Extensional Seismotectonic Motion and its Dynamics in the Eastern Margin of the Tibetan Plateau and its Surroundings

Analysis on Magnitude Characteristics of the Shallow Crustal Tectonic Stress Field in Qinghai‐tibet Plateau and Its Adjacent Region Based on In‐situ Stress Data

“…Due to its unique structure and geophysical background, the Qinghai-Tibet Plateau has become a natural laboratory for the study of continental geodynamics (Zheng, *E-mail: yaorui 4123@163.com 2005). Many geoscientific aspects of the Qinghai-Tibet Plateau have been taken as hot spots by geoscientists in their studies, such as the deformation of its lithosphere, lithospheric structure, stress-strain field, geologic structure, evolution and uplifting process, and the dynamic mechanism (Magni et al, 2016;Lu et al, 2016;Xu et al, 2016;Zuza et al, 2016;Chevalier et al, 2016;Ye et al, 2016;Sternai et al, 2016;Mao et al, 2016;Ding et al, 2016;Hong, 2016;Ye, 2016;Shi et al, 2015;Ge et al, 2015;Chen et al, 2014;Yang, 2013;Zhao et al, 2011;Zhang et al, 2007;Lu et al, 2006;Xu et al, 2006;Zhang et al, 2004;Ma et al, 2004). In recent years, many scholars have studied the Qinghai-Tibet Plateau and its peripheral tectonic stress fields in several aspects, such as the geologic structure differences in east and west areas, features of crust deformation, crust-mantle structure, features of regional stress field, and anisotropic characteristics of crustal medium (Xiao et al, 2005;Yu, 2006;Zhang, 2006;Li et al, 2006;Zhang, 2007;Liu, 2010;Sun et al, 2014;Shi, 2014;Guo et al, 2014;Xiao, 2015;Eva et al, 2015;Zhu et al, 2015;Chen et al, 2015;Kumar et al, 2015;…”