沂沭带形变、重磁场时空变化特征与地震活动  

The Characteristics of Geophysical Field and its Relations with Seismological Activities on the Yishu Fault Zone

作　　者：燕乃玲[1] 潘纪顺[1] 郭玉莲[2] 李建奎[2] 唐廷梅[2] 

机构地区：[1]中国科学技术大学地球与空间科学系,合肥230026 [2]山东省地震局,济南250014

出　　处：《地震研究》2001年第2期126-130,共5页Journal of Seismological Research

摘　　要：综合利用流动水准和流动重磁复测资料 ,分析沂沭断裂带上地壳形变场和地球物理场的时空强变化特征 ,揭示沂沭断裂带活动特征是以鲁中隆起的继承性活动为主 ,沂沭带北端的双山—李家庄断裂两盘的垂直形变受区域断裂控制并与区域地震活动有关 ,与 1983年菏泽地震和 1995年苍山地震有较好对应关系 ;沂水附近地磁场有“窗口效应” ,尤其与南黄海地震活动及沂沭断裂带上的小震活动有关。With the analysis of vertical leveling, geomagnetic and precise gravity data on the Yishu fault zone, the geophysical characteristic of the field is discussed. It shows that the vertical deformation tendency was dominated by the continuous upheaval of Luzhong territory but had been interrupted by the Heze earthquake in 1983 and the Cangshan earthquake in 1995. This is obviously detected across the Shangsha-Lijiiazhuang fault located at the north end of the Yishu fault zone. The earths local magnetic field nearby Yishui territory has changes as“window effect”, which corresponds the seismological activities in south Huanghai and the small events on the Yishu fault zone.

关 键 词：沂沭断裂带 地球物理场 区域地震构造活动 窗口效应 形变场 重磁场 地震活动 

分 类 号：P315.5[天文地球—地震学]