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GAO Tingbin, YANG Zhen, YAO Gang, et al. Redefinition of High Pressure Metamorphic Rocks from West Kunlun Orogen and Its Tectonic Significance[J]. Northwestern Geology, 2018, 51(1): 1-12.
Citation: GAO Tingbin, YANG Zhen, YAO Gang, et al. Redefinition of High Pressure Metamorphic Rocks from West Kunlun Orogen and Its Tectonic Significance[J]. Northwestern Geology, 2018, 51(1): 1-12.
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Redefinition of High Pressure Metamorphic Rocks from West Kunlun Orogen and Its Tectonic Significance

  • No.11 Geological Party, Xinjiang Bureau of Geological Mineral Exploration and Development, Changji 831100, Xinjiang, China

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  • Received Date: April 30, 2017
  • Revised Date: November 20, 2017
  • Available Online: July 28, 2022
  • Published Date: March 04, 2018
    Graphical Abstract
    • Abstract
  • A set of "Grt-Pl-Hbl gneiss and Sil-Grt-Bit-Pl gneiss" has been disintegrated from the eastern part of Tashkurghan area in West Kunlun.According to the geochemical characteristics study, the Grt-Pl-Hbl gneiss was derived from basic volcanic rocks, with the features of island-arc basalt.In the discrimination diagram, their samples are plotted in the field of island-arc basalt.The Sil-Grt-Bit-Pl gneiss was sourced from clastic rocks.In the discrimination diagram, their samples are plotted in the active continental margin and in the continental arc.According to the isotope chronology, the Grt-Pl-Hbl gneiss was formed in early Cambrian epoch.Since the formation of magma, the Grt-Pl-Hbl gneiss has experienced four notable thermal events in Silurian, Permian, Cretaceous and Miocene.The redefinition of high pressure metamorphic rocks in this area has a great significance to discussing the tectonic evolution in West Kunlun.
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