Delamerian Base Metals Project
The Delamerian project is located in the Delamerian Orogen in western New South Wales. The project consists of an area of 1,936 square kilometres at the northern end of the Koonenberry Belt, 60 kilometres east of Tibooburra and an area of 2,344 square kilometres in the Loch Lilly-Kars Belt, 55 kilometres southeast of Broken Hill.
The Delamerian Orogen comprises Late Neoproterozoic to Ordovician rock sequences stretching from eastern South Australia, through western New South Wales and Victoria to western Tasmania. It encompasses the remnants of an accretionary craton margin that hosts Late Neoproterozoic to Cambrian rift related mafic magmatism and Middle Cambrian to Early Ordovician felsic magmatism. The mineral potential of the orogen is well recognised in the areas where it outcrops – the Adelaide Fold Belt in South Australia, the Stavely Belt in Victoria and the Mount Read Volcanics in Tasmania – however large portions of the orogen are covered by younger basins, such as the Murray Basin. This has deterred exploration historically and has limited the understanding of the orogen’s full mineral potential.
The northern tenement area covers approximately 80 kilometres of strike of a covered extension of Late Neoproterozoic Kara Formation which hosts primitive mafic igneous intrusives of the Mt Arrowsmith Volcanics. The presence of extensive mafic/ultramafic sill complexes in craton margin sediments is considered analogous to settings that host large Ni-Cu -PGE sulphide systems globally (e.g. Albany Fraser Belt in Western Australia and the Circum-Superior Belt in Canada).
The southern tenement area covers approximately 150 kilometres of strike of the Loch Lilly-Kars Belt under the shallowing margins of the Murray Basin. The application has secured almost the entire Loch Lilly-Kars Belt. Based on geophysical and drill hole data, the belt is interpreted as consisting of geological sequences formed in a back-arc basin setting. These settings are known to host Volcanogenic Massive Sulphide (VMS) deposits. There is also evidence of felsic high-level subvolcanic intrusions, often associated with magmatic related copper deposits, and mafic intrusive complexes providing Ni-Cu-PGE potential. A series of major belt-scale faults are observable that would act as major fluid flow conduits during both early extensions and later deformation of the belt.
Pyramid Gold Project
The Pyramid tenement group is located southeast of Charters Towers in north Queensland. The project, covering 150 square kilometres, embraces two main areas prospective for gold, being the West Pyramid Range and East Pyramid Range. AIC Mines acquired the project as part of the takeover of Demetallica Limited in December 2022.
West Pyramid Range offers potential to expand the gold mineralisation footprint defined through historic work, especially along an 8 kilometre section of the Gettysberg Fault corridor. The East Pyramid Range offers potential for Intrusion Related Gold Systems (IRGS), similar in style to other well-known gold deposits in the district such as Mount Leyshon (+3.5Moz) and Mount Wright (+1Moz).
Windsor Base Metals Project
The Windsor tenements are located 60 kilometres south of Charters Towers in north Queensland. Covering 629 square kilometres, the tenements offer discovery potential for high-grade VMS style mines, such as the nearby Thalanga, Highway-Reward, Waterloo and Liontown deposits. AIC Mines acquired the project as part of the takeover of Demetallica Limited in December 2022.
Stratigraphic horizons encapsulating those deposits are interpreted to continue through the Windsor project area. Past exploration has been inhibited by the highly conductive nature of the cover sequence and previous drilling is sparse and shallow; thus most of the project area is relatively lightly explored.
The Marymia Project
The Marymia Project is located approximately 160 kilometres south of Newman in the eastern Gascoyne region of Western Australia and covers approximately 3,600 square kilometres. The project is prospective for both gold and copper deposits and is strategically located within trucking distance of the Plutonic Gold Mine and the DeGrussa Copper Mine.
Exploration by AIC is focused on the discovery of Archean orogenic gold mineralisation, within and on extensions of the highly endowed Plutonic-Marymia Greenstone belt (PMGB), and volcanogenic massive sulphide (VMS) style base-metal mineralisation along strike of the DeGrussa Copper Mine and on the northern margin of the Marymia Inlier.
