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HE Shi-ping, REN Bing-shen, YAO Wen-guang, et al. The division of tectonic units of Beishan area, Gansu-Inner Mongolia[J]. Northwestern Geology, 2002, 35(4): 30-40.
Citation: HE Shi-ping, REN Bing-shen, YAO Wen-guang, et al. The division of tectonic units of Beishan area, Gansu-Inner Mongolia[J]. Northwestern Geology, 2002, 35(4): 30-40.
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The division of tectonic units of Beishan area, Gansu-Inner Mongolia

  • Xi'an Institute of Geology and Mineral Resources, Xi'an, 710054, China

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  • Received Date: May 26, 2002
  • Revised Date: October 14, 2002
  • Published Date: December 04, 2002
    Graphical Abstract
    • Abstract
  • This paper gives some general principles about the division and naming of tectonic units of Beishan area. According to the theory of plate tectonics and polycyclic opening-closing tectonics,Beishan area is divided in to three first-order tectonic units,eight second-order tectonic units and twenty-six third-order tectonic units. There are two suture zones in Beis-han area:the Hongliuhe-Niujuanzi-Xichangjing suture zone(Early Paleozoicera)and the Hongshishan-Pengboshan suture zone(Upper Paleozoic era),and the latter is the final plate junction between the Tarim Plate and Kazakh stan Plate.
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    • References (12)
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