• Foreland basins are the key areas for the study of orogeny.

    前陆盆地研究造山运动关键地区之一

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  • Making new progress on the research for foreland basin is outlined.

    简述了国外前陆盆地研究进展

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  • Himalayan movement made the area developed as a para-foreland basin.

    喜马拉雅运动使本区发育陆盆地。

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  • Foreland basins are important areas of exploration for petroleum in China.

    前陆盆地中国重要油气勘探领域

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  • Simulation of plant root systems is a internal and overseas research foreland.

    植物根系模拟目前国内外研究前沿问题

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  • Kuche depression, a foreland depression, is situated in the northen Tarim Basin.

    库车位于塔里木盆地北部,为前陆坳陷。

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  • Foreland is concentration of Fujian Province population, economy developeds area.

    沿海地区福建省人口集中经济发达地区

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  • Zhungaer basin is a composite and superimposed foreland basin since late Paleozoic.

    准噶尔盆地古生代以来多期形成的复合叠加前陆盆地。

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  • Classification, sedimentary and structural features of foreland basin are discussed.

    前陆盆地类型划分沉积构造特征进行了研究。

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  • The foreland thrust belt has a characteristic of structural segmentation in general.

    陆冲断带普遍具有构造分段特点

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  • The leading research foreland mainly focuses on pre-stack depth domain and elastic wave.

    目前的研究前沿主要集中叠前深度弹性

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  • The paper also discusses the structural evolution history of the foreland basin in Mesozoic.

    讨论了龙门山中段中生代前陆盆地构造演化历史

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  • The late Permian it was changed into the back arc basin, and transformed into foreland basin.

    世末,该地区变成盆地进一步转化前陆盆地。

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  • With the uplift of marginal mountains, three foreland basin systems were formed in Juggar basin.

    随着周缘界山隆升,准噶尔盆地形成三大前陆盆地系统

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  • The results indicate that fault-related folding is the basic deformation style in this foreland basin.

    模拟结果表明库车前陆盆地是以断层相关褶皱作为滑动机制的前陆冲断带。

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  • Underfilled peripheral foreland basins develop in the initial stage of intercontinental orogenic belts.

    欠补偿周缘盆地发育山带早期阶段

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  • Fault-bend folds and fault-propagation folds are typical structural styles in the foreland thrust belts.

    断弯褶皱断展褶皱陆冲断带中的两种典型构造形式

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  • Western Sichuan Depression is a foreland basin developed in the west of Sichuan basin since late Triassic.

    川西四川盆地西部三叠世以来形成前陆盆地。

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  • The Upper Triassic reservoir in west Sichuan foreland basin has experienced normal compaction and ancompaction.

    川西盆地三叠统储层具有正常欠压实两种类型。

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  • The southwest foreland basins in Tarim Basin is composed of Paleozoic basins and the Meso Cenozoic foreland basins.

    塔西南盆地古生代克拉盆地中、新生代前陆盆地的复合,剖面上呈向北抬升的箕状结构。

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  • The Chuxiong basin in Yunnan on the southwestern margin of the Yangtze landmass is a Mesozoic peripheral foreland basin.

    云南楚雄盆地位于扬子块的西南边缘典型中生代周缘前陆盆地。

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  • From a tectonic point of view, foreland basins related to plate collision are areas favorable for petroleum accumulation.

    区域构造观点看,同板块碰撞有关的前盆地油气聚集的有利地区

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  • Preface: to explain the object, content, aim, significance, and ways in research, as well as foreland about this problem.

    前言:主要对本文研究对象内容,研究的目的意义,研究的方法以及学术界关于一问题研究的现状进行说明

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  • The lithological feature of the sediments in the foreland basin reflects the double-source supply and the orogenic-belt erosion.

    前陆盆地沉积物岩石学特征反映了双物源供给造山带剥蚀。

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  • In the process of south Alps Europe foreland collision, not only the vertical extrusion, but also the lateral extrusion develops.

    中部韧性层阿尔卑斯和欧洲碰撞过程中,既有挤出侧向挤出。

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  • The stratigraphic sequences in foreland basins have recorded a long and complex history of polycyclic sedimentary tectonic evolution.

    盆地地层层序反映前陆盆地构造演化史一个多旋回的沉积构造演化史。

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  • The physical chemical conditions of oil gas migration in the Kuqa foreland basin were studied with fluid geology method in this paper.

    本文运用流体地质学方法研究了库车前陆盆地油气运移物理化学条件

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  • The foreland sediments and structures also show the activity of the fault zone during the collision of the North and South China plates.

    沉积与变形构造表明断裂带华北华南板块碰撞中就发生活动

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  • The geodynamic environment in which foreland basin is developed is rather limited both temporally and spatially in the geological history.

    地质历史上,适于前陆盆地发育地球动力学环境,在时间空间相当有限的。

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  • The geodynamic environment in which foreland basin is developed is rather limited both temporally and spatially in the geological history.

    地质历史上,适于前陆盆地发育地球动力学环境,在时间空间相当有限的。

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