Half Yearly Report and Accounts
Released
Released
Announcement PDF
1
MRG Metals Limited
Half Year Financial Report
31 December 2023
Half Year Financial Report
MRG Metals Limited
ABN: 83 148 938 532
For the half-year ended 31 December 2023
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MRG Metals Limited
Half Year Financial Report
31 December 2023
Contents
Corporate Directory
3
Director’s Report
4
Auditor’s Independence Declaration
26
Statement of Profit or Loss and Other Comprehensive Income
27
Statement of Financial Position
28
Statement of Changes in Equity
29
Statement of Cash Flows
30
Notes to the condensed interim Financial Report
31
Directors’ declaration
35
Independent Auditor’s Review Report
36
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MRG Metals Limited
Half Year Financial Report
31 December 2023
Corporate Directory
Directors & Secretary
Andrew Van Der Zwan
Non Executive Chairman
Christopher Gregory
Non Executive Director
Shane Turner
Non Executive Director and Company Secretary
Principal place of business
12 Anderson Street West, Ballarat VIC 3350
Telephone: +61 3 5330 5800 Fax: +61 3 5330 5890
Email: info@mrgmetals.com.au
www.mrgmetals.com.au
Registered office
12 Anderson Street West, Ballarat VIC 3350
PO Box 237, Ballarat VIC 3353
Telephone: +61 3 5330 5800 Fax: +61 3 5330 5890
Corporate accountant and Registered ASIC Agent
RSM Australia Pty Ltd
12 Anderson Street West, Ballarat VIC 3350
PO Box 685, Ballarat VIC 3353
Telephone: +61 3 5330 5800
Fax: +61 3 5330 5890
www.rsm.com.au
Solicitors
Moray & Agnew
Level 6, 505 Little Collins Street, Melbourne VIC 3000
Telephone: +61 3 9600 0877
Fax: +61 3 9600 0894
www.moray.com.au
Share Registry
Automic Pty Ltd
Level 5, 126 Phillip Street, Sydney NSW 2000
Telephone: 1300 288 664
Auditor
William Buck Audit (Vic) Pty Ltd
Level 20
181 William Street, Melbourne Vic 3000
Telephone (office): +61 3 9824 8555
Website: www.williambuck.com
Stock Exchange Listing
ASX Codes: MRQ and MRQO
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MRG Metals Limited
Half Year Financial Report
31 December 2023
Director’s Report
The Directors of MRG Metals Limited (‘MRG’) present their Report together with the financial statements of
the consolidated entity, being MRG Metals Limited (‘the Company’) and its controlled entities, MRG Metals
(Australia) Pty Ltd, MRG Metals (Exploration) Pty Ltd, Lake Hope Lithium Pty Ltd, Sofala Resources Pty Ltd,
Sofala Mining & Exploration Lda, Sofala Mining & Exploration I Lda, Sofala Mining & Exploration II Lda,
Sofala Mining & Exploration III Lda, Sofala Mining & Exploration IV Lda, Sofala Mining & Exploration V
Lda, Sofala Mining & Exploration VI Lda, Sofala Mining & Exploration VII Lda, Sofala Mining & Exploration
VIII Lda, Sofala Mining & Exploration IX Lda and Sofala Mining & Exploration X Lda (‘the Group’) for the
half year ended 31 December 2023 and the Independent Auditor’s Review Report thereon.
Projects
MRG Metals is pleased to provide an update on activities undertaken in the six months to 31 December 2023
across the Company’s portfolio of projects in Mozambique, Zimbabwe and Australia.
MOZAMBIQUE
ADRIANO RARE EARTH ELEMENT LICENCE GRANTED
In December 2023, MRG advised it had been granted a new REE project named Adriano (11002L; 19,777.14
ha) situated 780km North-East of the Company’s Corridor Central (11142C) and Corridor South (11137C)
Heavy Mineral Sands (HMS) Mining licence applications (MLAs), 230km North-Northeast of the port city of
Beira.
Together with two conjunctive REE Exploration Licence Applications (ELAs 11000L and 10999, the two
exploration licences still under application), Adriano was generated based on a highly elevated Thorium (Th)
anomaly from historic regional airborne geophysical survey work and reconnaissance ground follow-up. A
handful of samples taken within ELA 11000L clearly showed the presence of Monazite, as well as elevated
REE grades (refer ASX Announcement 11 May 2022).
