摘要
通过对华北地区地震活动的分析，认为华北地震具有自西向东成串迁移活动特点和可公度性，并在一定条件下重演。认为该活动与青藏块体的地震活动相关，反映了印度板块运动对华北地震活动的影响。
Based on the analysis of seismic activity in North China, this paper considers that the seismic activity in North China shows active characters to migrate trom west to east in clusters, showing repeatability under certain condition and commensurability. The seismic activity in this area is related to that of Qinghai-Tibet block, and the migration pattern reflects the important action of indian Plate to the seismic activity in North China. It is possible to predict earthquakes (M≥6)in North China by using the dynamic migration pattern of earthquakes.
出处
《华北地震科学》
北大核心
1994年第1期35-42,共8页
North China Earthquake Sciences
关键词
板块运动
应力场
地震活动性
plate movemant, stress field, seismic cluster, strain wave, commenaurability
