燕山期是盆地油气运移和聚集的主要时期。
Yanshanian period is the main stage for migration and accumulation of oil and gas in this basin.
构造运动的性质及其强度对油气运移和聚集过程有重要的影响。
The tectonic movement nature and the intensity have the important influence to the petroleum migration and accumulation process.
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.
研究区油气形成的生、储、盖组合齐全，油气运移和聚集构造条件有利。
There are well-developed source-reservoir-cap assemblage and favourable oil-gas migration and accumulation condition.
在此基础上文中概括了盐构造、流体流动及油气运移和聚集相互关系的模式。
A model summarizing the relationships of salt tectonics, fluid flow, and hydrocarbon migration and accumulation is proposed based on it.
研究区油气形成的生、储、盖组合齐全，油气运移和聚集构造条件有利。通过卫星遥感影象解译出的五个环形构造都是有利的油气勘探远景区。
There are well-developed source-reservoir-cap assemblage and favourable oil-gas migration and accumulation condition. Five circular structures interpreted from Landsat MSS images are fav…
多期次的构造运动和适度的变形，为油气运移、聚集和圈闭的形成打下了良好的基础。
Owing to tectonic activity with multiple stages and appropriate deformation, it lays a good foundation for hydrocarbon migration, accumulation and trap forming.
利用整体、动态、综合的含油气盆地分析方法和油气运移的倒汇水模式，天然气自生成后至今主要运移聚集在五个有利区带；
Five prospective gas plays are outlined by means of a method of integral, dynamic and comprehensive basin analysis and synthesis prediction of oil and gas pool formation.
研究结果对压实流盆地油气运移、聚集理论模型和模拟方法的研究具有重要的地质意义。
The results can be important in studies of theoretical models and simulation methods of petroleum migration and accumulation for Mesozoic and Cenozoic basins of East China.
从油气运移的角度将延长矿区成藏模式归纳为就近聚集型、顺层运移型和穿层运移型三种类型。
At last the paper summarized the oil pool-forming models in Yanchang oil field as nearby accumulation type, along-layer migration type and trans-layer migration type.
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。
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。
The Himalayan movement controls final stereotype of local structures and faults, hydrocarbon migration and accumulation for forming reservoirs are also controlled by it.
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