[1] |
LIU Yuan-Zheng, MA Jin, MA Wen-Chao.
The role of the Zipingpu reservoir in the generation of the Wenchuan earthquake.
[J]. Earth Science Frontiers, 20140101, 21(1): 150-160.
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[2] |
LI Xi,XU Xiwei,Zhang Jianguo,XIE Yingqing,YU Jiang,ZHANG Yanqi.
Surface rupture characteristics of the seismogenic structure of the Ludian MS 6.5 earthquake and identification and dating of related paleoearthquakes
[J]. Earth Science Frontiers, 2018, 25(1): 227-239.
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[3] |
WANG Chi-Hua, GUO Zhao-Cheng, DU Meng-Liang, CHENG Zun-Lan.
Model study of predicting rainstorm induced landslide and debris flow at Niumian Gully, the focal area of 20080512 Earthquake.
[J]. Earth Science Frontiers, 2012, 19(1): 228-238.
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[4] |
YUAN Ren-Mao, TAN Ti-Bin, CHEN Gui-Hua, XU Ti-Wei.
Huge landslides occurred at the special places of the coseismic rupture and their mechanism explanation based on the formation model of tectonicgeomorphology: A case study of Donghekou ejection landslide.
[J]. Earth Science Frontiers, 2010, 17(5): 243-253.
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[5] |
GUO Zhao-Cheng, ZHOU Cheng-Hu, SUN Xiao-Yu, ZHANG Dun.
The distribution of landslide triggered by Wenchuan earthquake and its causative factors.
[J]. Earth Science Frontiers, 2010, 17(5): 234-242.
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[6] |
SHU Ai-Lan, JIE Chao-Di, XU Ti-Wei, ZHOU Yong-Qing, Lei Xinglin, WANG E-Li.
Investigation on the possible triggered seismicity in the peripheral areas of the Ordos block by the Wenchuan earthquake.
[J]. Earth Science Frontiers, 2010, 17(5): 206-214.
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[7] |
DENG Qi-Dong, GAO Xiang, CHEN Gui-Hua, YANG Hu.
Recent tectonic activity of Bayankala faultblock and the KunlunWenchuan earthquake series of the Tibetan Plateau.
[J]. Earth Science Frontiers, 2010, 17(5): 163-178.
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[8] |
JIAN Qi, HAN Zhu-Jun.
Determination of the initial rupture of the 2008 Wenchuan Ms 80 earthquake from analysis of fault interaction during the main shock process.
[J]. Earth Science Frontiers, 2010, 17(5): 84-92.
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[9] |
TAN Ti-Bin, YUAN Ren-Mao, XU Ti-Wei, CHEN Gui-Hua.
The special characteristics of rupture induced by Ms 80 Wenchuan earthquake, in Leigu area,and its mechanism.
[J]. Earth Science Frontiers, 2010, 17(5): 75-83.
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[10] |
WEI Tie-Yu, DAN Feng, GAO Xiang, XU Chang-Feng, HE Hong-Lin.
Topographic characteristics of rupture surface associated with Wenchuan earthquake.
[J]. Earth Science Frontiers, 2010, 17(5): 53-66.
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[11] |
WANG Hu, DAN Yong-Kang, CHEN Li-Chun, CHEN Wen-Shan, YANG Zhi-Cheng, XU Ti-Wei.
The study of nearfault horizontal shortening of the surface rupture in Wenchuan Ms 80 earthquake.
[J]. Earth Science Frontiers, 2010, 17(5): 43-52.
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[12] |
HE Hong-Lin, WEI Tie-Yu, CHEN Chang-Yun, DAN Feng.
Slip vectors on the Longmenshan fault during the Wenchuan earthquake of 2008.
[J]. Earth Science Frontiers, 2010, 17(5): 19-32.
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[13] |
XU Gui-Hua, XU Ti-Wei, Yann Klinger, DIAO Gui-Lian, CHEN Gui-Hua, FENG Xiang-Dong, LI Chen-Xia, SHU Ai-Lan, YUAN Ren-Mao, GUO Ting-Ting, TAN Ti-Bin, AN Yan-Fen, SUN Xin-Zhe.
Earthquake fault scarps and cascadingrupture model for the Wenchuan earthquake.
[J]. Earth Science Frontiers, 2010, 17(5): 1-18.
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[14] |
HAN Jin-Liang TUN Shu-Ren HE Chu-Jun SUN Wei-Feng ZHANG Chun-Shan WANG Chao YANG Jin-Zhong DAN Ju-Song.
Basal characteristics and formation mechanisms of geological hazards triggered by the May 12, 2008 Wenchuan earthquake with a moment magnitude of 8.0
[J]. Earth Science Frontiers, 2009, 16(3): 306-326.
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[15] |
BI Qi.
Major earthquakes by rheological diapirism of crustmantle material—Evidence from satellite gravity data
[J]. Earth Science Frontiers, 2009, 16(3): 282-293.
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