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On the tectonic landform of the Yumu Mountain, Hexi Corridor, Gansu

On the tectonic landform of the Yumu Mountain, Hexi Corridor, Gansu

Dizhi Lixue Xuebao = Journal of Geomechanics 3(4): 21-26

The Hexi Corridor, located in the northeastern margin of the Qinghai-Tibetan plateau, is a foreland basin system formed by the northeastward push of the plateau. The Yumu mountain is a transverse highland between the Zhangye basin and Jiudong basin in the system. Based on the field study of fault outcrops and landform deformations, combining with TL and (super 14) C ages, it is concluded that the north marginal fault of the Yumu mountain is a thrust with left-lateral slipping and the east marginal fault is a thrust with right-lateral slipping, and the Yumu Mountain developed form the resulting uplifting of the Yumu Mountain block along these faults.

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