16
October 2024
Premier African Minerals
Limited
Mineral Resource Update
Statement Zulu
Premier African Minerals
Limited ("Premier" or
the "Company"), is pleased
to report an important upgrade to the SAMREC compliant Mineral
Resource Estimate ("MRE" or
"Mineral Resource
Estimate") on its wholly owned Zulu Lithium and
Tantalum Project ("Zulu"). The updated MRE is also JORC
compliant.
Highlights
|
Ø
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This MRE is concerned only with the
Spodumene and Tantalum that is contained in the deposit and with
those areas of the Zulu tenements that are expected to be mined and
processed through the present plant only. This excludes the greater
EPO area.
|
Ø
|
This MRE estimates
Li2O
that is contained in spodumene, specifically
Li2O
that is attributable to spodumene at 131,627 tonnes and the direct
conversion of the contained Li2O to spodumene concentrate 6
(SC6) is 2,197,800 tonnes.
|
Ø
|
This MRE estimates that the ore body
contains 1,225,058 kg of Ta2O5.
|
Ø
|
Mineral Resource development
drilling is ongoing, with the aim of identifying extensions to the
current MRE and thereto having the potential to add additional
Mineral Resources.
|
George Roach, CEO commented:
"This updated MRE represents a 23% increase in contained Spodumene,
a 17% increase in contained tantalum and an improved grade at a 0%
cutoff of 0.54% Li2O compared to the MRE published
in February 2024. The increases are attributable to several reasons
that include the fact that mining development and grade control
indicates in situ grade estimates are understating the actual
grades being mined, an adjustment in ore body density, and
additional data now included. The updated MRE has been prepared on
a depleted basis following mining conducted to date.
It should be noted that with ongoing
mining activities, further sections of the ore body are expected to
be reclassified into a measured category that will be supported by
close-spaced in pit grade control assessments from time to
time.
It is worth noting that this MRE is
based on an assumed 80% of the total Li2O grade of the ore body being
attributable to the SQI dominant style of mineralisation, which the
Company believes is conservative and ongoing analysis of the
mineral assemblage may support an increase in this percentage with
potential increases in the contained spodumene. We have previously
set out our expectation that Zulu is likely to produce spodumene
concentrates with low iron and higher spodumene concentrate
grades.
Certain necessary plant issues are
being attended to and will be dealt with in a separate announcement
to follow shortly".
Mineral Resource Estimate:
The MRE is based on assay results
from 236 surface drill holes totalling 46,355 metres (m), 856 grade
control holes totalling 5,640 m and 123 surface trenches totalling
4,055 m between September 2016 and December 2023. This
MRE was carried out by an independent qualified
person, Mr Charles Muller of Shango Solutions (Shango).
All available data was verified prior to the development of the
3-dimensional geological model which was completed utilising
Datamine Studio RM.
The geological model has been
developed from extensive drilling, which was undertaken on a
nominal 50 m x 50 m drill spacing, as well similarly spaced surface
trenches. Variography indicates that 50 m spacing of the borehole
pierce points is sufficient for an Indicated Mineral Resource
classification.
The MRE set out in Table 1 is
prepared in accordance with JORC and SAMREC and in
compliance with Appendix 3 of the AIM Note for Mining and Oil &
Gas Companies. In this regard, specific attention is drawn to the
fact that Zulu is expected to produce spodumene concentrate and
certain by products. Not all Li2O identified in assay results
is contained in spodumene, with ongoing test work indicating that
spodumene accounts for more than 80% of the
Li2O
grade. Accordingly, the overall tonnage of the Mineral Resource is
reduced to reflect only the contained Li2O that is associated with
spodumene. Premier is the Operator and 100% owner of Zulu such that
the gross and net attributable MRE attributable to Premier is the
same.
Table 1: Mineral Resource Statement for Zulu
Project - 14th October 2024
Cut-Off
|
Tonnage
|
Grade
|
Metal
|
|
Losses
|
|
Li2O
|
Ta2O5
|
Li2O
|
Ta2O5
|
Li2O
%
|
Mt
|
%
|
Mt
|
%
|
g/t
|
t
|
kg
|
Measured
|
0
|
0.313
|
22%
|
0.244
|
0.57
|
83.98
|
1
392
|
20
510
|
Indicated
|
0
|
15.142
|
25%
|
11.357
|
0.52
|
50.94
|
59
055
|
578
507
|
Measured &
Indicated
|
0
|
15.455
|
25%
|
11.601
|
0.52
|
51.64
|
60
447
|
599
017
|
Inferred
|
0
|
18.914
|
30%
|
13.240
|
0.54
|
47.28
|
71
180
|
626
041
|
Total
|
0
|
34.369
|
28%
|
24.841
|
0.54
|
47.28
|
131
627
|
1 225
058
|
Notes
|
i. Losses: delineated pegmatites contain 80%
spodumene - tonnage is reduced by 20% to reflect the mineral
assemblage. In addition, geological losses of 5% for Indicated
Mineral Resources and 10% for Inferred Mineral Resources have been
applied.
