Apatite fission track dating is carried out on nine samples collected from the central part (Lianmuqin section) and from both northern and southern margins of Turpan Hami Basin. The fission track ages of seven Jurassic samples are distinctly younger than depositional ages. In contrast, the fission track ages of two Cretaceous samples are older than, or as old as depositional ages. These observations indicate that the Jurassic samples have been annealed or partially annealed, whereas the Cretaceous samples have not been annealed. The further thermal modelling results show that Turpan Hami Basin experienced a Late Cretaceous period (120-100 Ma) of tectonic uplift with rapid cooling and exhumation of sediments. The samples underwent a Cenozoic period of reburial and re heating and were exhumed again at 10-8 Ma. Apatite fission track dating is carried out on nine samples collected from the central part (Lianmuqin section) and from both northern and southern margins of Turpan Hami Basin. The fission track ages of seven Jurassic samples are distinctly younger than depositional ages. The observations indicate that the Jurassic samples have been annealed or partially annealed, but the cretaceous samples have not been annealed. The further thermal modeling results show that Turpan Hami Basin experienced a Late Cretaceous period (120-100 Ma) of tectonic uplift with rapid cooling and exhumation of sediments. The samples underwent a Cenozoic period of reburial and re heating and were exhumed again at 10-8 Ma.