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- W2353226798 abstract "Intensive coseismic surface deformation was produced by the 12 May 2008 Wenchuan Ms 8.0 earthquake along the pre- existing NE-trending Yingxiu-Beichuan and the Guanxian-Anxian faults,in the Longmen Shan fault zone.The post-earthquake geological investigation shows that the most of surface ruptures occurred along the carbonaceous argillite,shale and coal-bearing layers, which are low-frictional layers to form slip interface within the fault zone.We found that fresh fault gouges with a thickness of 1～2 cm occurred along the co-seismic surface rupture zone,which suggests that the coseismic slip concentrated in a narrow slip zone of thickness ranging from 0.5～2 cm although the coseismic vertical and horizontal dislocations are larger than 6 meters.These fresh fault gouges within co-seismic slip zone are resulted from both thermal pressurization and frictional melting during rapid faulting movement at the shallow crust level." @default.
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- W2353226798 date "2008-01-01" @default.
- W2353226798 modified "2023-09-27" @default.
- W2353226798 title "Preliminary study of coseismic fault gouge occurred in the slip zone of the Wenchuan Ms 8.0 earthquake and its tectonic implications" @default.
- W2353226798 hasPublicationYear "2008" @default.
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