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 (MAR) as in force in the United Kingdom pursuant to
the European Union (Withdrawal) Act 2018. Upon the publication of
this announcement via Regulatory Information Service (RIS), this
inside information will be in the public domain.
Andrada Mining LimiteD
("Andrada" or the
"Company")
Brandberg West Exploration
Drill Results
Continuation of notable tin,
tungsten and copper intersections
Andrada Mining Limited (AIM: ATM, OTCQB: ATMTF), a
critical raw materials producer with mining and exploration assets
in Namibia, is pleased to provide the final results from its
inaugural drilling programme at the historical Brandberg West mine,
situated within the exploration license, EPL5445. The aim of this
programme is to establish an initial understanding of the grade and
geology within the historical open pit area and to investigate
potential mineralised extensions to the north. These results
constitute the second and final batch of samples from this
programme, representing ten (10) out of the twenty (20) holes
drilled. (See announcement
released on 12 September 2024).
Highlights
All drill holes intersected mineralisation
containing the primary metals of interest, namely tin ("Sn"), tungsten ("W") and copper ("Cu"). Significant drill intersections
include:
§ Drill hole AT3 04:
− 2.25 m at 0.10% Sn,
0.60% W and 1.58% Cu from
9.92 m to 12.17 m
− 2.09 m at 0.80% Sn,
1.23% W and 0.16% Cu from 47.81 m to 49.90 m
− 0.58 m at
1.75% Sn, 0.78% W and 0.24%
Cu from 66.16 m to 66.74 m
− 0.66 m at
0.87% Sn, 3.53% W and 0.38%
Cu from 119.12 m to 119.78 m
§ Drill hole AT3
07:
− 0.42 m at
0.50% Sn, 1.85% W and 1.28%
Cu from 4.37 m to 4.79 m
− 0.31 m at
7.37% Sn, 1.04% W and 0.76%
Cu from 14.50 m to 14.81 m
− 0.68 m at
2.32% Sn, 1.64% W and 0.79%
Cu from 37.93 m to 38.61 m
− 0.28 m at
0.05% Sn, 1.85% W and 0.54%
Cu from 50.14 m to 50.42 m
− 0.25 m at
10.55% Sn, 1.06% W and
0.17% Cu from 151.02 m to 151.27 m
§ Drill hole AT3
20:
−
0.25 m at 1.69% Sn, 0.14% W and 0.07% Cu from 23.68 m to
23.93 m
−
0.42 m at 0.69% Sn, 1.26% W and 0.38% Cu from 25.16 m to
25.58 m
−
1.37 m at 0.19% Sn, 1.54% W and 0.30% Cu from 84.09 m to
85.46 m
−
0.65 m at 1.49% Sn, 1.79%
W and 0.13% Cu from 148.93 m to 149.58 m
§ Drill hole AT3 19:
− 0.34 m at
0.05% Sn, 0.06% W and 1.95%
Cu from 99.03 m to 99.37 m
− 0.51 m at
1.16% Sn, 0.04% W and 0.59% Cu from 100.05 m to 100.56 m
− 4.96 m at 0.86% Sn,
0.09% W and 0.46% Cu from 140.72 m to 145.68 m
Anthony Viljoen, Chief Executive Officer,
commented:
"The continuation of significant high-grade tin, tungsten and
copper intersections at the Brandberg West project endorses our
strategic outlook for this area and is demonstrative of the
untapped value at this asset. These second batch of drill results
reported grades as high as 10.55% for tin, 3.53% for tungsten and
1.95% for copper. These results also show that the mineralisation
continues along strike to the Northeast.
The full exploration results will be evaluated to optimise the
next exploration phase at Brandberg West. The addition of tungsten
and copper to our critical metals' portfolio complements our
strategy to becoming a developer of multiple critical metals to the
energy transition and future technological advancements. We look
forward to updating all stakeholders as we continue to develop this
promising asset."
