用镜质体反射率、流体包裹体测温和裂变径迹法对吐鲁番-哈密盆地的地质热历史进行了综合研究,认为该盆地地温具有古高今低、东高西低、南高北低、大断裂发育处高的特点,该规律主要受控于该区基岩埋深和热流值的差异,导致二叠纪烃源岩于三叠纪晚期成熟,侏罗纪烃源岩成熟于侏罗纪末期至早第三纪. The geothermal history of Turpan-Hami basin is studied comprehensively by the vitrinite reflectance, fluid inclusions temperature measurement and fission track method. It is concluded that the geothermal temperature in this basin is high, low, high in the east and low in the west, low in the south, high in the north, The characteristics of the fault development are high. The regularity is mainly controlled by the difference of bedrock depth and heat flow value in the area, resulting in Permian source rocks maturing in Late Triassic, Jurassic source rocks mature in the Jurassic Late to early Tertiary.