Earthquake-caused and non-earthquake-caused soft-sediment deformations
Du Yuansheng1, 2, Yu Wenchao1, 2
1 State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences(Wuhan),Wuhan 430074,Hubei; 2 School of Earth Sciences,China University of Geosciences(Wuhan),Wuhan 430074,Hubei;
Abstract Earthquake event deposit(seismites)is a “hot spot”in modern sedimentary geological study. Earthquake-caused soft-sediment deformations are easily confused with non-earthquake-caused soft-sediment deformations. This paper discusses earthquake-caused and non-earthquake-caused (ice melting process,natural gas hydrate leakage,hydrofracturing,slide,slump,debris flow,liquefiedsoft-sediment deformations) soft-sediment deformations and relationship between synsedimentary,penecontemporaneous earthquake-caused and non-earthquake-caused soft-sediment deformations.
Fund:Financially supported by the National Natural Science Fundation of China(No.41672106)
About author: About the first author Du Yuansheng,born in 1958,is a professor and Ph.D. supervisor of China University of Geosciences(Wuhan). He is mainly engaged in researches of sedimentology. E-mail: duyuansheng126@126. com.
Cite this article:
Du Yuansheng,Yu Wenchao. Earthquake-caused and non-earthquake-caused soft-sediment deformations[J]. JOPC, 2017, 19(1): 65-72.
Du Yuansheng,Yu Wenchao. Earthquake-caused and non-earthquake-caused soft-sediment deformations[J]. JOPC, 2017, 19(1): 65-72.
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