丽江7.0级地震前形变场动态演化与孕震信息提取研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
本文用分段速率整体动态平差法,处理了滇西水准监测网80年代以来的水准复测资料,并进行了形变速率多面函数拟合和垂直形变场信息分离。研究了1996年2月3日发生于滇西水准监测网北部的丽江70级地震前,形变场动态演化和信息分离得到的垂直形变剪切变形、扩张变形、体积变化及准加速度等信息指标分布变化特征。结果表明:80年代中前期,在滇西的丽江、永胜及其附近地区出现的大规模形变速率高梯度带和信息指标高值分布所反映的剧烈垂直差异运动,是丽江70级地震前10余年孕震应变能开始快速积累的显示;而1985~1992年形变场趋势转折与垂直差异运动显著减弱,可能意味着孕震能量积累到一定程度后,孕震区处于相对闭锁阶段。在此基础上,结合丽江70级地震前区域地震活动分析和不同地区强震孕震形变对比,进一步研究了强震前形变场非均匀态特征和孕震信息的识别提取,得出了一些用大地形变进行强震中期预测的有益结果。
Using the integral dynamic adjustment of the piece wise liner velocity,the paper processes the levelling repetition measurement data of the Dianxi(Western Yunnan) area since 1980s,and makes the fitting of the velocity surface for vertical deformation with multisurface function and splits information of vertical deformation field.The dynamic evolution of deformation field and vertical deformation information norm shear deformation,extension deformation,volumetric deformation and quasi acceleration,the distribution changing characteristic by the information splited before Lijiang earthquake with M S 7 0(February 3,1996) in the north of the Dianxi(Western Yunnan) levelling network have been researched.The results indicate that in Dianxi(Western Yunnan) area the acute vertical differential movement of the large scale deformation velocity high gradient belt and high information norm distribution on the Lijang,Yongsheng and its adjcent areas in the medium term of 1980s is the discovery of the startting seismogeny strain energy accumulation before Lijiang earthquake with M S 7 0 for ten years;during 1985~1992,the deformation field tendency dog leg had been notable weakened vertical differential movement may be seismogenic zone that is in the relative blocking stage for seismogenic energy accumulation to definite extent.On this basis,combine the seismicity analysis of this area before Lijiang earthquake with M S 7 0 with macroseismic seismogeny deformation for different areas,the pre seismic deformation field nonhomogeneous state and the seismogeny information retrieval have been further studied,the useful conclusion of macroseismic extended forecast by geodetic deformation have been obtained.
引文
大地形变测量方法攻关学术领导小组,1989,大地形变测量地震预报方法指南,震情研究,Vol.4,增刊,42~62。崔笃信,1994,利用复测水准资料寻求反映地壳纯变形的定量指标,地壳形变与地震,Vol.13,No.1,60~65。江在森、巩守文,1994,水准监测网的分段速率整体平差,武汉测绘科技大学学报,Vol.19,No.2,157~162。江在森、崔笃信、王双绪,1996,大地垂直形变场信息分离与强震危险区判断,中国地震学会第六次学术大会论文摘要集,中国地震学会,171,地震出版社,北京。梅世蓉,1995,地震前兆场物理模式及前兆分布特征与机理研究进展,地震,增刊,2~22。梅世蓉,1996,地震前兆场物理模式与前兆时空分布机制研究(三)———强震孕育时地震活动与地壳形变场异常及机制,地震学报,Vol.18,No.2,170~178。赵承坤、黄立人,1991,速率面拟合方法中核函数中心点的选择,地壳形变与地震,Vol.11,No.2,48~54。

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心