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