Brandberg West
The Brandberg West project is situated within
exploration license EPL 5445 in the Erongo region of Namibia. The
project area is approximately 100 km from the Uis Tin Mine, Andrada
Mining's flagship asset. The historical open pit mine at Brandberg
West was owned and operated by Gold Fields Limited until operations
ceased in the 1980's, with the cessation of exploration activities
coinciding with a global collapse of the tin price.
The historical Brandberg West mine produced a
tin and tungsten concentrate with secondary copper reported but
never concentrated. The mineralisation occurs within multiple
generations of quartz veins that trend mainly east - west in the
pit and northeast - southwest further north. Most of these
mineralised veins appear to be subvertical and are well exposed
within the historically mined and surrounding areas. These quartz
veins are hosted by metasediments of the Zebraputs Formation, with
an overlying marble unit that acted as an impermeable barrier to
the mineralising fluids.
Exploration Programme
The exploration programme comprised 20
oriented Diamond Drill (DD) holes for a total of 2 975m
drilled. The results of the first 10 drill holes, representing 1
471 drill meters, were previously reported (See announcement released on 12 September
2024), revealing grades of up to 4% for tin, over 2% for
tungsten and typically 0.5% - 2% for copper. This announcement
pertains to the remaining 10 holes, comprising 1 504 drill
meters. This drill programme investigated the
subsurface continuity and metal endowment of the quartz veins
within the historical pit as well as the mineralised extensions
identified at surface to the north. All holes were drilled at dip
angles of either 60° or 45° to target the sub - vertical
mineralised quartz veins. These intersections indicate apparent
widths, which are greater than true widths due to the angle of
intersection. This programme demonstrates that high grade
mineralisation occurs within the existing pit and extends to the
north.
The metals reported herein, namely Sn, W and
Cu, are the primary focus of this drilling campaign. The historical
operations did not produce any copper concentrate - however,
because of its strong correlation with tin and tungsten, future
metallurgical investigation will evaluate the recovery of all three
metals. It is noteworthy that anomalous concentrations of silver
and gallium were also identified in several of the analysed
samples. The economic potential of these metals will be
