摘要
应用一种新思路、新方法研究兴都库什－贝加尔地震带内的地震迁移，结果表明，地震沿地震带由南西西向北东东方向定向迁移，平均迁移速度为每年１２９ｋｍ，量级与中国大陆西部地震带（区）的地震迁移速度相当．研究结果为地震动力学和地震预报提供了一定的依据．
Using a new idea and method, the auther has investigated the earthquake migration phenomena along the Hirdukush-Baikalian seismic belt. The result shows that earthquakes migrate in the direction of SWW to NEE along the belt at the average speed of 129 km per year, which is almost the same speed as the earthquake migration in the west part of China. The result stated above can be used as a guide to the study of geodynamics and earthquake prediction.
出处
《地震地磁观测与研究》
1995年第1期15-19,共5页
Seismological and Geomagnetic Observation and Research
关键词
地震带
地震迁移
地震活动度
seismic belt
earthquake migration
seismicity rate
