Copper and Zinc Production,Disciplined Growth.
S I T E V I S I T | O C T O B E R 2 0 1 6
Macedonia Projects
Macedonia projectsKonjsko Historical alluvial Au
mining but no drilling or systematic exploration
Extensive soil anomalies Orogenic gold similar to
Red Lake / Timmins
Dvoriste Cu-Au porphyry project
near Ilovitsa (Euromax) project and Buchim Cu mine
Prospecting licenses Exclusive rights to claim
120km^@ of new exploration licenses
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Dvorishte Dacite porphyry intruding gneiss
/schist basement, with brecciated contact zones.
In same district
Ilovitsa porphyry copper-gold deposit (256.8 Mt @ 0.32 g/t Au & 0.21% Cu)
Buchim porphyry (exploitation) 150 Mt @ 0.3% Cu and 0.35 g/t Au
Kadiica HS and porphyry gold system
Porphyry-type stockwork veins (quartz-pyrite-chalcopyrite) and K-silicate alteration occur at margin of dacite intrusion
Soil sampling and IP to be completed
20 km
Dvorishte: Oxidized quartz limonite veinlets in quartz-clay-sericite altered intrusive
PB1
A2A2
Divorishte
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KonjskoDrilling to begin on orogenic gold targets at
Konjsko fall 2016
Mineralization in the regional Kozuf Massif:
Epithermal/”Carlin-like” Au+Sb+As+Tl at Alshar HS and porphyry Cu-Au at Dudica; Alluvial gold in Konjsko River
Konjsko includes two contrasting styles of mineralization:
Structurally controlled, carbonate-hosted, Sb-As-Tl±Au (stibnite, realgar, orpiment, lorandite) mineralization at Smrdliva Voda
Orogenic Gold (no As or Sb) mineralization in strongly structurised, quartz-veined and intensely altered basement schists / marbles:
19 m @ 2 g/t Au (range 0.075 – 9.85 g/t Au)
Work continuing to define the extent of the gold mineralization and investigate other occurrences including the Dudica high-sulphidation and porphyry Cu-Au Konsjko ‘Road Cut’: Mesothermal
quartz veins cutting basementschists (from a zone with 19m @2.00 g/t Au)
Konsjko – Smrdliva Voda:Sb-As-Tl +-Au zone Visiblerealgar / orpiment instructural zone
Konjsko
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