在大型逆冲断层活动中，所有的压力都会释放，且会造成一些世上最强烈的地震。
During a megathrust event, all of that stress releases and some of the world's most powerful earthquakes occur.
逆冲断层及边界走精断层是区内主要控矿构造。
Thrust- faults and strike-slip faults are the major structures in the studied area.
这些逆冲断层具有切割深、断距大、剖面宽度大的特点。
These thrust faults are found in the study to be characterized with deep dissection, big separation and major width of the section.
扇状逆冲断层往往在褶曲陡翼发育，产生于褶皱变形达到一定阶段之后。
The thrust faults with a fan-shaped often are evolved in the steep wing and are formed after the fold deformations have reached a definite stage.
撕裂断层与低角度正断层或逆冲断层相交时常形成有利圈闭，如活板构造等。
The tear fault intersected with low angle normal fault or thrust fault can form some traps, e. g. trap-door structure trap.
另一组为NW向走滑断层，形成时代较晚，破坏早期逆冲断层和NE向走滑断层。
The formation time of NE strike slip faults is earlier than that of NW strike slip faults.
淮南煤田阜凤逆冲断层是一压性断层，使寒武系灰岩、砂泥岩推覆于二叠系煤系地层之上。
Cambrain limestone and sandy mudstone were pushed onto the Permian coal measures by the Fufeng thrust in Huainan coalfield.
盐上构造包括盐上滚动背斜、断弯-断展背斜、背冲断块、逆冲断层遮挡构造和盐推覆构造等；
The suprasalt structure includes suprasalt rolling anticline, fault-bending anticline, suprasalt pop-up, thrust screened structure and salt nappe.
西部变形弱、以近ew向宽缓褶皱变形为主，东部变形强、并叠加了NE向褶皱和逆冲断层变形。
In the Western part the deformation was weak only EW-trending open folds occurred while in the Eastern part deformation was stronger but some NE folds and thrusts superposed on the EW folds.
由北向南分为前缘挤压滑脱构造带、斜歪倒转褶皱—逆冲断层带和逆冲推覆岩席及叠瓦状逆冲断层带。
From north to south, several tectonic belts can be distinguished: front compressive detachment belt, overturned thrusting belt, sheeted thrusting belt and imbricate thrusting belt.
一些盐壳覆盖的干涸湖泊 （西班牙语：salars）占据了普纳地区主要逆冲断层之间的地势低洼地（盆地）。
Several salt-crusted dry lakes (known as salarsin Spanish) occupy the basins between major thrust faults in the Puna.
挤压型逆冲断层地震在主震之后，应力传播和释放过程比较缓慢，可能导致余震强度较大，持续时间较长。
Compressive faults occurred after principal earthquake with slow variation in propagation and release of stress wave, this might lead to higher after shock intensity and longer duration.
卡斯卡迪亚被称为“大型逆冲”断层。
推覆构造体系是由几条逆冲断裂带及其逆冲席、逆冲片组成，主干断层与次级断层组成叠瓦式构造。
The structural system of nappe consists of several overthrust fracture belts, thrust sheets and thrust slices, and master fault and secondary fault form an imbricate structure.
次级断层和一些相关伴生构造（擦痕线理）的特征表明了本区逆冲推覆构造系统的逆冲方向为南东-北西向。
Thrusting direction of this system is from southeast to northwestjudging by some characteristics of secondary faults and the associated structures (scratchlineation).
该断裂带北段的木吉河断层运动特征以逆冲为主，兼有右旋走滑分量。
Mujihe fault lies on the northern segment and its main motion characteristics is thrusting, and have dextrorotation slip component.
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.
MCT1原为向南逆冲的韧性断层，后遭受北北东向褶皱作用而转变为正断层。
The MCT1 was originally a south-vergent ductile thrust, which was later transformed into a normal fault after it underwent NNE-trending folding.
金沙江溪洛渡水电站为一巨型水电站，库首区发育一逆冲推覆构造——马家河坝断层。
The Xiluodu Hydropower Station on the Jinsha River is a giant hydropower station, but a thrust nappe structure-Majiahe Dam fault-lies in the reservoir head region.
矿山梁构造几何学上表现为一个双重构造：浅层是一个晚三叠世形成的断层转折褶皱；深层则是在新生代形成的三个逆冲岩片叠置所构成的隐伏堆垛背斜构造。
The key structure in this area is a duplex that comprises of a shallow fault-bend fold of the Late Triassic and a deep blind stacking anticline imbricated by three thrust sheets of Cenozoic age.
矿山梁构造几何学上表现为一个双重构造：浅层是一个晚三叠世形成的断层转折褶皱；深层则是在新生代形成的三个逆冲岩片叠置所构成的隐伏堆垛背斜构造。
The key structure in this area is a duplex that comprises of a shallow fault-bend fold of the Late Triassic and a deep blind stacking anticline imbricated by three thrust sheets of Cenozoic age.
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