.
Enter the email you signed up with and we'll email it to you.
Location: 99 km NW from Esperance, Western Australia, Australia
39-43 Murray Road North, WelshpoolPO Box 635PerthWestern Australia, Australia6106
Stay on top of the latest gold discoveries. Examine the latest updates on drilling outcomes spanning various commodities.
Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
Shaft depth, mining scale, backfill type and mill throughput data.Full profiles of select mines and projects.
Equipment type, model, size and quantity.Full profiles of select mines and projects.
Camp size, mine location and contacts.Full profiles of select mines and projects.
MRCG is a wholly owned subsidiary of Mineral Commodities Ltd. (MRC). The MRC holds an existing 51% interest in Munglinup.
During 2024, negotiations were undertaken to secure terms for MRC to increase its share in the Project. As a result, the MRC announced on 25 June 2024 that its wholly owned subsidiary MRCG had reached an in-principle agreement with Gold Terrace to settle a dispute and acquire the remaining 49% interest in Project.
The total consideration to be paid to Gold Terrace in exchange for its 49% interest in Project is $A7.5M in cash.
Upon acquiring the remaining 49% interest, the MRC will become the 100% owner of Munglinup.
As at March 2025, the Formal Agreement has not yet been executed.
- subscription is required.
The graphite deposits are located in the northern foreland of the AlbanyFraser Orogen and are hosted by paragneisses of the Munglinup Gneiss. Structurally the prospect is located adjacent to the intersection between the northeast trending Fraser Range Fault and the northwest trending Merredin Fault.The Munglinup graphite deposits occur as discrete layers in a zone of graphitic schists within a sequence of hornblende and hornblende-garnet gneisses. The rocks have been broadly folded about a WNW/ESE axis, with superimposed minor anticlinal and synclinal flexures. Complex small-scale folding and faulting is common in the relatively incompetent graphitic rocks and the enclosing competent hornblendic gneisses appear to be less deformed.Targeted graphitic mineralisation occurs within saprolite consisting of clays, quartz, graphite (up to 42% flake) and goethite. Weathering extends down to at least 60m.The host geology comprises weathered metamorphic material.The Munglinup area comprises Archean to Paleoproterozoic, metamorphosed granitic and other metamorphic rocks of the Albany–Fraser Orogen, typically hornblende (± garnet) gneiss and migmatite.Within the gneissic rock mass, rocks containing the Munglinup graphite deposits consist of a succession of tightly folded metasedimentary rocks with a consistent dip from north north east to the south.The classification scheme most widely accepted for graphite deposits was introduced by Cameron (1960). It classifies known graphite deposits into five categories reflecting the different types of graphite.Using this classification scheme, it is most likely that the Munglinup deposit can be characterised as a type 1, disseminated flake graphite in silica-rich meta-sediments deposit.• Halberts Main Zone:- Length: 730m- Width: 90-130m- Depth: surface to -90m• Halberts South Zone:- Length: 560m- Width: 20-50m- Depth: surface to -60m• Harris Area:- Length: 435m- Width: 30-70m- Depth: surface to -35m• McCarthy West Area:- Length: 290m- Width: 100-110m- Depth: surface to -55m• McCarthy East Area:- Length: 260m- Width: 12-20m- Depth: surface to -30m
Success!