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- W2367897536 abstract "Longquanguan ductile shear zone(DSZ)is situated in the contact of Wutaishan granite-greenstone terrain and Fuping high-grade metamorphic terrain.It transformed not only the “Fuping group”,but also the “Wutai group”.The studies of macrostructure, microtexture and mineral assenblages show that Longquanguan DSZ underwent two stages of deformation.The early stage deformation occured in the collision of Hengshan terrain-Chechang island are-Fuping terrrain,and formed a low angle reversal DSZ,which led the crust to thicken obviously. The later stage deformation occured in the large scale logitudinal extention of the remarkable thickening crust,which led the crust to develop balancedly and formed a low angle extention DSZ.The deformation characteristics of Longquanguan DSZ reflect the tectonic evolution of the late Archaean collision orogenic belt in Wutaishan area." @default.
- W2367897536 created "2016-06-24" @default.
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- W2367897536 date "1997-01-01" @default.
- W2367897536 modified "2023-09-23" @default.
- W2367897536 title "A new wiewpoint of LONGQUANGUAN Ductile Shear Zong" @default.
- W2367897536 hasPublicationYear "1997" @default.
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