Copper exploration is focused along the Copper Hills Belt, which extends for over 50 kilometres along the northern margin of the project. The belt lies between the Archean PMGB and the Collier Group and is considered by AIC as belt of Paleoproterozoic age rocks, similar to the nearby Bryah and Yerrida sedimentary basins that are known to host VMS style mineralisation. Historical exploration in the belt has focussed on banded magnetite mineralisation but surface geochemistry, geological mapping, trenching and limited shallow drilling at the Copper Hills Prospect suggests the presence of felsic to mafic metavolcanic rocks associated with copper oxide mineralisation that is considered permissive and indicative of an unrecognised VMS belt. Airborne electromagnetics, surface geochemistry and RC drilling has been completed by AIC to understand the potential of this belt.
Gold exploration is focused on extensions of the Plutonic-Marymia Greenstone belt, which has produced in excess of 6 million ounces of gold. Mapping, surface geochemistry, ground gravity surveys and limited drilling indicates that extensive remnants of Archean greenstone occur within explorable depths and are contained within a broad area historically denoted as granite. While prospects containing gold mineralisation (such as Marymia NE) underscore the potential for gold in granite dominated regions, the perception of ‘barren’ granite means extensions of the inlier – both to the northeast and southwest – are relatively immature from an exploration perspective. Exploration by AIC is targeting this immature portion of the project through geophysical surveys and drilling.
Lamil Project (AIC 50%)
The Lamil Project is located in the Paterson Province of Western Australia, midway between the Telfer gold-copper mine and the Nifty copper mine. It covers an area of 1,200 square kilometres and is prospective for both gold and copper. AIC Mines and Rumble Resources (ASX: RTR) each hold a 50% joint venture interest in the project.
AIC is focussed on the discovery of Tier 1 gold and copper deposits similar to the world class Telfer gold-copper mine (approx. 15M oz gold) and the Nifty copper Mine (approx. 1.2Mt of copper).
The geological architecture at the Lamil Project is considered important in the development of major mineral deposits in the province. Two regionally extensive and deep penetrating belt parallel NNW trending structures coupled with a series of major NE trending cross fault underscore the prospectivity of the project, as these represent a vertically accretive plumbing system that is important in the transportation and trapping of rising mineralised fluids.
The prospective Proterozoic age rocks are obscured by younger Permian age sedimentary sequences to variable depths. This has been a deterrent to exploration in the past. However, an airborne magnetic survey completed by Rumble Resources in 2019 suggested the cover rocks could be less than 100m deep over an area defined by a domal response in the magnetics analogous to the Telfer Dome. Through broad spaced reverse circulation (RC) drilling of the target area in late 2020, AIC not only completed the first drill holes into the entire project area but confirmed that prospective rocks are within explorable depths and that they represent formations which host mineralisation at Telfer and elsewhere in the Paterson Province. Encouragingly, drilling intersected veining, alteration and anomalous copper intercepts warranting further exploration.
Further broad spaced reconnaissance RC drilling was completed at the Lamil Dome main target in Q3 2021 along with first-pass drilling at additional targets – Goodenia and Desert Pea. A schematic cross section through the project, shown below, illustrates the geological architecture model in relation to the target locations.
In addition to the magnetics and reconnaissance drilling programs, surface geochemistry, ground gravity and airborne time domain electromagnetic surveys have been completed to aid with the refinement of prospective target areas and to generate further targets.
Peake and Denison Copper Project
The Peake and Denison project is located 750km NNW of Adelaide along the NE margin of the Gawler Craton. The project covers approximately 2,500 square kilometres of the Peake and Denison Inlier within 4 granted exploration licenses. AIC Mines is targeting Iron-Oxide Copper-Gold style mineralisation. AIC Mines acquired the project as part of the takeover of Demetallica Limited in December 2022.
There are strong similarities between the Peake and Denison Inlier and the Iron-Oxide Copper-Gold (IOCG) mineral systems around Cloncurry. Visible copper mineralisation has been intersected at the Mawson and Wills targets and has strengthened the validity of the exploration model targeting IOCG mineral systems in the Peake and Denison Inlier.
Inlier basement rocks at Peake and Denison proffer excellent potential for IOCG mineralisation, based on data from limited historical drilling. The data show intense sodic-calcic-iron alteration developed at broadly the same age (1520-1470Ma) as mineralogical assemblages that occur as alteration with copper in the Cloncurry region. Additionally, granite intrusives at Peake and Denison at circa 1530Ma also correlate with the same age range (1547-1493Ma) as the Williams – Naraku granites around Cloncurry that are also linked to copper-gold mineralisation.
A maiden drilling program conducted in 2022 tested three magnetic anomalies: Wentworth; Mawson; and Wills each with a single drill hole. Drilling at the Mawson and Wills targets intersected visible copper mineralisation.