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WANG Jian-xin, Kang Kong-yue, HOU Ming-cai. Sedimentary Facies and Provenance Analysis of Upper Triassic Goulushankecuo Formation in Tuotuohe Area of Qinghai Province[J]. Northwestern Geology, 2014, 47(4): 123-130.
Citation: WANG Jian-xin, Kang Kong-yue, HOU Ming-cai. Sedimentary Facies and Provenance Analysis of Upper Triassic Goulushankecuo Formation in Tuotuohe Area of Qinghai Province[J]. Northwestern Geology, 2014, 47(4): 123-130.
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Sedimentary Facies and Provenance Analysis of Upper Triassic Goulushankecuo Formation in Tuotuohe Area of Qinghai Province

  • 1. No.282 Geological Party, Sichuan Bureau of Geology for Nuclear Industry, De'yang 618000, China;

  • 2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

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  • Received Date: June 09, 2014
  • Revised Date: October 04, 2014
  • Available Online: July 28, 2022
  • Published Date: December 04, 2014
    Graphical Abstract
    • Abstract
  • Through field profile measuring, sedimentary facies signs identification, thin section authentification and grading analysis, we studied the categories and features of sedimentary facies of Upper Triassic Goulushankecuo Formation. The results show that the Goulushankecuo Formation is a Delta-Neritic shelf facies system. Based on clasolite petrographic study, the statistics from provenance analysis show that the sedarenite of Triassic Goulushankecuo Formation in workspace are mainly feldspathic litharenite and lithic quartz sandstone. Lower textural and compositional maturity indicates a rapid accumulation of sediments, which is a characteristic of nearby provenance. By detrital composition analysis, it is revealed that the provenance of Upper Triassic Goulushankecuo Formation came from recycled orogen.
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