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机构地区:[1]山东省地震局,济南250014
出 处:《高原地震》1997年第2期51-57,共7页Plateau Earthquake Research
摘 要:据震例资料显示应变、应力测量异常形态与区域应力场增强失稳状态相关。主要特征:1.震前主应力方向发生明显偏转并指向震中区域;2.临震前应力测量异常显示四象限空间分布,张、压区域与震源机制解有明显相关性;3.异常形态与岩石破裂实验数值模拟结果有较好的一致性。According to the earthquake data, strain and stress measurement anomaly is related to the unstability of regional stress field. The main characteristics are: 1. The direction of principal stress is obviously turned to the epcentre region before the earthquake ; 2. Stress measurement anomaly distribute in four quadrants, the regions of tensile and compressive forces are related to the focal mechanism solution; 3. Anomaly shape is consistent well with the numerical simulation of the rock - breaking test.
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