Tectonic Transition from the Neoarchean to Paleoproterozoic in the Northern North China Craton: Constraints from Geochemistry and Zircon U–Pb–Hf Isotopes of the Daxigou Granitoids in a Greenstone Belt
The greenstone belt of the North China Craton (NCC) records the crustal evolution from the Neoarchean to the post-Archean period, offering critical insights into the ancient tectonic background. This study focuses on the late Paleoproterozoic granitoids in the Daxigou area, located within the greenstone belt of the Qia...