THIS ANNOUNCEMENT CONTAINS INSIDE
INFORMATION AS STIPULATED UNDER THE UK VERSION OF THE MARKET ABUSE
REGULATION NO 596/2014 WHICH IS PART OF ENGLISH LAW BY VIRTUE OF
THE EUROPEAN (WITHDRAWAL) ACT 2018, AS AMENDED. ON
PUBLICATION OF THIS ANNOUNCEMENT VIA A REGULATORY INFORMATION
SERVICE, THIS INFORMATION IS CONSIDERED TO BE IN THE PUBLIC
DOMAIN.
3 September 2024
Great Southern Copper
plc
("GSC" or the
"Company")
GSC Expands Target at Mostaza Cu-Ag-Au
Mine, Cerro Negro Project
Permitting for drilling at Mostaza mine
in progress
Great Southern Copper plc (LSE: GSCU), the
company focused on copper-gold and lithium exploration in Chile, is
pleased to announce that the scale of the target for the Company's
maiden drilling programme at the Mostaza mine has increased due to
the recognition of significant zones of additional Cu-Ag
mineralisation in historical drill-hole assays and surface rock
chip samples. Preparations for the start of drilling continue with
archaeological and environmental surveys now completed, and the
selection of the drilling company via tender.
Highlights:
·
Historical drilling at the Mostaza mine included
25 diamond holes for a total of 1,024m. Drilling targeted
high-grade lenses of Cu-Ag mineralisation with intercepts above 1%
Cu summarised on historical plans and sections. Intercepts below
this grade were not shown.
·
16 of the 25 historical holes were finished in
anomalous copper mineralisation (>0.1% Cu) and 4 of the holes
failed to reach the high grade target.
·
Ongoing compilation of the historical data,
together with re-interpretation and 3D modelling of assays and
geology has identified a significant halo of additional copper
mineralisation located either side of the high-grade lenses. These
haloes represent an important expansion of the mineralised
potential as shown by the following examples calculated using a
cut-off of 0.1% Cu:
§ VDH4: 17m
@ 0.62% Cu and 45.06ppm Ag from 18m, expanded
to
·
40m @ 0.4% Cu and 23.08ppm Ag from 0m.
§ VDH9: 18m
@ 0.72% Cu and 31.7ppm Ag from 18m, expanded
to
·
40m @ 0.44% Cu and 16.55ppm Ag from 0m.
§ EDH15: 14m
@ 1.92% Cu and 118ppm Ag from 36m
·
Incl 8m @ 2.63% Cu and 153ppm Ag from 37m,
expanded to
·
54m @ 0.62% Cu from 10m (Ag assays not
continuous).
§ EDH24: 8m
@ 0.88% Cu and 69.0ppm Ag from 57m, expanded
to
·
28m @ 0.38% Cu from 44m (Ag assays not
continuous), and
§ EDH25: 6m
@ 1.05% Cu and 81.0ppm Ag from 49m, now expanded to
·
33m @ 0.53% Cu from 46m (Ag assays not
continuous).
·
In addition, the inclusion of this additional
mineralisation allows for inclusion of drill hole intercepts not
considered in the original high-grade resource calculation, such
as:
·
VDH1: 31m @ 0.48% Cu and 18.04ppm Ag from
0m.
·
The Cu-Ag halo mineralisation has the potential to
significantly increase the size of the Mostaza deposit.
·
Preparation for the start of drilling at Mostaza
is underway with archaeological and environmental surveys completed
and a drill contractor selected via bidding process.
·
On-going exploration at Cerro Negro identifies
additional copper mineralisation hosted in multiple structures
parallel to the Mostaza trend further expanding global copper
potential.
Cerro Negro is situated within the Company's
Especularita project ideally located close to national
infrastructure including main highways, powerlines, and towns. The
project is located 170km from the port city of Coquimbo, and 130km
from Antofagasta Minerals' copper concentrate port at Los Villos.
The area lies at an elevation between 800 and 1200m and is
accessible year-round for all exploration and mining activity
(Figure 1).
