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- W2393036874 abstract "The mechanism of the regional tectonic is SN compression generally in the Yinshishan area, northern edge of Qinqhai-Tibet plateau. Main tectonic performances are as follows: EW-directed thrust faults and relevant different-uplifted fault-blocks, two phases of compressive folds in the Oligocene Aketashi Formation, neotectonic strike-slip faults and the relevant types of the strike-slip lakes. Late Neozoic extensional structure could not be discovered in detailed field geological survey in the area. The mechanism of neotectonic characteristics can be regarded as the upper lithospheric breakup and uplifting caused by the delamination of the late Cenozoic lithospheric mantle and upwelling of asthenosphere mantle.The persistent SN compression between Indian Plate and Tarim Plate results in the area under the violent compressive stress,which made crust surface thurst along the fracture,resulting in different uplifts." @default.
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- W2393036874 date "2003-01-01" @default.
- W2393036874 modified "2023-09-23" @default.
- W2393036874 title "The mechanisms of different uplifts in the Yinshishan area, northern edge of Qinghai-Tibet plateau" @default.
- W2393036874 hasPublicationYear "2003" @default.
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