The Company commenced its initial work program at Adriano in late January 2024. The exploration work
program will focus on identifying monazite and other mineralisation within both the primary hard-rock highgrade metamorphic gneiss area in the upper half of the licence and the secondary sedimentary sequences of
the Mozambique Basin sediments.
The first phase exploration work program involves the following:
• stream sedimentary sampling on the various large streams running from the gneiss in the north to the
alluvial sediments in the south;
• grid hand-auger and pit sampling of the alluvial sediments to test for detrital monazite in the
sediments; and
• geological mapping with associated grid outcrop and soil sampling on the gneiss terrain.
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31 December 2023
Figure 1: The location of MRG’s Adriano 11002L Rare Earth Exploration licence (EL), the other applied for REE ELs
(ELAs, 11000L and 10999L), and the location of the applied for REE and U ELs (ELA 11005L) in relation to MRGs
exiting Heavy Mineral Sands ELs and the port city of Beira.
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31 December 2023
Figure 2: Map showing the Rare Earth Element EL Adriano 11002L in relation to the 2 REE ELAs 11000L and
10999L plotted on airborne radiometric spectrometer data of a regional national airborne geophysical survey.
CORRIDOR NORTH LICENCE GRANTED
Following the granting of Adriano, MRG was also granted a new Heavy Mineral Sands exploration licence,
Corridor North 10779L, which targets extension of mineralisation from MRG’s Koko Massava deposit in the
south and the Dingsheng Minerals Corridor Sands mining operation in the northwest.
Corridor North (10779L; 6,421.43 Ha) is situated north of and abutting MRG’s Corridor Central (11142C)
licence, which contains MRG’s Koko Massava JORC Resource (1.4BT @ 5.2% THM). The mineralisation of
Koko Massava is open towards the north and interpreted to extend into the southern part of the Corridor
North licence.
Corridor North is also located east of and abutting the world-class Dingsheng Minerals, S.A (7054C) Corridor
1 Project, which is currently being mined and reportedly contains in excess of 2.7 billion tons of high-grade
HMS resource. Mineralisation of the Corridor 1 Project is interpreted to extend into the Corridor North
project.
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Figure 3: The location of Corridor North 10779L Heavy Mineral Sands (HMS) exploration licence (EL), in relation to
MRG’s other HMS ELs, Mining Licence Applications (MLAs) and exploration licence applications (ELAs).
Figure 4: Map showing the Dingsheng Minerals Corridor 1 licence and MRG’s Corridor Central in relation to the
new MRG Corridor North applied for licence, with the Dingsheng Corridor 1 and MRG Koko Massava
mineralisation footprint extending to the boundary of the Corridor North licence.
MRG will conduct an EMP and engage with all provincial, local and community structures in Q1 2024. On
receipt of the approved EMP, MRG will commence its ground exploration program.
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31 December 2023
MRG’s proven HMS exploration model which it applied to discover and develop world-class deposits such
as Koko Massava, Nhacutse and Poiombo, as well as other high value discoveries such as Azaria, Malambane
and Magone will be followed.
The exploration at Corridor North will involve:
• Wider spaced grid hand-auger drilling at approximately 1km by 200m drill spacing to 12m depth to
generate targets. This work will initiate in Q1 2024;
• Infill hand auger drilling on targets at approximately 500m by 100m drill spacing to 12m;
• Followed by Aircore drilling for depth extent within targets;
• Analytical work and mineralogical investigations will be taking place as an ongoing process during
drilling; and
• Modelling and resource work on return of positive results from exploration programs.
MARRUCA RELINQUISHED
MRG advised of the relinquishment of Marruca 6846L Heavy Mineral Sands exploration licence after
exploration showed no visually estimated grades of higher than 2% Total Heavy Minerals there.
MOU WITH LANQI TO FORM JV ON CORRIDOR SANDS PROJECTS
In July, MRG entered a Memorandum of Understanding (MOU) with Tianjin Lanqi Materials Company
Limited for a Joint Venture operation on its Mozambique Corridor Sands projects.
Post end of the half-year period, MRG and Lanqi ended the due diligence period of the MOU. Extensions to
the Due Diligence had previously been agreed (refer announcements 24 October, 4 December 2023 and 2
January 2024). However, Lanqi did not submit a formal Joint Venture proposal, with 6 months having passed
since commencing the Due Diligence process.