The project is located within the north-south
trending Cretaceous metallogenic belt that includes Teck's Carmen
de Andacollo Cu-Au Mine 80km to the north, and Pucobre's El Espino
Cu-Au development project 30km to the south. At Especularita, this
under-explored belt intersects with a northwest-trending structural
corridor that controls the "Colorada" advanced argillic lithocap
and extends to the Piuquénes porphyry Cu-Au deposit in
Argentina.
Sam Garrett,
Chief Executive Officer of Great Southern Copper,
said: "Exploration at Cerro Negro is rapidly
advancing with three key objectives - drill beneath the historic
Mostaza open pit to develop a high-grade copper-silver-gold
resource, expand the Mostaza deposit along strike targeting
extensions to the mineralised structures, and explore at depth
targeting large-scale porphyry copper type
deposits.
"It is very
encouraging to identify this additional potential before any metres
have even been drilled at Mostaza. This newly recognised
mineralisation has the potential to significantly increase the size
of the Mostaza deposit and provides additional optionality for
potential future mining operations.
"The
discovery of additional copper-mineralised structures hosted in the
advanced argillic lithocap above the Mostaza mine is also very
significant in terms of our porphyry copper exploration at Cerro
Negro. The potential of these anastomosing mineralised structures
to grade downward into porphyry type mineralisation is a genuine
target vector.
"The copper
bank at Cerro Negro is building and we eagerly await the start of
drilling. Drill sites have been selected and reviewed by the
drilling contractor and permitting for the drilling programme is
progressing with archaeological and environmental surveys already
completed."
Mostaza
Cu-Ag-Au Mine:
The Mostaza Cu-Ag-Au gold mine at Cerro Negro
was previously owned and mined by Antofagasta Minerals with
mixed oxide and sulphide ores processed at their nearby
Parral flotation plant1 also located within GSC's group
of concessions.
High-grade Cu-Ag-Au mineralisation at Mostaza is
hosted in a north-south trending shear zone which is intruded by
felsic dykes and breccias which have been overprinted by intense
advanced argillic to phyllic alteration. Copper
mineralisation is dominated by hypogene stromeyerite
(copper-silver) and chalcocite, covellite, digenite, bornite, plus
lesser chalcopyrite and pyrite1 as disseminations and in
quartz veinlets, crackle networks and breccias
The high-grade mineralisation forms
steeply-dipping tabular bodies, or lenses, which appear to "pinch
and swell" along the shear zones, however, this interpretation may
be a result of low drill density. Five lenses have been identified
within the Mostaza "Near-Mine" area with historical mining activity
at Lenses 1 and 2.
Historical exploration is limited to the
near-mine area with 25 diamond holes completed for a total of
1,024m (Figure 1). Significant intercepts for the drilling are
summarised in Table 1 below. Only 14 of the 25 holes are believed
to have reached target depth with the deepest hole drilling to only
92m. In 1981 these results, together with rock channel sampling of
mine workings, were used to calculate an internal non-JORC mineral resource estimate for Lens 1
and 2 reported at 190,600t of measured & indicated sulphide
with grades of 1.2% Cu, 80 g/t Ag, and 0.45 g/t Au, plus an
additional 63,000t of inferred sulphide
resource at depth1 (The 1981 Historical
Mineral Resource Estimate - HMRE)2.
The drilling clearly demonstrated
that the high-grade Cu-Ag mineralisation is open both at depth and
along strike, however, no further drilling or exploration activity
has since been conducted at Mostaza.
3D
Modelling of the Mostaza Cu-Ag Deposit:
Investigation of the historical drill data and
3D modelling of the deposit by GSC has subsequently revealed that
the high-grade, structurally controlled mineralisation at Mostaza
is enveloped by a broad halo of lower-grade copper mineralisation
(>0.1% Cu).
Significantly, 16 of the 25 historical drill
holes were terminated in anomalous copper mineralisation of
>0.1% Cu plus 4 of the holes reportedly failed to reach target
depths. Significant intervals (>0.1% Cu) are reported in Table
1. Consequently, to date, the extent of the mineralisation at
Mostaza is only limited by the depth of drill holes.
