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REG - Premier African Min - Zulu Assay Results

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RNS Number : 1149R  Premier African Minerals Limited  27 February 2023

27 February 2023

Premier African Minerals Limited

 

Zulu Assay Results

 

Premier African Minerals Limited ("Premier" or the "Company"), is pleased to
report on assay results at Premier's Zulu Lithium and Tantalum Project
("Zulu"). These results are from boreholes that are located within the area
planned to be mined under operation of the Pilot Plant and will constitute a
portion of the Mineral Resource update required to support the DFS.

George Roach, CEO commented, "We continue to see good intersections within the
main spodumene rich pegmatite that are both encouraging for the long term and
supportive of our decision to commence operations with the large-scale pilot
plant as we have done."

 

Drill Holes: Lithium & Tantalum Results

The table below sets out the composites determined, as per the outlined
compositing routine in the text below the table, from analyses received from
the independent external laboratory (SGS) for holes ZDD021, ZDD047, ZDD048,
MDI-GT-01A, MDI-GT-02, ZDD151, & ZDD154 .

Table 1 -Assay Summary Results

 Hole        From (m)  To (m   Width* (m)  Li(2)O%  Ta(2)O(5) ppm  Rb ppm
 ZDD021      34.90     37.02   2.12        0.64     43             1181

 ZDD021      42.26     46.38   4.12        0.79     14             1619

 ZDD047      84.24     89.24   5.00        1.49     79             900

 ZDD047      106.08    110.08  4.00        1.52     40             592

 ZDD047      118.23    127.00  8.77        1.00     73             1142

 Incl.       123.00    126.00  3.00        1.66     80             1252

 ZDD048      38.40     40.40   2.00        0.80     126            450

 ZDD048      47.06     56.18   9.12        0.86     68             1367

 Incl.       49.00     50.00   1.00        2.68     96             435

 ZDD048      119.36    122.36  3.00        1.08     75             750

 ZDD048      133.36    149.36  16.00       0.82     43             1134

 Incl.       133.36    134.36  1.00        1.67     7              937

 Incl.       136.36    137.36  1.00        2.23     40             656

 MDI-GT-01A  19.94     28.94   9.00        1.41     35             1474

 Incl.       19.94     20.94   1.00        2.23     26             316

 Incl.       21.94     22.94   1.00        2.20     16             846

 Incl.       23.94     24.94   1.00        3.05     35             1022

 MDI-GT-01A  44.68     46.96   2.28        0.53     32             1750

 MDI-GT-01A  53.59     55.59   2.00        0.75     33             4254

 MDI-GT-02   18.86     22.86   4.00        1.00     52             1318

 Incl.       19.86     21.86   2           2.14     45             1351

 MDI-GT-02   30.62     33.62   3.00        1.70     30             2135

 Incl.       31.62     32.62   1.00        2.88     8              1786

 MDI-GT-02   37.63     40.62   2.99        0.98     40             1872

 MDI-GT-02   46.51     62.93   16.42       1.43     33             1999

 Incl.       46.93     47.93   1.00        2.20     32             2177

 Incl.       51.93     55.93   4.00        2.53     38             1517

 MDI-GT-02   84.44     86.44   2.00        0.73     81             2196

 MDI-GT-02   97.26     102.17  4.91        1.50     43             2660

 ZDD151      184.26    216.77  32.51       1.56     129            1666

 Incl.       189.26    190.26  1.00        2.56     156            812

 Incl.       196.26    197.26  1.00        2.88     103            1513

 Incl.       209.54    210.54  1.00        2.57     154            1130

 ZDD151      267.55    283.86  16.31       1.49     95             1851

 Incl.       275.55    277.55  2           2.93     67             961

 ZDD154      110.30    112.45  2.15        1.18     79             482

*Not True Width but drilled width

**0.50% Li(2)O cut-off applied.

The following compositing routine has been applied:

 ·                                         0.50% Li(2)O cut-off was applied to the pegmatitic intersections only.
 ·                                         <2m standalone composites at the cut-off grade but with an overall weighted
                                           average grade of >0.5% Li(2)O are not reported.
 ·                                         Within any composite of >2m thickness, high-grade intersections of 1m and
                                           greater are reported provided the high-grade intersection is a multiple of x
                                           1.5 of the overall weighted composite grade, and
 ·                                         Within any composite, inclusions of country rock of <2m thickness are
                                           included within the composite provided the overall grade of the composite is
                                           not <0.50% Li(2)O.

