Typical porphyry style mineralization in supergene and hypogene settings.

Supergene zone locally extends to between 80-100 m depth and is characterized by disseminated azurite and malachite with fractures coated in tenorite. Covellite, cuprite, turquoise, and native copper are less common and are found in veins and fractures.

Hypogene mineralization is defined by vein-hosted and disseminated sulfides (i.e., chalcopyrite, pyrite, bornite, and molybdenite). Chalcopyrite is volumetrically the most abundant copper sulfide, typically within quartz veins and sulfide stringer veins, blebs and disseminations.  Molybdenite is locally present as very fine-grained disseminations or within quartz-sulfide veins as elongate, medium- to coarse-grained blebs along vein centres