Mineralization in the lithocap consists of pyrite, enargite, tetrahedrite/tennantite, and colusite.
Constantinos Mavrogonatos, Panagiotis Voudouris, Paul G. Spry, Vasilios Melfos, StephanKlemme, Jasper Berndt, Tim Baker, Robert Moritz, Thomas Bissig, Thomas Monecke, FedericaZaccarini 2018, 'Mineralogical Study of the Advanced Argillic Alteration Zone at the Konos Hill Mo–Cu–Re–AuPorphyry Prospect, NE Greece', Mineralshttps://www.mdpi.com/2075-163X/8/11/479. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
Alunite and kaolinite replaced sericite, accompanied with covellite, digenite, enargite, and tennantite replacing chalcopyrite and bornite.
Yang Song, Chao Yang, Shaogang Wei, Huanhuan Yang, Xiang Fang, Hongtao Lu 2018, 'Tectonic Control, Reconstruction and Preservation of the Tiegelongnan Porphyry andEpithermal Overprinting Cu (Au) Deposit, Central Tibet, China', Mineralshttp://www.mdpi.com/2075-163X/8/9/398. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)