Adyton Resources Corporation reported that petrology work carried out on the highly successful diamond drill hole ADK004 supports the existence of two styles of mineralization – a shallower epithermal style overprinting an earlier porphyry mineralization event, confirming that in a highly mineralized system. Petrological work carried out by Mintex Petrological Solutions on 14 drill core samples has confirmed the geological understanding that two styles of mineralization exist at the Kabang prospect. The first nine shallower samples show epithermal characteristics with pervasive adularia alteration overprinted by kaolinite-dickite and alunite (advanced argillic) alteration with variable paragenetically late pyrite-chalcopyrite-arsenopyrite mineralization in veins (azurite was observed in one sample).

The five deeper samples are plagioclase-phyric phenocryst-rich diorite porphyries with occasional apatite phenocrysts. These brecciated porphyries are chalcopyrite-rich with chalcopyrite replacement of clasts and matrix, as well as mineralized thin quartz veins indicative of porphyry style mineralization. Overall, the shallower samples from this deeper suite of rocks show adularia (potassic) alteration overprinted by advanced argillic alteration (hosting the shallower epithermal gold zone), and the deeper samples also have an advanced argillic overprint into the porphyry system (hosting the underlying porphyry copper /gold mineralization).