Matilda Copper Project - Exploration results confirm
project potential
Serabi Gold plc (AIM: SRB, TSX: SBI),
the Brazilian-focused gold mining and development company, is
pleased to provide an exploration update from its activities on the
Matilda Copper Prospect (“Matilda”) in the Tapajos region of Para
State, Northern Brazil. Matilda is being explored as part of the
Exploration Alliance between Serabi and Vale SA
To access a PDF copy of this news release
including all images please use the following link -
https://bit.ly/47aVgNr
Highlights
- The 2023
drilling programme in the Matilda district commenced in April and
was completed in November with a total of 7,597.21 meters drilled
from 21 holes and was completed in two phases. The first phase
comprised drill holes 23-MT-001 to 23-MT-010 and the second phase
drill holes 23-MT-011 to 23-MT-021(figure 1).
- Drilling
focussed on the main Matilda soil geochemistry anomaly, which was
initially tested in 2022 with three exploration holes.
- To date the
company has received results from 19 of the 21 drill holes executed
at Matilda, 12 of which have returned encouraging grades above 0.2%
Copper (“Cu”) over downhole intervals greater than 10m.
- Significant
intercepts from the second phase of drilling include.
- Hole 23-MT-010 –
21.45m @ 0.40% Cu and 0.11 g/t gold (“Au”) from 95.55m
- Hole 23-MT-015 –
25.00m @ 0.34% Cu and 0.09 g/t Au from 107.00m
- Hole 23-MT-016 –
34.00m @ 0.34% Cu and 0.10 g/t Au from 142.00m
- The drilling to
date has delineated a shallow mineralised zone with an exploration
target with a potential range of between 21 million tonnes (“Mt”) @
0.40% Cu up to 81Mt @ 0.28% Cu. In addition to this zone, the
system is open to the NW, SE and at depth. This potential volume
and grade is however, conceptual in nature as insufficient
exploration has been completed to define a mineral resource and it
is uncertain if a mineral resource estimate will be
delineated.
- In addition to
Matilda, the Company continues to investigate other copper/gold
systems in the same geological environment with anomalies and
positive results derived from exploration, particularly in Ganso
and Cinderela targets (see news release 2 November 2023).
- In November
2023, a 26 kilometre terrestrial geophysics Induced Polarisation
(IP) Pole-Dipole survey was completed over Matilda as part of
geological investigation. Serabi is currently processing,
integrating, and interpreting the data which will be used for
drillhole targeting in the 2024 programme.
Mike Hodgson CEO commented.
“We are excited about the positive results we
have received from the Matilda prospect and to intersect porphyry
mineralisation in 12 out of 19 holes is a very encouraging indeed.
The drilling has continued to expand our geological understanding
of the system.
“We believe that the Matilda prospect is still
in its infancy and has much more to deliver. Typically, first stage
drilling into porphyry systems would be in the region of
15,000-20,000 metres, so we are delighted with these results after
just 7,500 metres. The drilling indicates the copper potential
remains open along the strike and at depth, especially because of
results received for the recent holes MT-018 and MT-012. Matilda’s
geological characterisation as an Alkalic Porphyry style system
helps guide our exploration strategy and suggests that further
results can come from deeper drilling.
“Additionally, the discovery of new potential
porphyry systems at Ganso and Cinderela, in addition to the other
discoveries in the region, are advancing the Tapajos province as an
emerging copper province in the north of Brazil, and Serabi’s land
package and quality data puts us in an ideal position to take
advantage of this. The Company’s exposure to base metal demand
through the Vale alliance as well as its growth in gold production
primarily at Coringa positions the company well, and we look
forward to an exciting year in 2024.”
Figure 1: Location of drill holes
executed in the 2022 and 2023 drill programmes at
Matilda
To access an image of Figure 1 please use the
following link - https://bit.ly/48p8Eim
Detailed Results and Technical Discussion
The Phase 2 drilling programme focussed on
evaluating the extents of the mineralised system at the Matilda
Prospect as well as identifying key exploration vectors that can be
used to target higher grade mineralisation.
The results obtained to date are from the
shallowest part of the system, clustered within a large surface
geochemistry footprint measuring 4,000 metres by 2,500 metres.
