ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
汶川地震断裂作用研究新认识
  
关键词:Wenchuan earthquake  coseismic weakening  fault healing  friction coefficient  Yingxiu–Beixhuan fault  Longmen Mountain
基金项目:国科学技术部项目(汶川地震断裂带科学钻探WFSD);中国地质调查局项目(编号: 12120114075801);国家自然科学基金项目(编号: 41330211)
作者单位E-mail
王焕 中国地质科学院地质研究所  
李海兵 中国地质科学院地质研究所 lihaibing06@163.com 
司家亮 中国地质科学院地质研究所  
孙知明 中国地质科学院地质力学研究所  
付小方 四川省地质调查院  
刘栋梁 中国地质科学院地质研究所  
裴军令 中国地质科学院地质力学研究所  
李成龙 中国地质大学(武汉)
中国地质科学院地质研究所, 大陆构造与动力学国家重点实验室 
 
张佳佳 成都理工大学
中国地质科学院地质研究所, 大陆构造与动力学国家重点实验室 
 
宋圣荣 国立台湾大学  
郭力伟 国立台湾大学  
MORI James 日本京都大学  
薛莲 加州大学圣克鲁兹分校, 地球与行星科学系  
BRODSKY E. Emily 加州大学圣克鲁兹分校, 地球与行星科学系  
云锟 四川省地质调查院
中国地质科学院地质研究所, 大陆构造与动力学国家重点实验室 
 
龚正 中国地质科学院地质研究所, 大陆构造与动力学国家重点实验室  
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摘要:
Progress in the Study of the Wenchuan Earthquake Faulting
      After the 2008 Wenchuan earthquake, questions as to how earthquakes occur and when the next large earthquake happens have been asked. These questions are involved in the scientific questions which have been unsolved by geologists and geophysicists, for examples, how do faults rupture? How do faults heal in preparation for the next earthquake? The authors are trying to answer these questions by investigating the internal structures of the Wenchuan earthquake fault zone, fault friction behavior and healing process. The principal slip zone of the Wenchuan earthquake was determined by detailed research based on the WFSD-1 core and outcrop investigation. The dynamic weakening and friction behavior of the Wenchuan earthquake fault was analyzed by long-term temperature monitoring. Long-term hydrological monitoring reveals permeability variations in the Wenchuan fault zone which indicate fault healing process. Based on the information obtained, this paper discusses the Wenchuan earthquake faulting process and the above questions. It is confirmed that the Wenchuan earthquake fault zone (the Yingxiu-Beichuan fault zone) was 105~240 m wide and consisted of 5 different units with different fault rocks, where seismic events occurred repeatedly with multiple coseismic fault weakening mechanisms. Coseismic graphitization occurred during the Wenchuan earthquake; the lowest dynamic friction coefficient (0.02) was measured, and for the first time, the signals showing quick fault healing were recorded. These results not only directly answer the key questions that have puzzled geologists and seismophysiccal researchers for decades but also have important significance for improving the seismic faulting theory and understanding the Wenchuan earthquake fault mechanisms, thus providing a theoretical basis for seismic prevention and disaster mitigation.
WANG Huan,LI Hai-bing,SI Jia-Liang,SUN Zhi-ming,FU Xiao-fang,LIU Dong-liang,PEI Jun-ling,LI Cheng-long,ZHANG Jia-jia,SONG Sheng-rong,KUO Li-wei,MORI James,XUE Lian,BRODSKY E. Emily,YUN Kun,GONG Zheng.2015.Progress in the Study of the Wenchuan Earthquake Faulting[J].Acta Geoscientica Sinica,36(3):257-269.
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