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.
前巴达拉胡地震反射构造层具有杂乱反射特征，它填充在拗陷底部；
The pre-Badalahu layer on the bottom of the depression is characterized by chaotic reflections.
根据生物标志物的对比，认为凝析油来自于构造东部的辽中拗陷内高熟的泥岩。
According to the correlation of biomarkers, the condensate comes from the high mature mudstone in the Liao-zhong depression in the east of this structure.
这种四元结构的形成，起因于区域构造应力场转变成裂陷作用、拗陷作用和差异隆升反转作用的演化。
This four-element architecture may be caused by a regional stress field evolution from rifting, sagging to differential inversion uplifting.
其沉积—构造演化可划分为三个阶段：大陆边缘裂谷、弧后裂谷和拗陷盆地。
Tectono -sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段：大陆边缘裂谷、后裂谷和拗陷盆地。
Tectono - sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.
运用地质、地球物理和分析化验等综合资料，对济阳坳陷的断-拗转型阶段的构造层序及沉积体系作了系统的研究。
Integrated information about geology, geophysical and assaying, study structural sequence and sedimentary system of transition period of fault sag in Jiyang depression.
运用地质、地球物理和分析化验等综合资料，对济阳坳陷的断-拗转型阶段的构造层序及沉积体系作了系统的研究。
Integrated information about geology, geophysical and assaying, study structural sequence and sedimentary system of transition period of fault sag in Jiyang depression.
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