The first, covering the time from late Cretaceous toPaleogene, is called the Himalayan Movement.
第一亚旋回末期的造山运动称为喜山运动。
Also, the faults as channels for petroleum migration in the whole basin have been intensified by the Himalayan movement.
喜马拉雅运动在全盆地强化了断裂的运移通道作用。
There the crustal structure was relatively stable, but folding and faulting have been intense since the Himalayan movement.
但自喜马拉雅运动以来，断褶构造活动强烈。
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