fault-slipped

常見(jiàn)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(guò)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(guó)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(wú)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。
• This predictability most likely stems from the fact that water flowing from below subduction zones may exert significant control over when and where these faults slip silently.
  這樣的可預(yù)測(cè)性，很可能來(lái)自於隱沒(méi)帶下方所流出的水，它對(duì)於何時(shí)、何地會(huì)發(fā)生無(wú)聲的斷層滑動(dòng)，可能具有相儅大的操控力。
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