1) upthrust and fault belts
推覆体与断裂
2) nappe fault
推覆断裂
1.
During Yanshanian because of obduction of Cathyaysian tectonic from east to west, Hercynian and Indo- Sinian fold belts were reformed, formed brush nappe fault belt opened to southwestward and convergened to northeastward.
燕山期由于受华夏构造自东向西仰冲作用的影响、改造作西侧伏的海西、印支褶皱带形成ＮＥ向分布、断面南倾、向西南撒开、向北东收敛，形如帚状推覆断裂带，在靠近收敛部分控制着金矿的分布。
3) overthrust nappe
冲断推覆体
4) thrusting nappe fault
逆冲推覆断裂
5) Cover thrust nappes
盖层冲断推覆体
1.
Cover thrust nappes, developing mainly in the outer part of the orogenic belts or the foreland fold and thrust belts, formed by the rule of thin skinned tectonics; however, basement fold nappes, occurring mainly in the inner part of the orogenic belts, developed by the rule of thick skinned tectonics.
造山带外带即前陆褶皱冲断带 (主要发育盖层冲断推覆体 ,一般遵循薄皮构造变形规则 )与造山带内带 (主要是基底褶皱推覆体 ,呈现厚皮构造变形规律 )结晶逆冲推覆构造的几何学、运动学特征存在较大差异 ,二者形成机制也不相同 ,但其间仍有紧密的联系。
6) décollement fault
推覆体底部断层
补充资料：推覆
1.覆勘，重新审问。 2.倾覆，推翻。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条