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faulting plane in Chinese

Pronunciation:
How to pronounce "faulting plane""faulting plane" in a sentence

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  • 斷層面

Examples

  • One mode is slippage along the discontinuity provided by the lubricated fault plane .
    其中一種方式是沿著潤(rùn)滑的斷層面所形成的間斷面而發(fā)生滑動(dòng)。
  • Such faults are straight over long distances and the fault plane is nearly vertical .
    這種斷層筆直地延伸到很遠(yuǎn)的地方，而且斷層面幾乎是垂直的。
  • The np ii is the fault plane
    走向?yàn)?04的節(jié)面是斷層面。
  • The aftershocks were distributed on ( or near ) the fault plane and were triggered by the stress redistribution in the medium in the nearby region of the fault plane
    余震發(fā)生在主震的斷層面上(或其附近) ，是由主震斷層面附近介質(zhì)的應(yīng)力調(diào)整造成的。
  • To unerstand precursory process before seismic fault slip , this work focuses on earthquake nucleation process on a fault plane through numerical simulation
    摘要為了把握斷層上地震的前兆規(guī)律，對(duì)連續(xù)介質(zhì)中斷層面上的地震成核過程進(jìn)行了數(shù)值模擬研究。
  • The directivity shows that the np i is the fault plane , and that the earthquake ruptured unilaterally from the northeast to the southwest , nearly perpendicular to the strike of the java trench
    P波顯示的方向性效應(yīng)表明：走向?yàn)?99的節(jié)面是斷層面。破裂傳播方向?yàn)樽詵|北向西南方向，幾乎垂直于爪哇海溝走向。
  • A physical model for describing the fault movement along plate boundary is proposed , i . e . , the crust movement along plate boundary equals to the relative rigid plate motion plus negative dislocation distributions on the fault planes
    提出了一種描述板塊邊界斷層運(yùn)動(dòng)的力學(xué)模型，即將板塊邊界的地殼運(yùn)動(dòng)表述為板塊的相對(duì)剛體運(yùn)動(dòng)加邊界斷層面上的負(fù)位錯(cuò)分布。
  • The source time function directivity is in accordance with the p waveform directivity , clearly showing that the nodal plane of strike 199 is the fault plane and that the earthquake ruptured unilaterally from the northeast to the southwest
    震源時(shí)間函數(shù)的這種方向性效應(yīng)與p波的方向性效應(yīng)相一致，清楚地表明：走向?yàn)?99的節(jié)面為斷層面，地震是從東北向西南方向單側(cè)破裂的。
  • The strike - slip faulting was caused by asymmetrical distribution of barriers on the subducting plate . the nne - ssw distributed aftershocks occurred on , or near , the fault plane of the main shock ; while the nw - se distributed aftershocks , on , or near , the mentawai fault
    北北東?南南西向分布的余震發(fā)生在主震的斷層面上(或其附近) ；而西北?東南向分布的余震則發(fā)生在明打威斷層上(或其附近) 。
  • By means of the transformation from the focal coordinate system to the observation system , we obtained the external normal vector of the focal fault plane expressed in its observation system , and obtained the macrodamage degree of the researched block , which is calculated in dyadic
    由震源坐標(biāo)系表示的震源斷層面換算到觀測(cè)坐標(biāo)系得到其外法向矢量，可求得研究地塊以地震裂紋密度張量計(jì)算的宏觀損傷度的變化。
  • More examples：  1  2
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