The following Table 3 sets out the drill hole collar coordinates for the drill
holes reported in Table 1 above:

Table 2 - Drill Holes Collar Coordinates - This RNS

 Dhole       UTM 35S*    UTM 35S*     Elevation (AMSL)  Azimuth TN (°)   Collar Dip                EOH

             Easting     Northing                                                  (°)             (m)
 ZDD021      751438.462  7783147.247  1339.594          341.44           -60.4                     120.48

 ZDD047      751352.710  7782103.348  1309.051          26.38            -59.2                     160.23

 ZDD048      751356.133  7782103.526  1309.026          277.58           -60                       160.28

 MDI-GT-01A  751464.291  7783279.273  1355.150          200.27           -70.23                    150.00

 MDI-GT-02   751366.102  7783111.157  1350.944          187.99           -69.84                    202.93

 ZDD151      750809.107  7782183.866  1326.535          112.8            -49.53                    308.54

 ZDD154      751077.739  7782108.867  1320.744          291.6            -53.56                    291.6

 * ARC1950 Datum (10m local datum shift)

Table 3 - Drilling & Trenching Progress

A summary of the number of drill holes completed both prior to and for the
ongoing updated mineral resource estimate as part of the DFS is set out below:

 PROGRAMME                    No of Drill Holes  Drill Metres (m)  No of Surface Trenches  Trenched Metres (m)
 RST (1958)                   7                  903.90
 ZULU - Initial Exploration   6                  2,312.90
 ZULU - PEA                   43                 5,809.10
 ZULU - Pilot Plant DFS       127                29,134.54         7                       832.56
 ZULU - DFS (in progress) **  0                  0                 6                       *

* Heavy rains have delayed completion of the trenching programme
** Resource in-fill drilling scheduled to recommence in March

Table 4 - Analytical Pipeline

A summary of the status of DFS drill core analysis is set out below:

 Results received to date (excluding QA/QC samples)       7,853
 # QA/QC samples analysed                                 1,113
 Sample pulps at SGS Randfontein awaiting analysis        862
 Sample pulps ready to be shipped to SGS                  0
 Samples being pulped at Antec                            392
 Ongoing sampling of drill cores/trench samples at site*  0
 *Estimate

 

Quality Assurance/Quality Control (QA/QC)

The drill holes are initially sited using a hand-held GPS (Global Positioning
System device) within the tenement areas. Accurate coordinates and elevations
of drill holes collars are subsequently derived from a DGPS (Differential
Global Position devices) survey.

Drill cores are geologically logged, intersections of interest are selected
are marked-up with unique sample ID assigned before splitting and sampling.
Cores are cut in half using a core cutter, individual samples bagged, and sent
for analysis.

Alternating Certified Refence Materials (CRM), blank or duplicate samples are
inserted every 10(th) sample into the sample stream sent to the laboratory to
ensure QA/QC compliance. These QA/QC samples are assessed upon receipt of
analyses, checked and, if acceptable, accepted into the analytical database.
Follow-up with the laboratory is instigated in cases were any QA/QC sample
fails the QA/QC parameters.

Currently, drill core samples are crushed and pulverised at the Antec
Laboratory, Zimbabwe to 85% passing -75 microns. Sample pulps are inspected
for export in Harare by the competent government authorities and couriered to
the SGS Laboratory Services in Randfontein, South Africa where pulps are fused
with sodium peroxide and analysed by ICP-OES and ICP-MS to report 51-elements.
(SGS code ICP90A50 & IMS90A50).

 

The Geology of Zulu

The area, located in the Fort Rixon Greenstone Belt, is underlain by
Archaean-aged meta-volcanics and meta-sedimentary sequences of the Bulawayan
Supergroup, with serpentinites and banded iron formations at the base in the
east and metamorphosed volcano-sedimentary sequences to the west. The
greenstone belt is tear drop shaped measuring 30 km long and 19 km wide near
the broad section at the top. Metamorphism is retrograded to Greenschist
facies.

 

The Zulu Pegmatite is a LCT (Lithium-Caesium-Tantalum) pegmatite swarm which
intrudes along the contacts between serpentine and metamorphosed
volcano-sedimentary sequences over a strike length of several kilometres.
Outcrop widths vary between 10 and 50m. The pegmatite bodies strike N20° and
dip 70° to 90° to the west.

 

The area was first pegged in 1955 by J.S. Willemse and intensely explored,
under option, by mapping, trenching and drilling by Rhodesian Selection Trust
Co. Ltd. ("RST") in 1958. In 1961 and 1962 a small quantity of petalite from
the River Pegmatites (see below) was mined by W. Burchett in partnership with
J.S. Willemse. Premier later acquired the claims in 2013.

