摘要
本文根据转换波近年得出的地壳构造最新资料,结合地表地质的研究成果,探讨了燕山地区地壳构造和地壳运动的基本特征,同时着重分析了怀来—宁河段北西西向地震活动带的构造特征、活动方式及其两侧的差异,进而提出了本区强震的深部构造标志,并讨论了强震孕育过程及可能的潜在震源区等问题,为研究首都圈的地震预测、预报提供基础资料。
Based on the new data of crust structure revealed recent years by a method of P-SV converted waves from earthquakes and combined with the data of surface geological structure we have discussed the major features of crust structure and crust movement in Yanshan region, especially focused our attension on the analyses of structure characteristics, movement pattern of the crust in Huailai-Ninghe WNW seismic active zone and their differences between both sides of the zone.In the light of comparison between distribution of epicentres and crust structures we have found some diagnostic criteria of deep structure, similar for strong earthquake areas. The problems about deep process of strong earthquake preparation and potencial hypocentre zones have been discussed. All the results from this study are useful to the research on earthquake monitoring and prediction in the region of Capital Circle.
出处
《地震地质》
EI
CSCD
北大核心
1989年第1期65-76,共12页
Seismology and Geology
关键词
燕山
地壳构造
地壳运动
孕震条件
Yanshan region, Converted waves, Crust structure, Crust movement, Seismoactive zone, Conditions for earthquake preparation
