Mundoro Capital Inc. announce that the drill program at the East and West Zone on the Zeleznik license has been completed with 4,200 meters of diamond drilling over sixteen completed drill holes. The drill core has been cut and sampled with all assay results expected by end-February 2018. ZELEZNIK EAST ZONE AND WEST ZONE TARGET AREAS: The 2017 Phase III drill program on the East Zone and West Zone was designed to follow up on the previous two drilling campaigns that successfully intersected copper-gold mineralization at both zones. The focus of the Phase III fence drilling program was to define copper-gold bearing porphyry intrusions and dykes, as well as related sulphide mineralization. East Zone: The East Zone drill holes were designed as fences to previous completed holes ZELDD06, ZELDD05 and ZELDD04 and planned in order to further test the carbonate-replacement potential of the East Zone porphyry-marble contacts. Drill hole ZELDD05 intersected 81.2 m @ 0.22% Cu and 0.23 g/t Au from 24.5 m, including 2.8 m @ 2.11% Cu; 1.50 g/t Au while drill hole ZELDD06 ended in mineralization of 4.9 m @ 0.82% Cu; 1.00 g/t Au at a depth of 142.3 m. Thicknesses from inter sections from drill holes are down-hole drilled thicknesses. The current exploration model has not had sufficient drill testing to be able to determine true thickness of mineralization. Porphyry-marblized-limestone contacts are commonly marked by intervals of massive sulphide carbonate replacement origin and the reported copper and gold values from the East Zone are usually associated with these contact bodies. In addition to this type of mineralization, the recent drilling has also identified patches to semi-massive aggregates of fine-grained sooty pyrite and chalcopyrite mineralization within the porphyry intrusion. This is observed in drill hole 17-ZEL-23 which intersected a mineralized zone for approximately 100 meters starting at 76 m depth where fine-grained black sulfides, pyrite, chalcopyrite and/or magnetite were observed within the brecciated and faulted portion of the porphyry. This observed zone may be considered as a feeder to the porphyry mineralization. Drill hole 17-ZEL-23 was designed to test depth extension of the surface channel that returned 30 m with 0.66 g/t gold and 0.1% copper. West Zone: he West Zone drill holes were collared on three parallel sections at approximately 100 m between fences and 100 m between holes on each fence in order to further test the West Zone potential that is built by a swarm of porphyry dykes intruded into a gneiss complex. In a previous drilling campaign, drill hole ZELDD01 instersected one of the early-mineral porphyry dikes with intensive chalcopyrite veining that returned 25.8 m @ 0.39% Cu, 0.08 g/t Au. Thicknesses from intersections from drill holes are down-hole drilled thicknesses. The current exploration model has not had sufficient drill testing to be able to determine true thickness of mineralization. The Company has identified four types of porphyry dykes according to their textural composition that are intruded into a metamorphic unit which is part of Timok. Copper mineralization is associated with A-type quartz veinlets and B-type quartz-pyrite-chalcopyrite veins, as well as disseminated pyrite- chalcopyrite mineralization. Both the early-mineral dykes and the surrounding wall-rock gneiss are mineralized. The recently completed drill hole 17-ZEL-24, at the eastern part of the West Zone, intersected an interval of 30 metres from 35 m depth where chalcocite-covellite-chalcopyrite vein type mineralization was observed within the gneiss. This is new type of mineralization identified in the Phase III drill program.