In last ten years, people are cognized that formation ofgranitic magma and their evolution is controlled by the process ofasthenospheric upwellingand lithosphere mantle acting, and inaugurate a new direction that combine closely crust—mantle interaction with granitic magma formation and evolution. The scientific front of this new direction primarily is the relationship between granite formation and continent growth and deep process of lithosphere; and the granite anatexis with hot source and granite type andtectonicenvironment. These fronters try to cognizant the granite genesis from the level of continent growing and the continent dynamics, and hope to establish a associated frame between them, and through this frame further to trace their mechanism and region that thermal energy deliver when they formed. Therefore, study the granite can not only provides the information of granite material source and construct environment, but also can acquire the important information about the innate character of crust—mantle material sport appearance, process, dynamics...etc. problems, and deep a conduction and convection of energy (thermal energy). Study and translate these information can take on the function of lucid exposition of essential points for cognizing the continent growth, and is one of the key problems for resolving the nowadays continent geology evolution, establishing the continent dynamics. It can be regard as the beginning of the third milestone about granite research after the granite material source, the tectonic environment research, as a result have the important strategy meanings.