准噶尔弧后盆地与弧后残余盆地

ON THE JUNGGAR BACK—ARC BASIN AND BACK—ARC RELICT BASINS

  • 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.

     

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