Holes 23-MT-011, 23-MT-012 and 23-MT-18 suggest potential to extend
to the ENE and WSW, whilst the mineralisation also remains open at
depth,
Drillholes 23-MT-010, 23-MT-011 and 23-MT-012
stepped out to the north of the known mineralisation and all
returned grades of over 0.35% Cu within intervals greater than 10m,
indicating the system is open to the north and north-west.
Drillholes 23-MT-015, 23-MT-016, 23-MT-017 and
23-MT-019 were drilled to test the lateral extents of the
higher-grade core intercepted in drillholes 23-MT-004 and
23-MT-006, drilled during the first phase of drilling. All four
drillholes intercepted zones over 20m of 0.34% Cu including
discrete zones of up to 1.3% Cu, indicating that the higher-grade
zone is consistently mineralised. 23-MT-021 was drilled beneath
holes 23-MT-004 and 23-MT-006 to test the zone at depth and is
pending assay results.
Drillhole 23-MT-018 stepped out to the east of
known mineralisation and returned grades of up to 0.33% Cu over
16m, indicating that the system is open to the east.
These new results have extended mineralisation
to over 1 kilometre along a WNW-ENE trending de-magnetised zone.
The system remains open to west, east, north, and at depth (figure
2), and drilling has not yet delineated the size of the system.
Figure 2: Drill hole locations over
magnetic image showing 1200 metres long, northwest orientated
demagnetisation trend.
To access an image of Figure 2 please use the
following link - https://bit.ly/47kemBb
Drilling has intercepted narrow zones of
high-grade copper mineralisation related to potassic (K-feldspar,
biotite) and overprinting chlorite ± epidote, K-feldspar, albite,
scapolite alteration, as well as porphyry style quartz veinlets and
magnetite breccias. Strong “red rock” (hematite dusting of
feldspar) alteration commonly forms a halo to mineralised zones.
These styles of alteration and mineralisation share many
characteristics with silica-saturated alkalic porphyries such as in
Canada (e.g. Mount Milligan, B.C.) and Australia (e.g. NorthPark’s,
NSW). These alkalic systems typically have complex alteration
assemblages and small surface footprints, however, are often
vertically extensive, with high grade Cu-Au cores. They are also,
typically associated with breccias and multiple dyke like orebodies
rather than single stocks as commonly seen in typical calc-alkaline
porphyry systems.
The mineralisation intersected has been
interpreted as alteration “offshoots” that lie above and laterally
to the main porphyry core which is believed to be at depth.
Porphyry style veinlets and alteration have been intercepted in
every drillhole, even the drillholes without significant
intercepts, which indicates the scale of the system. The results
from the 2023 programme, combined with the scale of the surface
geochemical anomaly indicates the potential for high grade core
zones with multiple “offshoots” within a broad, alteration
halo.
To date, the causative intrusion(s) have not
been intercepted in drilling and remain a key exploration target
for large volumes of economic grade mineralisation. The 2024
drilling programme will aim to integrate all existing data and test
deeper parts of the system, where the narrow mineralisation
“offshoots” are interpreted to coalesce. It will also aim to
continue evaluating the extents and scale of the system and test
the multiple intrusive centres within the Matilda District
indicated by the geophysics and soil geochemistry, thereby
increasing the drill target pipeline.
Evaluation of the core by both Serabi’s and
Vale’s geologists and geological consultants has provided a
consensus that the setting and mineralisation style is consistent
with a silica-saturated alkalic porphyry-like system, and modelling
of the actual copper intercepts. The assumptions and premises of
this geological model are being used by the exploration team to
integrate and model the exploration data. Modelling of
mineralisation intercepts by the Vale’s exploration team suggests
an exploration target for potential for mineralisation with volume
of up to approximately 81Mt @ 0.28% Cu (figure 3 and
4). This potential volume and grade is however
conceptual in nature as insufficient exploration has been completed
to define a mineral resource and it is uncertain if a mineral
resource estimate will be delineated.
Figure 3: Drill section with 23-MT-001,
004 & 006 and copper results plotted over the magnetic
susceptibility model. Drill hole 21 is pending results, but core
logging indicates anomalous sulphides in the zone.
To access an image of Figure 3 please use the
following link - https://bit.ly/3vbjHwW
Figure 4: Mineralisation envelopes
modelled for Matilda totalling approximately 81Mt @ 0.28% Cu.
