在后续的构造沉积演化中，经埋藏而形成稠油封堵油藏，此类油藏具有较强的隐蔽性。
In consequent structural and deposit evolution, it tends to shape heavy oil-sealing reservoir with highly hidden nature.
在制定油气开发方案前，必须建立一个完整的构造演化、沉积作用、成岩作用的综合模式，进而预测有利构造沉积成岩相带。
So, before a development scheme of oil and gas is formulated, a synthetic model on structural evolution, sedimentation, and diagenesis should be set up to predict the favourable zones.
本文提出了拉伸煤盆地最一般的沉积—构造模式，并用以解释盆地结构的演化和泥炭聚积的条件。
A generalized sedimentary-tectonic model for extensional coal basin is presented, together with the explanation for the evolution of basin architecture and the conditions of peat accumulation.
并对组成喜马拉雅造山带各种主要沉积盆地进行了构造沉降分析，研究盆地演化动力机制；
The tectonic subsidence analysis and dynamic mechanism of the basin evolution are processed in the main sedimentary basins across this belt.
构造演化控制了盆地的沉降作用、沉积作用、火成活动和构造格架。
The tectonic evolution controlled the subsidence, sedimentation, pyrogenesis and structure framework of the basin.
沉积环境和构造运动对有机质丰度和热演化程度影响较大。
Sedimentary environment and tectonic movement have great influence on abundance and thermal evolution extent of organic matters.
地层是一切地质问题的基础，地层的划分直接影响着对盆地构造演化、沉积环境甚至对全盆地含油气远景的认识。
The classification of strata has a great effect on the knowledge about structural evolution, sedimentary environment and even evaluation of hydrocarbon potential in a basin.
煤层含气量主要受控于煤岩的沉积环境、煤演化程度、埋藏深度、水文条件与构造条件。
The amount of coal-seam gas is mainly controlled by the depositional environment, coal evolution degree, burial depth, hydrologic condition and structural conditions.
潜江组沉积充填主要受到盆地的构造演化和古气候条件控制。
The sedimentary fillings of Qianjiang Formation are mainly controlled by structural evolution and ancient climate conditions.
中国海域发育了一系列沉积盆地，各盆地地层发育之间的差异说明它们处于不同的构造位置以及各自特有的演化历史。
A series of sedimentary basins have been developed in China sea areas. Differences in development among the basins suggest different tectonic locations and evolutional histories.
这一沉积记录所反映的演化趋可能标志着古特提斯残留海的一次重大构造转折。
The evolutionary tendance reflected by the above sedimentary record probably signifies an important tectonic turn in the history of the residual Paleotethys ocean.
全球性旋回沉积是全球海平面变化、全球气候条件、全球构造演化、全球古地理背景及沉积特征综合作用的产物。
Cyclic deposition on a global scale is the product of the changes in sea-level, tectonics, climate, geography and depositional features of the global or the combination of these.
受沉积剥蚀及盆地构造—热演化的控制，生油岩系的生烃阶段与过程具有多期次的特征。
Controlled by the deposition and erosion as well as the basin thermal evolution, the hydrocarbon generation was of multi-phases.
乌尔逊凹陷沉积过程与构造演化对应，具有阶段性。
The sedimentary history of Wuerxun Depression includes a few stages corresponding with structural evolution.
进行了黄县盆地充填沉积的层序地层划分，并与盆地构造演化阶段分析有机的结合起来。
The sequence stratigraphic division of basin filling succession in Huangxian faulted basin is conducted, and combined with the analysis of tectonic evolution stages of basin.
重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。
This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.
根据对沉积充填与相邻大巴山造山带隆升之间的关系，重建了前陆盆地的构造演化。
The tectonic evolution of Dabashan foreland basin is reconstructed by studying the relationship between the sedimentary fill sequence and the uplift of adjacent Dabashan orogenic belt.
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.
同生构造控制了盆地的形成、沉积及演化。
Syngenetic structures controlled the basin 's forming, settling and evolving.
通过沉积特征、地层层序、构造运动等研究，盆地演化可分为张陷、挤压、张陷、稳定4个阶段。
Through the studying on sedimentary character, stratigraphic sequence and structural movement et, the evolution of the basin can be divided into 4 s...
前陆盆地地层的层序反映了前陆盆地构造演化史为一个多旋回的沉积构造演化史。
The stratigraphic sequences in foreland basins have recorded a long and complex history of polycyclic sedimentary tectonic evolution.
构造地质背景与新构造运动控制着长江三角洲沉积盆地的演化，影响着古地理环境与沉积格局。
The neotectonics controls the evolution of the sediment basin, paleo - depositional environment and pattern of the present Changjiang delta plain.
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.
对哥伦比亚亚诺斯盆地的地层与沉积、构造与演化以及石油地质等特征进行了综合研究。
An integrated study on lithology, sedimentology, structural evolution and petroleum geology in Llanos basin of Colombia is made.
在对该区构造演化史、沉积史深入研究的基础上，建立了成藏模式。
On the basis of researching on Structural evolution history and depositional history in the area, a reservoir formation mode is set up.
碎屑沉积物记录着有关源岩性质和构造演化等诸多重要的信息，对于沉积盆地分析和理解区域构造演化都有重要的指示意义。
Clastic sediments bears much information about the nature of source rocks and their tectonic evolution, which is significant for sedimentary basin analysis.
四川盆地是典型的经历了多期构造演化过程的克拉通盆地，在其多套沉积层序中富含天然气，天然气的开发利用历史悠久。
The Sichuan Basin is a kind of classic cratonic basin having undergone multistage evolution, and is rich of gas resources in the different sets of sedimentary sequences.
四川盆地是典型的经历了多期构造演化过程的克拉通盆地，在其多套沉积层序中富含天然气，天然气的开发利用历史悠久。
The Sichuan Basin is a kind of classic cratonic basin having undergone multistage evolution, and is rich of gas resources in the different sets of sedimentary sequences.
应用推荐