Geochemistry, Geochronology, and Prospecting Potential of the Dahongliutan Pluton, Western Kunlun Orogen
Triassic granitoids are abundant on the northwestern margin of the Tibetan Plateau.The Dahongliutan pluton, located in the eastern Western Kunlun orogen, formed in the Late Triassic.Previous field studies have identified potential mixing of crustal and mantle magmas.In this study, we used zircon U–Pb ages and major and trace elemental analyses to