 

Recent mapping and interpretation of the pegmatite swarm from
semi-quantitative X-Ray Diffraction (XRD) has identified three distinct phases
of pegmatites. A spodumene-rich, thick pegmatite named the Main Zone which
lies north and south of the Machakwe River, footwall low-spodumene pegmatites
with associated tantalum and rubidium and a suite of petalite-bearing
pegmatites of short strike length, named the River Pegmatites.

 

In general, the lithium minerals, occurring in varying quantities, are coarse
grained with associated feldspars and quartz with only very minor sulphides
being observed. In several contact zones, the lithium-bearing amphibole,
holmquistite, has been observed.

 

Qualified Person

Bruce Cumming, geologist with Premier, has reviewed and approved this release
to the extent that reference is made to Zulu. Mr. Cumming is a SACNASP and
GSSA registered geoscientist with 46 years' experience in exploration and
project management, in multicommodity projects throughout Africa.

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.

The person who arranged the release of this announcement on behalf of the
Company was George Roach.

Enquiries:

 George Roach                        Premier African Minerals Limited    Tel: +27 (0) 100 201 281

 Michael Cornish / Roland Cornish    Beaumont Cornish Limited            Tel: +44 (0) 20 7628 3396

                                     (Nominated Adviser)
 John More/Toby Gibbs                Shore Capital Stockbrokers Limited  Tel: +44 (0) 20 7408 4090

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.

 

In addition, the Company holds a 19% interest in MN Holdings Limited, the
operator of the Otjozondu Manganese Mining Project in Namibia.

 Glossary of Technical Terms:
 "amphibole"                    A class of rock-forming silicate or aluminosilicate minerals typically
                                occurring as fibrous or columnar crystals.
 "Banded Iron Formation (BIF)"  A sedimentary rock consisting of alternating layers of iron oxides and
                                iron-poor chert.
 "DFS"                          Definitive Feasibility Study.
 "Greenschist facies"           The Greenschist facies is at low pressure and temperature. The facies is named
                                for the typical schistose texture of the rocks and green colour of the
                                minerals chlorite, epidote and actinolite.
 "feldspar"                     An aluminosilicate mineral consisting of potassium, sodium, and calcium.
 "Holmquistite"                 A lithium-bearing amphibole related to hornblende with a formula as
                                (Na,K,Ca)Li(Mg,Fe)(3)Al(2)Si(8)O(22)(OH)(2.)
 "ICP-OES"                      Inductively coupled plasma-optical emission spectroscopy.
 "ICP-MS"                       Inductively coupled plasma mass spectrometry.
 "Lepidolite"                   A pink to lavender coloured lithium bearing mineral (KLi2Al(Si4O10)(F,OH)2).
 "Li to Li2O"                   x 2.153.
 "Li"                           Lithium.
 "Li(2)O"                       Lithium Oxide (Lithia) - an inorganic lithium compound used to assess lithium
                                minerals.
 "m"                            Meters.
 "meta-sediments"               Sedimentary rocks that have been metamorphosed.
 "meta-volcanics"               Volcanic rocks that have been metamorphosed.
 "PEA"                          Preliminary Economic Study
 "Petalite"                     A white coloured lithium bearing mineral (LiAl(Si4O10)).
 "ppm"                          Parts per million.
 "Rb"                           Rubidium.
 "SC6"                          Is a high-purity lithium ore with approximately 6 percent lithium content
                                being produced as a raw material for the subsequent production of lithium-ion
                                batteries for electric vehicles
 "serpentinite"                 A dark, typically greenish metamorphic rock, consisting of serpentine or
                                related minerals, formed when mafic igneous rocks are altered.
 "Spodumene"                    A white to pink coloured lithium bearing mineral (LiAlSi2O6).
 "Ta to Ta2O5"                  x 1.221.
 "Ta"                           Tantalum.
 "X-Ray Diffraction"            X-ray diffraction (XRD) is a widely used technique to assess the mineral
                                assemblage, crystallinity and structure of rocks, cores etc.

LITHIUM CLASSIFICATION AND CONVERSION FACTORS

Lithium grades are normally presented in percentages or ppm. Grades of
deposits are also expressed as lithium compounds in percentages, for example
as a percent lithium oxide (Li(2)O) content. The standard conversion factors
are set out in the table below:

Table: Conversion Factors for Lithium Compounds and Minerals

 Convert from           Convert to Li  Convert to Li(2)O
 Lithium        Li      1.000          2.153
 Lithium Oxide  Li(2)O  0.464          1.000

 
Ends

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