3D modelling of the deposit is in progress to
map the high-grade mineralisation and controlling structures, plus
assisting with drill targeting (Figure 2). In addition, calculation
of the 0.3% Cu cut-off shell clearly demonstrates the increased
size of the deposit (Figure 3).
Hole_ID
|
From_m
|
To_m
|
Interval
|
Cu_%
|
Ag_ppm
|
Notes:
|
VDH1
|
0
|
31
|
31
|
0.48
|
18.04
|
Hole terminated in
mineralisation
|
incl
|
0
|
3
|
3
|
0.9
|
27
|
|
and
|
10
|
14
|
4
|
0.96
|
65
|
|
VDH2
|
0
|
35
|
35
|
0.17
|
2.23
|
Hole terminated in
mineralisation
|
incl
|
9
|
14
|
5
|
0.23
|
7.8
|
|
VDH3
|
|
|
|
|
|
No significant. Hole terminated in
mineralisation
|
VDH4
|
0
|
40
|
40
|
0.4
|
23.08
|
Hole terminated in
mineralisation
|
incl
|
18
|
35
|
17
|
0.62
|
45.06
|
|
and
|
26
|
35
|
9
|
0.91
|
69.22
|
|
VDH5
|
0
|
11
|
11
|
0.16
|
1.82
|
Hole terminated in mineralisation
with Cu-Ag grades increasing
|
VDH6
|
1
|
10
|
9
|
0.13
|
0.89
|
|
|
15
|
21
|
6
|
0.19
|
1.67
|
Hole terminated in mineralisation
with Cu-Ag grades increasing
|
VDH7
|
|
|
|
|
|
No significant intercept
|
VDH8
|
0
|
22
|
22
|
0.29
|
4.23
|
Hole terminated in
mineralisation
|
incl
|
0
|
6
|
6
|
0.35
|
4.33
|
|
and
|
15
|
22
|
7
|
0.34
|
7.12
|
|
VDH9
|
0
|
40
|
40
|
0.44
|
16.55
|
Hole terminated in
mineralisation
|
incl
|
18
|
36
|
18
|
0.72
|
31.7
|
|
incl
|
19
|
23
|
4
|
1.05
|
55.75
|
|
and
|
25
|
30
|
5
|
1.04
|
50
|
|
VDH10
|
0
|
9
|
9
|
0.18
|
na
|
|
|
11
|
13
|
2
|
0.2
|
|
Hole terminated in
mineralisation
|
VDH11
|
1
|
41.3
|
40.3
|
0.17
|
1.06
|
Hole terminated in
mineralisation
|
EDH12
|
|
|
|
|
|
No significant intercept
|
EDH13
|
|
|
|
|
|
No significant intercept
|
EDH14
|
6
|
12
|
6
|
0.12
|
na
|
|
EDH15
|
10
|
63
|
54
|
0.62
|
na
|
|
incl
|
33
|
52
|
19
|
1.52
|
91.95
|
|
incl
|
36
|
51
|
15
|
1.82
|
113.67
|
|
incl
|
37
|
45
|
8
|
2.63
|
153
|
|
|
70
|
86
|
16
|
0.13
|
na
|
|
EDH16
|
23
|
30
|
7
|
0.12
|
na
|
|
|
31
|
36
|
5
|
0.11
|
na
|
|
|
38
|
43
|
5
|
0.1
|
na
|
|
|
46
|
51
|
5
|
0.12
|
na
|
|
|
55
|
87
|
32
|
0.15
|
na
|
|
|
88
|
90
|
2
|
0.1
|
na
|
|
EDH17
|
6
|
9
|
3
|
0.1
|
na
|
|
|
13
|
24
|
11
|
0.12
|
na
|
|
|
31
|
43
|
12
|
0.12
|
na
|
|
|
44
|
52
|
8
|
0.14
|
na
|
|
|
54
|
57
|
3
|
0.1
|
na
|
|
|
65
|
79
|
14
|
0.14
|
na
|
|
|
82
|
87
|
5
|
0.17
|
na
|
|
|
88
|
91
|
3
|
0.12
|
na
|
Hole terminated in
mineralisation
|
EDH18
|
10
|
12
|
2
|
0.1
|
na
|
|
|
19
|
43
|
24
|
0.35
|
na
|
|
incl
|
27
|
30
|
3
|
1.73
|
101.67
|
|
|
47
|
54
|
7
|
0.12
|
na
|
|
|
56
|
65
|
9
|
0.12
|
na
|
|
EDH19
|
16
|
24
|
8
|
0.11
|
na
|
|
|
27
|
36
|
9
|
0.13
|
na
|
|
|
43
|
48
|
5
|
0.52
|
37
|
Hole terminated in high grade
Cu-Ag
|
EDH20
|
10
|
19
|
9
|
0.1
|
na
|
|
|
22
|
25
|
3
|
0.1
|
na
|
|
EDH21
|
|
|
|
|
|
