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- W2355217596 abstract "Based on interpreting the artificial and natural seismic profiles,and analyzing the geologic survey data of the Northwestern margin of the Tarim basin,the spatial relationship of the Southern Tien Shan and Pamir of Western Kunlun thrust belts was studied.The results indicate that the structural junction of the two thrust belts at the shallow part was between the Atushi and Kelatuo-Mingyaole anticlinal belts.The Southern Tien Shan thrust belt can be divided into two parts vertically,an imbricate thrust system seated at the shallow and a complex duplex buried at the deep.The Pamir of the Western Kunlun thrust belt can be divided into two parts horizontally,the Kelatuo-Mingyaole anticlinal belt at the North and the Wuboer piggyback basin at the South which are separated by the Wuboer basement fault.At the deeper part,influenced by the collision of the Indian plate and Eurasia plate together,with the dextral strike-slip movement of the Wuboer fault since Cenozoic,the Tarim block subducted under the continental crust both at its north and south margins.This subduction caused the reactivation and uplift of the Southern Tienshan and Western Kunlun." @default.
- W2355217596 created "2016-06-24" @default.
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- W2355217596 date "2010-01-01" @default.
- W2355217596 modified "2023-09-25" @default.
- W2355217596 title "The Spatial Relationship of the Southern Tien Shan and Pamir of Western Kunlun Thrust Belts" @default.
- W2355217596 hasPublicationYear "2010" @default.
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