|
ii. The MRE is prepared at a 0 % cut-off grade as all
the spodumene is expected to be recovered.
|
iii. A density of 2.57 g/cm3 has been
utilised.
|
iv. A depth cut-off of 300 m below surface has been considered
based on cost parameters, although the majority of the pegmatites
have only been modelled to a depth to 200 m.
|
v. The effective date of the MRE is 14 October
2024
|
vi. The MRE is based on information compiled by the Company
and reviewed by Shango and prepared in accordance with JORC and
SAMREC. Mineral Resources are not Mineral Reserves and have not
demonstrated economic viability.
|
vii. The contained Li2O and Ta205 metal values are rounded,
actual grades and contained metal are accurately stated and any
differences in the totals are due to rounding.
|
The updated MRE estimates Li2O that is contained in spodumene,
specifically Li2O that is attributable to spodumene, at 131,627
tonnes (February 2024 MRE - 107,366 tonnes, a copy of which is set
out in the Appendix to the announcement).
About Zulu:
Zulu comprises 14 mineral claims
covering a surface area of 3.5 km² that are contained within a
larger Exclusive Prospecting Order (EPO), and which are prospective
for tantalum and lithium mineralisation. The project is located 80
km as east of Bulawayo. Fort Rixon is some 15 km further to the
west of the project; the nearest village is Pioneer
Village n°2, approximately 1 km to the south of the main
deposits.
Geological Setting:
The area of interest is located
within the Fort Rixon Greenstone Belt where the schist belt is
north-south trending and tear drop shaped, measuring 30 km long in
and 19 km wide near the broad section near the northern end of the
belt.
The central area of the claims are
underlain by Archaean-age schists of the Bulawayan Supergroup, with
serpentinites and banded iron formations at the base of
the Upper Bulawayan Group in the east, and metamorphosed
mafic volcanics (amphibolites and schists) and meta-sediments of
the Lower Bulawayan Group to the west. The principal
pegmatites at Zulu (the Main and South pegmatites) are developed
along the contact of the Upper and Lower Bulawayan groups.
Additional pegmatites are developed in the footwall sediments.
The metamorphic grade is retrograde Greenschist facies.
In the east of the claims blocks, epidosites, calc-silicate rocks
and gneissic granites prevail. The northern most part of the EPO is
underlain by a post-Bulawayan Supergroup aged massive
granite.
The Zulu pegmatites are typical
Lithium-Caesium-Tantalum (LCT) pegmatites. Outcrop widths for the
exposed pegmatites can vary between 1 m to 50 m.
The strikes of the individual
pegmatites may vary widely but the South, Main and NE pegmatites
and their subsidiary footwall pegmatites trend approximately NNE
for a distance of 1 600 m. In addition to the South and Main
pegmatites the petalite-rich River Pegmatites trend in an
approximate SW-NE direction for a distance of 180 m, while the
spodumene-rich SE Pegmatites strike in a NW-SE direction over a
proved distance of 220 m. Although dips can vary locally with each
pegmatite, the dip of the South and Main pegmatites is generally
subvertical towards the west, while the River Pegmatites are
dipping subvertical to the NW and the SE Pegmatites subvertical to
the SW.
The South and Main pegmatites have
exploited the serpentinite-amphibolites contact with the subsidiary
footwall pegmatites mainly hosted in amphibolite and sedimentary
rocks. Additional narrow mineralised pegmatites that are not
included within the MRE due to the lack of sampling information are
hosted within granites to the east and south of the
mine.
The drilled widths of individual
pegmatites can vary from less than a metre to greater than 20 m in
thickness down hole. Occasionally along the contacts between the
pegmatites and the host amphibolites, the amphibolites have
undergone intense sodium metasomatism resulting in the formation of
a lithium bearing amphibole called holmquistite.
Lithium Mineralisation at Zulu:
To date, three principal lithium
bearing minerals, spodumene, petalite and lepidolite have been
identified in the Zulu pegmatites. Locally the host rocks of
the pegmatites contain noteworthy amounts of holmquistite, a
lithium bearing amphibole.
Tantalum Mineralisation at Zulu:
Many of the lithium bearing
pegmatites at Zulu are weakly mineralised with tantalum with the
best mineralised pegmatite being the South Pegmatite (South Pit)
having an overall Indicated Mineral Resource grade of 86 ppm
Ta2O5.
