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.
准噶尔盆地南缘前陆冲断带构造演化与成藏过程复杂。
The tectonic evolution and hydrocarbon accumulation in the foreland fold-and-thrust belt of the southern JunggarBasin is complex.
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.
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.
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。
The results indicate that fault-related folding is the basic deformation style in this foreland basin.
准噶尔盆地西北缘前陆冲断带构造样式复杂多样，除规模较大的逆断层外，还发育一系列北西向的走滑断层。
The foreland thrust belt has complex and various structural styles. Besides the large-scale reverse faults, there are a series of north-west strike-slip faults.
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。
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.
洋岛玄武岩以弄槐枕状熔岩为代表性火山岩，原为古特提斯洋盆中的夏威夷型洋岛，现保存在印支期前陆褶皱冲断带的一个外来岩席中。
The oceanic island basalt is represented by the Nonghuai pillow lava, which is, originally Hawaii type one in the Paleotethyan ocean, an allochthon in the Indosinian foreland fold and thrust belt.
塔西南山前冲断带及其前陆盆地系统是一个油气勘探前景较好的地区，但目前对该地区的研究程度和勘探程度都比较低。
The overthrust fault zone and foreland basin in Southwestern Tarim is favorable areas for petroleum exploration. But the research and exploration degree here are still low.
大别与苏鲁造山带周边都出现了强烈的前陆褶皱冲断带。
The intensive foreland fold-and-thrust belts occurred on the both sides of the Dabie-Sulu orogenic belt.
江西北部地处欧亚大陆板块东南沿海前陆推覆冲断带，与扬子、华夏古板块结合带叠加部位。
North Jiangxi area is located in the superimposed part of foreland nappe thrust zone of the southeast coast of Eurasian Contiental Plate and Yangzi and Precambrian Cathaysia Plates.
在综合前人研究成果的基础上，认为造山楔进作用是前陆盆地与造山带耦合的主要动力学机制；冲断作用控制沉积物的分布和扩散型式；
Based on the analysis of the previous studies, the orogenic wedge process is considered to be the main dynamics of the coupling of foreland basins and orogenes.
基底冲断隆起带与川北类前陆盆地平缓褶皱带，在调节两侧造山带构造平衡时表现出明显的差异性。
Due to basement rock rigidity, basement thrustuplift zone and northern Sichuan paraforeland zone have marked disparity in the process of adjusting structural balance.
基底冲断隆起带与川北类前陆盆地平缓褶皱带，在调节两侧造山带构造平衡时表现出明显的差异性。
Due to basement rock rigidity, basement thrustuplift zone and northern Sichuan paraforeland zone have marked disparity in the process of adjusting structural balance.
应用推荐