Modelling uses 0.15% Cu cut-off for composites, minimum true width
of 10m and maximum internal waste of 15m.
To access an image of Figure 4 please use the
following link - https://bit.ly/3GLq1Oz
The Matilda pole-dipole induced polarisation
(IP) geophysical survey completed 6 lines totaling 26 kilometres,
in an approximate grid of 400m x 200m (figure 5). The IP geophysics
has been processed and integrated with the magnetic susceptibility,
geological and geochemical data available. This will provide a
basis to plan the 2024 exploration drilling campaign aiming for the
extensions of the current mineralization zones and their potential
source.
Figure 5: showing the IP surveyed lines
on top of the geochemistry footprint of Matilda.
To access an image of Figure 5 please use the
following link - https://bit.ly/3RNnyt4
The Company continues to investigate the
potential for other porphyry copper and epithermal gold systems
within Serabi’s large exploration license portfolio, and further
prospective targets have been identified. Initial drilling at
Ganso, located 13 kilometres NE from Matilda intersected a thick
zone of advanced argillic alteration. On going drilling at Ganso
has intersected hematitic breccias with phyllic alteration and
porphyry style B-veins. This potentially suggests a porphyry type
system at depth. Drilling is in progress and news is expected in Q1
of 2024. Soil sampling at Leticia has indicated a very large
intrusive center in a similar structural setting to Matilda. An
initial field visit indicated outcrops like those seen at Ganso,
associated with the zone of advanced argillic alteration. On the
southern flank of this intrusive centre, there is a 4km long, WNW
trending soil gold anomaly just north of a sub-parallel drainage
with extensive garimpeiro workings. Just to the south, the soil
sampling program has delineated a series of small intrusive stocks
associated with magnetic anomalies. One of these is associated with
a Copper-Molybdenum anomaly. The Company will look to undertake
further reviews of all of these targets as part its 2024
exploration program (figure 6).
Figure 6: showing the location of
Cinderela related to São Chico base camp and Matilda porphyry
system.
To access an image of Figure 6 please use the
following link - https://bit.ly/48rajE1
Matilda Drill Results: Intersections
included in mineralisation wireframes to model the copper
potential.
HOLE_ID |
EAST (UTM SAD69) |
NORTH (UTM SAD69) |
RL |
DEPTH (m) |
DIP/Azm (°/°UTM) |
Obs |
From |
To |
Interval (m) |
True Intersect Lenght (m) |
Copper Grade
(Cu %) |
Gold Grade (Au g / t) |
23-MT-001 |
609314 |
9291988 |
292 |
548,8 |
60 / 180 incl. |
|
122,6 |
133,15 |
10,55 |
5,28 |
0,37 |
0,12 |
|
|
|
|
|
|
and |
148,25 |
179,5 |
31,25 |
15,63 |
0,21 |
0,06 |
23-MT-002 |
609004 |
9291497 |
265 |
359,37 |
60 / 000 incl. |
|
|
|
|
|
NSI |
NSI |
23-MT-003 |
608289 |
9291882 |
237 |
149,44 |
60 / 000 incl. |
|
|
|
|
|
NSI |
NSI |
23-MT-004 |
609332 |
9292162 |
237 |
398,58 |
60 / 180 incl. |
|
29,85 |
165,05 |
135,2 |
67,60 |
0,33 |
0,09 |
|
|
|
|
|
|
and |
217 |
305 |
88 |
44,00 |
0,36 |
0,09 |
23-MT-005 |
609002 |
9291696 |
299 |
404,69 |
60 / 000 incl. |
|
43 |
60 |
17 |
8,50 |
0,23 |
0,08 |
23-MT-006 |
609332 |
9292162 |
261 |
443,49 |
60 / 000 incl. |
|
