从大西洋流向地中海的瀑布不像直布罗陀海峡连接那些海洋时发生的地壳调整和断层运动那样壮观。
The cascades of water from the Atlantic to the Mediterranean were not as spectacular as the crustal adjustments and faulting that occurred when the Strait of Gibraltar was connected to those seas.
它们的力学性质和展布格局为断层运动的研究提供重要的线索。
Their mechanical property and spreading pattern give an important clue of investigating the mode of fault movements.
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.
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