摘要
准噶尔盆地是由准噶尔及吐鲁番、哈密地区石炭纪弧后盆地未完全关闭演化而来的二叠纪-侏罗纪弧后残余盆地组成。白垩纪—第三纪则是起源于特提斯区的板块运动对这里的挤压与走滑运动,在天山山前形成的类前陆盆地。多旋回叠加盆地控制了盆地的构造格局与热演化,扩大了盆地油气勘查领域。
The Junggar Basin consists of the Permian-Jurassic back-arc relict basins as the survival of the Carboniferous unfinished closure back-arc basins. During the time of Cretaceous to Tertiary, the foreland basin developed under the compressions and strike-slipings caused by plate movements in the Tethyan tectonic domain. However, the polycyclic superimposed basins controlled over the tectonic framework of the basin and the thermal evolution enlarged the oil/gas prospect in this basin.
出处
《石油实验地质》
CAS
CSCD
北大核心
1992年第4期323-332,共10页
Petroleum Geology & Experiment