investigated as the project evolves. The results of this programme
will be utilised to produce an updated geological model that will
form the basis for follow-up exploration programmes. In the table
below, lithology describes the dominant rock unit for each sample -
in most instances where the lithology is listed as a schist the
presence of smaller quartz veins or greisen have been logged as
secondary units.
Table: Mineralised drill
intersections from this programme. The reported intersections were
selected using a 0.2% cut off for Sn, W and Cu combined. Where
multiple samples were taken from a single quartz vein, the results
were combined to provide a length-weighted average grade for the
vein.
Hole ID
|
Dip Angle
(Degrees)
|
From - To
|
Length (m)
|
Lithology
|
Sn (%)
|
W (%)
|
Cu (%)
|
AT3 01
|
-60
|
18.42 -
18.74
|
0.32
|
Quartz
vein
|
0.23
|
0.02
|
0.65
|
20.38 -
21.05
|
0.67
|
Schist
|
0.04
|
0.07
|
0.26
|
24.07 -
24.42
|
0.35
|
Quartz
vein
|
0.62
|
0.01
|
0.26
|
25.38 -
26.23
|
0.85
|
Quartz
vein
|
0.40
|
0.39
|
0.17
|
27.97 -
28.29
|
0.32
|
Quartz
vein
|
0.87
|
0.01
|
0.21
|
28.85 -
30.73
|
1.88
|
Quartz
vein
|
0.17
|
0.00
|
0.55
|
43.79 -
45.02
|
1.23
|
Quartz
vein
|
0.88
|
0.31
|
0.33
|
48.94 -
49.33
|
0.39
|
Quartz
vein
|
0.14
|
0.59
|
1.02
|
61.11 -
61.48
|
0.37
|
Quartz
vein
|
0.18
|
2.73
|
0.53
|
63.88 -
64.14
|
0.27
|
Quartz
vein
|
0.06
|
0.33
|
0.10
|
68.61 -
68.96
|
0.35
|
Quartz
vein
|
4.50
|
0.03
|
0.18
|
82.79 -
83.20
|
0.41
|
Quartz
vein
|
0.03
|
0.04
|
0.23
|
84.26 -
84.49
|
0.23
|
Schist
|
0.01
|
0.07
|
0.41
|
89.77 -
90.01
|
0.25
|
Quartz
vein
|
1.01
|
0.01
|
0.27
|
93.83 -
94.28
|
0.45
|
Quartz
vein
|
0.23
|
0.07
|
0.07
|
95.27 -
96.27
|
1.00
|
Schist
|
0.01
|
0.84
|
0.01
|
AT3 04
|
-45
|
7.98 -
9.00
|
1.02
|
Quartz
vein
|
0.08
|
0.06
|
0.45
|
9.92 -
12.17
|
2.25
|
Quartz
vein
|
0.10
|
0.60
|
1.58
|
29.19 -
29.48
|
0.29
|
Quartz
vein
|
0.07
|
0.00
|
0.24
|
38.53 -
39.15
|
0.62
|
Quartz
vein
|
0.03
|
0.02
|
0.93
|
44.39 -
47.60
|
3.21
|
Quartz
vein
|
0.98
|
0.11
|
0.38
|
47.81 -
49.90
|
2.09
|
Quartz
vein
|
0.80
|
1.23
|
0.16
|
66.16 -
66.74
|
0.58
|
Quartz
vein
|
1.75
|
0.78
|
0.24
|
67.74 -
68.30
|
0.56
|
Quartz
vein
|
0.41
|
0.01
|
0.27
|
71.16 -
72.04
|
0.88
|
Quartz
vein
|
0.03
|
0.02
|
0.30
|
103.39 -
104.32
|
0.93
|
Quartz
vein
|
0.43
|
0.52
|
1.25
|
107.48 -
109.20
|
1.72
|
Quartz
vein
|
0.07
|
0.01
|
0.51
|
119.12 -
119.78
|
0.66
|
Quartz
vein
|
0.87
|
3.53
|
0.38
|
122.10 -
122.89
|
0.79
|
Quartz
vein
|
0.74
|
1.39
|
0.76
|
124.09 -
124.94
|
0.85
|
Quartz
vein
|
0.06
|
0.44
|
0.04
|
Hole ID