MRG remains open to receiving a formal JV proposal from Lanqi but in the best interests of shareholders,
decided to commence discussions with alternative potential partners.
ZIMBABWE
In October, MRG announced it had entered into a binding MOU with Wickbury Investments (Pvt) Ltd
(“Wickbury”) for a Joint Venture on a package of 10 mining licences held by Wickbury over the Shawa
Carbonatite Complex in Zimbabwe.
Key aspects of the MOU:
• MRG has acquired exclusive rights to exploration and development for all commodities within the
10 mining licences of Wickbury (refer Table 2) from signature of the MOU (refer Table 1).
o The Shawa Carbonatite Complex is well mineralised, with proven and mapped mineralisation of
the following:
Rare Earth Elements (REEs) - Niobium, Strontium
▪ The trench sampling on Wickbury licences recorded peak Total Rare Earth Elements
(TREE) concentration of 2186ppm
▪ Historical gravity survey showed significant depth extent to the Carbonatite of >500m.
Phosphate (Note, DLC operating Phosphate mine adjacent), Vermiculite (Dormant Mine
operation), Magnetite (Mapped) and Magnesite (Mapped)
▪ Very limited exploration has been conducted on the Wickbury licences, with potential for
other mineralisation often associated with carbonatites, such as Fe, Cu, barite, CaCO3, Ti,
nepheline and Zr.
• Infrastructure, including offices and sheds associated with the dormant vermiculite mine
is available for use.
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Terms of the Agreement:
• Wickbury to receive 20 million MRQ Shares on signing of the MOU (Stage 1)
• Following a Stage 2 Due Diligence process, a Joint Venture Company (JVC) will be set up under the
same terms as the MOU, with MRG having the right during Stages 3 to 5 to earn 80% equity in the
JVC as follows:
Stage 3
US$250,000 expenditure to achieve
MRG to own 30%
Stage 4
A further US$250,000 to achieve
MRG to own 51%
Stage 5
A further US$1,500,000 spend
MRG to own 80%
• Upon completion of Stage 5, MRG’s expenditure would total US$2,000,000. Wickbury will then have
the option to co-invest at the 20% equity level, or dilute at a rate of 1% per US$100,000 to a floor of
10% equity.
• Wickbury will be responsible for maintaining all tenements (both existing and future), in good
standing, for government reporting (including technical and environmental reporting) and ESG
compliance.
About Wickbury
Wickbury is a Zimbabwean company which was formed to identify and develop mineral deposits associated
with the Shawa Carbonatite Complex.
The two founding directors and 90% shareholders of Wickbury, Mr Nathan Kalumbu and Mr Paul
Chimbodza, both Zimbabwe nationals, bring significant experience to the partnership. Nathan holds a
Master's Degree in Business Administration from Emory University and a Bachelor’s Degree in Business
Studies. He is former president of the Coca-Cola Company - East & Central Africa Business Unit. Paul is a
geologist and mining executive with 30 years of industry experience. He holds BSc General and BSc Geology
Honours degrees. Paul is acknowledged for bringing Prospect Lithium Zimbabwe’s world-class lithium
deposit to market; the deposit is now in feasibility stage. The project is managed by Prospect Resources
Limited (ASX: PSC).
The remaining 10% of Wickbury is held by a local community group, which MRG regards as an ESG benefit
to the partnership.
Key highlights of the Shawa Carbonatite Complex
• The Shawa Carbonatite Complex is well mineralised, with known mineral occurrences of the
following:
o Rare Earth Elements (REEs)
▪ The trench sampling on Wickbury licences recorded peak Total Rare Earth Elements
(TREE) concentration of 2186ppm
o Phosphate
▪ Resource of 20.3 million tonnes containing 10.8% P2O5 on IDC licences
▪ Results from two trenches on Wickbury licences of 42m with 23.03 P2O5% and 5m with
33.58 P2O5%
o Vermiculite
▪ Active vermiculite mining operations taking place on an adjacent SAMREC property
▪ Inferred resources on Wickbury licences of 164,000t @ 24.1% vermiculite and 106,250t
@ 27.2% from two areas
o Niobium
▪ Trench sampling on Wickbury licences recorded highest Nb grade to of 1114ppm Nb
o Strontium
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▪
o
o
o
Two trenches on Wickbury licences have shown appreciable SrO values of 3m with 1.13%
SrO and 6m with 1.11% SrO
Magnetite (mapped)
Magnesite (mapped)
Very limited exploration has been conducted on the Wickbury licences to date, with possibility for
other mineralisation often associated with carbonatites.
