Foreland basins are the key areas for the study of orogeny.
前陆盆地是研究造山运动的关键地区之一。
Making new progress on the research for foreland basin is outlined.
简述了国外前陆盆地研究的新进展。
Himalayan movement made the area developed as a para-foreland basin.
喜马拉雅运动使本区发育为类前陆盆地。
Foreland basins are important areas of exploration for petroleum in China.
前陆盆地是中国重要的油气勘探领域。
Simulation of plant root systems is a internal and overseas research foreland.
植物根系的模拟是目前国内外研究的前沿问题。
Kuche depression, a foreland depression, is situated in the northen Tarim Basin.
库车坳陷位于塔里木盆地北部，为一前陆坳陷。
Zhungaer basin is a composite and superimposed foreland basin since late Paleozoic.
准噶尔盆地是晚古生代以来多期形成的复合叠加前陆盆地。
Classification, sedimentary and structural features of foreland basin are discussed.
对前陆盆地类型划分、沉积、构造特征进行了研究。
The foreland thrust belt has a characteristic of structural segmentation in general.
前陆冲断带普遍具有构造分段的特点。
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在叠前深度域和弹性波。
The paper also discusses the structural evolution history of the foreland basin in Mesozoic.
并讨论了龙门山中段中生代前陆盆地的构造演化历史。
The late Permian it was changed into the back arc basin, and transformed into foreland basin.
晚二叠世末，该地区变成弧后盆地，进一步转化成前陆盆地。
With the uplift of marginal mountains, three foreland basin systems were formed in Juggar basin.
随着周缘界山的隆升，准噶尔盆地形成三大前陆盆地系统。
The end of the sedimentation of the foreland basin indicates completion of the collisional orogeny .
前陆盆地的终结标志着碰撞造山作用的结束。
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。
Underfilled peripheral foreland basins develop in the initial stage of intercontinental orogenic belts.
欠补偿周缘前陆盆地发育于陆间造山带的早期阶段。
Fault-bend folds and fault-propagation folds are typical structural styles in the foreland thrust belts.
断弯褶皱和断展褶皱是前陆冲断带中的两种典型构造形式。
Western Sichuan Depression is a foreland basin developed in the west of Sichuan basin since late Triassic.
川西坳陷是指四川盆地西部晚三叠世以来形成的前陆盆地。
The Upper Triassic reservoir in west Sichuan foreland basin has experienced normal compaction and ancompaction.
川西前陆盆地上三叠统储层具有正常压实和欠压实两种类型。
The southwest foreland basins in Tarim Basin is composed of Paleozoic basins and the Meso Cenozoic foreland basins.
塔西南前陆盆地是古生代克拉通盆地与中、新生代前陆盆地的复合，在剖面上呈向北抬升的箕状结构。
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陆块的西南边缘，为一典型的中生代周缘前陆盆地。
From a tectonic point of view, foreland basins related to plate collision are areas favorable for petroleum accumulation.
从区域构造的观点看，同板块碰撞有关的前陆盆地是油气聚集的有利地区。
Preface: to explain the object, content, aim, significance, and ways in research, as well as foreland about this problem.
前言：主要对本文研究的对象、内容，研究的目的和意义，研究的方法以及学术界关于这一问题研究的现状进行说明。
The lithological feature of the sediments in the foreland basin reflects the double-source supply and the orogenic-belt erosion.
前陆盆地沉积物的岩石学特征反映了双物源供给和造山带的剥蚀。
In the process of south Alps Europe foreland collision, not only the vertical extrusion, but also the lateral extrusion develops.
中部韧性层在南阿尔卑斯和欧洲前陆碰撞过程中，既有垂向挤出，也有侧向挤出。
The stratigraphic sequences in foreland basins have recorded a long and complex history of polycyclic sedimentary tectonic evolution.
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 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的物理化学条件。
The foreland sediments and structures also show the activity of the fault zone during the collision of the North and South China plates.
前陆沉积与变形构造也表明该断裂带在华北与华南板块碰撞中就发生了活动。
The geodynamic environment in which foreland basin is developed is rather limited both temporally and spatially in the geological history.
在地质历史上，适于前陆盆地发育的地球动力学环境，在时间和空间上均是相当有限的。
An analysis of geophysical data shows that geological structures of Junggar basin in plane and in profile have the foreland basin features.
地球物理资料分析表明，准噶尔盆地地质结构在平面和剖面上具前陆盆地系统的结构特征。
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