Karonga Licence Granted
Released
Released
Announcement PDF
ASX Announcement
ASX:DY6
19 March 2025
Karonga Prospecting Licence Granted
DY6 Metals Ltd (ASX: DY6, “DY6” or the “Company”) is pleased to advise that it has received
confirmation from Malawi’s Mining & Minerals Regulatory Authority (MMRA) that the licence area for
its Karonga project (previously under application) has now been formally granted as Prospecting
Licence No. EL0782/24.
Located in northern Malawi, the licence covers an area of approximately 36km2 and has the potential
for copper mineralisation, as confirmed from preliminary reconnaissance/surveillance work
undertaken by DY6’s in country technical team.
KEY HIGHLIGHTS
•
Karonga Prospecting Licence has been granted over a recently identified high potential
Copper (Cu) mineralisation anomalous area in the Karonga district.
•
The licence grants to DY6 the exclusive right to prospect for copper, rare earth elements,
lithium and other minerals for a term of 3 years with an option to renew the licence for a period
not exceeding 2 years.
•
Preliminary reconnaissance/ surveillance sampling work on the licence area revealed
occurrence of elevated Cu grades, with initial portable XRF results ranging from 1.4 to 7.8%
Cu in rock (refer Table 1). Results are to be verified using standard laboratory-based XRF
analytical assaying methods*.
•
DY6 has recently acquired and completed reprocessing of historic hyperspectral survey data,
which has been used to map areas with high probability for copper mineralisation. The results
from this exercise correlate well to the mineralisation identified in the sampling work.
•
Historic anomalies from regional airborne geophysical radiometric and magnetic data appear
to correlate with both the hyperspectral probability copper mineralisation mapping and the
preliminary sampling reconnaissance work conducted.
•
Exploration for Cu and other minerals will continue on the licence area.
* Cautionary Statement on pXRF – pXRF (Portable X-Ray Fluorescence) results that are announced
in this report are from uncrushed, rock-chip samples and are preliminary only. The use of pXRF is an
indication only of the order of magnitude of expected final assay results.
Registered Office
Level 8, 99 St Georges Terrace
Perth WA 6000
P: +61 8 9486 4036
E: info@dy6metals.com
dy6metals.com
Figure 1. Location map of newly granted Karonga licence
The Project is located about 440km north of the capital Lilongwe Figure 1. It can easily be accessed
using Karonga-Chitipa M1 Road turning to the west at Kasikisi School signpost along the M1 Road
(Figure 2).
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Figure 2. Topographical map of the Karonga licence EL0782/24
Geology and Mineralisation
The Karonga area is associated with a series of NW-SE and N-S trending ridges with metamorphic
Basement complex rocks commonly identified as windows within the Karroo System which overlies
the basement. The Karroo System units are typically sandstones with carbonaceous shale formations.
The eastern part of the licence area is overlain by several patches of Karoo sediments and Cretaceous
to recent lacustrine sediments, the interrelations of which are complex due to unconformities and
faulting (Figure 3A). This area is part of the northern sub-province of the Malawi Province of the
Mozambique belt, active between about 700-400 million years ago. The major lithological components
are gneisses and intrusives of the Misuku Belt, representing the south-eastern extension of the
Ubendian Mobile Belt of south-western Tanzania into Malawi.
On a more local scale, the licence area is comprised of a suite of quartzite rocks, pegmatitic rocks
and amphibole gneisses that intrude into the basement gneissic rocks forming the wall rock of the
project area. The lithologies have a general NW-SE trend and are dipping west / south-west at very
steep angles ranging from 600 to 850.
The presence of base metals and other related metal mineralisation is evident in the pegmatitic rocks
and quartz zone (quartzite) group. The quartzite unit have clear malachite and azurite coexisting with
sulphides minerals indicating the presence of copper and other base metals.
