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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.

    Ductile shear deformation characteristics of Pianshishan in Yumenzhen area, in east section of the Sanweishan fault, Gansu

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    • Received Date: April 04, 2005
    • Revised Date: September 20, 2005
    • Published Date: December 04, 2005
    • 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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