火焰山构造带受基底逆冲断裂控制，断裂控制背斜圈闭形成。
Huoyanshan structure belts are controlled by the basement thrusts. The formation of anticline traps is controlled by the faults.
中部背斜带中发育的构造主要为断层转折褶皱和少量断层传播褶皱，开始形成于中新世上新世中期；
The Central Anticline Zone composed of fault-band folds and a few fault-propagation folds, which started to form during Miocene to the middle stage of Pliocene.
茌平构造带处于鲁西隆起西北倾伏区的中部，是被带内次级断层复杂化的呈北北东向展布的断层背斜带。
Chiping structural zone is a north north east trending fracture anticline belt being complicated by secondary faults, which located in the center of the northwest plunging area of Luxi uplift.
温吉桑-温南地区历经燕山、喜山运动，形成了一系列成排成带展布的断背斜、断鼻等复杂构造圈闭。
Wenjisang - Wennan area had experienced Yanshan and Himalayan movement, and resulted in a series of complicated structural traps such as faulted anticline and faulted nose, etc.
第二排构造带继承第一排由侏罗系煤层传递而来的位移量，在中段由于受阻而发育构造三角楔，形成背斜。
The monocline observed in the field is the forelimb of fault-bend foldings. The second anticline belt inherits the first belt's displacement forming structure wedges.
大池干井构造带的形成不仅在石炭系内形成了众多的裂缝，而且使背斜核部的孔隙度增高。
The formation of Dachigan steep structural zone not only generates many fissures in Upper Carboniferous, but also makes the porosity of Upper Carboniferous higher in the core of these anticlines.
从构造几何学分析来看，乌夏断裂带发育12种主要的构造样式类型，其中断层相关褶皱类型以纵弯背斜、断展背斜及其生长类型为主。
From structural geometry, Wuxia fault belt developed twelve structural styles, among them fault-propagation folds and buckle-propagation anticline are the most important.
从构造几何学分析来看，乌夏断裂带发育12种主要的构造样式类型，其中断层相关褶皱类型以纵弯背斜、断展背斜及其生长类型为主。
From structural geometry, Wuxia fault belt developed twelve structural styles, among them fault-propagation folds and buckle-propagation anticline are the most important.
应用推荐