摘要
霍山地区基岩滑坡与该区地震活动有重要联系。该区浅源中小地震十分频繁,是大华北有名的地震窗口,其原因既与大华北区域应力场变化息息相关、也与基岩滑坡密切有关。该区既因地震活动而发育基岩滑坡、又因基岩滑坡而产生地震活动。
The bedrock slide is an important apptarance of the seismicity in Huoshan region. The small to medium shallow focus earthquakes occur frequently in this region, which is well-known as 'the seismic window' of North China. The earthquakes have close relations to the change of stress field in North China and the bedrock sliding. The bedrock sliding has caused the occurence of earthquakes, while the Latter has given rise to the bedrock slide too.
出处
《地震地质》
EI
CSCD
北大核心
1989年第3期65-72,共8页
Seismology and Geology
关键词
基岩
滑坡
地震
霍山
Anhui Provence, Huoshan, Bedrock slide, Earthquake