Several epigenetic stratifiorm copper mineralisation (manto type) bodies with variable thicknesses between 20 to 40m are distributed along 900m strike length mineralised corridor named Cinabrio zone. Mineralisation is composed of crisocole, brochantita and malachite in upper oxide levels turning into a mixed zone composed of malachite, crisocole and chalcopyrite. Main sulphide zones are composed of pyrite, bornite and chalcopyrite. All mineralisation is distributed in calcareous shales also within minor pre-existing faults. Dalmacia deposit is located 7km south of the Punitaqui concentrator plant. Also described as a stratiform copper deposit the mineralisation occurs as irregular lenses of chalcopyrite, chalcocite and covellite sulphides within the porphyritic andestites of the reloj formation.