The ratio of poloidal to toroidal component of mantle convection determined the proportion of seismic energy released in the thrust, normal, or strike-slip earthquakes.
地幔对流的垂直运动与水平运动分量的比率，决定了逆冲、引张与走滑型强震的能量释放份额。
The focal mechanism is mainly left-lateral strike-slip, with a small thrust component.
震源机制主要是左旋走滑，带有很小的逆冲倾滑分量。
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