▪ Historical gravity survey showed significant depth extent to the carbonatite of >500m.
▪ There is infrastructure on the Wickbury licences at the dormant vermicular mine.
Table 1: MOU funding and equity in Joint Venture.
Stage
Stage
Expenditure
MRG
(USD)
1
20 Million
MRQ Shares
Cumulative
Expenditure
MRG (USD)
Cumulative
Acquisition in
JV Company
MRG
(%)
0
2
3
N/A
250,000
N/A
250,000
30
Estimated Work Program
Estimated
Time Frame
(Months)
•
Sign and Commence the MOU
•
•
•
Geological Mapping and sampling, Ground truthing.
Soil Sampling – (grid Soil Sampling if IDC deal is possible).
Commence negotiation with IDC. (Minimum Work
Commitment)
6
Target Testing by Auger/Aircore etc Drilling
Sighter metallurgy/mineralogy as required
12
•
•
Decision
Point at
End of
Stage
**
**
4
250,000
500,000
51
5
1,500,000
Ω
2,000,000
80
•
•
Infill/Extension drilling +/- MRE
MRE, Metallurgical Study +/- Scoping Study
**
24
***
Table 2: Wickbury mining licences.
Tenement Name
James 13
James 10
Shawa 72
Shawa 36
Shawa 37
Shawa C 1
Shawa C2
Shawa C3
Shawa 58
Gono 2
Total
12
Area Coverage (Ha)
62.0
77.9
150.0
79.9
111.5
132.0
132.0
110.0
146.7
40.0
1042 Ha
Ownership
Wickbury Investments
Wickbury Investments
Wickbury Investments
Wickbury Investments
Wickbury Investments
Wickbury Investments
Wickbury Investments
Wickbury Investments
Wickbury Investments
Wickbury Investments
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Figure 5: Shawa Carbonatite in relation to Harare and the Mozambican Beira Port shown on Google Earth image,
yellow roads national tar roads. Insert close-up of Shawa and adjacent Dorowa carbonatites.
Figure 6: Shawa Carbonatite licences shown on Google Earth image, Wickbury licences in Black, IDC licences in
Green, SAMREC licences in magenta.
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Figure 7: Shawa licences shown on the geology map of the Shawa carbonatite complex from the Dorowa-Shawa
1:100,000 geology map, geology by J.N. Lauderdale, 1984-1986.
Economic importance of Carbonatite Complex deposits
Carbonatite and alkaline-carbonatite Complexes are multi-element deposits and host some very significant
metallic and industrial mineral deposits (Figure 8). Two examples, the Palabora Carbonatite Complex and the
Dorowa Carbonatite Complex (due to its proximity to the Shawa Carbonatite Complex), are briefly discussed
further.
The Palabora Carbonatite Complex in the Limpopo Province of South Africa is recognised as one of the
most important carbonatites in the world, being not only one of the world's major sources of copper, but also
the host of a wide range of other valuable commodities besides. The Palabora orebody is vertical and the
reserve extends to a depth of 1,800m over an area of 700m by 200m.
The central complex of the carbonatite measures about 7km north-south and varies between about 1.5 and
3.5km in width, with an area of 15km². There are also numerous associated plugs and dykes of syenite and
carbonate-bearing breccias. The Carbonatite Complex is mined and processed by the Palabora Copper Pty
Ltd (PC) (Palabora Mining Company, or PMC). Mining started in 1965 by open cut mining methods, which
transitioned to underground operations in 2003. The open-pit measures almost 2km wide and reached 800m
deep at the end of the open-pit mining phase.
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The PMC underground copper mine employs a block caving mining method for the extraction of ore beneath
the old open cut void. Production has been sourced from Lift I of the block cave from 500m below the floor
of the open cut void. In 2011, PMC developed a plan to extend the life of the underground mine up to 2033
through the construction of a Lift II block cave 450m beneath the current Lift I, thus nearly 1,800m deep.
The Lift II Feasibility Study has been completed.
