1) thrust
逆冲-挤压
2) thrust
逆冲
1.
Near - west - east thrust fault system and north - south slide fault system resulted from the system separate the west area into different chess - type structural blocks .
台北凹陷西部构造活动晚期形成的差异逆冲推覆体系与该区构造格架的定型、油气的运聚具有十分密切的关系。
2.
Accordingto different shapes,they can be divided into 3 types: the eastern thrust nappe belt,the central thrust fold belt and the western compressive nappe belt.
通过地表与深部地球物理资料分析,论证了福建推覆构造的存在,并根据其不同表现形式,划分为东部逆冲推覆带、中部逆冲褶皱带和西部挤压推覆带。
3) thrust fault
逆冲断层
1.
Research on Majiaheba thrust fault in Leibo of Sichuan;
四川雷波马家河坝逆冲断层研究
2.
A study on mechanical mechanism on development of thrust fault;
逆冲断层发育的力学机制研究
3.
The volume of displacement along the NNW-verging master thrust fault is estimated to be about 13.
断层上盘逆冲方向指向NNW,沿着主干逆冲断层发生的倾向位移量约为13。
4) overthrust
逆冲推覆
1.
Characteristics of overthrust structures on northern edge of East Qinling-Dabie orogenic belt and hydrocarbon potentials;
东秦岭-大别造山带北缘逆冲推覆构造特征及油气前景
2.
The strongly fractured layers overthrust from southeast to northwest, which is proved through tensile fractures and boudins in the layers.
是由此产生的推覆体差异剥蚀的结果，这种次级逆冲推覆作用发生在扬子板块前陆褶冲带的变形之后。
5) thrust fault
逆冲断裂
6) thrust
逆冲断层
1.
They are characteri zed by thrust and southward dip.
乌当地区平面上呈东西向展布的五条断层，其断层性质均为向南倾斜的逆冲断层，五条逆冲断层的扩展方式为由北向南依次形成的后展式，逆冲推覆构造的形成时间为三迭纪之后，白垩纪之前。
2.
Yingjisu subsidence of the Meso - Cenozoic was a piggyback foreland basin that developed on the base of fold - thrust belts of the Paleozoic.
盆地的沉积作用和变形作用严格受基底参与的逆冲断层的控制。
参考词条
补充资料：冲击挤压(见冷挤压)
冲击挤压(见冷挤压)
impact extrusion
ehongji jiya冲击挤压(impaet extrusion)见冷挤压。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。