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LIU Ming-qiang, DANG Yin-ye, GONG Quan-sheng. The feature of Pingtoushan thrust-nappe structure in Beishan, Gansu[J]. Northwestern Geology, 2002, 35(1): 22-27.
Citation: LIU Ming-qiang, DANG Yin-ye, GONG Quan-sheng. The feature of Pingtoushan thrust-nappe structure in Beishan, Gansu[J]. Northwestern Geology, 2002, 35(1): 22-27.
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The feature of Pingtoushan thrust-nappe structure in Beishan, Gansu

  • Lanzhou Research Institute of Geology and Mineral Resources, Gansu Bureau of Geology and Mineral Exploration and Development, Lanzhou 730050, China

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  • Received Date: July 27, 2000
  • Revised Date: November 20, 2001
  • Published Date: March 04, 2002
    Graphical Abstract
    • Abstract
  • Based on 1:250000 scale regional geological surveys,the paper describes in detail the geometrical,kinematical and dynamical characteristics of Pingtoushan thrust-nappe structure.The thrust is from north to south in direction and the extension pattern of the thrust is pickaback.The thrust-nappe structure of Pingtoushan is formed from end of the Silurian to Early Devonian.It is one of the forms of foreland a rea of arccontinent collision oroginic belt in the Caledonian stage.In Indosinian Stage,the tecnotic movement changed original position of thrust-nappe structure,and formed the present complex tectonic frame-work.
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