指出该区地质构造是燕山运动的产物。
It point out that the geologic structure is the outcome of Yanshan movement.
盆地经历印支运动、燕山运动、喜山运动的改造。
This basin was reformed in Yinzhi movement, Yanshan movement and Ximalaya movement.
燕山运动控制着盆地次一级构造单元的格局及局部构造的形成。
Formation of the secondary structural units of the basin and formation of local structures are controlled by Yanshan movement.
晚海西运动、晚燕山运动对盆地烃源岩的成熟具有重要的影响。
The thermal events of late Hercynian movement and late Yanshanian movement has great effects on the maturation of source rocks.
桌子山形成于燕山运动时期，山体主要由古老的结晶片岩和砂岩构成。
Table mountain was formed in Yanshan movement period, the mountain mainly by the crystallization of ancient schist and sandstone.
燕山运动造成了本区基底构造的基本轮廓—北东向雁列式隆起与拗陷。
The fundamental framework of geological structure of bedrock in Beijing plain was created due to Yanshan Movement in this region.
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 effect of Yanshan movement and Himalayan orogeny on hydrocarbon migration and accumulation in Junggar basin is analyzed.
也就是说，燕山运动是东亚构造体制转变的产物，其出现有着深刻的地球动力学背景。
That is, the Yanshan Movement is the result of the conversion of tectonic regimes in East Asia, which has profound global geodynamic Settings.
文中数值模拟工作对进一步理解“燕山运动”发生的深部背景即来源于软流圈的贡献有一定的意义。
The numerical simulation of this paper is of significance in understanding the deep tectonic background of the generation of Yanshan movement.
湖南晚燕山运动发生于晚白垩世中早期与晚白垩世晚期之间，其构造形迹为角度不整合及假整合关系。
In Hunan province, it took place in the period between early-middle stage and late stage of late Cretaceous epoch. Its structural features are angular disconformity or paraconformity.
所以，这些强过铝质侵入岩的岩石化学数据提供了关于燕山运动峰期地壳发生部分熔融时的温压条件的信息。
Therefore, the petrochemical data provide the P-T conditions of crustal melting in the peak period of the Yanshanian orogeny.
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 periods of early, middle-late Yanshan movement and Himalayan movement are its major periods for hydrocarbon generation and expelling.
它是在燕山地壳运动时期形成的。
燕山断块南边界的北东向断裂存在着较显著的左旋运动。
The north east fracture which is the south boundary of Yanshan fault block shows relative notable sinistral movement.
燕山晚期运动为本区的油气聚集提供了有效的圈闭。
The effective traps for petroleum accumulation were developed mainly in late Yanshan orogeny.
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。
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.
燕山早期运动主要为NW-SE向的挤压褶皱作用，断裂带走向开始弯曲变形；
Near NW-SE compressive folding occurred in early Yanshan orogeny, when it began to buckle.
受燕山早中期构造运动影响，河流相、时令湖相与间歇湖相发育。
The early and middle Yanshanian tectonic movements permitted the fluvial, seasonal lake and intermittent lake facies to be developed.
其成因主要为燕山和海西期的构造运动下形成的。
Origin cause of formation its form under the tectonic movement, the west of issue for swallow mountain and sea mainly.
阐述了分布于燕山板内造山带中段的近东西向中生代右行走滑构造系统的几何学与运动学特征。
The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described.
印支、燕山、喜山运动使断裂带附近的油气藏破坏形成古油藏，但构造相对稳定地区的油气藏仍然得以保存。
After the Indosinian, Yanshan, and Himalayan movements, the previous pools near the faults were damaged, but that in the relatively stable areas were preserved.
印支、燕山、喜山运动使断裂带附近的油气藏破坏形成古油藏，但构造相对稳定地区的油气藏仍然得以保存。
After the Indosinian, Yanshan, and Himalayan movements, the previous pools near the faults were damaged, but that in the relatively stable areas were preserved.
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