|
Dip Angle
(Degrees)
|
From - To
|
Length (m)
|
Lithology
|
Sn (%)
|
W (%)
|
Cu (%)
|
AT3 06
|
-60
|
6.40 -
9.00
|
2.60
|
Quartz
vein
|
0.05
|
0.01
|
0.24
|
18.96 -
19.90
|
0.94
|
Quartz
vein
|
0.27
|
0.05
|
0.71
|
33.39 -
36.03
|
2.64
|
Quartz
vein
|
0.69
|
0.04
|
0.40
|
47.68 -
47.96
|
0.28
|
Quartz
vein
|
0.02
|
0.03
|
0.31
|
55.28 -
55.94
|
0.66
|
Quartz
vein
|
1.40
|
0.85
|
0.29
|
77.89 -
78.88
|
0.99
|
Quartz
vein
|
0.05
|
0.01
|
1.21
|
80.14 -
80.56
|
0.42
|
Quartz
vein
|
0.01
|
2.90
|
0.43
|
84.45 -
85.31
|
0.86
|
Quartz
vein
|
0.19
|
0.32
|
1.20
|
94.59 -
95.60
|
1.01
|
Quartz
vein
|
0.05
|
0.01
|
0.33
|
96.41 -
98.08
|
1.67
|
Quartz
vein
|
0.03
|
0.01
|
0.72
|
130.07 -
131.07
|
1.00
|
Quartz
vein
|
6.07
|
1.56
|
1.11
|
138.76 -
140.00
|
1.24
|
Quartz
vein
|
0.68
|
0.45
|
0.39
|
145.98 -
147.88
|
1.90
|
Quartz
vein
|
0.04
|
0.01
|
0.25
|
149.86 -
151.73
|
1.87
|
Quartz
vein
|
0.26
|
0.11
|
0.75
|
AT3 07
|
-60
|
4.37 -
4.79
|
0.42
|
Quartz
vein
|
0.50
|
1.85
|
1.28
|
9.12 -
10.10
|
0.98
|
Quartz
vein
|
0.18
|
0.25
|
0.33
|
14.50 -
14.81
|
0.31
|
Quartz
vein
|
7.37
|
1.04
|
0.76
|
22.28 -
23.04
|
0.76
|
Quartz
vein
|
0.33
|
0.13
|
1.15
|
25.40 -
26.26
|
0.86
|
Quartz
vein
|
0.94
|
0.54
|
1.04
|
32.17 -
32.56
|
0.39
|
Quartz
vein
|
0.45
|
0.55
|
0.59
|
34.02 -
34.65
|
0.63
|
Quartz
vein
|
1.01
|
0.02
|
0.11
|
37.93 -
38.61
|
0.68
|
Quartz
vein
|
2.32
|
1.64
|
0.79
|
50.14 -
50.42
|
0.28
|
Quartz
vein
|
0.05
|
1.85
|
0.54
|
62.23 -
62.68
|
0.45
|
Quartz
vein
|
0.02
|
0.02
|
0.39
|
71.00 -
71.52
|
0.52
|
Schist
|
0.05
|
0.04
|
0.28
|
92.28 -
92.74
|
0.46
|
Quartz
vein
|
0.03
|
1.41
|
0.36
|
94.37 -
95.40
|
1.03
|
Schist
|
0.21
|
0.07
|
0.06
|
99.00 -
100.00
|
1,00
|
Schist
|
0.06
|
0.79
|
0.05
|
106.32 -
107.51
|
1.19
|
Quartz
vein
|
0.06
|
0.01
|
0.52
|
119.39 -
120.39
|
1,00
|
Schist
|
0.22
|
0.00
|
0.01
|
127.08 -
127.36
|
0.28
|
Quartz
vein
|
0.02
|
0.05
|
0.20
|
132.94 -
133.95
|
1.01
|
Quartz
vein
|
0.30
|
0.58
|
0.08
|
139.89 -
140.19
|
0.30
|
Quartz
vein
|
0.03
|
0.01
|
0.68
|
151.02 -
151.27
|
0.25
|
Quartz
vein
|
10.55
|
1.06
|
0.17
|
163.56 -
163.88
|
0.32
|
Quartz
vein
|
0.11
|
0.01
|
0.80
|
177.35 -
177.74
|
0.39
|
Quartz
vein
|
0.42
|
0.96
|
0.54
|
182.71 -
183.06
|
0.35
|
Quartz
vein
|
0.08
|
0.01
|
0.64
|
188.12 -
188.46
|
0.34
|
Quartz
vein
|
0.06
|
0.35
|
0.49
|
197.00 -
198.00
|
1.00
|
Schist
|
0.26
|
0.02
|
0.05
|
199.86 -
200.26
|
0.40
|
Quartz
vein
|
0.28
|
0.32
|
1.21
|
Hole ID
|
Dip Angle
(Degrees)
|
From - To
|
Length (m)
|
Lithology
|
Sn (%)
|
W (%)
|
Cu (%)
|
AT3 08
