A Preliminary Study of the Relationship between Mesozoic Lithosphere Evolution in
In recent years, the authors examined lithosphere evolution in eastern China from the lithosphere-asthenosphere deep geological process and found that Early Mesozoic lithospheric evolution and the subduction of the Pacific Plate to the Eurasia Plate had no direct relationship, and they might have been the results of the joint action, i.e., the subduction of some oceanic basins of the East Asian seas that originated in China’s eastern periphery to the East China continental and collisional orogenic belt and the asthenosphere upwelling caused by such actions.