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1)  Overthrust fault zone
逆掩断裂带
2)  overthrust [英]['əuvəθrʌst]  [美]['ovɚ,θrʌst]
逆掩断裂
1.
The Ke-Bai fault is a large overthrust fault.
克百断裂为一大型逆掩断裂,其封闭性能控制了克拉玛依—百口泉地区油气的分布。
3)  thrust set
逆掩断裂组
4)  fault overriding oil zone
断裂掩覆含油带
5)  thrusting fault belt
逆冲断裂带
1.
Based on the interpretation of geophysical data in the western margin of Ordos Basin, it is suggested that the formation and evolution of tri-shaped rift formed by Qinling -Qilian -Helan mountains would be the main factor to form south and north large thrusting fault belts in the western edge of Ovdos Basin.
对鄂尔多斯盆地西缘物探资料解释研究认为:秦祁贺三叉裂谷的形成和演化,是鄂尔多斯盆地西缘形成南北两大不同逆冲断裂带的主要原因。
6)  overthrust fault
逆掩断层
1.
By the analysis and study of a special kind of overthrust fault occurred in the lower layer B 2 of B coal group in Furong Mine,a new method for quantitative prediction,the method of elevation difference value of relative bed interval,is presented.
通过对芙蓉煤矿B煤组下分层B2煤层中出现的一种特殊逆掩断层的分析和研究,提出了一种新的定量预测预报方法——相对层间距高差值法。
2.
Qingxi field is located in middle of overthrust nappe in northern margin(Kulongshan)of Qilianshan mountain where in-tensive piedmont fold is associated with a series of huge overthrust fault structures which are characterized by advanced and im-bricate overthrust faulting toward surface and related folds.
青西油田位于祁连山北缘窟窿山逆掩推覆带的中部,其山前强烈褶皱并伴随一系列大型的逆掩断层,构造表现为断层向地表的前展式叠瓦状逆掩断裂带及其相关褶皱。
3.
Based on the research of development characteristics of overthrust fault, its sealing mechanism is ana- lyzed.
本文通过逆掩断层发育特征研究,分析了逆掩断层封闭机理,在断裂带填充物性质与断层封闭性定量关系模拟实验和膏泥岩变形特征模拟实验基础上建立了断层封闭性评价标准及评价方法,以此对库车坳陷几个典型构造上逆掩断层垂向封闭性进行了评价,结果表明现今断层多是封闭的。
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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