|
-60
|
22.08 -
23.32
|
1.24
|
Quartz
vein
|
0.67
|
0.15
|
0.21
|
30.59 -
32.12
|
1.53
|
Quartz
vein
|
0.15
|
0.23
|
0.26
|
35.17 -
35.51
|
0.34
|
Quartz
vein
|
0.11
|
0.02
|
0.86
|
44.45 -
45.45
|
1.00
|
Schist
|
0.31
|
0.09
|
0.05
|
46.96 -
47.85
|
0.89
|
Quartz
vein
|
0.12
|
0.97
|
0.59
|
59.25 -
60.09
|
0.84
|
Quartz
vein
|
0.02
|
0.00
|
0.47
|
70.00 -
70.79
|
0.79
|
Quartz
vein
|
0.03
|
0.01
|
0.30
|
76.31 -
77.43
|
1.12
|
Quartz
vein
|
0.05
|
0.01
|
0.43
|
90.30 -
90.56
|
0.26
|
Quartz
vein
|
0.05
|
0.01
|
1.47
|
92.50 -
93.06
|
0.56
|
Quartz
vein
|
0.38
|
0.02
|
1.89
|
114.28 -
114.58
|
0.30
|
Quartz
vein
|
0.02
|
0.00
|
0.37
|
142.65 -
143.19
|
0.54
|
Quartz
vein
|
0.02
|
0.53
|
0.15
|
146.56 -
146.82
|
0.26
|
Quartz
vein
|
0.01
|
0.00
|
0.21
|
148.53 -
149.18
|
0.65
|
Quartz
vein
|
0.04
|
0.00
|
0.25
|
AT3 09
|
-60
|
3.66 -
4.01
|
0.35
|
Quartz
vein
|
0.10
|
0.14
|
0.78
|
29.90 -
30.16
|
0.26
|
Quartz
vein
|
0.13
|
0.11
|
0.38
|
49.84 -
50.12
|
0.28
|
Quartz
vein
|
1.67
|
0.03
|
0.25
|
AT3 18
|
-60
|
18.69 -
22.34
|
3.65
|
Quartz
vein
|
0.03
|
0.75
|
0.33
|
53.57 -
56.60
|
3.03
|
Quartz
vein
|
0.64
|
0.14
|
1.29
|
69.81 -
70.54
|
0.73
|
Quartz
vein
|
0.02
|
0.04
|
0.29
|
83.30 -
84.47
|
1.17
|
Schist
|
0.02
|
0.21
|
0.34
|
85.50 -
86.45
|
0.95
|
Quartz
vein
|
0.01
|
0.04
|
0.67
|
95.47 -
95.97
|
0.50
|
Quartz
vein
|
0.02
|
0.00
|
0.20
|
110.24 -
110.65
|
0.41
|
Quartz
vein
|
0.03
|
0.00
|
0.70
|
130.96 -
131.64
|
0.68
|
Quartz
vein
|
0.02
|
0.00
|
0.49
|
158.67 -
159.64
|
0.97
|
Schist
|
1.11
|
0.01
|
0.15
|
AT3 19
|
-60
|
9.08 -
9.51
|
0.43
|
Quartz
vein
|
0.19
|
0.00
|
0.35
|
16.35 -
16.59
|
0.24
|
Quartz
vein
|
0.07
|
0.00
|
1.02
|
24.00 -
24.93
|
0.93
|
Schist
|
0.53
|
0.03
|
0.11
|
32.87 -
34.00
|
1.13
|
Schist
|
0.39
|
0.00
|
0.03
|
41.28 -
42.31
|
1.03
|
Schist
|
0.26
|
0.17
|
0.07
|
97.03 -
98.03
|
1.00
|
Schist
|
0.03
|
0.03
|
0.20
|
99.03 -
99.37
|
0.34
|
Quartz
vein
|
0.05
|
0.06
|
1.95
|
100.05 -
100.56
|
0.51
|
Quartz
vein
|
1.16
|
0.04
|
0.59
|
100.91 -
102.21
|
1.30
|
Quartz
vein
|
0.03
|
0.02
|
0.37
|
115.50 -
116.49
|
0.99
|
Schist
|
0.26
|
0.01
|
0.01
|
137.33 -
138.70
|
1.37
|
Schist
|
0.22
|
0.11
|
0.68
|
Hole ID
|
Dip Angle
(Degrees)
|
From - To
|
Length (m)
|
Lithology
|
Sn (%)
|
W (%)
|
Cu (%)
|
|
|
139.00 -
140.23
|
1.23
|
Schist
|
0.14
|
0.09
|
0.24
|
140.72 -
145.68
|
4.96
|
Schist
|
0.86
|
0.09
|
0.46
|
152.00 -
152.88
|
0.88
|
Schist
|
0.04
|
0.46
|
0.15
|
154.00 -
155.18
|
1.18
|
Schist
|
0.04
|
0.05
|
0.22
|
173.82 -
175.00
|
1.18
|
Schist
|
0.93
|
0.56
|
0.25
