date: February 18, 2004
  • Published Date: March 29, 2004
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    • Abstract
  • The occurrence, petrology and geochemistry are dealt with in details for the corsite identified for the first time in the southern Altun fault, Xinjiang. The corsite appears generally in back-arc basins or on active continental margins as the mixtures derived from the consumed oceanic crust and overlying wedge-shaped (mantle)-derived rocks. The magmas of the corsite resulted from the direct melting of the consumed oceanic crust, and were often reacted with the wedge-shaped mantle-derived rocks during their migration to the surface, (accompanied) by crystallization and differentiation.
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