Petrogenesis of Permian high-Mg diorites in the northern margin of the North China Craton: Evidence of crust–mantle interaction

The investigation of sanukitoids is particularly important for improving our understanding of crust–mantle interaction. This paper presents zircon and titanite U–Pb and bulk −rock major element, trace element, mineral major element and Sr–Nd–Pb–Hf isotope data for newly discovered Xinhure high-Mg di...