Earthquake Sedimentary Event Record In Early Triassic In Southeastern Sichuan Basin, Sw China
Abstract:There are some macroscopic and microscopic sedimentary structures of seismic events in the outcrops in Lower Triassic Feixianguan Fm (T1 f). and Jialingjiang Fm (T1 j). in southeastern parts of Sichuan Basin. The following basic types of sedimentary structures could be observed: Soft-sediment liquefied deformation structures include curled deformation (sliding deformation structure," sausage structure") and microscopic folds (laminated plastic deformation). Seismites emerge in T1 f 1 and T1 f 2 in Baimiaozi … Show more
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