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fault plane中文是什么意思

  • 斷層面
  • 斷面

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  • 例句與用法
  • One mode is slippage along the discontinuity provided by the lubricated fault plane .
    其中一種方式是沿著潤滑的斷層面所形成的間斷面而發(fā)生滑動。
  • 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的地方,而且斷層面幾乎是垂直的。
  • The np ii is the fault plane
    走向為104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的應力調整造成的。
  • 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,對連續(xù)介質中斷層面上的地震成核過程進行了數(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表明:走向為199的節(jié)面是斷層面。破裂傳播方向為自東北向西南方向,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動的力學模型,即將板塊邊界的地殼運動表述為板塊的相對剛體運動加邊界斷層面上的負位錯分布。
  • 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
    震源時間函數(shù)的這種方向性效應與p波的方向性效應相一致,清楚地表明:走向為199的節(jié)面為斷層面,地震是從東北向西南方向單側破裂的。
  • 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
    由震源坐標系表示的震源斷層面換算到觀測坐標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算的宏觀損傷度的變化。
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