The fundamental theoretical framework of the multisphere tectonic view of the earth system is as follows: ① advancing geotectonics from study of the crustal structure and lithospheric structure on the earths surface to a new stage involving study of the multisphere tectonics of the earth system as an integrated whole. ② The global dynamics derived from the interaction of the celestial bodies and the earth systems: The solar energy, multispheric interactions of the earth system, and the combined actions of the motions of celestial bodies in the cosmos system that are the driving forces of various geological processes. The solar energy drives the interactions among the atmosphere, hydrosphere, lithosphere and biosphere on the earth`s surface, which is the main driving force of the earth`s exogenous geological processes. ③ The continent- ocean transformation theory: The continent and the ocean are the two opposite and unified geological units that can be transformed into each other; neither continent nor ocean will survive forever; there is no one- way development of continent accretion or ocean extinction; the simple theory of one- way continental accretion is regarded as invalid. ④ The crust and mantle of the continent are characterized by multiple layers, that can slide along the interfaces between them, but it needs to be corroborated whether the continent arbitrarily or unconditionally moves as a whole. ⑤ The cyclic evolution: the development of the earths tectonics is not a uniform change, but a forward spiralling evolution with a combination of non- uniform and non- linear, gradual and catastrophe changes; different evolution stages (tectonic cycles) of the earth have unique global tectonic patterns and characteristics, one tectonic pattern should not be applied to different tectonic cycles and evolutional stages of the earth. ⑥ The structure and evolution of the crust and mantle are asymmetric and heterogeneous, and thus one tectonic pattern cannot be applied to different areas in the world. ⑦ The polycyclic evolution of the continental crust: The continental crust is not formed by simple lateral or vertical accretion, but the product of combination of the polycyclic tectonic evolution and magmatism. ⑧ Deep fault controls: The deep fault zones cutting through different layers of the crust and mantle usually play an important role in tectonic evolution. For example, the present- day fault zones at mid- ocean ridge fault zones, transform fault zones and Benioff zone outline the global tectonic framework. Different tectonic cycles and stages of the earth`s development had their own distinctive deep fault systems, which controlled the global tectonic framework and evolutional process of different tectonic cycles and stages. Based on Jason (Pacific) and Tuzo (Africa) two mantle supertrees, studying the evolution process of composition and structure of the crust and mantle during the significant transformation and reorganization Meso- Cenozoic tectonic framework in China and Asia is a good entry point to study geotectonics in the multisphere tectonic view of the earth system.