This study focuses on the lithospheric tectonic evolution and crust-mantle interaction mechanism. In view of the limitations of traditional geochemical methods in tracing the multi-stage transformation process, the North China Craton and the Tanlu fault zone are taken as the research objects, and the zircon micro-area geochemical and isotope tracer data are integrated to systematically explore the evolution law of the crustal magma system and its control mechanism on the lithospheric rheological structure. Studies have shown that the geochemical similarity between late Mesozoic high-Mg potassic granites and Archean magmatic rocks in eastern North China reveals the deep material recycling process, while the zircon REE characteristics of Sulu ultra-high pressure metamorphic rocks record multi-stage crustal reconstruction events. In this paper, a joint analysis system of zircon Hf-O isotope and tectonic magmatic activity is established. Combined with geophysical characterization of lithospheric structure evolution, the process of crust-mantle interaction around Tanlu fault zone is analyzed. By establishing a spatio-temporal coupling model of tectonic-magma-metamorphism, the internal relationship between lithospheric thermal structure evolution and brittle deformation is clarified, and the composite control mechanism of ancient Pacific plate subduction and asthenosphere upwelling on craton destruction is revealed. It has important application value for deep high temperature resource exploration and lithospheric stability evaluation.