No significant intercept
|
EDH22
|
0
|
3
|
3
|
0.12
|
na
|
|
|
5
|
14
|
9
|
0.13
|
na
|
|
|
18
|
49
|
31
|
0.14
|
na
|
Hole terminated in mineralisation
with Cu-Ag grade increasing
|
EDH23
|
15
|
26
|
11
|
0.12
|
na
|
|
|
33
|
49
|
16
|
0.47
|
na
|
Hole terminated in
mineralisation
|
incl
|
39
|
46
|
7
|
0.87
|
57.29
|
|
EDH24
|
35
|
41
|
6
|
0.12
|
na
|
|
|
44
|
72
|
28
|
0.38
|
na
|
Hole terminated in
mineralisation
|
incl
|
57
|
68
|
11
|
0.75
|
52.73
|
|
incl
|
57
|
65
|
8
|
0.88
|
69
|
|
EDH25
|
46
|
79
|
33
|
0.53
|
na
|
Hole terminated in
mineralisation
|
incl
|
48
|
58
|
10
|
0.77
|
54.6
|
|
incl
|
49
|
55
|
6
|
1.05
|
81
|
|
and
|
62
|
71
|
9
|
0.92
|
72.56
|
|
Table
1: Significant intercepts for
historical resource and exploration drill holes at Mostaza mine,
Cerro Negro. New intervals calculated using a 0.1% Cu cut-off are
indicated in italics.
Figure
1: Map of the
Mostaza Mine area adapted from the 1981 Historical Mineral Resource
Estimate, showing historical drill holes and geological
cross-sections on the pre-mining topography. To date mining
activity has only centred on Lenses 1 and 2, with minimal
exploration and drilling outside of the mine
area.
Figure
2: Oblique
view of the Mostaza trend looking to the SE showing Lens 2 (red and
yellow) and the surface expression of the other lenses and
alteration zones along trend to the south.
Figure
3: Oblique
section view of the Mostaza open pit looking to the NNE showing
high-grade Cu-Ag-Au mineralisation (>1.0% Cu) in Lens 2 (red)
with newly recognised halo mineralisation >0.3% Cu (orange).
Historical drill holes traces are shown in
blue.
Cautionary
note:
The Company cautions that all references to
"resources", "mineral resources", or "mineral resource estimates"
in this RNS are historical and were prepared and reported prior to
the implementation of the JORC code and therefore are non-JORC
compliant. The Company advises that the resource
categories used in the historical estimates, for example "measured,
indicated, demonstrated and inferred", may not have the same
meaning or degree of confidence as current JORC
categories. Historical records indicate that the
quoted non-JORC resources were calculated using the
polygonal method based on underground sampling, 1024m of
drilling in 25 holes, and geological cross-sections and level
plans. GSC is presenting this information
for historical context only and is not treating it as a current
mineral resource estimate. The Company has not been
able to independently verify the results of historical drilling or
mine channel samples.
References:
1. RNS 4027V
(08 July 2024): GSC signs Cerro Negro Purchase Option
Agreement.
2. 1981
Mineral Resource Estimate; Internal report by Jeraldo Gold
Mining.
