摘要
周口坳陷发育有古生界潜山,古生界潜山的形成主要受构造运动的控制,燕山期、喜山期拉张应力场控制了古生界潜山的分布,印支期、燕山期挤压应力场主要使古生界潜山的内幕结构更加复杂化。大断裂控制古生界潜山的分布。周口坳陷主要发育北西和北东向的古生界潜山。
Buried hills of Paleozoic developes in Zhoukou depression .The formation of Paleozoic buried hills is mainly controlled by tectonic movements. The distribution of buried hills is controlled by the stressed field of stretching during Yanshan and Himalayan period ,and the stressed field of compressing during indosinian and Yanshan period mainly makes the inside structure of paleozoic buried hills more complex .The distribution of paleozoic buried hills is controlled by regional fault. Paleozoic buried hills of NW , NE trending developes well in Zhoukou depression.
出处
《重庆科技学院学报(自然科学版)》
CAS
2005年第2期16-19,共4页
Journal of Chongqing University of Science and Technology:Natural Sciences Edition
关键词
周口坳陷
古生界潜山
构造运动
分布规律
Zhoukou depression
Paleozoic buried hills
Tectonic movements distribution law