EVOLUTION CHARACTERISTICS OF SEISMICITY PATTERN BEFORE WEST TO KUNLUN MOUNTAIN PASS M_S8.1 EARTHQUAKE
Dong Zhi
Abstract
Dong Zhi
Abstract
Seismogenic process of west to Kunlun Mountain Pass MS8.1 earthquake is consists of three evolutionary stages for seismicity pattern.The first stage is background formed by MS≥6 earthquake from 1959;the second stage is pregnant formed by MS≥5 earthquakes from in 1994, and the third stage,imminent earthquake gap lasts 4 months before the MS8.1 earthquake.At the later period of the pregnant gap,seismic bands in 1~2 years appeared in Qinghai-Xizang block and western China. Along with the formation of the imminent earthquake gap, no small earthquake occurred in the region.The timespace evolutionary feature of MS8 earthquakes in western China is discussed at the end.
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Seismogenic process of west to Kunlun Mountain Pass MS8.1 earthquake is consists of three evolutionary stages for seismicity pattern.The first stage is background formed by MS≥6 earthquake from 1959;the second stage is pregnant formed by MS≥5 earthquakes from in 1994, and the third stage,imminent earthquake gap lasts 4 months before the MS8.1 earthquake.At the later period of the pregnant gap,seismic bands in 1~2 years appeared in Qinghai-Xizang block and western China. Along with the formation of the imminent earthquake gap, no small earthquake occurred in the region.The timespace evolutionary feature of MS8 earthquakes in western China is discussed at the end.
Key concepts: Induced seismicity, Seismology, Geology, Intraplate earthquake, Seismic gap, Interplate earthquake, Mountain pass, Stage (stratigraphy)