There are three large opencast mines on the Phalaborwa complex producing copper, apatite and vermiculite,
together with a range of other valuable by-products, particularly from the copper mine. It provides copper
ore to the company's copper processing plant, smelting and refinery plants on site to produce copper rod and
copper cathode sheet. Vermiculite ore is mined from a series of shallow open cuts (up to 50m deep) and is
upgraded through a processing plant to produce saleable vermiculite products. Magnetite is recovered from
old tailings dumps and pumped to a magnetic separator for production of a magnetite concentrate. Apatite
is mined from an open pit on pyroxenite at the northwestern margin of the complex. Apatite is absent from
the central part of the northern pyroxenite, but an average of 6.7% P2O5 is found in an outer 500m-wide zone.
FOSKOR, which holds the rights to exploitation of phosphate at Phalaborwa, also receives large tonnages of
phosphate-bearing tailings from the Palabora Mining Company mine together with phoscorite, from which
FOSKOR recover copper, baddeleyite and magnetite in addition to apatite.
By-products of the copper exploitation are linked to impurities in different phases of the processing phase
and results in the following by-products: nickel sulphate hexahydrate crystals, Silver (Ag), Arsenic (As), Gold
(Au), Bismuth (Bi), Lead (Pb), Antimony (Sb), Selenium (Se) and Tellurium (Te). Sulphuric acid is also a major
product.
The Dorowa Carbonatite Complex adjacent to the Shawa Carbonatite (14km northeast, Figure 6) has two
principal apatite phosphate orebodies with resources in the weathered zone of the southern body amounting
to 40 million tonnes and in the northern body with 33 million tonnes. The phosphate produced at Dorowa is
used in the production of phosphate fertiliser blends. The mine also produces magnetite, which is exported
to Mozambique. Ore from the pit is at 6.5% P2O5 and the concentrates being dried and sent to Zimbabwe
Phosphate Industries (ZimPhos) are at 37% P2O5. The dried concentrates are sent to the railhead at Nyazura
along the Mutare highway, some 65km away, by road and 190km to Zimbabwe Phosphate Industries, in
Harare by rail.
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Figure 8: Vertical section of a hypothetical carbonatite mineralising system displaying the relationship between
metallic and industrial mineral deposits relative to lithological units and geological contacts, not to scale (image
sourced from Carbonatites: related ore deposits, resources, footprint, and exploration methods; George J. Simandl
&Suzanne Paradis).
•
•
•
•
•
•
Large REE resources (e.g. Bayan Obo, China; Maoniuping, China; Mountain Pass, USA and Mount
Weld, Australia), mostly strongly enriched in Light Rare Earth Elements (LREE), however, they also
contain significant resources of heavy rare earth elements (HREE).
Alkaline carbonatite complex related deposits are also the main source of Nb (e.g. Catalão, Brazil;
Lueshe, Democratic Republic of Congo; and St. Honoré, Oka, and Aley, Canada).
Vermiculite and phlogopite deposits are predominantly hosted by mafic or ultramafic rocks of the
alkaline-carbonatite complex (e.g. Northern pyroxenite at Palabora, South Africa); near the contacts
of carbonatites with these rocks, or within mafic country rocks (e.g. Upper Fir carbonatite, Canada).
Apatite (phosphate mineral) deposits currently in production are mostly enriched by weathering, such
as Tapira, Brazil; Ipanema, Brazil; Catalão I, Brazil; Matongo, Burundi and Dorowa, Zimbabwe; with
examples of the exceptions the Siilinjärvi mine, Finland, and Cajati mine, Jacupiranaga Complex,
Brazil.
Cu, U, Th, and baddeleyite (natural zirconia) were produced for decades from the Palabora
carbonatite-phoscorite complex in South Africa, but baddeleyite is currently produced only from the
Kovdor deposit in Russia (Dickson Citation 2015).
Other materials produced from carbonatites or related rocks are: iron (e.g. Kovdor, Russia; Bayan
Obo, China; and Palabora, South Africa); fluorite (e.g. Mato Preto, Brazil; Okorusu, Namibia; and
Amba Dongar, India); carbonates for lime and cement production (e.g. Tororo, Uganda and Xiluvo,
Mozambique; and Jacupiranga, Brazil; Alves Citation2008); and sodalite for use as dimension,
ornamental, and semi-precious stone (e.g. Swartboosdrift, Namibia; and Cerro Sapo, Bolivia).