The only tantalum bearing mineral observed to date is
tantalite. The highest tantalum grade to date is 3,203 ppm
Ta2O5 from a surface trench.
Exploration History:
The pegmatite was first pegged in
1955 by J.S. Willemse. Subsequently the Rhodesian
Selection Trust Co. Ltd. ("RST") took an option on the claims and
carried out an extensive drilling and excavation programme.
Although much development work was carried out, the RST declined to
exercise their option on the claims. In 1961 and 1962 a small
quantity of petalite was mined by W. Burchett in partnership with
J.S. Willemse.
In 2010, after decades of no
activity, consulting geologist Richard B. Dollar registered the
claims in his name and subsequently carried out diamond drilling
and trenching programmes which were financed by Premier. In 2013
the Company exercised an option to acquire the claims.
Drilling Techniques and Hole Spacing:
All the boreholes available for the
Mineral Resource estimation were diamond drill boreholes. The
drilling and trenching statistics for each exploration phase are
detailed in Table 2.
In 2011, six diamond drill holes
totalling 2,312 m were drilled by Ox Drilling from Zambia. Core
diameters ranged from PQ (85 mm) PQ3 (83 mm) and HQ (63.5 mm). The
aim of this drilling campaign was to establish continuity of the
pegmatite mineralisation at depth. Four boreholes, totalling 1,153
metres were surveyed in early 2017 by the new drilling contractor
as only two of the six drill holes had been surveyed in 2011.
Several of the holes had partly collapsed at depth.
Table 2: Zulu Drilling Statistics
PROGRAMME
|
Drill Holes
|
Surface
Trenches
|
No.
|
Metres
|
No.
|
Metres
|
RST (1958)
|
7
|
903.9
|
|
|
ZULU - 2011 Exploration
|
6
|
2,312.9
|
|
|
ZULU - 2016-2017
|
43
|
5,809.1
|
|
|
ZULU - MRE (2021-2023)
|
130
|
31,538.2
|
33
|
2,534.8
|
ZULU - Geotechnical
(2021-2023)
|
17
|
3,285.0
|
|
|
ZULU - RC Drilling
|
33
|
4,786.0
|
|
|
TOTAL
|
236
|
46,335.1
|
33
|
2,534.8
|
The second diamond drilling programme, totalling 43 boreholes and
5,809 m of drilling, commenced in September 2016 and was
completed by February 2017. The Zimbabwean company Geodrill
from Bulawayo supplied and operated one and later two drill rigs on
the project. 5,288 m of downhole surveys were completed for 40
drill holes with three holes not being surveyed due to drill hole
collapses. Drill holes commenced with HQ (63.5 mm) diameter cores
in the weathered zone and once in stable ground, the holes were
completed with NQ (47 mm) coring.
The third diamond drilling programme
commenced in 2021 and will continue through 2025. To date, 143
drill holes totalling 34,100.16 m have been completed. Drill holes
are sited on a nominal 50 m x 50 m drill spacing. Holes are
collared and drilled HQ size until the base of the weathered zone,
cased and then completed with NQ-sized coring. Two drill
contractors, supplying up to a six drill rigs, were deployed in
2022.
In addition 17 boreholes were
drilled for geotechnical purposes and 33 reverse circulation (RC)
boreholes were drilled in order to test surface exposures that were
not previously tested.
856 grade control boreholes and 90
channel samples collected on the benches were included in the MRE.
The borehole sampling is collected from the blast holes on a 5 m
sampling basis. These holes are restricted to the current
operations on the South Pegmatite.
Sampling:
2016-2017 Drill
Programme:
Drill cores were packed into metal
core boxes which were secured on the drill site prior to being
transported to the RHA Mine by truck. At the mine, the
core was photographed and logged by Mr Wolfgang Hampel, the then
Exploration Manager of Premier. Pegmatite intersections were
marked-up, assigned unique sample numbers and cut in half, with one
half subsequently being quartered. A diamond saw was utilised to
cut the core. The quartered core was bagged for lithium and
tantalum analysis, the balance of the core was stored at the RHA
core shed, until transported to the new Zulu core shed in 2022. The
lengths of the sampled cores varied between 0.16 m and 8.79 m,
depending on the lithology (pegmatite / host rock) and the
homogeneity of the pegmatites. Any identified zoned pegmatites were
sampled across their logged mineralogical zones.
