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- W2362307390 abstract "The direct evidence of an earthquake hazard event is seismite—the special sedimentary record left in strata. A typical seismite-tsunamite sequence consisting of carbonate micrite veins, liquefied curl deformation structure, hummocky bedding and rudaceous layers is developed at the base of the Neoproterozoic Shiwangzhuang Formation in the southern Shandong area, which suggests that a very long-continued seismically active phase occurred in the area in the Proterozoic. According to the characteristics of its sediment associations, 7 seismic episodes and more than 30 earthquakes may be distinguished. The main cause of this earthquake hazard event was the earth rifting of the ancient Tanlu fault zone." @default.
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- W2362307390 date "2007-01-01" @default.
- W2362307390 modified "2023-09-26" @default.
- W2362307390 title "Sequence of earthquake episodes and occurrences in a Neoproterozoic seismically active phase in southern Shandong, China" @default.
- W2362307390 hasPublicationYear "2007" @default.
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