supported by a grant from the Chinese Earthquake Administration (No.201308013);the National Natural Science Foundation of China (Nos.41604057, 40974034, and 41021003);a key project from the Institute of Geodesy and Geophysics
On April 20, 2013, an M_s 7.0 earthquake struck Lushan County in Sichuan Province, China, and caused serious damage to the source region. We investigated the rupture process of the M_s7.0 Lushan earthquake by jointly ...
supported by the National Natural Science Foundation of China (Nos. 41174086, 41074052, 40974034, and 41021003)
A linear projection approach is developed to present geoscience research result in planar coordinate system projected from spherical coordinate system. Here, the sphere is intersected by a plane and its surface is pro...
supported by National Natural Science Foundation of China (Grant Nos.41074052,41174086,40974034);Key project from Institute of Geodesy and Geophysics,Chinese Academy of Sciences,and Foundation for Innovative Research Groups of the National Science Foundation of China (Grant No.41021003)
Following the M w 7.9 Wenchuan earthquake, the M w 6.6 Lushan earthquake is another devastating earthquake that struck the Longmenshan Fault Zone (LFZ) and caused severe damages. In this study, we collected continuous...
supported by Chinese Seismic Array Detecting Project (Grant No.201008001);National Natural Science Foundation of China (Grant Nos.41174086,40974034,41021003)
On April 20, 2013 at 8:02 am, a magnitude 7.0 earthquake occurred in Lushan County, Sichuan Province, China, which induces massive landslides, causes great losses to life and property. Based on the locations of after...
supported by the Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX2-SW-142);the National Natural Science Foundation of China (41021003, 40974034 and90814009);the Key Project of Earthquake Science (201008007)
Based on co-seismic displacements recorded by terrestrial GPS stations and seafloor GPS/acoustic stations, the static slip model of the 2011 Mw 9.0 Tohoku earthquake was determined by inverting the data using a layere...
supported by grant 201008007 from China Earthquake Administration,National Natural Science Foundation of China(40974034,41174086)
Co-seismic deformation and gravity field changes caused by the 2011 Mw6. 8 Myanmar and Mw6. 9 India-Nepal earthquakes are calculated with a finite-element model and an average-slip model, respectively, based on the mu...
supported by the Knowledge Innovation Key Program of the Chinese Academy of Sciences (KZCX2-SW-142);the National Natural Science Foundation of China (41021003, 40974034 and 90814009);the Key Project of Earthquake Science (201008007)
用为 8 h 的测量 GPS 的 coseismic 和 seismic 以后排水量跟随 M w 2011 年 3 月 11 日, coseismic 和 seismic 以后差错的 9.0 仙台地震滑动模型基于一个分层的外壳的模型被开发。主要吃惊的测地学的时刻大小是被测量近似 M w 8.98。...
supported by Chinese Academy of Sciences (Nos.KZCX2-YW-116 and KZCX2-YW-142);National Natural Science Foundation of China (No. 40974034)
Based on the elastic dislocation theory, multilayered crustal model, and rupture model obtained by seismic waveform inversion, we calculated the coand post-seismic surface deformation and gravity changes caused by the...