31,65 |
143 |
111,35 |
55,68 |
0,20 |
0,05 |
|
|
|
|
|
|
and |
183,2 |
216,9 |
33,7 |
16,85 |
0,33 |
0,07 |
23-MT-007 |
608978 |
9292372 |
283 |
350,91 |
60 / 180 incl. |
|
22 |
68 |
46 |
23,00 |
0,20 |
0,06 |
23-MT-008 |
608626 |
9289542 |
267 |
398,62 |
60 / 000 incl. |
|
|
|
|
|
NSI |
NSI |
23-MT-009 |
608598 |
9289763 |
249 |
150,46 |
60 / 180 incl. |
|
|
|
|
|
NSI |
NSI |
23-MT-010 |
609313 |
9292614 |
242 |
404,78 |
60 / 180 incl. |
|
95,55 |
117 |
21,45 |
10,73 |
0,40 |
0,11 |
|
|
|
|
|
|
and |
215 |
233 |
18 |
9,00 |
0,38 |
0,03 |
23-MT-011 |
609025 |
9292819 |
232 |
426,01 |
60 / 180 incl. |
|
238 |
248 |
10 |
5,00 |
0,37 |
0,14 |
23-MT-012 |
609039 |
9292648 |
263 |
401,89 |
60 / 180 incl. |
|
104 |
148 |
44 |
22,00 |
0,22 |
0,06 |
|
|
|
|
|
|
and |
192 |
202 |
10 |
5,00 |
0,29 |
0,15 |
23-MT-013 |
609000 |
9291920 |
299 |
410,58 |
60 / 000 incl. |
|
|
|
|
|
NSI |
NSI |
23-MT-014 |
609002 |
9291295 |
233 |
434,13 |
60 / 000 incl. |
|
|
|
|
|
NSI |
NSI |
23-MT-015 |
609267 |
9292080 |
282 |
150,21 |
45 / 000 incl. |
|
41 |
150 |
109 |
77,07 |
0,25 |
0,07 |
23-MT-016 |
609267 |
9292080 |
282 |
219,97 |
60 / 000 incl. |
|
30 |
40 |
10 |
5,00 |
0,26 |
0,06 |
|
|
|
|
|
|
and |
52 |
62 |
10 |
5,00 |
0,23 |
0,06 |
|
|
|
|
|
|
and |
78 |
204 |
126 |
63,00 |
0,30 |
0,09 |
23-MT-017 |
609367 |
9292065 |
280 |
142,84 |
45 / 000 incl. |
|
102 |
122 |
20 |
14,14 |
0,35 |
0,09 |
23-MT-018 |
609667 |
9291960 |
267 |
395,02 |
60 / 000 incl. |
|
26 |
50 |
24 |
12,00 |
0,27 |
0,08 |
|
|
|
|
|
|
and |
230 |
252 |
22 |
11,00 |
0,22 |
0,06 |
23-MT-019 |
609367 |
9292065 |
280 |
229,43 |
60 / 000 incl. |
|
149 |
179 |
30 |
15,00 |
0,32 |
0,08 |
23-MT-020 |
609002 |
9291295 |
233 |
550,22 |
70 / 180 incl. |
|
|
|
|
|
NSI |
NSI |
23-MT-021 |
609303 |
9292320 |
252 |
627,77 |
65 / 180 incl. |
|
|
|
|
|
NSI |
NSI |
22-MT-001 |
609071.42 |
9292164.65 |
299 |
234.2 |
60 / 90 incl. |
|
56 |
201,6 |
145,6 |
72,80 |
0,20 |
0,06 |
|
|
|
|
|
|
and |
215,12 |
232,8 |
17,68 |
8,84 |
0,42 |
0,14 |
22-MT-002 |
608976.11 |
9292462.98 |
282 |
210.57 |
60 / 173 incl. |
|
38,25 |
81,75 |
43,5 |
21,75 |
0,21 |
0,07 |
|
|
|
|
|
|
and |
176,55 |
196,6 |
20,05 |
10,03 |
0,24 |
0,11 |
22-MT-003 |
609120.0 |
9292222.0 |
226 |
250.78 |
60 / 180 incl. |
|
44,3 |
80,45 |
36,15 |
18,08 |
0,22 |
0,08 |
|
|
|
|
|
|
and |
127,1 |
153 |
25,9 |
12,95 |
0,33 |
0,11 |
Reported intercepts calculated based on a minimum weighted average
grade using a minimum true mineralization width of xm, lower cut of
0.20% Cu and a maximum internal waste interval of 15.0m. Analyses
were performed by ALS Laboratories a Certified geochemical
laboratory. * Note: Geometries of the mineralization model, and
changes to the minimum mineralization width and internal wate
parameters used for 3D modelling has generated differences in the
results presented in the previous press release “Matilda Copper
Project – exploration update from September 7th, 2023” due to the
new results received, geological knowledge acquired and modelling
applied. All results are correct based on the parameters used and
geological knowledge at the time. |
NSI – No Significant Intersection. |
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 for the release of this
announcement on behalf of the Company was Clive Line, Director.
