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[1]Rupture branching, propagation, and termination at the eastern end of the 2021 Mw 7.4 Maduo earthquake, northern Tibetan plateau
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[2]Fault Orientation Trumps Fault Maturity in Controlling Coseismic Rupture Characteristics of the 2021 Maduo Earthquake
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[3]Late Quaternary slip rate of the Zihong Shan branch and its implications for strain partitioning along the Haiyuan Fault, northeastern Tibetan Plateau
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[4]Airborne LiDAR-Based Mapping of Surface Ruptures and Coseismic Slip of the 1955 Zheduotang Earthquake on the Xianshuihe Fault, East Tibet
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[5]Discontinuous Surface Ruptures and Slip Distributions in the Epicentral Region of the 2021 Mw7.4 Maduo Earthquake, China
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[6]High-resolution Structure-from-Motion models covering 160 km-long surface ruptures of the 2021 Mw 7.4 Madoi earthquake in northern Tibet
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[7]Coseismic slip gradient at the western terminus of the 1920 Haiyuan Mw 7.9 earthquake
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[8]Reevaluation of the Late Pleistocene slip rate of the Haiyuan fault near Songshan, Gansu province, China
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[9]利用构造地貌方法限定走滑断裂第四纪滑动速率的不确定性及意义：以海原断裂带为例
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[10]2021年青海玛多MW7.4地震同震地表破裂长度的讨论
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[11]基于机器学习的地表破裂自动识别和填图——以2021年青海玛多MW7.4级地震为例
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[12]基于摄影测量技术对玛多MW7.4地震地表破裂特征的快速提取及三维结构的室内重建
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[13]2021年玛多MW7.4地震震中区地表破裂的精细填图及阶区内的分布式破裂讨论
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[14]利用R语言半自动化提取河流阶地—以米家山黄河阶地为例
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[15]Detailed mapping of the surface rupture of the 12 february 2014 yutian m s 7.3 earthquake, altyn tagh fault, xinjiang, china
