| 1. | One mode is slippage along the discontinuity provided by the lubricated fault plane .
其中一种方式是沿着润滑的断层面所形成的间断面而发生滑动。 |
| 2. | Such faults are straight over long distances and the fault plane is nearly vertical .
这种断层笔直地延伸到很远的地方，而且断层面几乎是垂直的。 |
| 3. | The np ii is the fault plane
走向为104的节面是断层面。 |
| 4. | 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
余震发生在主震的断层面上(或其附近) ，是由主震断层面附近介质的应力调整造成的。 |
| 5. | To unerstand precursory process before seismic fault slip , this work focuses on earthquake nucleation process on a fault plane through numerical simulation
摘要为了把握断层上地震的前兆规律，对连续介质中断层面上的地震成核过程进行了数值模拟研究。 |
| 6. | 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波显示的方向性效应表明：走向为199的节面是断层面。破裂传播方向为自东北向西南方向，几乎垂直于爪哇海沟走向。 |
| 7. | 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
提出了一种描述板块边界断层运动的力学模型，即将板块边界的地壳运动表述为板块的相对刚体运动加边界断层面上的负位错分布。 |
| 8. | 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
震源时间函数的这种方向性效应与p波的方向性效应相一致，清楚地表明：走向为199的节面为断层面，地震是从东北向西南方向单侧破裂的。 |
| 9. | 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
北北东?南南西向分布的余震发生在主震的断层面上(或其附近) ；而西北?东南向分布的余震则发生在明打威断层上(或其附近) 。 |
| 10. | 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
由震源坐标系表示的震源断层面换算到观测坐标系得到其外法向矢量，可求得研究地块以地震裂纹密度张量计算的宏观损伤度的变化。 |
