Since 90's, there have been acquiring a lot of researching achievements about Tibet Plateau uplift owing to better methods and the wider thoughts. It not only emphasized the multi-part, multi-phase, multi-factor of Tibet Plateau uplift, but also found the important function of the deep dynamics, the collision of plates and history of uplift. On the one hand, the diachronism of the India-Eurasia collision is about 10 Ma, so it would not be accurate if thinking of the 45 Ma as the start of the collision; On the other hand, although it is different for different geologist thinking about the uplift history of Tibet Plateau, the Plateau has undergone multi-phase uplift which has been generally acknowledged.