The individual breccia can be used to indicate the direction of displacement of fault walls and the mode of occurrence of the fault surface.
利用单个角砾即可指示断层两盘位移方向和断层面产状。
However, not all the fault surface and the source directly linked to the movement, they also may be due to seismic waves caused by secondary impact.
但并不是所有的地表断裂都直接与震源的运动相联系,它们也可能是由于地震波造成的次生影响。
However, not all the fault surface and the source directly linked to the movement, they also may be due to seismic waves caused by secondary impact.
但并不是所有的地表断裂都直接与震源的运动相联系,它们也可能是由于地震波造成的次生影响。
应用推荐