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Surveillance/Initial Reconnaissance Work Done
1. Surveillance Site Visit
Four samples (Table 1) were collected on a recent reconnaissance visit to the site. The visit targeted
an anomaly which was identified using a combination of geology and aeromagnetic data (Figures 3A
& B). The samples were collected on a mineralised quartzite zone, which displayed disseminated
mineralisation of malachite and azurite with sulfides (Figure 4, A-D). These samples were analysed
using an Olympus Avanta Portable XRF (pXRF) machine.
Table 1: Samples collected on surveillance site visit Cu analytical results (pXRF-based)
Sample ID
KARS022
KARS022B
KARS022C
KARS022D
Longitude
8898932
8898988
8898977
8898992
Latitude
594735.6
594714.62
594714.15
594715.84
Altitude (m) Cu (%) – pXRF Reading
577.49
1.4
572.51
6.1
581.93
7.5
576.97
7.8
Results showed elevated Cu grades ranging from 1.4% to 7.8% Cu (Table 1 & Figure 3B). These
samples were collected on a 60cm thick zone of an exposed portion of a 40 – 50m long quartzite
zone.
The samples will be sent to SGS Randfontein laboratory in South Africa for a standard XRF analytical
procedure to verify the Cu grades and other minerals grades obtained from the pXRF.
Figure 3: A – Geology of the Karonga Licence & B – Aeromagnetic signature of the Karonga
Licence
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Figure 4: A – D: Sampled Points and Copper Mineralisation in Karonga Licence Area
2. Hyperspectral Data Analysis and Interpretation
Historical satellite imagery data has been acquired, re-processed and interpreted by an experienced
spectral data analyst from Dirt Exploration. This is intended to assist with probability mapping of
several minerals including Cu mineralisation.
The data is extracted by spectral unmixing of the Sentinel-2 VNIR (Visible & Near Infrared) and SWIR
(Short Wave Infrared) satellite imagery. Sentinel-2 VNIR/SWIR imagery is the highest spatial
resolution satellite imagery available with 10m resolution.
Using a geochemical exploration technique called Mobile Metal Ions (MMI) the extracted and unmixed
spectral bands provide some diagnostic mineral responses in the regolith (overburden / outcrop rock
material) above a buried mineral deposit.
In the case of Cu mineralisation, six endmembers are anomalous over Cu occurrences: azurite,
gypsum, illite, hypersthene, beryl and jarosite.
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Figure 5B shows azurite probability mapping and the anomalous areas for Cu mineralisation are
highlighted in red. These anomalies correlate relatively well with the aeromagnetic data in Figure 3B,
and the sampled points fall within the northern NE-SW trending anomaly.
Figure 5: A – Imagery of the Karonga Licence & B – Hyperspectral Probability Mapping of Azurite
Mineralisation
The results of the spectral data analysis combined with the aeromagnetic data signatures and
confirmed by the four geochemical samples analysed using the pXRF machine shows the potential of
the Karonga licence area for copper mineralisation and possible occurrence of a copper deposit that
requires to be investigated further.
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Next Steps
•
Further exploration work is currently planned to follow the anomalies identified in the surveillance
activities, including geochemical analysis of the four collected samples at SGS Randfontein
laboratory in South Africa to verify and validate the results obtained from the pXRF machine;
•
Detailed geological mapping of the licence area; and
•
Detailed geochemical sampling of surface outcrop rock chips, soils and where possible trenching
to be considered.
The outcome of the activities above will lead to target generation for a future drill program, which will
in turn be used for mineral resource and reserve estimations.
-ENDSThis announcement has been authorised by the Board of DY6.