2021-2024 Drill
Programme:
Drill cores are packed into metal
core boxes at Zulu, with core block markers being inserted into the
core boxes after each core run. Core is then transported to the
Zulu core shed by company representatives. In the core shed, basic
core measurements are captured (i.e. core recoveries and Rock
Quality Designation - RQD). The core is then photographed and
geologically logged. All pegmatite intersections, together with 1 m
samples in the immediate hangingwall and footwall of the pegmatite,
are marked up for cutting and sampling. The nominal sampling
interval across a pegmatite intersection was 1 m but, in all cases,
geological contacts were respected and no sampling across contacts
took place. Unique sample numbers are assigned to each core sample.
Core is cut in half and half cores were bagged and labelled. Bulk
density determination on 10 cm lengths of core are then measured
(Archimedes Principle) for each sample.
Samples are then transported under
company supervision to Antec Laboratories in Kwekwe, for
sample preparation.
Sample Analysis:
To date 10,129 core and trench
sample assays have been returned. In addition, 1,528 QA/QC
(Quality-Assurance / Quality-Control) samples (blanks, duplicates
and standards), or 15.1% of the analysed core samples were inserted
to ensure adequate QA/QC.
2016-2017 Drill
Programme:
All sample preparation was carried
out at RHA's sample preparation facility at the mine. Every sample
of quarter core was dried, and its bulk density was determined
using a density scale (Archimedes principle). Samples were crushed
to -4 mm in a jaw crusher and a 200-250 g split was pulverised
(minimum of 85% passing 75 microns (μm)). A 50 g aliquot of the
pulverised samples was labelled and sent to SGS South Africa
(Randfontein) for multi-element analysis (49 elements). SGS code
ICM90A Multi Elements by sodium peroxide fusion, ICP-OES and ICP-MS
finishes. The sodium peroxide fusion technique is considered to be
a "total" dissolution technique for lithium-bearing silicate and
tantalum bearing oxide minerals. Detection limits for lithium are
10 ppm to 10% (i.e. 100,000 ppm) and 0.5 ppm to 1% (i.e. 10,000
ppm) for tantalum. Certified Reference Material samples
(AMIS0343) for lithium and tantalum were introduced into the sample
stream at a rate of 1:16. Blanks were introduced at the same rate,
the blank being sourced from a massive barren quartz vein found
some 8 km from Zulu. A number of core samples from the earlier 2011
drilling campaign were re-assayed using the method described above.
Initially, the samples of 2011 had only been dissolved using a
multi-acid digestion, which is a semi-quantitative technique and
not adequate to dissolve certain minerals including spodumene and
tantalite.
2021-2024 Drill
Programme:
Samples were prepared at Antec
Laboratories in Zimbabwe. At Antec, samples were crushed to -2
mm then a 200 g aliquot was pulverised to a minimum specification
of 85% passing 75 μm. Pulverised samples (pulps) were transported
by an independent logistics company to the Premier offices in
Johannesburg, where they were inspected and transported to SGS
Lakefield by a company representative. SGS performed a sodium
peroxide fusion with the 51 multi-element analytical finishes
(ICP90A50 and IMS90A50). Detection limits for lithium are 10 ppm to
5% (50,000 ppm) and tantalum 0.5 ppm to 1% (10,000 ppm). QA/QC
samples, (i.e. Certified Reference Material, blanks and duplicates)
were inserted on site into the sample stream with each sample
represented with a unique sample number. The QA/QC samples
represent 15% of the total number of samples analysed.
Estimation Methodology:
3-dimensional geological modelling
was conducted in Datamine Studio RM on a lithological basis by an
external consultant, Shango. Information utilised to construct the
models was sourced from 237 diamond drill boreholes, 856 grade
control holes and 123 trenches together with surface mapping. All
data that was included within the models were verified and checked
prior to modelling. At the time of model development assays from
202 surface boreholes were available. Wireframe models were
constructed on lithological parameters as opposed to grade
parameters. This method was imposed in order to remove the effect
of holmquistite, which is a lithium bearing amphibole that is
present in the host rock. Therefore, the wireframes constructed for
the geological model only included mineralised pegmatites. Each of
the 39 mineralised pegmatites was modelled separately and
subsequently reviewed by Premier prior to the Mineral Resource
estimation.
Each of the 39 mineralised
pegmatites were flagged and estimated separately. The sample data
were composited on a 1.5 m basis. For this exercise both Li2O and
Ta2O5 were estimated. Statistical analyses were performed
including descriptive statistics, histogram plots, probability
plots and capping of outliers. Spatial variances were modelled in
the form of downhole and planar variograms. Kriging neighbourhood
analysis (KNA) determined the optimal block model cells sizes and
search parameters for the estimation process. Ordinary Kriging (OK)
was applied for the grade estimation and detailed model validations
and checks were performed. Visual checks and various estimation
parameters, including search volumes, number of samples, distance
to samples, kriging efficiencies and regression slope, were
utilised to classify the Mineral Resource into Measured, Indicated
and Inferred categories.
