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LI Yihao, DU Xingxing, LI Tianxiu. 2022. Characterization of the Holocene extensional structures in the Wuwei Basin, northeastern margin of the Xizang Plateau, and their formation mechanism. Journal of Geomechanics, 28(3): 353-366. doi: 10.12090/j.issn.1006-6616.2021151
Citation: LI Yihao, DU Xingxing, LI Tianxiu. 2022. Characterization of the Holocene extensional structures in the Wuwei Basin, northeastern margin of the Xizang Plateau, and their formation mechanism. Journal of Geomechanics, 28(3): 353-366. doi: 10.12090/j.issn.1006-6616.2021151
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Characterization of the Holocene extensional structures in the Wuwei Basin, northeastern margin of the Xizang Plateau, and their formation mechanism

  • 1.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China

  • 3.

    Research Center of Neotectonism and Crustal Stability, China Geological Survey, Beijing 100081, China

  • 4.

    Xinjiang Oilfield Heavy Oil Development Company, Karamay 834000, Xinjiang, China

    • Fund Project: This research is financially supported by the Geological Survey Project of China Geological Survey (Grants No.DD20190018, DD20221644)
More Information
Received Date:  04 November 2021
Revised Date:  25 February 2022
Publish Date:  28 June 2022
    Abstract

  • The Wuwei Basin at the eastern end of the Hexi Corridor, between the North Qilian Mountain and the Longshou Mountain in the northeastern margin of the Xizang Plateau, was in a NE-trending compressional environment during the Holocene. Our field survey results indicate that there are two groups of near-vertical normal faults, namely the NWW-trending and NE-trending faults. The OSL dating results show that the two groups of normal faults experienced two periods of tectonic activity in 0.70 ka and 0.49~0.18 ka. The analysis concludes that the NWW-trending normal faults were formed by the differential stress perpendicular to the stratigraphy, which was produced by the continuous uplift of the Fenmenshan uplift in the Wuwei Basin. The NE-trending normal faults could be the extensional rupture (T rupture) produced by the nearly EW-trending sinistral strike-slip faults on both sides of the Wuwei Basin, or be formed by the extension vertical to the NE-trending compression of the Xizang Plateau. Therefore, the tectonic deformation in the Wuwei Basin was controlled by the tectonic activities in the northeastern margin of the Xizang Plateau during the late Holocene.

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