“…In the central zones of the diorite stocks, phyllic alteration accompanies chalcopyrite ± bornite ± molybdenite mineralization, while in the peripheral zone, propylitic alteration dominates with pyrite-chalcopyrite mineralization and occasional magnetite and hematite. The latest-stage mineralization, which occurs in the periphery of the Kalinovskoe deposit, includes various Bi-sulfosalts (bismuthinite–aikinite series, matildite), native gold, galena, sphalerite, tetrahedrite (Plotinskaya et al ., 2014 b ) with bornite, chalcopyrite and rare Au-Ag, Ag, Pb, Bi, and Hg tellurides. The oxidation zone is up to 40 m thick and contains malachite, azurite and chalcocite.…”