|
AT3 20
|
-60
|
6.31 -
7.25
|
0.94
|
Quartz
vein
|
0.06
|
1.04
|
0.64
|
11.38 -
12.15
|
0.77
|
Schist
|
0.01
|
0.28
|
0.03
|
14.55 -
15.52
|
0.97
|
Schist
|
0.01
|
0.27
|
0.01
|
23.68 -
23.93
|
0.25
|
Quartz
vein
|
1.69
|
0.14
|
0.07
|
25.16 -
25.58
|
0.42
|
Quartz
vein
|
0.69
|
1.26
|
0.38
|
31.78 -
32.24
|
0.46
|
Quartz
vein
|
0.01
|
0.22
|
0.08
|
33.24 -
34.06
|
0.82
|
Schist
|
0.01
|
0.30
|
0.01
|
59.87 -
60.33
|
0.46
|
Schist
|
0.22
|
0.29
|
0.34
|
65.12 -
65.60
|
0.48
|
Quartz
vein
|
0.01
|
0.21
|
0.10
|
70.10 -
71.72
|
1.62
|
Quartz
vein
|
0.03
|
0.00
|
0.25
|
84.09 -
85.46
|
1.37
|
Quartz
vein
|
0.19
|
1.54
|
0.30
|
91.35 -
92.19
|
0.84
|
Quartz
vein
|
0.05
|
0.83
|
0.81
|
103.18 -
103.66
|
0.48
|
Schist
|
0.27
|
0.03
|
0.12
|
105.70 -
105.95
|
0.25
|
Quartz
vein
|
0.04
|
0.00
|
0.20
|
118.60 -
118.86
|
0.26
|
Quartz
vein
|
0.04
|
0.03
|
0.22
|
148.93 -
149.58
|
0.65
|
Schist
|
1.49
|
1.79
|
0.13
|
AT5 14
|
-60
|
1.00 -
1.32
|
0.32
|
Quartz
vein
|
0.01
|
0.02
|
0.23
|
7.14 -
7.69
|
0.55
|
Quartz
vein
|
0.02
|
0.00
|
0.23
|
14.20 -
14.47
|
0.27
|
Quartz
vein
|
0.06
|
1.11
|
0.81
|
32.35 -
32.78
|
0.43
|
Quartz
vein
|
0.02
|
0.06
|
0.25
|
39.19 -
39.42
|
0.23
|
Quartz
vein
|
0.21
|
0.08
|
0.64
|
58.60 -
60.50
|
1.90
|
Quartz
vein
|
0.11
|
0.42
|
0.41
|
60.50 -
61.24
|
0.74
|
Quartz
vein
|
0.07
|
0.38
|
0.21
|
89.50 -
89.90
|
0.40
|
Quartz
vein
|
0.77
|
0.03
|
0.18
|
Downhole orientation surveys were undertaken
for each hole after drilling using a magnetic deviation probe that
collected readings at two metre intervals. Collar locations were
surveyed using a differential GPS. Veins that did not meet the
metal content cut off criteria have not been reported as they are
not currently considered to be of economic significance.
Each drill hole was geologically and
structurally logged and sampled as half core. The sampling
programme attempted to follow geological contacts while also
maintaining consistency in data representativity. The shortest
sampled length was 25cm while the longest length was limited to
125cm wherever possible.
Once sampled, the material was dispatched to
the laboratory for preparation and analysis. Sample analysis was
undertaken by UIS Analytical Services, a certified independent
laboratory in South Africa, using a lithium borate fusion
process. ICP-OES analysis was utilised for major and minor
elements, whereas ICP-MS was utilised for the trace elements,
including Sn, W and Cu. No top cut was applied in calculating the
weighted average grades for mineralised intersections.
