... stress momentum tensor应力动量张量 stress of rocks岩石应力 stress of the first kind第一类应力 ...
基于28个网页-相关网页
stress s of rocks 岩石应力
stress limit of wall rocks 极限围岩压力
stress-state of virgin rocks 原岩应力状态
stress of surrounding rocks Calculation 围岩应力计算
stress field of surrounding rocks 围岩应力场
Seismic porosity and seismic stress of rocks can be inverted with seismic and geological data based on the theory of two phase medium.
根据双相介质理论，使用地震、地质资料反演出地震孔隙率和岩石地震应力。
When enough stress builds to fracture the stuck rocks, the plates jump past each other, releasing energy in the form of earthquakes.
压力增大到一定程度会造成岩层碎裂，而板块弹起形成错位，地震发生并成为能量释放的一种形式。
The magnitude and timing of an earthquake depend on the size of the fault being ruptured, the stiffness of the rocks in question and the amount of stress that has accumulated in them.
地震的震级和发生时机，取决于断层破裂的范围，相关的岩石刚度以及其内部积聚的压力。
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