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Anisotropic upper crust above the aftershock zone of the 2013 Ms 7.0 Lushan earthquake from the shear wave splitting analysis 期刊论文
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2015, 卷号: 16, 期号: 10
作者:  Liu, Ying;  Zhang, Haijiang;  Zhang, Xin;  Pei, Shunping;  An, Meijian;  Dong, Shuwen
收藏  |  浏览/下载:18/0  |  提交时间:2022/06/21
SAN-ANDREAS FAULT  W 6.6 LUSHAN  2008 WENCHUAN EARTHQUAKE  KARADERE-DUZCE BRANCH  SEISMIC ANISOTROPY  FOCAL MECHANISMS  SICHUAN  STRESS  RELOCATION  PARKFIELD  
Pn wave velocity and anisotropy beneath Pamir and its adjacent regions 期刊论文
EARTHQUAKE SCIENCE, 2012, 卷号: 25, 期号: 5-6
作者:  Feng, Biao;  Pei, Shunping
收藏  |  浏览/下载:25/0  |  提交时间:2022/06/21
Pn Tomographic Velocity and Anisotropy beneath the Iran Region 期刊论文
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2012, 卷号: 102, 期号: 1
作者:  Lu, Yan;  Liu, Bin;  Pei, Shunping;  Sun, Youshun;  Toksoez, M. Nafi;  Zeng, Xiangfang
收藏  |  浏览/下载:12/0  |  提交时间:2022/06/21
SURROUNDING REGIONS  PLATEAU  WAVE  DEFORMATION  EVOLUTION  TURKEY  PROPAGATION  GEOLOGY  TETHYS  CHINA  
Three-dimensional seismic velocity structure across the 2008 Wenchuan Ms 8.0 earthquake, Sichuan, China 期刊论文
TECTONOPHYSICS, 2010, 卷号: 491, 期号: 1-4
作者:  Pei, Shunping;  Su, Jinrong;  Zhang, Haijiang;  Sun, Youshun;  Toksoez, M. Nafi;  Wang, Zhi;  Gao, Xing;  Jing Liu-Zeng;  He, Jiankun
收藏  |  浏览/下载:22/0  |  提交时间:2022/06/21
DOUBLE-DIFFERENCE TOMOGRAPHY  CALIFORNIA  FAULT  
S wave tomography of the crust and uppermost mantle in China 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2008, 卷号: 113, 期号: B11
作者:  Sun, Youshun;  Tokoz, M. Nafi;  Pei, Shunping;  Zhao, Dapeng;  Morgan, F. Dale;  Rosca, Anca
收藏  |  浏览/下载:9/0  |  提交时间:2022/06/21
VELOCITY STRUCTURE  P-WAVE  BENEATH  INVERSION  WESTERN  SHEAR  ALGORITHM  MODEL  
The layered shear-wave velocity structure of the crust and uppermost mantle in China 期刊论文
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2008, 卷号: 98, 期号: 2
作者:  Sun, Youshun;  Toksoez, M. Nafi;  Pei, Shunping;  Morgan, F. Dale
收藏  |  浏览/下载:25/0  |  提交时间:2022/06/21
TOMOGRAPHY  INVERSION  MODEL