Geometry, slip rate, and the latest earthquake of the Jinta Nanshan Fault: Interactions of the Altyn Tagh Fault and the Qilian Shan at the northern margin of the Tibetan Plateau

Author:

Zhang Bo,Allen Mark B.,Yao Yunsheng,Zhu Junwen,Wu Ming,Wang Weitong,Wen Yameng,He Wengui,Lei Zhongsheng,Pang Wei

Funder

National Natural Science Foundation of China

China Scholarship Council

Publisher

Elsevier BV

Reference67 articles.

1. An Introduction to Optical Dating: The Dating of Quaternary Sediments by the Use of Photon-Stimulated Luminescence;Aitken,1998

2. Partitioning of oblique convergence coupled to the fault locking behavior of fold-and-thrust belts: evidence from the Qilian Shan, northeastern Tibetan Plateau;Allen;Tectonics,2017

3. An oblique subduction model for closure of the Proto-Tethys and Palaeo-Tethys oceans and creation of the Central China Orogenic Belt;Allen;Earth Sci. Rev.,2023

4. Geodetic evidence for a low slip rate in the Altyn Tagh fault system;Bendick;Nature,2000

5. Constraining the distribution of vertical slip on the South Heli Shan Fault (Northeastern Tibet) from high-resolution topographic data;Bi;J. Geophys. Res. Solid Earth,2018

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