摘要
湖泊渗水使其下部的活动构造成了地壳中的弱点，因此可作为构造分段的地点，即将来发震时可能为震源断层传播的始点或终点。湖泊也是震中迁移始发点穴位之一。另外在短临预报巾湖泊也是震前地壳形变、长周期波动和地下冒气的前兆放大点。
Due to the penetration of lake-water,the crust beneath became weakened. In this paper,the author suggests this weakened,tectonic site could be considered as separating point of tectonic segmentation,which might be either the starting or end point of focal fault propagation,and the initial place of epicentral migration as well.Furthermore,prior to earthquakes,lake -water can amplify the abnormal features of crustal deformation,long-period motion and earth gas,it is one of the methods in short-term and impending earthquake prediction.
出处
《内陆地震》
1995年第1期80-85,共6页
Inland Earthquake
基金
国家地震局子课题
关键词
渗透
地壳形变
地震预报
湖泊
Percolation Infiltration Crustal deformation Earthquake prediction Lake
