1) contemporaneous reversed fault
同生逆断裂
1.
Structural features and evolution of contemporaneous reversed faults in Gas faulted depression in western Qaidam basin;
柴西地区尕斯断陷同生逆断裂构造特征与形成演化
2) reverse growth fault
逆同生断裂
3) contemporaneous thrust faults
同生逆冲断裂
1.
Structural features of contemporaneous thrust faults in Hongche fault belt of Junggar Basin;
准噶尔盆地红车断裂带同生逆冲断裂特征
4) contemporaneous faults
同生断裂
1.
The evolution of contemporaneous faults,as the major ore-controlling conditions for the Yindongzi deposit,not only controlled the sedimentary basin,but also made the ore-forming matters exchangeable between upper crust and deeper part.
同生断裂的演化,既是沉积盆地的主宰者,又沟通了地壳上部与更深处的成矿物质的交流,是银硐子矿床的主要控矿条件。
5) contemporaneous thrust sequence
同生逆断层序
6) thrust fault
逆冲断裂
1.
At the same time,tectonic evolution experienced ocean crust diving-collision and intense orogenesis stage,weakly compressing occlude instant volcanic action stage and revived strongly thrust stage,generating many thrust faults to influence sedimentation and denudation and control formation and evolution of thrust belt.
受海西运动晚期的影响,构造演化经历了强烈俯冲碰撞造山期、弱冲断夹短暂伸展火山期和强烈冲断复活期3个阶段,并形成了众多走向不同却又彼此相互切割叠加的逆冲断裂,影响了地层的沉积与剥蚀,控制了断裂带的形成和演化。
补充资料：同逆
1.共同叛逆。
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