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1·Himalayan movement made the area developed as a para-foreland basin.

喜马拉雅运动使本区发育为类前陆盆地。

2·They were the products of the early-, middle- and late- magmatic cycles of Himalayan movement.

是喜山运动早、中、晚三个岩浆旋迥的产物；

3·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。

4·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。

5·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。

6·The periods of early, middle-late Yanshan movement and Himalayan movement are its major periods for hydrocarbon generation and expelling.

主要发育二叠系、三叠系、侏罗系多套烃源岩，燕山运动早期、中—晚期及喜马拉雅运动期为烃源岩的主要生、排烃高峰期。

7·The reservoirs were uplifted to be exposed and be denuded and were changed into the present oil sands finally during the Himalayan movement.

进入喜山运动，早先形成的油藏抬升暴露、剥蚀而最终形成了目前的油砂矿体。

8·The present tectonic features of the East Asian continent are the product of the Himalayan movement since the Cenozoic and this process is now still going on.

东亚大陆现今构造面貌是新生代以来喜山运动产物，这一过程迄今还在进行。

9·Through the restoration of Wuzhishan tectonic history and analysis of apatite fission track, Wuzhishan structure was buildup at Himalayan movement stage has been shown.

通过对五指山邻区构造史恢复和磷灰石裂变径迹分析，指出五指山构造形成于喜山期。

10·The Himalayan movement controls final stereotype of local structures and faults, hydrocarbon migration and accumulation for forming reservoirs are also controlled by it.

喜马拉雅运动控制着局部构造和断裂的最后定型以及油气运移、聚集成藏。