Situated in the Vertiskos Unit of the Serbo-Macedonian Massif, the Koryfi porphyry system formed during Early Miocene magmatism, intruding a basement of granitic gneisses, amphibolites, and serpentinized peridotites. Its structural controls, influenced by regional faulting, and mineralization style align with porphyry systems in northern Greece, such as Skouries, though Koryfi is older and more tectonically impacted.