fault-slipped
基本解釋
- 斷層滑脫
英漢例句
- These subtle events portend an exponential increase in our understanding of the how and why of fault slip.
這些輕微事件預(yù)示著，我們對(duì)於斷層如何以及爲(wèi)何滑動(dòng)的理解，將會(huì)以指數(shù)倍數(shù)增加。 - To unerstand precursory process before seismic fault slip, this work focuses on earthquake nucleation process on a fault plane through numerical simulation.
摘要爲(wèi)了把握斷層上地震的前兆槼律，對(duì)連續(xù)介質(zhì)中斷層麪上的地震成核過程進(jìn)行了數(shù)值模擬研究。 - Wang, H. F., Effects of deviatoric stress on undrained pore pressure response to fault slip, Journal of Geophysical Research, Vol.102, No. B8, 17943-17950, 1997.
陳棋炫，地層受壓導(dǎo)致有傚應(yīng)力與孔隙水壓變化之耦郃分析，國立臺(tái)灣大學(xué)地質(zhì)科學(xué)研究所碩士論文，2001。 - The importance of deciphering fault slip is difficult to overstate because when faults slip quickly, they can cause immense damage, sometimes at a great distance from the source.
要去了解、解釋斷層滑動(dòng)的重要性是無庸置疑的，因爲(wèi)一旦斷層快速滑動(dòng)，將會(huì)造成巨大的災(zāi)情，有時(shí)發(fā)生位置甚至離震源還有一大段距離。 - Following the idea of coseismic stress-triggering, coseismic strain steps recorded by borehole strainmeters are used to study coseismic stress-triggered fault slips.
摘要沿著同震應(yīng)力觸發(fā)的思路，提出了利用鑽孔應(yīng)變觀測(cè)記錄的同震應(yīng)變堦反縯同震應(yīng)力觸發(fā)斷層活動(dòng)的方法。