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About Shawa Carbonatite Complex
Introduction
The Shawa Carbonatite is approximately 165km SE of Harare (Figure 5), accessible via tar road, with good
access on the 10 Wickbury mining licences (Table 2) on the carbonatite. The Nyazura rail head is
approximately 80km via tar road northeast of the Shawa Carbonatite Complex. The carbonatite is c 5.9km in
diameter, or c 34.8km².
Limited exploration has been undertaken over the Wickbury licences on the Shawa Carbonatite Complex,
with mainly historical exploration focused on phosphate and vermicular mineralisation, and more recently
exploration for mainly REEs. The Shawa carbonatite complex has already demonstrated endowment for the
following minerals:
• REE mineralisation;
• Phosphate mineralisation;
• Vermiculite mineralisation;
• Magnetite mineralisation (probably associated with V2O5);
• Magnesite mineralisation;
• Niobium; and
• Strontium.
The current mining licences over the Shawa Carbonatite are shown in Figure 8, with the Wickbury mining
licences in black (10 licences covering 1042ha), the IDC mining licences in green and SAMREC Zimbabwe
(Pvt) Ltd (SAMREC) mining licences in magenta. The Wickbury licences cover a large portion, approximately
60% of the carbonatite (Figures 9 and 10), including a portion of the central carbonatite plug / intrusion.
Active vermiculite mining is taking place at the Shawa Vermiculite Mine (Figure 9) within the SAMREC
licence. The SAMREC vermiculite deposit is reportedly (by the SAMREC company) one of the larger
vermiculite deposits in the world.
The dormant Wickbury Dinhidza Vermiculite Mine lies in the northwest of the Shawa Carbonatite on the
Wickbury James 10 and 13 mining licences. There is infrastructure on the mine that will be used during
exploration (plant area, loading shed, administration block and laboratory, Technical Services Office, Mine
Stores, Mine guest House camp and mine workers’ compound).
Previous exploration on the Shawa Carbonatite Complex
i.
Hawkmoth Mining and Exploration
Exploration by Hawkmoth Mining and Exploration (Hawkmoth) took place on Wickbury licences in 2022
under an option agreement, the option was not exercised. The work included soil sampling, followed by
outcrop rock chip sampling, then a limited amount of trenching.
a.
Soil sampling
During the soil sampling program soil samples were collected at 20m intervals along 7 lines, the 7
lines were oriented radially to cover the oval shape of the carbonatite complex targeting the zone
between the inner carbonatite ring and the circular inner ring. The first 30 soil samples were sent to
Geolabs South Africa for XRD and 700 samples to SGS South Africa for multi-element ICP. The
soil Geochem REEs results showed a relative enrichment of LREEs (La+Ce+Pr+Nd) in comparison
to HREEs (Tb+Dy+Er+Tm+Yb+Lu+Lu+Y) and MREEs (Sm+Eu+Gd), with an average ratio
HREE_ppm: MREE_ppm: LREE_ppm of 1:0.56:4.56. The assays for LREEs i.e., Ce, La, Nd and
Pr in order (from highest concentration) have contributed bulk of TREE content additionally with Y
(HREEs), as all have peaks >100ppm. Soil Geochem line 7, outlined a REE and Nb target zone with
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TREE values ranging 1000ppm – 1508ppm and Nb 236ppm – 1075ppm, which aligned with eastern
inner contact zone of the main carbonatite with the serpentinite. From the results an P anomaly was
picked up by line 2 and 4 on the western part of the main carbonatite ring and specifically towards
the outer and inner contacts. P is more enriched on the outer contacts of ring carbonatite where peaks
for P were up to 10.9%.
b.
Rock Chip Sampling
Follow up of random 205 rock chip sampling was done on the main ring carbonatite outcrops along
and/or in proximity with the anomalous soil Geochem lines 2, 6 & 7. The peak REE assay results for
the rock chips recorded TREE 355.8 ppm with the LREEs bulk Ce (peak @ 133ppm), Nd (peak @
123ppm) and La (max @ 67ppm), where they are spatially associated with “Line 7 eastern anomaly”
inner contact of the main carbonatite ring and oxidised serpentinite. LREEs are more enriched as
compared to HREE and MREEs in this Eastern target anomaly with average ratio HREE:MREE:
LREE as 1.4; 1; 7. The “Eastern target contact” is also well associated with Nb enrichment with peak
(max) @ 428ppm, which shows a positive linear correlation of R2= 0.47 with TREE concentration
and as well Sr values with peak 6851ppm. Phosphate recorded values range from 0.6% - 2.4% from
the rock samples.
c.
