Matilda Copper Project -
Exploration
Update
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 Project in
the Tapajos region of Para State, Northern Brazil. The Matilda
Copper Project is being developed as part of the
Exploration
Alliance between the Company and Vale
SA.
A full PDF version of this news release
can be accessed using the following link -
https://bit.ly/45Viw1Q
Highlights
- Significant intercepts from the 2023
first phase drilling lie within a broad zone of pervasive Cu-Au
mineralisation and include.
- Hole 23-MT-004 (partial results) – 59.45m @ 0.49% Cu and 0.13
ppm Au from 29.85m (including 6.93m @ 0.95% Cu and 0.28 ppm Au from
78m)
- Hole
23-MT-006 (full
results) – 13.81m @ 0.47% Cu and 0.10 ppm Au from 200,95m
- 3,204 meters of diamond drilling
have been completed in 9 holes at Matilda.
- The copper mineralisation and
hosting rocks have many characteristics that typify alkalic
porphyry deposits found in Australia and Canada.
- Reprocessing of data from the
airborne geophysical survey completed in 2022 indicates that the
positive drill results may lie within a 1.2 kilometre by 800 metre
demagnetized structural zone. The zone remains untested both
laterally and at depth.
- A further 3,200 metre Phase 2 drill
programme commenced in August 2023 to test the geochemical /
geophysical trend along strike, and secondary targets generated
from the interpretation of the drilling to date.
- In addition, deep penetrating Induced Polarisation (“IP”) and
Audio-Magnetotelluric (“AMT”) geophysical programmes have been
designed to complement the drilling. The IP survey will begin in
September 2023.
Mike Hodgson CEO
commented
“We are very excited about these results and
therefore the potential of Matilda. The new drilling results
confirm the presence of good grades of copper mineralisation and
opens new perspectives for the future of the Company. The results
demonstrate that the Serabi tenement portfolio is located in a very
fertile area of the Tapajós and the limited historic exploration
activity provides a significant first mover advantage for the
Company.
“We are still in the process of understanding
the copper system at Matilda and while younger porphyry systems
provide some reference, the Matilda system is Proterozoic in age
and formed under considerably different conditions. This fact
brings challenges but at the same time opens new perspectives in
terms of the potential of our exploration ground.”
“The Exploration Alliance with Vale is working
extremely well and both teams continue to collaborate closely, to
improve the understanding and definition of the copper system.
These initial results are exceptionally positive, and bodes well
for further encouraging results from the next phase of
drilling”.
To access Figure 1 please use the following link
- https://bit.ly/3RbsLeh
Detailed
Results and
Technical Discussion
The 2023 first phase drill programme has
confirmed the discovery of the copper system, first announced in
July 2022 (see news release dated 5 July 2022 - Drilling confirms
new Porphyry discovery at Matilda). This Proterozoic aged copper
system has geological, mineralogical, and genetic features found in
modern alkalic porphyry systems such as those found in Australia
and Canada. The geochemical footprint from soil sampling suggests a
target area measuring 4,000 metres by 2,500 metres which remains
open to the west and southwest.
The Phase 1 drilling programme has focussed on
the strongest part of the Matilda coincident copper / gold / silver
soil anomaly with six drill holes along two drill sections spaced
400 metres apart. (see Figure 1). This initial focus area is also a
semi-coincident magnetic susceptibility high, (see Figures 2 and
3), potentially associated with potassic (magnetite)
alteration.
Mineralisation in hole 23-MT-001 occurs close to
the top of the hole in an alteration assemblage associated with
secondary biotite and magnetite replacement by chalcopyrite. The
magnetic anomaly reflects an unmineralised magnetic, monzodiorite.
Holes 23-MT-004 and 23-MT-006, (same drill section) both
intersected mineralised zones. Partial results from the section are
listed below and shown graphically in Figure 2.
23-MT-0016.06m @ 0.36% Cu and 0.07 ppm Au from
30.00m3.25m @ 0.44% Cu and 0.12 ppm Au from 102.00m9.14m @ 0.36% Cu
and 0.11 ppm Au from 122.60m4.11m @ 0.27% Cu and 0.09 ppm Au from
187.40m 23-MT-004 72.88m
@ 0.44% Cu and 0.12 ppm Au from
29.85m 5.37m
@ 0.39% Cu and 0.09 ppm Au from 138.80m
48.49m
@ 0.42% Cu and 0.11 ppm Au from 220.00m
** 23-MT-006 12.99m
@ 0.22% Cu and 0.05 ppm Au from
28.00m 23.77m
@ 0.24% Cu and 0.06 ppm Au from
50.00m 12.12m
@ 0.20% Cu and 0.04 ppm Au from
106.00m 6.97m
@ 0.24% Cu and 0.02 ppm Au from
161.20m 29.19m
@ 0.32% Cu and 0.07 ppm Au from
183.20m Including
13.81m @ 0.47% Cu and 0.10 ppm from
200.95m 12.12m
@ 0.20% Cu and 0.05 ppm Au from 305.00m
** Final Certified analyses awaited. These
preliminary results are from analyses carried out at the Palito
Mine Laboratory and are used for quick response in the further
planning of the drill programme.