Enquiries
SERABI GOLD plcMichael
Hodgson t
+44 (0)20 7246 6830Chief
Executive m
+44 (0)7799 473621
Clive
Line t
+44 (0)20 7246 6830Finance
Director m
+44 (0)7710 151692
e
contact@serabigold.com
www.serabigold.com
BEAUMONT CORNISH LimitedNominated
Adviser & Financial AdviserRoland Cornish / Michael
Cornish t
+44 (0)20 7628 3396
PEEL HUNT LLPJoint UK
BrokerRoss
Allister t
+44 (0)20 7418 9000
TAMESIS PARTNERS LLPJoint UK
BrokerCharlie Bendon/ Richard
Greenfield t
+44 (0)20 3882 2868
CAMARCOFinancial PRGordon
Poole / Emily
Hall t
+44 (0)20 3757 4980
Copies of this announcement are available from
the Company's website at www.serabigold.com.
See
www.serabigold.com for more information
and follow us on twitter @Serabi_Gold
GLOSSARY OF TERMS
The following is a glossary of technical
terms:
“actinolite” |
amphibole silicate mineral commonly found in metamorphic rocks,
including those surrounding cooled intrusive igneous rocks |
“Ag” |
means silver. |
“Alkalic porphyry” |
A class of copper-porphyry mineral deposits characterised by
disseminated mineralisation within and immediately adjacent to
silica-saturated to silica-undersaturated alkalic intrusive centres
and being copper/gold/molybdenum-rich. |
“albite” |
is a plagioclase feldspar mineral |
“aplite” |
An intrusive igneous rock in which the mineral composition is the
same as granite, but in which the grains are much finer |
“argillic alteration” |
is hydrothermal alteration of wall rock which introduces clay
minerals including kaolinite, smectite and illite |
“Au” |
means gold. |
“assay” |
in economic geology, means to analyse the proportions of metal in a
rock or overburden sample; to test an ore or mineral for
composition, purity, weight, or other properties of commercial
interest. |
“biotite” |
A phyllosilicate mineral composed of a silicate of iron,
magnesium, potassium, and aluminum found in crystalline rocks and
as an alteration mineral. |
“brecciation” |
Describes the process where large angular broken fragments of
minerals or rocks become cemented together by a fine-grained
matrix. |
“CIM” |
means the Canadian Institute of Mining, Metallurgy and
Petroleum. |
“chalcopyrite” |
is a sulphide of copper and iron. |
“Cu” |
means copper. |
“cut-off grade” |
the lowest grade of mineralised material that qualifies as ore in
each deposit; rock of the lowest assay included in an ore
estimate. |
“Dacite porphyry intrusive” |
a silica-rich igneous rock with larger phenocrysts (crystals)
within a fine-grained matrix |
“deposit” |
is a mineralised body which has been physically delineated by
sufficient drilling, trenching, and/or underground work, and found
to contain a sufficient average grade of metal or metals to warrant
further exploration and/or development expenditures; such a deposit
does not qualify as a commercially mineable ore body or as
containing ore reserves, until final legal, technical, and economic
factors have been resolved. |
“electromagnetics” |
is a geophysical technique tool measuring the magnetic field
generated by subjecting the sub-surface to electrical
currents. |
“epidote” |
is a calcium aluminium iron sorosilicate mineral |
“garimpo” |
is a local artisanal mining operation |
“garimpeiro” |
is a local artisanal miner. |
“geochemical” |
refers to geological information using measurements derived from
chemical analysis. |
“geophysical” |
refers to geological information using measurements derived from
the use of magnetic and electrical readings. |
“Geophysical techniques” |
include the exploration of an area by exploiting differences in
physical properties of different rock types. Geophysical methods
include seismic, magnetic, gravity, induced polarisation and other
techniques; geophysical surveys can be undertaken from the ground
or from the air. |
“gossan” |
is an iron-bearing weathered product that overlies a sulphide
deposit. |
“grade” |
is the concentration of mineral within the host rock typically
quoted as grams per tonne (g/t), parts per million (ppm) or parts
per billion (ppb). |
“g/t” |
means grams per tonne. |
“granodiorite” |
is an igneous intrusive rock like granite. |
“hectare” or a “ha” |
is a unit of measurement equal to 10,000 square metres. |
“hematite” |
is a common iron oxide compound |
“igneous” |
is a rock that has solidified from molten material or magma. |
“IP” |
refers to induced polarisation, a geophysical technique whereby an
electric current is induced into the sub-surface and the
conductivity of the sub-surface is recorded. |