More information
Mr Dan Smith
Mr John Kay
Mr Luke Forrestal
Chairman
Director & Company Secretary
Investor Relations
dan.smith@dy6metals.com
john.kay@dy6metals.com
+61 411 479 144
Competent Persons Statement
The Information in this announcement that relates to exploration results, mineral resources or ore reserves
is based on information compiled by Mr Allan Younger, who is a Member of the Australasian Institute of
Mining and Metallurgy. Mr Younger is a consultant of the Company. Mr Younger has sufficient experience
which is relevant to the style of mineralisation and type of deposits under consideration and to the activity
that he is undertaking to qualify as a Competent Person as defined in the 2012 edition of the `Australian
Code for Reporting Exploration Results, Mineral Resources and Ore Reserves’ (the JORC Code). Mr
Younger consents to the inclusion of this information in the form and context in which it appears in this
announcement. Mr Younger holds shares in the Company.
Mr Younger has not yet visited the site or conducted an in-depth due diligence of the data presented in this
announcement. Mr Younger confirms the information in this market announcement is an accurate
representation of the available data for the exploration areas mentioned herein, but that further investigation
is ongoing.
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Cautionary Statement
Visual observations of the presence of rock or mineral types and abundance should never be considered
a proxy or substitute for petrography and laboratory analyses where mineral types, concentrations or
grades are the factor of principal economic interest. Visual observations and estimates also potentially
provide no information regarding impurities or deleterious physical properties relevant to valuations. At this
stage it is too early for the Company to make a determinative view on the abundances of any of these
minerals. These abundances will be determined more accurately through petrography, assay, and XRF
analysis. The observed presence of known copper-bearing minerals does not necessarily equate to copper
mineralisation. It is not possible to estimate the concentration of copper by visual estimation and this will
be determined by chemical analysis.
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JORC Code, 2012 Edition – Table 1 report template
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
Criteria
JORC Code explanation
Commentary
Sampling
techniques
• Nature and quality of sampling (eg cut channels, random chips, or
specific specialised industry standard measurement tools appropriate
to the minerals under investigation, such as down hole gamma
sondes, or handheld XRF instruments, etc). These examples should
not be taken as limiting the broad meaning of sampling.
• Include reference to measures taken to ensure sample representivity
and the appropriate calibration of any measurement tools or systems
used.
• Aspects of the determination of mineralisation that are Material to the
Public Report.
• In cases where ‘industry standard’ work has been done this would be
relatively simple (eg ‘reverse circulation drilling was used to obtain 1
m samples from which 3 kg was pulverised to produce a 30 g charge
for fire assay’). In other cases more explanation may be required,
such as where there is coarse gold that has inherent sampling
problems. Unusual commodities or mineralisation types (eg
submarine nodules) may warrant disclosure of detailed information.
• Drill type (eg core, reverse circulation, open-hole hammer, rotary air
blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple
or standard tube, depth of diamond tails, face-sampling bit or other
type, whether core is oriented and if so, by what method, etc).
• Method of recording and assessing core and chip sample recoveries
and results assessed.
• Measures taken to maximise sample recovery and ensure
representative nature of the samples.
• Whether a relationship exists between sample recovery and grade
and whether sample bias may have occurred due to preferential
loss/gain of fine/coarse material.
• Nature and Quality of sampling – Fresh non-weathered random rock
chip samples have been collected from outcrops within a small part of
the licence area.
• Sample Representivity- Over 2kg of rock chip samples taken on each
sampling point to ensure sufficient material to be crushed and
homogenised to prepare a sample to be sent to the laboratory for
analysis.
• These samples are representative of the potential copper
mineralisation in the licence area.
• Determination of Mineralisation - Samples were analysed in the field
using an Olympus Vanta handheld / portable XRF (pXRF) machine
• The samples will be prepared and dispatched to an accredited SGS
laboratory in South Africa, for standard XRF analytical assaying to
verify results obtained from the pXRF machine.
Drilling
techniques
Drill sample
recovery
• No drilling undertaken and therefore no drilling techniques are being
reported
• No drilling undertaken and therefore no drill sample recoveries are
being reported
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Criteria
JORC Code explanation
Commentary
Logging
• Whether core and chip samples have been geologically and
geotechnically logged to a level of detail to support appropriate
Mineral Resource estimation, mining studies and metallurgical
studies.
