1)  Thrust belt
逆断裂带
2)  fold-reverse fault zone
褶皱-逆断裂带
1.
As a result, several rows of fold-reverse fault zones have been progressively formed within the foreland basins.
新生代以来,由于印度板块与欧亚板块的碰撞,天山晚古生代褶皱和断裂构造重新复活隆起,并向南北两侧推挤,在前陆盆地中渐进式地形成多排褶皱-逆断裂带
3)  Active folding and faulting belt
活动背斜-逆断裂带
4)  reversed fault
逆断层
1.
How to think over oil & gas exploration in thrust belt?Firstly,we should discuss the definiton of thrust belt,thrust fault,overthrust belt,reversed fault and overthrust fault and their differences,and then analyze the causes of formation and mechanisms as well as the tectonic background.
如何看待冲断带油气勘探,首先要讨论冲断带、冲断层、掩冲带、逆断层、逆掩(或掩冲)断层的定义及其差异,然后分析冲断带的成因机制和形成的大地构造背景,冲断带油气勘探的兴衰历史。
2.
In compress-shear oil and gas bearing basin exploration, early exploration is concentrated on the high position of fault-fold structural zone, many fault-anticline, fault-nose hydrocarbon reservoirs are found, but with the deepening of exploration, the fault trap formed by the reversed fault and convergent torsion fault of these fault-fold structural footwall has to be considered.
在压扭性含油气盆地勘探中,早期主要集中在断褶构造带的构造高部位,并已找到了许多断背斜、断鼻型油气藏;但随着勘探的深入,不得不考虑这些断褶构造下盘由逆断层和聚敛型扭断层封闭所形成的断层圈闭。
3.
How to think over oil & gas exploration in thrust belt? Firstly,we should discuss the definition of thrust belt,thrust fault,overthrust belt,reversed fault and overthrust fault and their differences,and then analyze the causes of formation and mechanisms as well as the tectonic background.
如何看待冲断带油气勘探,首先要讨论冲断带、冲断层、掩冲带、逆断层、逆掩(或掩冲)断层的定义及其差异,然后分析冲断带的成因机制和形成的大地构造背景,冲断带油气勘探的兴衰历史。
5)  reverse fault
逆断层
1.
Dynamic simulation of effect field of strong ground motions and deformation of ground near reverse fault;
逆断层地震近场地震动影响场和地表形变模拟
2.
Study of algorithm for Delaunay triangular irregular network of constrained data field with reverse fault;
带地质逆断层约束数据域的Delaunay三角剖分算法研究
3.
In the tectonic system in Subei Basin, there exist reverse faults, nose-like blocks in an echelon arrangement, pinnate faults occurring at both sides of a major controlling fault of the depression, sinistral step dislocation arrangement of the major fault and northwest regional structural belt.
在苏北盆地构造体系中 ,存在着逆断层、雁行状排列的断鼻断块群、凹陷主控断层两侧的羽状断层、主控断层的左阶式错位排列及区域北西向延伸的构造带等构造特征。
6)  inverse transversal
逆断面
1.
Certain subsemigroups of regular semigroups with an inverse transversal;
具有逆断面的正则半群的一些子半群
2.
Constructions of cryptogroups with inverse transversals;
具有逆断面的密群的构造(英文)
3.
Identities for the Classes of Regular Semigroups with Inverse Transversals;
具有逆断面的正则半群类的等式(英文)
参考词条
补充资料:断裂带

亦称“断层带”。有主断层面及其两侧破碎岩块以及若干次级断层或破裂面组成的地带。在靠近主断层面附近发育有构造岩,以主断层面附近为轴线向两侧扩散,一般依次出现断层泥或糜棱岩、断层角砾岩、碎裂岩等,再向外即过渡为断层带以外的完整岩石。断层带的宽度以及带内岩石的破碎程度,决定于断层的规模、活动历史、活动方式和力学性质,从几米至几百米甚至上千米不等。一般压性活压扭性断层带比单纯剪切性质的断层带宽。在一些大型的断层带中,由于被后期不同方向的断层切错,和夹有一些未破碎的大型岩块,只是断层带的结构趋于复杂化,从而在近代的断层活动中容易形成运动的阻抗,是应力易于积累和发生地震的场所。

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