Ongoing metallurgical test work
indicated that spodumene accounts for more than 80% of the
contained Li2O and the tonnages have been reduced to reflect only
the contained Li2O that is associated with spodumene. Test work
also indicated that all of the spodumene will be recovered and
therefore a zero cut-off Li2O grade has been applied for the
Mineral Resource statement. A zero cut off is considered applicable
to this project as the Mineral Resource reflects the recovery of
mineral (spodumene), as opposed to a metal. A further 3% geological
loss has been applied for the Measured category, 5% for the
Indicated category and 10% for the Inferred category.
Mineral Resource Classification:
Extensive close-spaced drilling
allows that 50% of this MRE falls within the Indicated category. A
combination of results from mining activities and further in-fill
drilling is likely to see an increase in the Indicated category.
Similarly, it is anticipated that the Mineral Resource
classification will likely change to a Reserve classification with
ongoing mining activity and grade control sampling, providing real
time confirmation of the validity of the modifying factors that may
be applied to the Mineral Reserve.
Mining and Metallurgy:
The Company has developed Zulu as an
open pit mine. Plant and process design was based on metallurgical
test work conducted by German based Dorfner-Anzaplan in 2016 and
2022 and is supported by extensive additional test work undertaken
by Geolabs in South Africa and the laboratory established at Zulu
in 2023.
More Information:
Lithium
Lithium (Li) is recovered from
minerals such as spodumene, petalite and lepidolite as well as
lithium-rich brines and is used in a range of products such as
ceramics, glass, batteries and pharmaceuticals. Lithium use has
expanded significantly in recent years due to the increasing use in
rechargeable batteries in portable electronic devices and batteries
and electrical motors for hybrid and electrical motor
vehicles.
Lithium grades are normally
presented in percentages or parts per million (ppm). Grades of
deposits are also expressed as lithium compounds in percentages,
for example as a percent lithium oxide (Li2O) content or percent
lithium carbonate (Li2CO3) content.
At Zulu, SC6 is the product
recovered. Zulu will therefore report that the estimated tonnage of
lithium is directly associated with spodumene. This assumes 100%
recovery and no process losses in the concentration
of spodumene in the plant are considered in this
MRE.
Lithium standard conversion factors
are set out in the Table 3 below:
Table 3: Conversion Factors for
Lithium Compounds and Minerals
Convert from
|
|
Convert Li
|
to Li2O
|
to Li2CO3
|
Lithium
|
Li
|
1.000
|
2.153
|
5.323
|
Lithium Oxide
|
Li2O
|
0.464
|
1.000
|
2.473
|
Lithium Carbonate
|
Li2CO3
|
0.188
|
0.404
|
1.000
|
The current pricing of Li is set out
below (Source: Metal.Com):
i.
|
Spodumene concentrate, SC6 6%
Li2O,
CIF China US$760/t.
|
ii.
|
Spodumene concentrate, >7%
Li2O,
CIF China: US$820/t.
|
Li content of pure Spodumene
concentrate is 8.03%.
Tantalum
The primary source of tantalum is
from minerals including tantalite, columbite, wodginite and
microlite which are typically hosted in pegmatite ore bodies. The
largest deposits are located in Australia, Brazil and Africa.
Tantalum's major use is in the production of electronic components,
especially for capacitors, with additional use in components for
chemical plants, nuclear power plants, airplanes and missiles. It
is also used as a substitute for platinum.
The tantalum market is niche in size
with around 1,300 tonnes required each year. However, the market is
rapidly growing due to capacitor use in wireless and handheld
devices.
Competent Persons Statement:
Mineral Resource Estimate
The scientific and technical
information contained in this announcement that relates to the
Mineral Resource Estimate is based on data compiled and verified by
Mr Charles Muller of Shango Solutions, including the sampling,
preparation, security and analytical procedures.
Shango Solutions has reviewed the
information in this announcement that relates to
the Mineral Resource Estimate and has confirmed that the
information presented is balanced and complete and not inconsistent
with the reported MRE.
Mr Charles Muller is a Competent
Person who is a Professional Natural Scientist registered with
the South African Council for Natural Scientific
Professions (No. 400201/04) and a Fellow of
the Geological Society of South Africa, each of which is a
"Recognised Professional Organisation" (RPO). Mr Charles Muller has
sufficient experience that is relevant to the style of
mineralisation and type of deposit under consideration and to the
activity being undertaken to qualify as a Competent Person as
defined in the 2014 Edition of the "South African Code for the
Reporting of Mineral Resources and Mineral Reserves". Mr Charles
Muller consents to the release of the report and the information
contained therein.
