塔里木盆地低幅度构造和碳酸盐岩裂缝中普遍存在着速度各向异性。
Velocity anisotropy can be widely seen in low-relief structures and carbonate fractures of Tarim basin.
地球的内核是—磁铁，内核的铁磁性已被观察到的地震波速度各向异性所证实。
The new theory admits the Earth's inner core to be a ferromagnet. The ferromagnetism of inner core is supported by observed anisotropic property of inner core in transmitting seismic waves.
岩石质量，速度，衰减及各向异性。
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