Determination of Seismogenic Structure for the Shenyang M5 1/2 Earthquake in 1765

详细信息   
摘要

The deep-shallow geological structural conditions and seismic activities for the Shenyang M5 1/2 earthquake in 1765 are analyzed, the activities and seismic hazards for the Changbaixiang-Guanyinge faultF6, the Yilan-Yitong fault, the Hunhe fault which around the epicenter are also evaluated. It is analogised of seismic structure for mid-strong earthquakes in the area of Liaoning Province. It is determined that the modern tectonic deformation features for the F6 is coincident with the effect of modern tectonic stress. The results of shallow seismic prospectings, progressive features of fault ruptures, aging data and offset landform show that the F6 is still active in Late Quaternary.

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