摘要
本文在广泛收集研究区相关资料的基础上,以实测地应力值为依据,对研究区的地应力状态进行了模拟分析,进而对地应力状态与地质灾害的关系进行了探讨。得到如下认识:地震活动是地应力积累到一定程度而释放的结果,强震活动一般发生在最大主应力方向与断裂走向呈锐角的部位,地震活动往往发生在局部高应力区。崩塌、滑坡、泥石流灾害在空间分布上与最大差应力的高值区存在较好的对应关系,但与最大主应力高值区则无明显的对应关系。
On the basis of the data collected from the study region extensively, this paper simulates the ground stress state of the region and discusses the relation between the stress state and geological hazards according to the measured values of the ground stress. The conclusion is as follows ： earthquake activity is the result of release of ground stress when it is accumulated to a certain extent; strong earthquake activity generally occurs at a site where the direction of the maximum principal stress makes an acute angle with the fault strike; earthquake activity usually took place in a local high-stress region. The distribution of collapses, landslides and mud flows has a good corresponding relation with the high-value region of the maximum differential stress but no distinct corresponding relation with the high-value region of the maximum principal stress.
出处
《地质力学学报》
CSCD
2007年第3期270-277,269,共9页
Journal of Geomechanics
基金
地质大调查项目"黄河上游新构造活动与地壳稳定性研究"(编号:DKD2003003)资助
关键词
黄河上游
地应力
地质灾害
upper reaches of the Yellow River
ground stress
geological hazard
