Thermal history modeling of fission track can be used to reconstruct time-temperature histories of a sample and reflect subsidence-uplifting process resulted from tectnonic activity and sedimentation in a basin.On the basis of apatite fission track thermal history modeling results of intrusive rock samples from Yichang and Tongshan in the periphery of Jianghan Basin

we think that the samples have come through four stages of cooling with different cooling rates since Mesozoic

indicating the constant uplifting since the Indosinian period in the periphery of Jianghan Basin.Two rapid cooling stages respectively correspond to two quick uplifting in the Yanshan and Late-Himalayan Periods in the periphery of Jianghan Basin.This kind of process is coupled with the tectonic setting

tectonism-sedimentation and tectonic deformation since the Indosinian period in Jianghan Basin.