Mundoro Capital Inc. reported assay results from drilling on the company's 100% owned Byalo exploration license which is located in southeastern Bulgaria in the Rhodopean region of the Tethyan metallogenic belt. The Chuka drill program included 1,000 m in three inclined diamond drill holes. A porphyry unit with stockwork mineralisation and banded quartz veins outcropping at surface returned a significant copper, gold intersection at depth from drillhole CDD001. 146.5 m at 0.40% Cu and 0.12 g/t Au (0.48% CuEq); from 66.8 m to 213.3 m. Including: 80.5 m at 0.51% Cu and 0.15 g/t Au (0.61% CuEq); from 74 m to 154.5 m; including: 20.9 m at 0.72% Cu and 0.11 g/t Au (0.79% CuEq); from 74 m to 94.9 m. These three drill holes were successful in cutting significant copper-gold mineralisation related to intense stockwork veining showing the Chuka system is capable of hosting higher grades. The hydrothermal breccia intersected in the drill holes was not a recognized feature at surface and therefore further drilling is required to investigate how the hydrothermal breccia relates to the porphyry environment, diatreme or milled fault breccia and if copper-gold grades related to it increase at depth. Recognition of fine grained covellite and chalcocite copper bearing minerals and argillic-phyllic style of alteration suggest the Chuka system maybe part of an epithermal system transitioning to a porphyry system. Drill hole CDD-001 was collared into the outcropping quartz-sulfide stockwork mineralisation defined through mapping, soil and rock sampling. The drill hole intersected significant copper - gold mineralisation related to strong quartz stockwork veining containing pyrite, chalcopyrite, covellite and chalcocite. The stockwork continues for 213.3 m and is hosted by sericitic altered latite porphyry interpreted as an early mineralising event. At 213.3 m the latite porphyry is cut by a late mineral sanidine porphyry which is argillic altered and contains anomalous lead-zinc and gold values without significant mineralisation. At 257.5 m the hole intersected a fault contact and re-entered the latite porphyry however without the intense stockwork mineralisation which may have been shifted due to faulting. Alteration of the latite porphyry after the fault is phyllic-argillic to advanced argillic. Drill hole CDD-002 was drilled 150 m north-east from CDD-001. The drillhole intersected the latite porphyry from 34.8 m to 103.1 m then transitioned to hydrothermal breccia to 212 m and was completed in late mineral sanidine porphyry at 257.8 m. Although no significant copper-gold intervals were intersected, the latite porphyry and the hydrothermal breccia are highly anomalous in copper-gold and especially Molybdenum (Mo). Intersected Mo grades and intervals in this drillhole are significant with single samples returning above 700 ppm Mo. Some high grade Mo intervals include: 79.9 m at 173 ppm Mo from 36.9 m to 116.8 m; 39.2 m at 330 ppm Mo from 129.9 m to 169.1 m; and 19 m at 295 ppm Mo from 178 m to 197 m. Drill hole CDD-003 was drilled as a step back 150 m north-west from CDD-001. It intersected milled hydrothermal breccia probably after latite porphyry from 17.7 m to the end of the drillhole. The breccia is cut by late mineral sanidine porphyry from 250.9 m to 270 m and from 303.7 m to 355.3 m. The breccia is carrying copper-gold-molybdenum mineralisation throughout and is also partly anomalous in lead and zinc. The drillhole was bottomed in hydrothermal breccia carrying copper-gold mineralisation after contact of post mineral sanidine porphyry.