成排的库房用带褶皱的铁皮或者陶瓦做顶，立在早已堵塞的下水道前。
Rows of squat warehouses roofed in corrugated steel or terra-cotta tile front sewage-choked waterways.
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.
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.
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.
一些于前地槽、地槽阶段形成的褶皱构造体系所控制的内生金矿产，在形成时代上也属于中-新生代。
Some endogenetic gold deposits controlled by the fold systems which situated in the pre geosynclinal and the geosynclinal stages are formed in the Meso Cenozoic eras also.
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.
在东秦岭前寒武系变质岩中，发育了许多Z字型叠加褶皱。它们是由近直立的片麻岩和长英质脉形成的。
Z-shaped superposed folds formed by nearly vertical gneiss and feldspar-quartz veins are widely developed in East Qinling Precambrian metamorphic rocks.
通过勘探地震信息可以看出：中国西部推覆前锋带的拆离型、褶皱型、前冲型、反冲型等前锋构造。
Through the exploration, earthquake information, we can reach the nappe leading structure modes in the West of China including fold, advance, recoil and so on.
该带不仅是一个地理界线，而且是一个由基底断裂带控制的前第三系雁列褶皱带和第三系构造转换带。
It serves not only as a geographic boundary but also as pre-tertiary en-echelon drapes and a Cenozoic tectonic conversion zone controlled by the basement fault zone.
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.
早白垩世褶皱冲断作用和弧背前陆盆地系 统的发育暗示了拉萨地块发生地壳缩短增厚的时间可能从早白垩世就已经开始。
The presences of Early Cretaceous thrusting and foreland basin system suggest that crustal thickening in the Lhasa terrane likely initiated during the Early Cretaceous.
早白垩世褶皱冲断作用和弧背前陆盆地系 统的发育暗示了拉萨地块发生地壳缩短增厚的时间可能从早白垩世就已经开始。
The presences of Early Cretaceous thrusting and foreland basin system suggest that crustal thickening in the Lhasa terrane likely initiated during the Early Cretaceous.
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