Mr Charles Muller is an employee of
Shango Solutions (Shango), registered as Dunrose Trading 186 (Pty)
Ltd and established in April 2004. Shango provides a diverse
range of services to the mineral and mining sectors. Areas of
specialisation include target generation, exploration, geodatabase
compilation and management, geological modelling, resource
estimation, mineral asset valuations, due diligences, desktop
project reviews and technical reporting.
Mr Charles Muller provides
independent technical geological services to Premier. Furthermore,
Mr Muller has extensive experience in preparing technical and
competent persons' reports for exploration and mining
companies.
Mr Charles Muller is not employed by
or related to any employees, representatives or directors of
Premier Minerals. In addition, neither Shango nor its employees
have or have had any personal interest in this project resulting in
a conflict of interest.
Geology
Bruce Cumming, a consulting geologist
to Premier, has reviewed and approved this release to the extent
that reference is made to the geology and mineralogy of the Zulu
pegmatites. Mr. Cumming is a SACNASP and GSSA registered
geoscientist with 48 years' experience in exploration and project
management, in multicommodity projects throughout
Africa.
Market Abuse Regulations:
The information contained within
this announcement is deemed by the Company to constitute inside
information as stipulated under the Market Abuse Regulations (EU)
No. 596/2014 as it forms part of UK Domestic Law by virtue of
the European Union (Withdrawal) Act 2018 ("UK
MAR").
The person who arranged the release
of this announcement on behalf of the Company was George
Roach.
A copy of this announcement is
available at the Company's website, www.premierafricanminerals.com
Enquiries:
George Roach
|
Premier African Minerals Limited
|
Tel: +27 (0) 100 201 281
|
Michael Cornish / Roland Cornish
|
Beaumont Cornish Limited
(Nominated Adviser)
|
Tel: +44 (0) 20 7628 3396
|
Douglas Crippen
|
CMC
Markets UK Plc
|
Tel: +44 (0) 20 3003 8632
|
Toby Gibbs/Rachel Goldstein
|
Shore Capital Stockbrokers Limited
|
Tel: +44 (0) 20 7408 4090
|
Beaumont Cornish
Limited ("Beaumont
Cornish"), which is authorised and regulated in the United
Kingdom by the Financial Conduct Authority, is acting as
nominated adviser to the Company in connection with this
announcement and will not regard any other person as its client and
will not be responsible to anyone else for providing the
protections afforded to the clients of Beaumont Cornish or for
providing advice in relation to such proposals. Beaumont Cornish
has not authorised the contents of, or any part of, this document
and no liability whatsoever is accepted by Beaumont Cornish for the
accuracy of any information or opinions contained in this document
or for the omission of any information. Beaumont Cornish as
nominated adviser to the Company owes certain responsibilities to
the London Stock Exchange which are not owed to the
Company, the Directors, Shareholders, or any other
person.
Forward Looking Statements:
Certain statements in this
announcement are or may be deemed to be forward looking statements.
Forward looking statements are identified by their use of terms and
phrases such as ''believe'' ''could'' "should" ''envisage''
''estimate'' ''intend'' ''may'' ''plan'' ''will'' or the negative
of those variations or comparable expressions including references
to assumptions. These forward-looking statements are not based on
historical facts but rather on the Directors' current expectations
and assumptions regarding the Company's future growth results of
operations performance future capital and other expenditures
(including the amount. Nature and sources of funding thereof)
competitive advantages business prospects and opportunities. Such
forward looking statements reflect the Directors' current beliefs
and assumptions and are based on information currently available to
the Directors. A number of factors could cause actual results to
differ materially from the results discussed in the forward-looking
statements including risks associated with vulnerability to general
economic and business conditions competition environmental and
other regulatory changes actions by governmental authorities the
availability of capital markets reliance on key personnel uninsured
and underinsured losses and other factors many of which are beyond
the control of the Company. Although any forward-looking statements
contained in this announcement are based upon what the Directors
believe to be reasonable assumptions. The Company cannot assure
investors that actual results will be consistent with such forward
looking statements.
Notes to Editors:
Premier African Minerals
Limited (AIM: PREM) is a multi-commodity mining and natural
resource development company focused on Southern Africa with its
RHA Tungsten and Zulu Lithium projects in Zimbabwe.