“intrusive” |
is a body of rock that invades older rocks. |
“mineralisation” |
the concentration of metals and their chemical compounds within a
body of rock. |
“mineralised” |
refers to rock which contains minerals e.g. iron, copper,
gold. |
“Mo-Bi-As-Te-W-Sn” |
Molybdenum-Bismuth-Arsenic-Tellurium-Tungsten-Tin |
“magnetite” |
Magnetic mineral composed of iron oxide found in intrusive rocks
and as an alteration mineral. |
“monzodiorite” |
Is an intrusive rock formed by slow cooling of underground
magma. |
“monzogranite” |
a biotite rich granite, often part of the later-stage emplacement
of a larger granite body. |
“mt” |
means million tonnes. |
“ore” |
means a metal or mineral or a combination of these of sufficient
value as to quality and quantity to enable it to be mined at a
profit. |
“oxides” |
are near surface bed-rock which has been weathered and oxidised by
long term exposure to the effects of water and air. |
“paragenesis” |
Is a term used to describe the sequence on relative phases of
origination of igneous and metamorphic rocks and the deposition of
ore minerals and rock alteration. |
“ppm” |
means parts per million. |
“phyllic alteration” |
is a hydrothermal alteration zone in a permeable rock that has been
affected by circulation of hydrothermal fluids |
“proterozoic” |
means the geological eon (period) 2.5 billion years ago to 541
million years ago |
“saprolite” |
is a weathered or decomposed clay-rich rock. |
“scapolites” |
are a group of rock-forming silicate minerals composed of
aluminium, calcium, and sodium silicate with chlorine, carbonate
and sulfate |
“sulphide” |
refers to minerals consisting of a chemical combination of sulphur
with a metal. |
“vein” |
is a generic term to describe an occurrence of mineralised rock
within an area of non-mineralised rock. |
“VTEM” |
refers to versa time domain electromagnetic, a particular variant
of time-domain electromagnetic geophysical survey to prospect for
conductive bodies below surface. |
Assay ResultsAssay results reported within this
release include those provided by the Company's own on-site
laboratory facilities at Palito and have not yet been independently
verified. Serabi closely monitors the performance of its own
facility against results from independent laboratory analysis for
quality control purpose. As a matter of normal practice, the
Company sends duplicate samples derived from a variety of the
Company's activities to accredited laboratory facilities for
independent verification. Since mid-2019, over 10,000 exploration
drill core samples have been assayed at both the Palito laboratory
and certified external laboratory, in most cases the ALS laboratory
in Belo Horizonte, Brazil. When comparing significant assays with
grades exceeding 1 g/t gold, comparison between Palito versus
external results record an average over-estimation by the Palito
laboratory of 6.7% over this period. Based on the results of this
work, the Company's management are satisfied that the Company's own
facility shows sufficiently good correlation with independent
laboratory facilities for exploration drill samples. The Company
would expect that in the preparation of any future independent
Reserve/Resource statement undertaken in compliance with a
recognised standard, the independent authors of such a statement
would not use Palito assay results without sufficient duplicates
from an appropriately certificated laboratory.
Forward-looking statementsCertain 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. Several 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.
Qualified Persons StatementThe scientific and
technical information contained within this announcement has been
reviewed and approved by Michael Hodgson, a Director of the
Company. Mr Hodgson is an Economic Geologist by training with over
30 years' experience in the mining industry. He holds a BSc (Hons)
Geology, University of London, a MSc Mining Geology, University of
Leicester and is a Fellow of the Institute of Materials, Minerals
and Mining and a Chartered Engineer of the Engineering Council of
UK, recognizing him as both a Qualified Person for the purposes of
Canadian National Instrument 43-101 and by the AIM Guidance Note on
Mining and Oil & Gas Companies dated June 2009.
Neither the Toronto Stock Exchange, nor any other securities
regulatory authority, has approved or disapproved of the contents
of this news release
- Matilda exploration update - Dec 2023
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