摘要
在对我国西部本世纪第五个地震活跃幕以来地震群体活动时空强演变规律回顾的基础上,研究了近1~2年中强地震的分布特点,结合大地形变的演变状况,对本区地震活动进行了研究,并认为本区处于本活跃幕末的翘尾活动阶段。
Based on the time-space intensity evolution of grouping seismicity during the seismically fifth active period since this century in western China, the distribution charac- teristics of moderately earthquakes in last 2 years has been studied. Combining with evolu- tional situation of geodetic deformation, the seismic activity is researched in the area. The conclusion is drawn as follows: the seismically active period is being in last re-activated stage.
引文
①王继英,我国西部1999年度地震活动分析,1998。
[1]江在森,王双绪,赵振才.南北地震带和青藏块体东部近期大地形变与地震特征[J].中国地震,1997,13(2):139-150.
[2]张国民.印度板块北边界地震活动和中国大陆地震[J].地震,1994,(3):1-3.
[3]赵振才.青藏块体及其周边活动的迁移[J].西北地震学报,1995,17(2):26-32.