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.
通过对跨断层测量特点的分析，提出断层运动中趋势性成分具有反映区域地壳形变及应变能累积程度的意义。
By analyzing features of across fault measurement, the trend components of deformation can reflect the strength of strain energy accumulation in regional area.
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.
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