论文部分内容阅读
前言山西临汾盆地震是华北地区著名地震活跃区之一。有史记载以来,在临汾这一狭长构造盆地内就以地震频度高、强度大的特点为人们所重视。地震地质工作者和考古工作者们在临汾盆地中已作有不少有意义的工作(1)。但是在恢复该区的构造活动史中,史前地震活动以往研究很少。1981年3—4月间作者等在临汾以东大阳公社、东张公社、乔李公社等涝河两侧进行了古地震遗迹的调查,并以东堡村为重点,探槽开挖,分层取样,初步确定该
Preface The Linfen basin earthquake in Shanxi Province is one of the famous seismic active areas in North China. Since the record of history, people pay great attention to the characteristics of high seismicity and high intensity in this long and narrow basin of Linfen. Seismological geologists and archaeologists have done a lot of meaningful work in the Linfen basin (1). However, in the history of the tectonic activities of the restoration of the area, there are few studies of prehistoric seismic activity in the past. From March to April 1981, the authors conducted surveys of ancient earthquakes on both sides of the flood river, such as Dayang commune east of Linfen, Dongzhang Commune and Qiaoli commune, and focused on Dongpu village, excavation of trench, Stratified sampling, the initial determination of the