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《Journal of Stratigraphy》 2006-02
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AN OVERVIEW OF SEISMITE RESEARCH IN CHINA

ZHAO Wei-wei, ZHA Ming, and YANG Jian-ping(Faculty of Geo-Resource and Information, University of Petroleum, Dongying, 257061)  
Seismite is a type of catastrophic deposits with recognizable evidence for seismic activities and sequence. During past ten years comparative study of modern and ancient seismites reveals some significant difference between seismite and other sedimentary rocks. Seismite can be recognized by such distinct features as earthquake fissures, fault-graded beds, synsedimentary micro-fractures, within-bed folds, fake nodules, liquefaction sandstone(mudstone) veins, flame structure, and vibrational liquefaction deformation structure. We also review recent studies of seismo-deposition and seismite, earthquake-tsunami sequence, seismic sequence of vibrational liquefaction in carbonate rocks, seismite and seismo-unconformity, seismite sequence in continental margin, seismite in continental fault lacustrine basin, and vertical squence of seismite. Through the observation and description of drill cores, we can study seismite deposits in terrestrial enviroments. Such studies are important to the characterization of source rocks in fault-bound lacustrine basins.
【Fund】: 国家“十五”科技攻关项目(编号:2001BA605A09)资助。
【CateGory Index】: P539.1
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