Abstract Earthquake event deposit has become a “hot spot” in modern sedimentary geology.By reviewing the history of domestic seismites study，the main achievements and problems about the seismites studies in China have been summed up in this paper，which focused on the earthquake-caused soft-sediment deformation，timing， distribution and sequences of earthquake event deposits etc.Earthquake-caused soft-sediment deformation is divided into syndepositional，penecontemporaneous and epigenetic deformation.The differences were also discussed respectively among earthquake-caused syndepositional veins，liquefied veins and epigenetic veins，micro-fold，liquefied convolute deformation and epigenetic folds，seismic shocks deformation and liquefied deformation，pillow structures and pillow beds.
About author: Du Yuansheng,born in 1958, is a professor and Ph.D. supervisor of China University of Geosciences(Wuhan)，and is mainly engaged in researches of sedimentology and geology of orogenic belt.E-mail:duyuansheng126@126.com.
Cite this article:
Du Yuansheng. Discussion about studies of earthquake event deposit in China[J]. JOURNAL OF PALAEOGEOGRAPHY, 2011, 13(6): 581-590.
Du Yuansheng. Discussion about studies of earthquake event deposit in China[J]. JOPC, 2011, 13(6): 581-590.
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