Figure
1: Map displaying the localities of the reported holes. Line
A-A' indicates the cross section in Figure 2
below.
Figure 2: Section line A-A' displaying a projection of the drill hole
AT3 07. Only selected intersections in the drill hole are labelled;
the complete set of mineralised vein intersections is listed in the
table above. The veins shown have been extrapolated a small
distance from the drill hole and have been orientated in accordance
with structural measurements from the core logs.
Competent person
statement
The technical data in this
announcement has been reviewed by Professor Laurence Robb ("Prof.
Robb"), who is a non-executive director of Andrada Mining. Prof.
Robb has over 30 years of industry related exploration and economic
geology experience and is a Competent Person for the reporting of
exploration results. He has reviewed both the technical disclosures
in this release as well as the quality assurance protocols (QA/QC)
and results for this programme.
GLossary of Abbreviations
%
|
Symbol for Percentage
|
Cu
|
Symbol for Copper
|
DD
|
Diamond Drilling
|
ICP-MS
|
Inductively Coupled Plasma-Mass
Spectrometry
|
ICP-OES
|
Inductively Coupled Plasma-Optical Emission
Spectrometry
|
QA/QC
|
Quality Assurance / Quality
Control
|
Sn
|
Symbol for Tin
|
W
|
Symbol for Tungsten
|
GLossary of technical
terms
Apparent thickness
|
The thickness of a drill hole intersection at a
non-perpendicular angle to the dip of the mineralised body, which
is always greater than the true thickness by an amount proportional
to the angular difference between the intersection trace and the
perpendicular
|
Dip angle
|
The angle of inclination measured
downward from horizontal
|
Geological model
|
An interpretation of mineralisation
and host rock geology. This is usually generated in a
three-dimensional computer environment
|
Greisen
|
Type of alteration characterized by micas,
quartz and other accessory minerals
|
Quartz vein
|
Distinct, sheet-like body of crystallized
quartz within a host lithology, formed when hydrothermal fluids
precipitate minerals while circulating through fractures or
cavities.
|
Schist
|
A metasedimentary unit showing
pronounced foliation
|
Top cut
|
The technique of restricting the
grade value of outlier high-grade samples during geostatistical
averaging or estimation methodologies to prevent
overestimation
|
CONTACT
Andrada Mining
Anthony
Viljoen, CEO
Sakhile
Ndlovu, Investor Relations
|
+27 (11)
268 6555
|
NOMINATED ADVISOR &
BROKER
|
|
Zeus Capital
Katy
Mitchell
Harry
Ansell
Andrew de
Andrade
|
+44 (0) 20 2382 9500
|
CORPORATE BROKER &
ADVISOR
|
|
H&P Advisory Limited
Andrew
Chubb
Jay
Ashfield
Matt
Hasson
|
+44 (0) 20
7907 8500
|
Berenberg
Jennifer
Lee
Natasha
Ninkov
|
+44 (0) 20
3753 3040
|
FINANCIAL PUBLIC
RELATIONS
|
|
Tavistock (United Kingdom)
Emily
Moss
Josephine
Clerkin
|
+44 (0) 207
920 3150
andrada@tavistock.co.uk
|
About Andrada Mining
Limited
Andrada Mining Limited is listed on
the London Stock Exchange (AIM) with mining assets in Namibia, a
top-tier investment jurisdiction in Africa. Andrada strives to
produce critical raw materials from a large resource portfolio, to
contribute to a more sustainable future, improved living conditions
and the upliftment of communities adjacent to its operations.
Leveraging its strong foundation in Namibia, Andrada is on a
strategic path to becoming a leading African producer of critical
metals including lithium, tin, tungsten, copper and tantalum. These
metals are important enablers of the green energy transition, and
essential for components of electric vehicles, solar panels and
wind turbines.