On the section, the overall mineralised package
is approximately 600 metres wide and still potentially open to the
north.
Figure
2: Drill section with
23-MT-001,
004 &
006 and copper results plotted
over the magnetic susceptibility model.
To access Figure 2 please use the following link
- https://bit.ly/3OZNxuM
Figure
3: Drill hole locations over magnetic
image showing 1200
metres long, northwest
orientated demagnetization trend.
To access Figure 3 please use the following link
- https://bit.ly/44G04JM
Figure
4: Simplified model of an alkalic porphyry
system based on preliminary core logging at Matilda.
To access Figure 4 please use the following link
- https://bit.ly/481qTLg
Hole 23-MT-007 was drilled 200 metres south of
drill hole 22-MT-001 that was completed in early 2022. Hole
23-MT-07 has extended the low-grade zone intersected in 22-MT-001.
The upper part of 23-MT-007 has 39.84 metres of weak mineralisation
from 22 metres to 68 metres at 0.20% Cu followed by isolated
intervals of high-grade mineralisation including 3.46 metres @
0.67% Cu from 160 metres, 5.20 metres @ 0.58% Cu from 201 metres
(see drill hole intercepts below).
All the current holes test a small part of a
northwest-southeast trending magnetic structure which extends over
1,200 metres, (see Figure 3 above) associated with high copper,
gold and silver values in soils. To date, only 400 metres of this
trend has been tested by the two drill sections.
Holes 23-MT-002 and 23-MT-005 (figure 3) aimed
to test a different northeast trending structure approximately 400
metres to the south. These holes returned no significant
mineralisation but the mineralogical interpretation at the top of
23-MT-002 indicates similarities with the positive drill holes in
the other section. A new drill hole will be programmed to be
located 200 metres south of 23-MT-002.
Hole 23-MT-003 was a shallow exploratory drill
hole into the central part of the molybdenum anomaly and had no
significant intersections. Holes 23-MT-008 and 23-MT-009 are
situated on the South Matilda soil anomaly that need a better
understanding of their position in the system.
At Matilda the main mineralised zone is
interpreted as being at least 1.2 kilometres long by 800 metres
wide and is related to magnetite brecciation associated with
potassium feldspar with actinolite/apatite/biotite alteration and
chalcopyrite. Copper grades vary from 0.2% to 1.8% with grade,
thickness and shallow depth to the mineralisation suggesting good
potential for the discovery of an economically viable deposit.
The mineralisation occurs as disseminated and
veinlet hosted chalcopyrite and lesser pyrite replacing magnetite
within locally brecciated magnetite rich zones. The observed
alteration is both potassic (red haematite-potassium-feldspar with
secondary biotite) and sodic-calcic (carbonate veinlets and
epidote) with a vein paragenesis similar to alkalic porphyry copper
systems.
Interpretation of the core indicates that
mineralisation occurs in sub-vertical corridors, open along strike
and at depth. Mineralisation in 23-MT-004 and 23-MT006, starts just
below the weathering profile, indicating near-surface
potential.
Serabi is continuing its drilling at Matilda and
also over other regional exploration tenements and has now
completed 8,435 metres of drilling in 2023. The initial first phase
programme at Matilda comprised 3,204 metres with the remaining
5,231 metres being drilled on other regional targets including
Cinderella, Ganso, Highway and Isla.
The Phase 2 drilling programme at Matilda
commenced in August and will comprise a further 3,200 meters of
diamond drilling. The programme will evaluate the mineralisation
intercepted along strike with 400m deep drill holes and also test
new targets based on ongoing geologic, geophysical and geochemical
interpretations.
In September a 43 kilometre pole-dipole IP
programme will be initiated and is expected to take two months. The
programme will focus on mapping zones of increased sulphide content
and structures and generate new drill targets. An AMT survey is
also programmed on the same lines to identify deep controlling
structures. It is expected that these surveys will help prioritise
other soil geochemical targets within the Matilda zone.
Figure 5 showing the planned IP
programme
To access Figure 5 please use the following link
- https://bit.ly/3P7ErvZ
Examples of Alteration and Mineralisation from Matilda drill
core.
Alteration
To access images of the alteration please use the
following link - https://bit.ly/3Lej6jv
Mineralisation
To access images of the mineralisation please use
the following link - https://bit.ly/460KcCx
Multi-element geochemistry data from the 3,204
metres completed, is being processed to aid in the definition of
lithologies, alteration and mineralization and better understand
the potential of the copper system.
