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CHARACTERISTICS OF SEISMICITY PATTERN EVOLUTION BEFORE THE WEST KUNLUN MOUNTAINS EARTHQUAKE WITH M s8.1

MA Wen-jing

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Abstract

Seismicity patterns are many abnormal shapes before the earthquake with M s 8 1 ,such as background gaps,belts and quiet of small earthquakes.Epicenters of aftershocks are far away from the main shock,and formed a rupture belt with 350km. Middle earthquakes are quiet in the middle segment of the eastern Kunlun fault,the stress field is blocking,and is a strong earthquake seismogenic zone.

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What this paper is about

Seismicity patterns are many abnormal shapes before the earthquake with M s 8 1 ,such as background gaps,belts and quiet of small earthquakes.Epicenters of aftershocks are far away from the main shock,and formed a rupture belt with 350km. Middle earthquakes are quiet in the middle segment of the eastern Kunlun fault,the stress field is blocking,and is a strong earthquake seismogenic zone.

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Available abstract

Seismicity patterns are many abnormal shapes before the earthquake with M s 8 1 ,such as background gaps,belts and quiet of small earthquakes.Epicenters of aftershocks are far away from the main shock,and formed a rupture belt with 350km. Middle earthquakes are quiet in the middle segment of the eastern Kunlun fault,the stress field is blocking,and is a strong earthquake seismogenic zone.

Key concepts: Induced seismicity, Aftershock, Seismology, Geology, QUIET, Shock (circulatory), Foreshock, Fault (geology)

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CHARACTERISTICS OF SEISMICITY PATTERN EVOLUTION BEFORE THE WEST KUNLUN MOUNTAINS EARTHQUAKE WITH M s8.1 — Research Paper | ScholarLens