Enquiries:
Great Southern
Copper plc
|
|
Sam Garrett, Chief Executive Officer
|
+44 (0) 20 4582 3500
|
|
|
SI Capital
Limited
|
|
Nick Emerson
|
+44 (0) 1483 413500
|
|
|
Gracechurch
Group
|
|
Harry Chathli, Alexis Gore, Henry
Gamble
|
+44 (0) 20 4582 3500
|
Notes for
Editors:
About Great
Southern Copper
Great Southern Copper PLC is a UK-listed
mineral exploration company focused on the discovery of copper-gold
and lithium deposits in Chile. The Company has the option to
acquire rights to 100% of two projects in the under-explored
coastal belt of Chile that are prospective for large scale
copper-gold deposits. In addition, the Company has the option to
acquire rights to 100% of a lithium project located in the Salar de
Atacama district of Chile. Chile is a globally significant mining
jurisdiction being the world's largest copper producer and the
second-largest producer of lithium.
The two, early-stage Cu-Au projects comprise
the San Lorenzo and Especularita Projects, both located in the
coastal metallogenic belt of Chile which hosts significant copper
mines and deposits, including Teck's Carmen de Andacollo copper
mine, and boasts excellent access to infrastructure such as roads,
power and ports. Significant historical small-scale and artisanal
workings for both copper and gold are readily evident in both
exploration project areas.
The Company's Monti Lithium project is
strategically located in the pre-Andean region of Salar de Atacama
which is Chile's premier lithium-producing region with
well-established lithium mining operations and
infrastructure.
Great Southern Copper is strategically
positioned to support the global market for copper and lithium -
both critical battery metals in the clean energy transition around
the world. The Company is actively engaged in exploration and
evaluation work programmes targeting both large tonnage, low to
medium grade Cu-Au and Li deposits as well as high-grade Cu-Au
deposits.
Further information on the Company is available
on the Company's website: https://gscplc.com
Competent
Person Statement
The information in this announcement that
relates to exploration results is based on and fairly represents
information reviewed or compiled by Mr Sam Garrett, a Competent
Person who is a Member of the Australian Institute of Geoscientists
and a Fellow of the Society of Economic Geologists. Mr Garrett is
the CEO and a shareholder of Great Southern Copper PLC. Mr Garrett
has sufficient experience that is relevant to the styles of
mineralisation and types of deposit under consideration and to the
activity being undertaken to qualify as a Competent Person as
defined in the 2012 Edition of the "Australasian Code for Reporting
of Exploration Results, Mineral Resources and Ore Reserves". Mr
Garrett has provided his prior written consent to the inclusion in
this announcement of the matters based on information in the form
and context in which it appears.
This announcement includes information that
relates to Exploration Results prepared and first disclosed under
the JORC Code (2012) and extracted from the Company's previous LSE
announcements as noted, and the Company's Prospectus dated 20
December 2021. Copies of these announcements are available from the
LSE Announcements page of the Company's website: www.gscplc.com.
The Company confirms that it is not aware of
any new information or data that materially affects the information
included within the Prospectus dated 20 December 2021.
Forward Looking and Cautionary
Statements
Some statements in this announcement regarding
estimates or future events are forward-looking statements. They
include indications of, and guidance on, future earnings, cash
flow, costs and financial performance. Forward-looking statements
include, but are not limited to, statements preceded by words such
as "planned", "expected", "projected", "estimated", "may",
"scheduled", "intends", "anticipates", "believes", "potential",
"predict", "foresee", "proposed", "aim", "target", "opportunity",
"could", "nominal", "conceptual" and similar expressions.
Forward-looking statements, opinions and estimates included in this
report are based on assumptions and contingencies which are subject
to change without notice, as are statements about market and
industry trends, which are based on interpretations of current
market conditions. Forward-looking statements are provided as a
general guide only and should not be relied on as a guarantee of
future performance. Forward-looking statements may be affected by a
range of variables that could cause actual results to differ from
estimated or anticipated results and may cause the Company's actual
performance and financial results in future periods to materially
differ from any projections of future performance or results
expressed or implied by such forward-looking statements. So, there
can be no assurance that actual outcomes will not materially differ
from these forward-looking statements.