表明应力应变异常形态的时间特征与地震的孕育和发生有较明显的关系。
The results show that the anomalies' shape character of stress and strain has obvious relation with the development and occurring of earthquakes.
分析了拐角频率和应力降随时间的变化趋势，并讨论了震源参数相互之间的关系。
The variation of corner frequency and stress drop with time are analyzed, and the relations between focal parameters are discussed.
从位错理论出发导出了湿软土壤的剪切应力—剪切应变—时间关系。
The shear stress - shear rate - time relationship of wet and soft soils is determined from the point of view of dislocation theory.
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