Seismic porosity and seismic stressofrocks 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。
2
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。
3
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 ofstress that has accumulated in them.