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哈鲁番－哈密盆地是一个聚煤而又富含油气的盆地，已发现了一系列侏罗系煤成烃油气田。地质历史时期的吐哈盆地是一个压缩盆地，并带有左旋扭动性质，因而盆内以扭动构造居多，构造样式复杂多变。盆地基底为前二叠系，沉积盖层以中、新生界为主体。中下侏罗统是含煤层段，也是重要的生烃层系。中侏罗统是煤成烃的主要储油层段，上侏罗统棕红色泥岩是区域性盖层。煤成烃的形成演化具有多元复合、早生早排、富油富气的特点。生油凹陷、古构造、油源断裂及各种三角洲砂体联合控制了油气田的平面分布。
The Haruban-Hami basin is a coal-rich and hydrocarbon-rich basin. A series of Jurassic coal-to-gas fields have been discovered. The Turpan-Hami basin during geologic history is a compression basin with a left-handed twist. Therefore, the basin is dominated by twisting and the structural styles are complex and changeable. The basement of the basin is the Pre-Permian, and the sedimentary cover is dominated by Meso-Cenozoic. Middle-lower Jurassic is a coal-bearing section, which is also an important hydrocarbon generation system. The Middle Jurassic is the main hydrocarbon reservoir formation and the upper Jurassic reddish-brown mudstone is a regional cap rock. The formation and evolution of coal hydrocarbon formation with multiple complex, early row early row, rich oil-rich features. Oil depressions, palaeotectonics, oil source faults and various deltaic sand bodies control the plane distribution of oil and gas fields.