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。
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；
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。
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。
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。
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。
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。
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。
A large scale migration and accumulation took place during Later Himalayan movement, as a result a type of called remained gas pools with higher gas columns were formed.
喜山构造运动使研究区天然气重新大规模运移聚集，形成充满度很高的残余气藏。
Wenjisang - Wennan area had experienced Yanshan and Himalayan movement, and resulted in a series of complicated structural traps such as faulted anticline and faulted nose, etc.
温吉桑-温南地区历经燕山、喜山运动，形成了一系列成排成带展布的断背斜、断鼻等复杂构造圈闭。
The area has undergone six stages of tectonic deformation with the second episode of Caledonian Movement (D_2) and the fifth episode of Himalayan Movement (D_5) as the most important ones.
该区经历了六个构造形变期，以相当于 主加里东期的第二期（D_2）与喜马拉雅期的第五期（D_5） 形变期最为重要。
Cu-Mo-Au deposits in Machangqin are typical ores relevant to alkali-rich porphyries of Himalayan movement in"Sanjiang"metallogenic belt, locating at collision environment of Yangtz and Indian plates.
马厂箐铜钼金矿床是“三江”成矿带上与喜马拉雅期富碱斑岩有关的典型矿床之一，产于印支板块与扬子板块碰撞构造环境。
The effect of Yanshan movement and Himalayan orogeny on hydrocarbon migration and accumulation in Junggar basin is analyzed.
分析了燕山运动和喜马拉雅运动在准噶尔盆地油气运移和聚集中的作用。
The Himalayan tectonic movement has caused great tectonic changes in the west China, with deep influence on sedimentary stratum generation and tectonic deformation of the Junggar basin.
喜马拉雅运动使中国西部构造面貌发生了深刻地改变，它给准噶尔盆地无论是沉积地层的发育，还是构造变形打下了深深的烙印。
Himalayan tectonic movement adjusted the initial pressure field in abnormal pressure compartment.
喜马拉雅期构造运动对原始高压封存箱的压力场进行调整改造。
Himalayan tectonic movement adjusted the initial pressure field in abnormal pressure compartment. Based on the circumstances of DE...
喜马拉雅期构造运动对原始高压封存箱的压力场进行调整改造。
Himalayan tectonic movement adjusted the initial pressure field in abnormal pressure compartment. Based on the circumstances of DE...
喜马拉雅期构造运动对原始高压封存箱的压力场进行调整改造。
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