1000-9116
2011 Issue 3
Internal structure of Longmenshan fault zone at Hongkou outcrop,Sichuan,China,that caused the 2008 Wenchuan earthquake
Tetsuhiro Togo~ Toshihiko Shimamoto~2 Shengli Ma~2 Xueze Wen~3 and Honglin He~2 1 Department of Earth and Planetary Systems Science;Graduate School of Science;Hiroshima University;Higashi-Hiroshima;739-8526;Japan 2 State Key Laboratory of Earthquake Dynamics;Institute of Geology;China Earthquake Administration;Beijing 100029;China 3 Earthquake Administration of Sichuan Province;Chengdu 610041;China
Tetsuhiro Togo~ Toshihiko Shimamoto~2 Shengli Ma~2 Xueze Wen~3 and Honglin He~2 1 Department of Earth and Planetary Systems Science;Graduate School of Science;Hiroshima University;Higashi-Hiroshima;739-8526;Japan 2 State Key Laboratory of Earthquake Dynamics;Institute of Geology;China Earthquake Administration;Beijing 100029;China 3 Earthquake Administration of Sichuan Province;Chengdu 610041;China
..............page:249-265
High-velocity frictional behavior of Longmenshan fault gouge from Hongkou outcrop and its implications for dynamic weakening of fault during the 2008 Wenchuan earthquake
Tetsuhiro Togo~ Toshihiko Shimamoto~2 Shengli Ma~2 and Takehiro Hirose~3 1 Department of Earth and Planetary Systems Science;Graduate School of Science; Hiroshima University;Higashi-Hiroshima;739-8526;Japan 2 State Key Laboratory of Earthquake Dynamics.Institute of Geology;China Earthquake Administration;Beijing 100029;China 3 Kochi Institute for Core Sample Research;Japan Agency for Marine-Earth Science and Technology;200 Monobe-otsu;Kochi 783-8502;Japan
Tetsuhiro Togo~ Toshihiko Shimamoto~2 Shengli Ma~2 and Takehiro Hirose~3 1 Department of Earth and Planetary Systems Science;Graduate School of Science; Hiroshima University;Higashi-Hiroshima;739-8526;Japan 2 State Key Laboratory of Earthquake Dynamics.Institute of Geology;China Earthquake Administration;Beijing 100029;China 3 Kochi Institute for Core Sample Research;Japan Agency for Marine-Earth Science and Technology;200 Monobe-otsu;Kochi 783-8502;Japan
..............page:267-281
Theoretical and experimental study of 3-D initial fracture and its significance to faulting
Shiyu Li~ Taiming He~1 Chunkai Teng~2 Xuyao Zheng~1 and Kuksenko Viktor~3 1 Institute of Geophysics;China Earthquake Administration;Beijing 100081;China 2 Institute of Geology and Geophysics;Chinese Academy of Sciences;Beijing 100029;China 3 A F Ioffe Physical-Technical Institute;Russian Academy of Sciences;St.Petersburg 194021;Russia
Shiyu Li~ Taiming He~1 Chunkai Teng~2 Xuyao Zheng~1 and Kuksenko Viktor~3 1 Institute of Geophysics;China Earthquake Administration;Beijing 100081;China 2 Institute of Geology and Geophysics;Chinese Academy of Sciences;Beijing 100029;China 3 A F Ioffe Physical-Technical Institute;Russian Academy of Sciences;St.Petersburg 194021;Russia
..............page:283-298
Crustal structure beneath Beijing and its surrounding regions derived from gravity data
Wenliang Jiang~ Jingfa Zhang~1 Xiaocui Lu~2 and Jing Lu~1 1 Institute of Crustal Dynamics;China Earthquake Administration;Beijing 100085;China 2 Science and Technology University of Shandong;Qingdao 252600;China
Wenliang Jiang~ Jingfa Zhang~1 Xiaocui Lu~2 and Jing Lu~1 1 Institute of Crustal Dynamics;China Earthquake Administration;Beijing 100085;China 2 Science and Technology University of Shandong;Qingdao 252600;China
..............page:299-310
Evaluation model of landslide hazards induced by the 2008 Wenchuan earthquake using strong motion data
Xiuying Wang~ Gaozhong Nie~2 and Mujun Ma~3 1 Institute of Crustal Dynamics;China Earthquake Administration;Beijing 100085;China 2 Institute of Geology;China Earthquake Administration;Beijing 100029;China 3 National Earthquake Response Support Service;Beijing 100049;China
Xiuying Wang~ Gaozhong Nie~2 and Mujun Ma~3 1 Institute of Crustal Dynamics;China Earthquake Administration;Beijing 100085;China 2 Institute of Geology;China Earthquake Administration;Beijing 100029;China 3 National Earthquake Response Support Service;Beijing 100049;China
..............page:311-318