ZHANG Yan-jie, MA Hui-ping, ZHANG Hong-bin. Discovery of ductile shear zone and its geological significance in the Huajialing -Huluhe area, Gansu[J]. Northwestern Geology, 2003, 36(3): 24-28.
Citation: |
ZHANG Yan-jie, MA Hui-ping, ZHANG Hong-bin. Discovery of ductile shear zone and its geological significance in the Huajialing -Huluhe area, Gansu[J]. Northwestern Geology, 2003, 36(3): 24-28.
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Discovery of ductile shear zone and its geological significance in the Huajialing -Huluhe area, Gansu
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1.
Geological Survey of Gansu Province, Lanzhou 730000, China
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2.
Department of Land and Resources of Gansu Province, Lanzhou 730000, China
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3.
Geological Survey of Gansu Province, Lanzhou 730000, China
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Abstract
The ductile shear zone of Huajialing-Huluhe,a disco rdogenic fracture of North Qilian orogenic and median Qilian land mass,is brittle-ductile shear zone with multip eriodic activity,strike NWW.By analyse and research of geomet rics,kinematics,dynamics,etc.We think the deformation peak is convergence coilision of North plate and South plate at late-Caledonian,matching weak continental crust (North Qilian) of south border of North china plate oblique thrusting overlap to median Qilian rigid block at south,soit produced obduction tenacity shear structu refrom NEE to SWW and right-slip.
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References
张维吉,孟宪恂,胡键民,等.祁连-北秦岭造山带结合部位构造特征与造山过程[M].西安: 西北大学出版社,1994.
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