AuKing Mining Limited Prospectus

A U K ING M INING L IMITED I NDEPENDENT T ECHNICAL A SSESSMENT R EPORT – W ESTERN A USTRALIAN M INERAL A SSETS CSA Global Report Nº R278.2020 12 Figure 6: Geological map of the Koongie Park property showing tectonic units and mineral occurences Koongie Park Formation The KPF occurs in the southern portion of the Central Zone of the Halls Creek Orogen (Figure 6). The KPF within the Koongie Park property is broadly characterised as metamorphosed low-grade composed of mafic and felsic volcanic and associated sedimentary facies including sandstone, mudstone, carbonate, chert and ironstone intruded by rhyolitic to rhyodacitic sills, dolerite bodies and basalt dykes. The KPF hosts numerous base metal occurrences and two significant base metal deposits, Onedin and Sandiego (Figure 6). Figure 7 provides a graphic presentation of the detailed stratigraphy of the KPF in the area of the Onedin and Sandiego base metal deposits. The Coolibah Tuff Member is the lowest stratigraphic unit, overlain by the Mimosa Member, followed by the Camp Shale Member, with the Weldons Creek Lava Member at the top of AuKing Mining Limited | PROSPECTUS 87