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大陆边缘震积岩序列──以金沙江中段震积岩为例
引用本文:孙晓猛,梁定益.大陆边缘震积岩序列──以金沙江中段震积岩为例[J].现代地质,1995,9(3):271-278.
作者姓名:孙晓猛  梁定益
作者单位:China University of Geoscieaces,Beijing,100083
摘    要:通过对金沙江中段震积岩的研究,建立了大陆边缘震积岩序列。该序列包括递交断裂层、震碎角砾岩、震褶岩及层内断层、滑塌巨角砾岩、震积角砾岩及震浊积单元,它具有原地相的地震扰动层和异地相的滑来震积层双层结构,两层之间被震积不整合面所分隔。该序列反映了一次地震事件的全过程,将为地质学家识别大陆边缘地震事件提供对比标准。

关 键 词:震积岩,震积岩序列,大陆边缘,金沙江

SEISMITE SEQUENCE IN CONTINENTAL MARGIN ──TAKE SEISMITE IN MIDDLE REGION OF JINSHA RIVER AS AN EXAMPLE
Sun Xiaomeng, Liang Dingyi, Nie Zetong.SEISMITE SEQUENCE IN CONTINENTAL MARGIN ──TAKE SEISMITE IN MIDDLE REGION OF JINSHA RIVER AS AN EXAMPLE[J].Geoscience——Journal of Graduate School,China University of Geosciences,1995,9(3):271-278.
Authors:Sun Xiaomeng  Liang Dingyi  Nie Zetong
Abstract:A new seismite sequence in continental margin is established by authors studying the seismites in the middle region of the Jinsha River.This sequence consists of a series of units, such as graded fault bed,seismic breccia, seismic corrugated rock and ladder fault,slip megabreccia,seismobreccia and. seismoturbidite.The seismites are composed of twolayer structures:the seismodisturbed beds of dominate factes and the slumping seismites of heterochthonous factes. This two layers contact with seismodisconformity surface.
Keywords:seismite  seismite sequence  continental margin  the Jinsha River  
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