该断裂带北段的木吉河断层运动特征以逆冲为主，兼有右旋走滑分量。
Mujihe fault lies on the northern segment and its main motion characteristics is thrusting, and have dextrorotation slip component.
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 ratio of poloidal to toroidal component of mantle convection determined the proportion of seismic energy released in the thrust, normal, or strike-slip earthquakes.
震源机制主要是左旋走滑，带有很小的逆冲倾滑分量。
The focal mechanism is mainly left-lateral strike-slip, with a small thrust component.
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