Trenching
The trenching exercise was conducted as follow up of the TREE and Nb and P anomalies identified
on soil Geochem. A total of 7 trenches with a cumulative length of 1419m were excavated and sited
radially inside the inner circular ridge only, exposing the contact between the main ring carbonatite
and serpentinite. The trench rock chip samples recorded a relatively higher peak TREE concentration
with 2186ppm and a few peaks above 1500ppm as compared to the regolith soil profile samples. Ce
records the highest peak in rock chip samples with 863ppm, whilst in trench soil profiles Y (HREE)
has the highest of 614ppm. In both sets of samples, it is important to note that LREE concentration
is relatively higher than MREE and HREEs. Trench ATSHTR004, out of the 7 trenches has the 3
most interesting REEs target with 2 zones showing peak TREE grades @ 1620ppm (@182m – 188m
over 6m) and 1793ppm (@ 234m – 236m over 2m), which are associated with a carbonatised
serpentinites. Also, a major contribution of MREEs to TREE has been identified on trench
ATSHTR007 @ 59m – 69m, with weighted average grades of TREE 891ppm, MREE 419ppm and
LREEs 391ppm. Peak phosphate grades were identified on the trenches ATSHTR006 @ 68m – 110m
over 42m (widest) with 23.03 P2O5% and ATSHTR007 @ 82m – 87m over 5m with 33.58 P2O5%.
The trenches ATSHTR003 and ATSHTR004 have shown appreciable SrO values @ 150m – 153m
over 3m (ATSHTR003) with 1.13% and @ 182m – 188m over 6m with 1.11%. Outstanding Nb
targets from trench rock chips were sporadically distributed along trench ATSHTR004 @ 75m –
120m over 45m with weighted average grade Nb 401ppm, and with peak grade Nb 1007ppm @ 116m
– 117m. This zone is arguably passively continuous towards trench ATSHTR005 @ 101.5m – 142.5m
with Nb in soils ranging 335 ppm – 894 ppm and Nb in rocks ranging 56ppm – 861ppm, which can
be as well influenced by multiple crystalline carbonatite intrusions. However, the highest Nb grade
from trench rock chips is isolated @ 200m – 201m in trench ATSHTR004 with Nb 1114ppm.
ii.
Steffen, Robertson and Kirsten (SRK)
SRK conducted exploration on the vermiculite deposit on licences now belonging to Wickbury in 2001
(work done for Dinidza Vermiculite Mining Private Limited), culminating in a resource potential report
in August 2001.
SRK conducted a trenching program (trenches planned to 2m depth), mainly focused on the then named
James 13 and James 14 licences (now James 10 and James 13) where the Watts, Griffis and McQuat
17
MRG Metals Limited
Half Year Financial Report
31 December 2023
resources mentioned below were situated. SRK could not replicate the resource results of Watts, Griffis
and McQuat, reporting an Inferred resource of 164,000t @ 24.1% vermiculite from one area within the
licences; and an Inferred resource of 106,250t @ 27.2% vermiculite from another area.
iii.
Watts, Griffis and McQuat
Watts, Griffis and McQuat (2000) reported 43-101 resources and reserves on then James 13 and James
14 licences (now James 10 and James 13) of Indicated 426,530t @ 50% vermiculite and Inferred
4,590,000t at 49% vermiculite.
iv.
Dodd (1971)
Dodd supplied resource estimation figures in 1971 for the phosphate mineralisation in weathered ijolite,
with the majority of this resource situated within the IDC mining licences. The resource from Dodd is
20.3 million tonnes containing 10.8% P2O5, 31.4% Fe2O3 and 1.3% CO2. Dodd calculated a lower CO2
resource with CO2 at 0.8% then with 16.3 million tonnes at 10.4% P2O5 and 32.5% Fe2O3.
v.
Gravity survey
A gravity survey was conducted on the Shawa Carbonatite Complex to establish the subsurface of both
the dunite and the Complex as a whole. Figure 9A shows the distribution of the gravity observation
points. The essentially circular symmetry observed in outcrop is very strongly reflected in the gravity
anomaly, allowing the observed Bouguer anomalies for all points to be projected to a radial line as shown
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