Drillhole Intercepts
HOLE ID |
EAST(UTM SAD69) |
NORTH (UTM SAD69) |
RL |
DEPTH (m) |
DIP/Azm(°/°UTM) |
Obs |
From |
To |
True Intersect length (m) |
CopperGrade(Cu
%)) |
GoldGrade(Au
g/t) |
23-MT-001 |
609314 |
9291988 |
292 |
548.80 |
60 / 180 incl. |
|
30.0 |
37.0 |
6.06 |
0.36 |
0.07 |
|
|
|
|
|
|
and |
102.0 |
105.75 |
3.25 |
0.44 |
0.12 |
|
|
|
|
|
|
and |
122.6 |
133.15 |
9.14 |
0.36 |
0.11 |
|
|
|
|
|
|
and |
187.4 |
192.15 |
4.11 |
0.27 |
0.09 |
23-MT-002 |
609004 |
9291497 |
265 |
359.37 |
60 / 0 incl. |
|
|
|
|
NSI |
NSI |
23 MT-003 |
608289 |
9291882 |
237 |
149.44 |
60 / 0 incl. |
|
|
|
|
NSI |
NSI |
23-MT-004 |
609332 |
9292162 |
237 |
398.58 |
60 / 180 incl. |
|
29.85 |
114.0 |
72.88 |
0.44 |
0.12 |
|
|
|
|
|
|
including |
29.85 |
98.0 |
59.45 |
0.49 |
0.13 |
|
|
|
|
|
|
including |
78.0 |
86.0 |
6.93 |
0.95 |
0.28 |
|
|
|
|
|
|
and |
138.8 |
145.0 |
5.37 |
0.39 |
0.09 |
|
|
|
|
|
|
and* |
220.0 |
276.0 |
48.49 |
0.42* |
0.11* |
23-MT-005 |
609002 |
9291696 |
299 |
404.69 |
60 / 0 incl. |
|
43.0 |
54.0 |
9.53 |
0.24 |
0.08 |
23-MT-006 |
609332 |
9292162 |
261 |
443.49 |
60 / 0 incl. |
|
28.0 |
43.0 |
12.99 |
0.22 |
0.05 |
|
|
|
|
|
|
and |
50.0 |
77.45 |
23.77 |
0.24 |
0.06 |
|
|
|
|
|
|
and |
106.0 |
120.0 |
12.12 |
0.20 |
0.04 |
|
|
|
|
|
|
and |
161.2 |
169.25 |
6.97 |
0.24 |
0.02 |
|
|
|
|
|
|
and |
183.2 |
216.9 |
29.19 |
0.32 |
0.07 |
|
|
|
|
|
|
including |
200.95 |
216.9 |
13.81 |
0.47 |
0.10 |
|
|
|
|
|
|
and |
305.0 |
319 |
12.12 |
0.20 |
0.05 |
23-MT-007 |
608978 |
9292372 |
283 |
350.91 |
60 / 180 incl. |
|
22.0 |
68.0 |
39.84 |
0.20 |
0.06 |
|
|
|
|
|
|
and |
160.0 |
164.0 |
3.46 |
0.67 |
0.04 |
|
|
|
|
|
|
and |
201.0 |
207.0 |
5.20 |
0.58 |
0.07 |
23-MT-008 |
608626 |
9289542 |
267 |
298.62 |
60 / 0 incl. |
|
|
|
|
NSI |
NSI |
23-MT-009 |
608598 |
9289763 |
249 |
150.46 |
60 / 180 incl. |
|
36.55 |
46.0 |
8.18 |
0.20 |
0.11 |
Reported intercepts calculated based on a minimum weighted average
grade and lower cut of 0.20% Cu and a maximum internal waste
interval of 6.0m based on analysis by ALS Laboratories. *Exception
for 23-MT-004 from 218.6m to 353m depth which had only Serabi´s
on-site lab reported analyses with the analysis from ALS still
pending. Based on the past analysis of 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, wherever practical,
use independent assay results and also verify the correlation with
Serabi’s internal laboratory analysis. |
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. |
“apatite” |
A mineral consisting of calcium phosphate with some fluorine,
chlorine, and other elements |
“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 a
given 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 matrixi |
“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. |
“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 similar to granite. |
“hectare” or a “ha” |
is a unit of measurement equal to 10,000 square metres. |
“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. |
“phyllosilicate
minerals” |
are a group of minerals that are fundamentally composed of extended
flat sheets of linked silicon-oxygen tetrahedra |
“ppm” |
means parts per million. |
“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. |
“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. 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.
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 - Sept 2023
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