Zulu Assay Results and Pilot Plant Update

RNS Number : 3483X
Premier African Minerals Limited
26 August 2022
 

26 August 2022

Premier African Minerals Limited

 

Zulu Assay Results and Pilot Plant Update

 

Premier African Minerals Limited ("Premier" or the "Company"), is pleased to report on assay results at Premier's Zulu Lithium and Tantalum Project ("Zulu").

Highlights:

·

Multiple thick high-grade zones intersected

George Roach, CEO commented , "I am pleased to note continuity in the quality of assays from ongoing work at Zulu. At the same time, the large number of outstanding results remains as much a concern as an opportunity.

Work progresses well in relation to the pilot plant installation and we remain on target for hot commissioning in Q1 of 2023. At the same time, recent forecasts suggesting extended shortages of Spodumene and prices projected at current levels through to 2025, are both encouraging and supportive of the approach we have taken to target production early in 2023. Of particular interest is that our ongoing resource development is strongly supportive of the use of sensor-based ore sorting and we remain confident that this is likely to see wider utilisation of the available resource, particularly lower grade sections and potentially an overall lower production cost."

Drill Holes: Lithium & Tantalum Results

The table below sets out the independent external laboratory analyses for holes ZDD075, ZDD083, ZDD094, ZDD096, ZDD099, ZDD102 & ZDD106.

Table 1 - Assay Summary Results  

Hole

From (m)

To (m)

Width* (m)

Li2O%

Ta2O5 ppm

Rb ppm

ZDD075

 

53.22

 

56.96

 

3.74

 

1.29

 

62

 

3242

 

ZDD075

 

61.14

 

63.52

 

2.38

 

0.92

 

36

 

3167

 

ZDD075

 

102.00

 

105.89

 

3.89

 

1.16

 

15

 

2704

 

ZDD083

 

199.70

 

202.15

 

2.45

 

0.77

 

46

 

1460

 

ZDD094

 

126.60

129.60

 

3.00

 

0.93

 

90

 

1589

 

ZDD094

 

146.81

 

159.78

 

12.97

 

1.42

 

58

 

3452

 

Incl.

147.81

 

154.81

 

7.00

 

1.82

 

69

 

4295

 

ZDD096

146.60

 

148.60

 

2.00

 

1.51

 

63

 

2327

 

ZDD099

107.66

 

116.74

 

9.08

 

1.14

 

74

 

2996

 

Incl.

107.66

 

111.26

 

3.60

 

1.55

 

143

 

2950

 

Incl.

113.97

116.74

 

2.77

 

1.25

 

32

 

2911

 

ZDD102

146.45

 

149.45

 

3.00

 

0.75

 

81

 

3937

 

ZDD102

151.90

 

160.69

8.79

 

1.52

 

57

 

2815

 

Incl.

153.90

 

158.90

 

5.00

 

1.84

 

55

 

2950

 

ZDD102

165.89

 

169.48

 

3.59

 

1.29

 

46

 

2589

 

ZDD106

53.00

 

57.27

 

4.27

 

1.18

 

198

 

2572

 

Incl.

54.00

 

55.39

 

1.39

 

1.69

 

106

 

2286

 

ZDD106

58.55

 

64.36

 

5.81

 

0.62

 

119

 

3797

 

ZDD106

69.13

 

73.13

 

4.00

 

1.43

 

91

 

3348

 

Incl.

71.13

 

73.13

 

2.00

 

1.58

 

108

 

3228

 

ZDD108

159.70

 

163.80

 

5.10

 

0.95

 

65

 

1319

 

Incl.

158.70

 

159.70

 

1.00

 

1.93

 

86

 

1319

 

Incl.

161.80

 

162.80

 

1.00

 

1.34

 

71

 

2043

 

ZDD108

197.66

 

205.68

 

8.02

 

1.20

 

83

 

1796

 

Incl.

201.80

 

203.14

 

1.34

 

2.09

 

76

 

1158

 

Incl.

204.14

 

205.14

 

1.00

 

1.61

 

51

 

1259

 

ZDD109

185.46

 

188.91

 

3.45

 

0.79

 

65

 

1396

 

ZDD109

192.62

 

196.27

 

3.65

 

0.98

 

58

 

1843

 

Incl.

192.62

 

193.86

 

1.24

 

1.30

 

57

 

1740

 

ZDD109

210.80

 

212.81

 

2.01

 

1.60

 

67

 

1607

 

Incl.

211.80

 

212.81

 

1.01

 

1.95

 

94

 

1786

 

ZDD109

224.22

 

227.83

 

3.61

 

0.75

 

49

 

1960

 

Incl.

225.18

 

226.18

 

1.00

 

1.26

 

67

 

1261

 

ZDD110

211.78

 

216.55

 

4.77

 

1.37

 

83

 

2105

 

Incl.

211.78

 

212.78

 

1.00

 

1.52

 

79

 

1564

 

*Not True Width but lineal width

**0.50% Li2O cut-off applied.

The following compositing routine was applied:

·

0.50% Li2O 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% Li2O are not reported however,

·

Within any composite >2m thickness, high-grade intersections of 1m are reported; 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% Li2O.


Table 2 - Drilling Progress

A summary of the number of drill holes completed both prior to and for the ongoing DFS is set out below:

PROGRAMME

No of Drill Holes Completed

Metres (m)

RST (1958)

7

903.90

ZULU - Initial Exploration

6

2,312.90

ZULU - PEA

43

5,809.10

ZULU - DFS (completed)

111

25,727.29

ZULU - DFS (in progress) *

See note below


*Given the number of outstanding analyses as set out in the table below, a temporary suspension has been imposed on the Resource drilling. Three drill rigs remain on-site and will continue Resource drilling in the next 10 days to more targeted area of the Resource.


Table 3 - Analytical Pipeline

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

DFS - results received to date

2,997

DFS - sample pulps at SGS Randfontein awaiting analysis

1,735

DFS - sample pulps ready to be shipped from to SGS

401

DFS - samples being pulped at Antec

209

DFS - ongoing sampling of drill cores at site*

400

*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 10th 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 25 m. 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 an option, with mapping, trenching and drilling by Rhodesian Selection Trust Co. Ltd. ("RST") in 1958. In 1961 and 1962 a small quantity of petalite was mined by W. Burchett in partnership with J.S. Willemse. Premier later acquired the claims the Zulu in 2013.

 

The thickest pegmatite, north and south of the Machakwe river, is rich in spodumene, petalite and lepidolite while the thinner footwall pegmatites tend to be lower in Li-grade but carry good tantalum and rubidium grades.

 

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.

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 a ccepted 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.


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

John More/Toby Gibbs

Shore Capital Stockbrokers Limited

Tel: +44 (0) 20 7408 4090

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)3Al2Si8O22(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 (KLi 2 Al(Si 4 O 10 )(F,OH) 2 ).

"Li to Li2O"

x 2.153.

"Li"

Lithium.

"Li2O"

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.

"Petalite"

A white coloured lithium bearing mineral (LiAl(Si 4 O 10 )).

"ppm"

parts per million.

"Rb"

Rubidium.

"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 (LiAlSi 2 O 6 ).

"Ta to Ta2O5"

x 1.221.

"Ta"

Tantalum.

 

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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