临清地区中新生代盆地的形成演化与油气

THE FORMATION, EVOLUTION OF MESO-CENOZOIC BASINS AND THEIR RELATIONSHIP TO OIL/GAS IN LINQING REGION

  • 摘要: 临清地区自三叠纪末—侏罗纪经历了拉张—挤压—拉张的交替更迭的地洼发展阶段。由于受边界条件的影响,控制两个地洼盆地发展期构造活动是多因素的,在盆地内形成的构造期也因地而异,故其内部构造显得十分复杂。

     

    Abstract: Linqing Region was experienced transformation from platform to Diwa(geodepression)stages during the period from Late Triassic to Early Jurassic.Severe extensions and faultdown took place during Jurassic-Early Cretace-ous and Paleogene,respectively.Thereafter,the two cycles of Mesozoic and Cenozoic Diwa(geodepression)basins and oil formations were formed.In addition to various basin types and complex structural patterns,combined with possible Paleozoic-Triassic platform type oil/gas in this region,it becomes a promising oil/gas prospect area.

     

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