吐哈盆地是一个典型的多旋回叠合型盆地,既具有断陷型盆地特征,又具有坳陷型盆地性质。在该盆地内部既有可能发育断陷期陡坡带的岩性油气藏,又有可能发育坳陷期缓坡带的岩性油气藏,其胜北洼陷在中侏罗统-白垩系沉积时期主要发育5种陆相沉积相类型、10种沉积亚相类型。根据层序地层和沉积微相分析,认为胜北地区岩性油气藏发育的有利相带主要分布在辫状河三角洲前缘水下分流河道、冲积扇扇中辫流河道、扇三角洲前缘水下分流河道和滨浅湖滩坝当中。

Turpan-Hami basin is a typical multicycle and multiplex basin, it has both the character of depression basin and that of rifted basin. The lithologic pool such as that developed in the actic region while the basin is rifting or in the glacis region while the basin is depressing all which can be found in this basin. Five kinds of sedimentary facies and thirteen sedimentary parfacies can be found in the Shengbei concave during the period of Jurassic series and Cretaceous series. Based on the research of succession of strata and the sedimentary parfacies, it shows that such as braided stream delta front submersed channel, alluvial middle fan rival chanel, fan delta front submersed channel and front-shallow lake beach and dam are mainly areas of lithologic pool developing.