The modern tectonic stress field on the eastern side of the Tanlu fault is regionally very stable.
郯庐断裂东侧的现代构造应力场在区域上具有极大的稳定性。
This seismic zone is a recent crust shear rupture zone under the uniform modern tectonic stress field in a large scale;
此地震带具有统一的现代区域构造应力背景，是华北东南部的一条现代地壳剪切破裂带；
The modern tectonic stress field of Shishen 100 area has been found by in situ testing, laboratory core experiment, logging data analysis and 3D finite element numerical simulation.
采用现场测试研究、室内岩心实验、测井资料分析及三维有限元数值模拟技术，获得了史深100 地区的现代构造应力场。
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