论文详情
准噶尔弧后盆地与弧后残余盆地
石油实验地质
1992年 14卷 第4期
阅读：106
查看详情
Title
ON THE JUNGGAR BACK—ARC BASIN AND BACK—ARC RELICT BASINS
单位
地质矿产部石油地质综合大队, 湖北江陵 434100
Organization
Research Parly of Petroleum Geology, MGMR
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。
Abstract
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.
关键词：
弧后盆地;
弧后残余盆地;
多旋回叠加盆地;
“多层楼式”含油气组合;
油气勘查领域;
DOI
https://doi.org/10.11781/sysydz199204323
论文详情