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。
Strain steps recorded by borehole strainmeters are of special values in studies of coseismic stress triggered fault activities.
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.
钻孔技术问世以来，由于能够记录大量地质实体单元的原始信息，而一直受到地质工作者的青睐。
Since technology of drill comes out, it was recognized by geologist engineers always in case of having the ability of recording a great deal barbarism information of geology entity cell.
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