摘要
用三峡及邻区（东经１０８°～１１３°，北纬２９°～３３°）地质资料，地震资料，现 场地应力测量资料论证三峡及邻区晚第三纪以来构造应力场稳定性及其分区特 征。
In this paper, it is concluded that the most prominent feature based on the statistical assessment of earthquake fault plane solutions, insitu stress measurements,geodetic strain measurements and the features of fault activity in the recent tectonic stress field is the regionalization of compressive principal stress direction in Three Gorges and its neighbouring area.
出处
《海洋科学》
CAS
CSCD
北大核心
1995年第2期36-41,共6页
Marine Sciences
关键词
区域构造
构造应力场
晚第三纪
Tectonic stress field regionalization,Regional tectonic stress field, Local tectonic stress field