The Company has a diverse portfolio
of projects, which include tungsten, rare earth elements, lithium
and tantalum in Zimbabwe and lithium and gold in Mozambique,
encompassing brownfield projects with near-term production
potential to grass-roots exploration. The Company has accepted a
share offer by Vortex Limited ("Vortex") for the exchange of Premier's
entire 4.8% interest in Circum Minerals
Limited ("Circum"),
the owners of the Danakil Potash Project in Ethiopia, for
a 13.1% interest in the enlarged share capital of Vortex. Vortex
has an interest of 36.7% in Circum.
APPENDIX
Table 1: Mineral Resource Statement for Zulu
Project - 31st January
2024
Tonnage
|
Grade
|
Metal
|
Category
|
Mt
|
Li2O
|
Ta2O5
|
Li2O
|
Ta2O5
|
%
|
g/t
|
t
|
kg
|
Indicated
|
|
|
14.78
|
0.45
|
43.83
|
66,498
|
647,687
|
Inferred
|
|
|
9.97
|
0.41
|
39.95
|
40,869
|
398,222
|
Indicated and Inferred
|
|
|
24.75
|
0.43
|
42.20
|
107,366
|
1,045,908
|
Notes
|
i.
|
Losses: delineated pegmatites contain 80% spodumene - tonnage
is reduced by 20% to reflect the mineral assemblage. In addition,
geological losses of 5% for Indicated Mineral Resources and 10% for
Inferred Mineral Resources have been applied.
|
ii.
|
The MRE is prepared at a 0 % cut-off grade as all the
spodumene is expected to be recovered.
|
iii.
|
A
density of 2.78 g/cm3 has been utilised.
|
iv.
|
A
depth cut-off of 300 m below surface has been considered based on
cost parameters, although the majority of the pegmatites have only
been modelled to a depth to 200 m.
|
v.
|
The effective date of the MRE is 31 January
2024
|
vi.
|
The MRE is based on information compiled by the Company and
reviewed by Shango and prepared in accordance with SAMREC. Mineral
Resources are not Mineral Reserves and have not demonstrated
economic viability.
|
vii.
|
The contained Li2O and Ta205 metal values are rounded, actual
grades and contained metal are accurately stated and any
differences in the totals are due to rounding.
|
Glossary of Technical Terms:
|
|
"Albite"
|
is a sodium rich feldspar and
typically is the plagioclase mineral found in
pegmatites.
|
|
"Albitite"
|
is a rock consisting almost entirely
of albite and quartz. It can be classed as an
alkali-feldspar-granite, however it is usually a high to
medium-temperature metasomatic rock formed by the sodic alteration
of various rocks.
|
|
"Amphibole"
|
a group term for various rock
forming silicates with the general chemical formula
Ca-Mg-Fe-Al-OH-Si-O.
|
|
"Chlorite"
|
a group term for various rock
forming silicates (Mg,Fe)6(Si,Al)4O10(OH)8.
|
|
"Chlorite
facies"
|
metamorphism under certain pressures
and temperatures that lead to the formation of the mineral
chlorite.
|
|
"Columbite"
|
a black mineral group that is an ore
of niobium and tantalum, [(Fe, Mn)Nb2O6].
|
|
"Epidosite"
|
a highly altered epidote and quartz
bearing rock.
|
|
"felsic"
|
refers to igneous rocks that are
relatively rich in elements that form feldspar and
quartz.
|
|
"Indicated
Resource"
|
are economic mineral occurrences
that have been sampled (from locations such as outcrops, trenches,
pits and drill holes) to a point where an estimate has been made,
at a reasonable level of confidence, of their contained metal,
grade, tonnage, shape, densities, physical
characteristics.
|
|
"Inferred
Resource"
|
that part of a Mineral Resource for
which tonnage, grade and mineral content can be estimated with a
low level of confidence. It is inferred from geological evidence
and sampling and assumed but not verified geological and/or grade
continuity. It is based on information gathered through appropriate
techniques from locations such as outcrops, trenches, pits,
workings and drill holes that may be limited or of uncertain
quality and reliability.
|
|
"Gneiss/gneissic"
|
a foliated rock formed by regional
metamorphism, in which bands or lenticles of granular minerals
alternate with bands or lenticles in which minerals having flaky or
elongate prismatic habits predominate. Generally, less than 50% of
the minerals show preferred parallel orientation.
|
|
"Holmquistite"
|
is a lithium rich amphibole
(Li2Mg3Al2(Si8O22)(OH)2).
|
|
"K-feldspar"
|
is a general term for potassium
bearing feldspars KAlSi3O8, a common rock forming
mineral. Microcline is the low temperature variety found in
pegmatites.
|
|
"Lepidolite"
|
is the mineral name for lithium
bearing mica KLi2Al(Si4O10)(F,OH)2 an important ore of lithium.
