Strain steps recorded by borehole strainmeters are of special values in studies of coseismic stress triggered fault activities.
钻孔应变观测记录的同震应变阶对于研究同震应力触发断层活动具有特殊的价值。
Earthquake liquefaction, caused by coseismic shakes, is controlled by soil conditions which are the results of geomorphic processes.
地震液化是同震震动引起的，同时也受地貌活动创造的土壤条件控制。
Following the idea of coseismic stress-triggering, coseismic strain steps recorded by borehole strainmeters are used to study coseismic stress-triggered fault slips.
沿着同震应力触发的思路，提出了利用钻孔应变观测记录的同震应变阶反演同震应力触发断层活动的方法。
Following the idea of coseismic stress-triggering, coseismic strain steps recorded by borehole strainmeters are used to study coseismic stress-triggered fault slips.
沿着同震应力触发的思路，提出了利用钻孔应变观测记录的同震应变阶反演同震应力触发断层活动的方法。
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