岩性圈闭和地层圈闭的形成与海平面变化和褶皱运动有关。
For lithologic and stratigraphic traps, their origination might relate to sea level changes and folding.
由于受区域构造长期作用的影响，在北天山山前地区逐步发育形成了多排褶皱背斜及活动断裂，且运动方式具有独特性。
Under the effect of regional tectonics there develop many raws drape anticline and active fault in the front of mountain and they have especial motion fashion.
在地壳中一些柔弱地带往往较易受地壳运动剧烈而产生褶皱隆起，而造成绵亘的山脉，世界上许多山脉就是这样形成的。
In the crust some weak areas often more susceptible to intense crustal movement and fold uplift caused by stretching, the mountains, many of the world's mountains is formed.
它们之间特定的位置能创造出运动的效果和水中的反射效果，或如真丝面料般的褶皱。
Their specific positions in relation to each other recreate the effect of movement and reflection in water, or the sensuous folds of silk fabric.
构造运动产生的断裂和褶皱则为成矿提供导矿通道和赋矿空间。
The folds and faults brought by tectonic movement provide routeways and ore-hosting sites for ore-forming.
由于受区域构造长期作用的影响，在北天山山前地区逐步发育形成了多排褶皱背斜及活动断裂，且运动方式具有独特性。
Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion.
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.
该区经历了多期构造运动的改造，不同层系发育的褶皱类型不同。
As a result of multistage tectonic activities, different strata developed different fold types.
根据新测构造地质剖面资料，指出印支运动导致地台盖层和右江盆地构造层全面褶皱的主张是一大误解。
It is confirmed that the theory of the overall folds of the platform cover and the Youjiang basinal synthem of South China caused by the Indosinian movement is a great misunderstanding.
利用断层相关褶皱理论、运动学特征，对准噶尔盆地南缘区域局部构造进行了构造建模研究。
By using the theory of fault-related fold and kinematics characters, research of tectonic modeling about local structures of south margin of Junggar basin was made.
早期韧性简单剪切机制下产生的平卧褶皱，经后期挤压再次发生褶皱，显示构造运动的多期性与构造环境的复杂性。
Recumbent folding was formed by simple ductile-shear dynamics in the early stage, which was refolded by succeeding compression, showing the complexity of multiphase tectonics.
中元古代末的神功运动表现强烈，青白口纪末的晋宁运动叠加褶皱明显。
The Shengong Movement in late Middle Proterozoic Era was strong and the superimposed fold of Junning Movement in late Qingbaikou Period was clear.
断层相关褶皱的几何学运动学分析方法是复杂构造带构造解释的重要工具。
Geometric analysis of the fault related folding is a very important approach to complicated structure interpretation.
断层相关褶皱的几何学运动学分析方法是复杂构造带构造解释的重要工具。
Geometric analysis of the fault related folding is a very important approach to complicated structure interpretation.
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