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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.

    The division of tectonic units of Beishan area, Gansu-Inner Mongolia

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    • Received Date: May 26, 2002
    • Revised Date: October 14, 2002
    • Published Date: December 04, 2002
    • 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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