Recently discovered paleo-weathering sedimentary rutile-type titanium deposits in the Benxi Formation of North China have raised critical scientific questions regarding their mineralizing material sources. Taking the Luxi area in the southeastern North China Craton as a case study, this research employs zircon in-situ microgeochemical analysis, integrates zircon geochemical big data, and conducts systematic comparisons with regional tectonic-sedimentary evolution to identify potential mineral sources. The findings provide insights for further scientific research and prospecting strategies. Key discoveries include: (1) Detrital zircons from mineralized geological bodies are predominantly Paleozoic magmatic in origin, exhibiting severe morphological damage indicative of long-distance transport; (2) In-situ microgeochemical analysis reveals that source rocks were primarily granitoids (granodiorite, tonalite, or syenite) formed in continental margin arc settings; (3) By integrating the Paleozoic source-to-sink evolution of the North China Craton, we propose that mineralizing materials likely derived from the North Qinling Orogenic Belt or analogous paleo-orogenic belts (now extinct), with the Qingshui-Taibai and Danfeng-Tongbai regions identified as potential source areas. Through three-dimensional analysis encompassing the craton"s Paleozoic continental evolution, source-to-sink tectonic history, and tectonic-sedimentary dynamics, we establish a comprehensive model for the craton"s geodynamic evolution and source-sink control effects. This framework elucidates the intrinsic causes of regional variations in rutile-type titanium mineralization potential across the North China Craton, providing theoretical foundations for further metallogenic studies and macro-scale prospecting strategies.