|
|
"Li2O"
|
chemical formula of dilithium
oxide.
|
|
"Lithium Carbonate Equivalent
(LCE)"
|
is the industry standard terminology
for, and is equivalent to, Li2CO3.
|
|
"mafic"
|
pertaining to or composed dominantly
of the ferromagnesian rock-forming silicates; said of some igneous
rocks and their constituent minerals.
|
|
"JORC"
|
The Australian code for reporting
Mineral Resources.
|
|
"Measured Mineral
Resource"
|
that part of a Mineral Resource for
which quantity, grade or quality, densities, shape, and physical
characteristics are so well established that they can be estimated
with confidence sufficient to allow the appropriate application of
technical and economic parameters, to support production planning
and evaluation of the economic viability of the deposit. The
estimate is based on detailed and reliable exploration, sampling
and testing information gathered through appropriate techniques
from locations such as outcrops, trenches, pits, workings and drill
holes that are spaced closely enough to confirm both geological and
grade continuity.
|
|
"Metamorphism"
|
the mineralogical, chemical, and
structural adjustment of solid rocks to physical and chemical
conditions that have generally been imposed at depth below the
surface zones of weathering and cementation, and that differ from
the conditions under which the rocks in question
originated.
|
|
"Metasomatism"
|
the chemical alteration of a rock by
hydrothermal and other fluids. It is the replacement of one rock by
another of different mineralogical and chemical composition. The
minerals which compose the rocks are dissolved and new mineral
formations are deposited in their place. Dissolution and deposition
occur simultaneously, and the rock remains solid.
|
|
"Mica"
|
is a general term for a group of
sheet silicate minerals, it includes several closely related
minerals having nearly perfect basal
cleavage, KAl2(Si3Al)O10(OH,F)2; micas are common rock forming
minerals.
|
|
"Microlite"
|
is a pale-yellow, reddish-brown, or
black mineral composed of sodium calcium tantalum oxide with a
small amount of fluorine (Na,Ca)2Ta2O6(O,OH,F); locally a tantalum
ore.
|
|
"Mineral
Resource"
|
concentration or occurrence of
diamonds, natural solid inorganic material or natural fossilized
organic material including base and precious metals, coal, and
industrial minerals in or on the Earth's crust in such form and
quantity and of such a grade or quality that it has reasonable
prospects for economic extraction. The location, quantity, grade,
geological characteristics and continuity of a mineral resource are
known, estimated or interpreted from specific geological evidence
and knowledge.
|
|
"Mn"
|
is the symbol for the chemical
element manganese.
|
|
"Pegmatite"
|
an exceptionally coarse-grained
igneous rock, with interlocking crystals, usually found as
irregular dikes, lenses, or veins, esp. at the margins of granitic
intrusions.
|
|
"Petalite"
|
the mineral name for lithium
aluminium silicate LiAl(Si4O10) an important ore of
lithium.
|
|
"Plagioclase"
|
a group term for sodium to calcium
dominant feldspars (Na,Ca)(Al,Si)4O8, a common rock forming
silicate mineral.
|
|
"ppm"
|
means parts per million.
|
|
"Quartz"
|
one of the most common rock forming
minerals with the chemical composition SiO2 (silicon
dioxide).
|
|
"SAMREC"
|
is the South African Code for the
Reporting of Mineral Resources and Mineral Reserves.
|
|
"Schist"
|
a strongly foliated crystalline
rock, formed by dynamic metamorphism, that can be readily split
into thin flakes or slabs due to the well-developed parallelism of
more than 50% of the minerals present, particularly those of
lamellar or elongate prismatic habit, e.g., mica and
amphibole.
|
|
"Serpentinite"
|
a rock consisting almost wholly of
serpentine-group minerals, e.g., antigorite and chrysotile or
lizardite, derived from the alteration of ferromagnesian silicate
minerals, such as olivine and pyroxene. Accessory chlorite, talc,
and magnetite may be present.
|
|
"Spodumene"
|
the mineral name for lithium
aluminium silicate LiAlSi2O6 an important ore of
lithium.
|
|
"Ta2O5"
|
chemical formula of ditantalum
pentoxide.
|
|
"Tantalum pentoxide"
|
is the inorganic compound with the
formula Ta2O5.
|
|
"Tantalite"
|
a mostly dark grey to black mineral,
manganese bearing varieties are called manganotantalite or
tantalite-(Mn) MnTa2O6; a major tantalum
ore.
|
|
"Wodginite"
|
is a manganese, tin, tantalum oxide
mineral with formula Mn(Sn, Ta)Ta2O8, locally used as a tantalum
ore.
|
|
Ends