Abstract: Pre-, syn-, and post-orogenic (pre-, syn- and post-collisional) granitic rocks are a hot topic of granite research. However, vague and contradictory views exist about the concepts of pre-, syn-, and post-orogeny. Therefore the authors present a new concept and discrimination method for pre-, syn-, and post-orogeny and discuss some case histories of Africa, Turkey and Brazil. The focus is on granitic rocks of the Qinghai-Tibet Plateau related to collision. They point out that only the pre- and syn-orogenic stages occurred on the Qinghai-Tibet Plateau. The collision on the Qinghai-Tibet Plateau took place at ~50 Ma. The 25-3 Ma adakite and leucogranite formed in the collision stage. The features of the 25-3 Ma granitic rocks imply that the Qinghai-Tibet Plateau had been uplifted wholesalely before 25 Ma, and the extensional tectonics (such as southern detachment system, large-scale strike-slip faults and N-S-striking rift) that developed after 25 Ma formed by compression in the syn-orogenic stage, rather than crustal extensional thinning and collapse in the post-orogenic stage.