With the development of the low temperature thermochronology, numerous relevant studies have been conducted in various tectonic belts around the world. We collected published data involving zircon fission track (ZFT), apatite fission track (AFT), zircon (U-Th)/He, and apatite (U-Th)/He ages that can be applied to reconstructed thermal history of the geological bodies at ~300-55℃. This large low temperature thermochronological datasets can provide clear imaging of the spatial and temporal exhumation for the entire tectonic belts. Furthermore, the significant role of tectonic or climate in setting up regional exhumation pattern during a certain geological history period can also be clarified.