Hans-Peter Schertl

Tectono-magmatic–volatile coupling in postcollisional giant porphyry Cu formation: Evidence from slab tearing and mantle inputs at Qulong, Tibet

The origin of postcollisional porphyry copper deposits (PCDs) within thickened crust remains debated, particularly regarding the coupling between tectono-magmatic–volatile evolution and ore formation. At Qulong, Tibet, new geochemical and isotopic data across four Miocene intrusi...