摘要
根据龙门山构造带的地震地质特征、地震活动规律及新构造活动特征 ,综合分析认为该地区区域稳定性受控于龙门山断裂带。而断裂带又以韧性切变形为主 ,蠕滑运动为特征 ,决定该带在相当长的一段时间内 。
On the basis of seismogeological characteristics, seismicity regularity and new tectonic movement, the authors point out that the regional stability in this belt is controlled by fault zone in Longman Mountains The fault zone is deforming on ductile shear function and creeping slide motion So, it is impossible to bring about strong earthquake in this region for a long time
出处
《地震研究》
CSCD
北大核心
2000年第4期378-383,共6页
Journal of Seismological Research
