这个特别的地方归一位前陆军上校掌管。
简述了国外前陆盆地研究的新进展。
Making new progress on the research for foreland basin is outlined.
前陆盆地是中国重要的油气勘探领域。
Foreland basins are important areas of exploration for petroleum in China.
前陆冲断带普遍具有构造分段的特点。
The foreland thrust belt has a characteristic of structural segmentation in general.
喜马拉雅运动使本区发育为类前陆盆地。
Himalayan movement made the area developed as a para-foreland basin.
前陆盆地是研究造山运动的关键地区之一。
库车坳陷位于塔里木盆地北部，为一前陆坳陷。
Kuche depression, a foreland depression, is situated in the northen Tarim Basin.
欠补偿周缘前陆盆地发育于陆间造山带的早期阶段。
Underfilled peripheral foreland basins develop in the initial stage of intercontinental orogenic belts.
并讨论了龙门山中段中生代前陆盆地的构造演化历史。
The paper also discusses the structural evolution history of the foreland basin in Mesozoic.
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。
Western Sichuan Depression is a foreland basin developed in the west of Sichuan basin since late Triassic.
随着周缘界山的隆升，准噶尔盆地形成三大前陆盆地系统。
With the uplift of marginal mountains, three foreland basin systems were formed in Juggar basin.
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。
Zhungaer basin is a composite and superimposed foreland basin since late Paleozoic.
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。
Fault-bend folds and fault-propagation folds are typical structural styles in the foreland thrust belts.
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 Upper Triassic reservoir in west Sichuan foreland basin has experienced normal compaction and ancompaction.
晚二叠世末，该地区变成弧后盆地，进一步转化成前陆盆地。
The late Permian it was changed into the back arc basin, and transformed into foreland basin.
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。
The lithological feature of the sediments in the foreland basin reflects the double-source supply and the orogenic-belt erosion.
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。
From a tectonic point of view, foreland basins related to plate collision are areas favorable for petroleum accumulation.
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。
The Chuxiong basin in Yunnan on the southwestern margin of the Yangtze landmass is a Mesozoic peripheral foreland basin.
前陆冲断带是前陆盆地内油气聚集的主要场所，也是油气勘探中最难的领域。
Foreland thrust belt is the primary region for the petroleum assemble in the foreland basin, which is the most difficult fields in the petroleum exploring.
特提斯洋关闭和印度板块持续推挤是中国西部前陆盆地形成的构造动力学背景。
Closing of Tethys and continuous compressing and squeezing of Indian plate were the tectonic dynamics background for the formation of foreland basins in western China.
榆木山是位于河西走廊前陆盆地系中张掖盆地和酒东盆地之间的横向隆起山地。
The Yumu mountain is a transverse highland between the Zhangye basin and Jiudong basin in the system.
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。
In the process of south Alps Europe foreland collision, not only the vertical extrusion, but also the lateral extrusion develops.
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.
盆地中的所有构造特征都是这三大前陆盆地系统各构造组成要素叠加复合的结果。
All of the structures in the basin are resulted from the piling-up and compounding of the three systems.
中生代构造快速沉降的沉积体的楔形展布表明盆地具有前陆岩石圈挠曲成因特征；
The Mesozoic rapid tectonic subsidence and wedge shaped sedimentary bodies indicate the origin of lithospheric flexure in the Chuxiong Basin.
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。
The geodynamic environment in which foreland basin is developed is rather limited both temporally and spatially in the geological history.
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。
An analysis of geophysical data shows that geological structures of Junggar basin in plane and in profile have the foreland basin features.
由此，提出了A区带动力层序由前陆挠曲变形体系域(FST)和前陆塑性变形体系域(VST)组成。
It follows that the dynamic sequences in Zone a are made up of the flexural deformation systems tract (FST) and viscoelastic deformation systems tract (VST).
曾母盆地是南沙块体向南俯冲与婆罗洲块体发生软碰撞而形成的一个周缘前陆盆地，经历了四个不同的构造演化阶段。
Zengmu basin is a peripheral foreland basin, formed from southern subduction of Nansha Block and gentle collision with Borneo Block, and experienced four stages of tectonic evolution.
曾母盆地是南沙块体向南俯冲与婆罗洲块体发生软碰撞而形成的一个周缘前陆盆地，经历了四个不同的构造演化阶段。
Zengmu basin is a peripheral foreland basin, formed from southern subduction of Nansha Block and gentle collision with Borneo Block, and experienced four stages of tectonic evolution.
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