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- W2361944136 abstract "The Zhangbaling uplift is located in a tectonic transition zone(collision-amalgamation zone)between the North and South China blocks. It is bounded on the west by the famous Tanlu fault zone, and on its eastern side there occurs a foreland fold-and-thrust belt of the pre-Jurassic sedimentary cover of the Yangtze block. The authors found a 2.5 km wide strike-slip ductile shear zone in the metamorphic basement rocks in the Lai'an area along the eastern side of the Zhangbaling uplift. Detailed field surveys and analyses of the lithology, microfabrics and deformation kinemics of this strike-slip shear zone have been conducted. The results show that the shear zone is composed of protomylonite, mylonite and ultramylonite; the foliations are nearly upright and the lineations on the foliations dip gently dipping to SW at plunge angles of 10-30°. S-C fabrics and asymmetric rotational augens in mylonite indicate sinistral shear and locally dextral shear. Based on the dislocation density measurements in matrix quartz, the differential stresses have been estimated at 65-75 MPa for this shear zone. Analysis of the mineral composition and microstructures of mylonite suggests that the basement ductile shear zone formed at temperatures of 250-400℃ and at depths equivalent to the transition zone(10-20 km deep)between the upper and lower crust." @default.
- W2361944136 created "2016-06-24" @default.
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- W2361944136 date "2007-01-01" @default.
- W2361944136 modified "2023-09-28" @default.
- W2361944136 title "Discovery of a basement strike-slip ductile shear zone on the eastern margin of the Zhangbaling uplift, Anhui, China, and its tectonic significance" @default.
- W2361944136 hasPublicationYear "2007" @default.
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