2016
DOI: 10.4172/2381-8719.1000234
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Extensional Seismotectonic Motion and its Dynamics in the Eastern Margin of the Tibetan Plateau and its Surroundings

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“…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;…”
Section: Introductionmentioning
confidence: 99%
“…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;…”
Section: Introductionmentioning
confidence: 99%