漆家福. 由微(小)震综合断层面解推测林县地区的现代应力场[J]. 华北地震科学, 1985, 3(2): 41-45.
引用本文: 漆家福. 由微(小)震综合断层面解推测林县地区的现代应力场[J]. 华北地震科学, 1985, 3(2): 41-45.
Qi Jiafu. PRESENT STRESS FIELD INFERRED FROM FAULT-PLANE SOLUTION OF MICROEARTHQUAKES IN LIN-XIAN REGION, HENAN PROVINCE[J]. North China Earthquake Sciences, 1985, 3(2): 41-45.
Citation: Qi Jiafu. PRESENT STRESS FIELD INFERRED FROM FAULT-PLANE SOLUTION OF MICROEARTHQUAKES IN LIN-XIAN REGION, HENAN PROVINCE[J]. North China Earthquake Sciences, 1985, 3(2): 41-45.

由微(小)震综合断层面解推测林县地区的现代应力场

PRESENT STRESS FIELD INFERRED FROM FAULT-PLANE SOLUTION OF MICROEARTHQUAKES IN LIN-XIAN REGION, HENAN PROVINCE

  • 摘要: 本文利用短期临时台网对林县微(小)震活动监测的资料,经过统计处理求出微(小)震综合断层面解,推测林县地区现代应力场的状况:主压应力(P)轴方向为78°,仰角49°;主张应力(T)轴方向为330°,仰角14°。最后简要讨论了林县地区应力场与华北地区区域应力场的关系。

     

    Abstract: Based on the microseismic data in Lin-xian region observed by temporary station network, the Composite fault plane solution of micro-earthquakes has been obtained with stereographic projection of first p-wave motion。The present stress field inferred in Lin-xian region is as follows: the direction of maximum pricipal stress is of NE78°, and its angle of elevation is of 49°;the direction of minimum principal stress is of NW330°, and its angle of elevation is of 14°.In addition, the relationship between Lin-xian region and North China stress fields has been briefly discussed.

     

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