张北-尚义地震区及其邻区地壳上地幔结构  

THE STRUCTURE OF THE CRUST AND UPPER MANTLE FOR THE ZHANGBEISHANGYI SEISMIC AREA AND ITS NEIGHBOURING REGION

作　　者：赵国泽[1] 刘国栋[1] 詹艳[1] 江钊[1] 刘铁胜[1] 汤吉[1] 王继军[1] 李文军[1] 梁竞阁[1] 

机构地区：[1]中国地震局地质研究所

出　　处：《地震地质》1998年第2期155-156,共2页Seismology and Geology

基　　金：国家地震局"八五"攻关项目;国家自然科学基金

摘　　要：对张北－尚义地震区及其邻区的深部结构的研究表明，张家口－蓬莱构造带与其两侧的山西裂谷系、华北裂谷盆地和燕山褶皱带相比，具有低阻性质，地壳内的速度界面及莫霍面的深度分布显示出明显的不同。以延怀盆地为界，把张家口－蓬莱构造带分成西北和东南两段。最新的大地电磁观测研究表明，张北－尚义地震区电性结构与周围有一定差别，壳内有一近北北西向构造，主震和绝大多数余震都发生在壳内低阻带以上。t is shown that the structure of the crust and upper mantle (thickness, geothermal field etc.) beneath the ZhangbeiShangyi earthquake area, which belongs to Inner Mongolia geoaxes, has the nature of a transition zone as compared to its surrounding regions, Yanshan mountain fold belt, rifting basin of North China, rift system of Shanxi province and Erdos block. The ZhangbeiShangyi earthquake area is located near the ZhangjiakouBohai SeaPenglai tectonic belt (ZPB) which is a significant tectonic boundary. Along the ZPB a relative low resistivity zone appears in the whole lithosphere. The width of ZPB is about 40km and becomes bigger with increasing depth. The structure of seismic velocity similar to electricity also occurrs along the ZPB. A NNW trending tectonic belt in the crust is newly detected beneath ZhangbeiShangyi earthquake area. The NNW trending tectonic belt and ZPB are postulated to play an important role in a combining way for pregnancy and genesis of the earthquake. The recent results of magnetotelluric observation indicate that there is a low resistivity layer at the depth of about 15km beneath earthquake area, which is deeper and thinner than that to the south of ShangyiChongli fault, which is tectonic boundary between InnerMongolia geoaxes and other southern tectonic units. The foci of main shock and most aftershocks are located above the low resistivity layer in the crust.

关 键 词：地震区 张北-尚义 地壳 上地幔 深部结构 

分 类 号：P315.2[天文地球—地震学] P183.2[天文地球—固体地球物理学]