• Triangle zones normally develop in foreland fold-and-thrust belts and become favorable object of petroleum exploration.

    构造三角带通常发育于褶皱冲断带中,是油气勘探的重要目标。

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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陆块的西南边缘,为一典型的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.

    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。

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  • Advantaged geographic location gives this city an opportunity to become the foreland connecting "World Factory" and "World Market".

    得天独厚的地理条件使得这里有机会成为了“世界工厂”与“世界市场”接靠的最前沿。

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  • Customer Relationship management (CRM) is a new problem in enterprise management theory foreland and got broad attention of numerous experts and scholars.

    客户关系管理(CRM)是企业管理理论中的前沿性新课题,受到众多专家学者的广泛关注。

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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的新进展。

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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为类前陆盆地。

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  • 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。

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  • 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。

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  • 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。

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  • 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。

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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在叠前深度域和弹性波。

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  • 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。

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  • 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。

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

    随着周缘界山的隆升,准噶尔盆地形成三大前陆盆地系统。

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  • 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。

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  • 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。

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  • 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。

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  • The intensive foreland fold-and-thrust belts occurred on the both sides of the Dabie-Sulu orogenic belt.

    大别与苏鲁造山带周边都出现了强烈的前陆褶皱冲断带。

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  • 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。

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  • 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。

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  • The covered structural belt and the depression of foreland basin are favorable belts for oil and gas exploration.

    逆掩推覆带和前陆坳陷带是油气勘探的有利区带。

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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。

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  • The exploration revealed that the Kuqa foreland depression was becoming an important giant gas accumulating area by degrees.

    随着勘探的深入,库车前陆坳陷逐渐成为我国重要的大气区。

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

    前陆盆地沉积物的岩石学特征反映了双物源供给和造山带的剥蚀。

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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。

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  • From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

    在与国外前陆盆地对比的基础上,得出四川盆地是一个受多方向挤压应力综合作用的前陆盆地。

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  • 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。

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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的物理化学条件。

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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.

    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。

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