1、

The shallow faults are the result of extensional fracturing of the overlying strata due to lateral compressional warping deformation ( longitudinal buckle deformation) of the basement ( pre-Mesozoic tectonic layer) in the north of the Tabei uplift in the stage of the Kuqa regenerated foreland basin.

浅层断裂是库车再生前陆盆地阶段塔北隆起北部基底(前中生界构造层)受水平挤压翘曲变形(纵弯变形)导致上覆岩层引张破裂的结果。

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2、

Tectonic pattern and dynamic mechanism of the foreland deformation in the lower Yangtze Region

下扬子地区前陆变形构造格局及其动力学机制

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3、

There are some differences between the two types of foreland basins: ( 1) The epicontinental foreland basin went through passive continental margin or retro?-arc rift stage during tectonic evolution stage, but the intracontinental foreland basin lacked this period.

它们之间的主要区别表现在:(1)从盆地构造演化上看,陆缘前陆盆地经历了裂谷被动边缘或弧后裂谷阶段,陆内前陆盆地则缺乏这一阶段;

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4、

From the balanced cross section, it can be revealed that the tectonic style of front and foreland edge was mainly imbricate overthrust fault and related fold, with large reduction of fault and front expansion structure development.

平衡剖面恢复揭示了前山带及前缘地区的构造构造样式主要是叠瓦推覆断层及相关的褶皱,构造缩短量很大;构造发展主要呈前展式。

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5、

Terrestrial heat flow distribution in Kuqa foreland basin, Tarim, NW China

库车前陆盆地大地热流分布特征

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6、

Physical Models of Thick-Skinned Contractional Salt Tectonics in a Foreland Fold-and-Thrust Belt

前陆褶皱冲断带厚皮缩短盐构造运动的物理模拟

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7、

Scaled physical modeling investigated structures formed during thick-skinned contractional salt tectonics in a foreland fold-and-thrust belt. Dry quartz sand simulated brittle sedimentary rocks, and viscous silicon polymer simulated viscous rock salt.

尺度物理实验用干石英砂和聚合硅树脂为实验材料,模拟了前陆褶皱冲断带厚皮缩短盐构造,并与薄皮缩短盐构造及无盐层的褶皱冲断带构造模型进行了对比。

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8、

Accommodation Space Evolution and Third-Order Sequence Correlation in the Second-Order Sequence of a Foreland Basin

前陆盆地二级层序内可容纳空间发育演化及三级层序对比

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9、

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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10、

Foreland basin is rich in oil and gas and foreland thrust fault belt is the focus of current exploration.

前陆盆地的油气资源丰富,前陆盆地的前陆冲断带(山前褶皱&冲断带),是油气勘探的重要领域。

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11、

Under the main thrust fault is a part of the Mesozoic and Cenozoic foreland depression of Jiuquan Basin.

主逆冲断层的下盘掩覆了酒泉盆地中、新生代前陆坳陷的一部分,发育了一受控于深部滑脱断层的断层传播褶皱。

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12、

The evolvement process of the Longmen Shan foreland basin consist of several stages of thrust belt tectonic load and several stages of thrust belt denudation unload. It can be divided into three tectonic load stages and three denudation unload stages.

龙门山前陆盆地的演化过程是由冲断带若干次构造负载阶段与剥蚀卸载阶段组成的,总体上可以分为三个构造负载阶段和三个剥蚀卸载阶段。

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13、

The foreland thrust belt in northwestern margin of Junggar basin is a large-scale imbricated thrust system developed since Late Carboniferous.

准噶尔盆地西北缘前陆冲断带是自石炭纪晚期发育起来的大型叠瓦冲断系统,哈拉阿拉特山冲断带为其冲断前锋构造带的东段。

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14、

Laojunmiao structural belt is located in Cenozoic foreland thrust belt of south margin, Jiuquan basin, which is superposed over the south uplift and Shida depression of Early Cretaceous faulted basin.

老君庙构造带是中国发现最早的老君庙油田所处的构造带,位于酒泉盆地南缘新生代前陆冲断带,叠置于早白垩世断陷盆地的南部隆起和石大凹陷之上。

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15、

Foreland fold-thrust belt thrust structure movement is intense, faults were developed. oil and gas easy to escape, so the preservation condition is the key to oil and gas accumulation.

因其位于冲断带构造活动强烈地段,断裂发育使得油气易于散失,因此,保存条件是该区油气成藏的关键。

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16、

In the Yanshanian period, with continuous NW-directed propagation of the front of the southeastern Guangxi thrust nappe structure, the Jurassic-Cretaceous foreland basin also migrated continuously in a NW direction.

进入燕山期,随着桂东南逆冲推覆构造前缘不断地向NW方向扩展,侏罗纪&白垩纪时期的前陆盆地也不断地向NW方向迁移。

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17、
18、

In this paper, the observed land surface height data and tidal data in the Yellow River delta foreland area are used to describe the variations in depth datum and tidal level in the area.

通过黄河三角洲前沿陆地高程的变化和验潮获得的资料,介绍了黄河三角洲前沿深度基准面的变化和潮位变化情况。

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19、

_cratons, and Verhne_yanskoe and Kuqa depressions belong to the foreland basins or cratonic marginal depressions, and the Northeast Sakhalin and the East China Sea are the back_arc basins.

上扬斯克坳陷和库车坳陷则属于前陆盆地或克拉通边缘坳陷;东北萨哈林和东海为弧后盆地。

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20、

Tectonic Significance of Meso-Cenozoic Conglomerate in the South of the West Sichuan Foreland Basin

川西前陆盆地南部中新生代砾岩的构造意义

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