As a new tectonic framework, the Late Mesozoic tectonic-magma belts in North China transverse in the NNE strike over different tectonic units of the Paleo-Asian domain with distinct characteristics. Much information marking the Early Mesozoic transfer of the tectonic frameworks can be found in eastern North China. The information is expounded in the paper: Late Triassic mafic-ultramafic and alkaline intrusives, cumulate and granulite are products of crust-mantle interaction in the lowermost of the continental crust; Early-Middle Jurassic diabase dyke swarms, basalts and latite reflect magmatisms in the upper-middle crust; coal-bearing quasi-molasse and volcano-molasse formation controlled by the fault basins formed in J1-2 are responses of the surface to the deep geological process. The new ENE-trending framework marked by sedimentary-tectonic-magmatic belts is controlled by neogenic and inherited tectonic factors. In summary, an idea is proposed that the deep geological process dominates the transfer of different tectonic frameworks, and deformation and formation of the surface are its responses.