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WANG Yun-bin, DING Xue-feng, ZHAO Zhi-gang, et al. Ductile shear deformation characteristics of Pianshishan in Yumenzhen area, in east section of the Sanweishan fault, Gansu[J]. Northwestern Geology, 2005, 38(4): 8-13.
Citation: WANG Yun-bin, DING Xue-feng, ZHAO Zhi-gang, et al. Ductile shear deformation characteristics of Pianshishan in Yumenzhen area, in east section of the Sanweishan fault, Gansu[J]. Northwestern Geology, 2005, 38(4): 8-13.
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Ductile shear deformation characteristics of Pianshishan in Yumenzhen area, in east section of the Sanweishan fault, Gansu

  • 1.

    School of Earth Science, Chang'an University, Xi'an 710054, China

  • 2.

    Gansu Institute of Geological Survey, Lanzhou 730000, China

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  • Received Date: April 04, 2005
  • Revised Date: September 20, 2005
  • Published Date: December 04, 2005
    Graphical Abstract
    • Abstract
  • Sanweishan fault is one of the Altun tectonic system which lies in the joint of the Huabei slab and Tarim slab.In the 1:250000 regional geological mapping of Yumenzhen,the two different characteristics, depth and different styles assemblage ductile deformation was found in Pianshishan in Yumenzhen area in Late Paleozoic and Mesozoic.
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    • References (9)
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