thrust margin

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。

This effort concentrated in some areas as Kuqa. However, few work concentrated in the thrust belt in north margin of Qilian mountains.

但这些工作主要集中在库车等少数几个地区，祁连山北缘冲断带的研究还刚刚起步。

The prospecting practices indicate that this foreland thrust belt in northeastern margin of Junggar basin has a great deal of explorative potentials with obvious realms and clear targets, being an important domain for the incremental reserves and productions in Junggar basin.

勘探实践证明，准噶尔盆地前陆冲断带勘探潜力巨大、前景广阔、领域明朗、方向清楚，是准噶尔盆地油气勘探增储上产的重要领域。

Foreland thrust belts are developed extensively margin of Meso Cenozoic sedimentary basins in northwestern China.

我国西部的诸多中新生代含油气盆地周缘广泛发育前陆冲断带.

On styles and mechanism of thrust on the south margin of Inner Mongolia axis

内蒙地轴南缘盖层中逆冲断层的样式及形成机制

The arcuate thrust nappe structure on the southern margin of the southern Qilian Mountains is a nappe system with a double overlapping structure.

南祁连南缘弧形逆冲推覆构造是一个具有双重叠置结构的推覆系统。

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。

The main type of the west margin tectonics belt of the Ordos massif is characterised by thrust nappe.

鄂尔多斯地块西缘构造带的主要形式是逆冲推覆构造。