• Whether logging is qualitative or quantitative in nature. Core (or
costean, channel, etc) photography.
• The total length and percentage of the relevant intersections logged.
• If core, whether cut or sawn and whether quarter, half or all core
taken.
• If non-core, whether riffled, tube sampled, rotary split, etc and
whether sampled wet or dry.
• For all sample types, the nature, quality and appropriateness of the
sample preparation technique.
• Quality control procedures adopted for all sub-sampling stages to
maximise representivity of samples.
• Measures taken to ensure that the sampling is representative of the in
situ material collected, including for instance results for field
duplicate/second-half sampling.
• Whether sample sizes are appropriate to the grain size of the material
being sampled.
• The nature, quality and appropriateness of the assaying and
laboratory procedures used and whether the technique is considered
partial or total.
• For geophysical tools, spectrometers, handheld XRF instruments, etc,
the parameters used in determining the analysis including instrument
make and model, reading times, calibrations factors applied and their
derivation, etc.
• Nature of quality control procedures adopted (eg standards, blanks,
duplicates, external laboratory checks) and whether acceptable levels
of accuracy (ie lack of bias) and precision have been established.
• The Rock chip samples were geologically logged, in terms of
lithological name, visible mineralogy and texture and coordinates
recorded.
• High resolution photographs of the samples were taken.
• The verification of significant intersections by either independent or
alternative company personnel.
• The use of twinned holes.
• No drilling undertaken therefore no verification of sampling
intersections required.
Subsampling
techniques
and sample
preparation
Quality of
assay data
and
laboratory
tests
Verification
of sampling
• No sub-sampling has been undertaken since they were
reconnaissance samples and therefore no reporting of sub-sampling
techniques and sample preparation.
• The pXRF analysis technique is considered partial.
• Details and parameters of the pXRF machine used:
o Make & Model: Olympus Vanta C Series
o Profile used is Geochem 3 (comprising of 3 test beams)
o Reading Times for:
• Beam 1: 20 seconds
• Beam 2: 20 seconds
• Beam 3: 10 seconds
o Calibration Factors Applied & Derivation
• No calibration or user factor applied
• Accuracy is within +/- 3 sigma
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Criteria
JORC Code explanation
and
assaying
• Documentation of primary data, data entry procedures, data
verification, data storage (physical and electronic) protocols.
• Discuss any adjustment to assay data.
• Accuracy and quality of surveys used to locate drill holes (collar and
down-hole surveys), trenches, mine workings and other locations
used in Mineral Resource estimation.
• Specification of the grid system used.
• Quality and adequacy of topographic control.
• Data spacing for reporting of Exploration Results.
• Whether the data spacing and distribution is sufficient to establish the
degree of geological and grade continuity appropriate for the Mineral
Resource and Ore Reserve estimation procedure(s) and
classifications applied.
• Whether sample compositing has been applied.
• Whether the orientation of sampling achieves unbiased sampling of
possible structures and the extent to which this is known, considering
the deposit type.
• If the relationship between the drilling orientation and the orientation
of key mineralised structures is considered to have introduced a
sampling bias, this should be assessed and reported if material.
• The measures taken to ensure sample security.
Location of
data points
Data spacing
and
distribution
Orientation
of data in
relation to
geological
structure
Sample
security
Audits or
reviews
• The results of any audits or reviews of sampling techniques and data.
Commentary
• Albeit not to be used in Mineral resource Estimation, all rock chip
sample locations determined by handheld GPS using WGS 84 datum
in Zone 36S.
• Sample types and spacing used in this exercise are not designed to
be used in an MRE because the sampling was of a reconnaissance
nature.
• No compositing has been applied.
• Sampling was of a reconnaissance nature only and was designed to
achieve unbiased sampling.
• No drilling being reported.
• Samples were bagged in the field, labelled and transported to DY6
Metals core & sample processing warehouse by DY6 staff.
• No audits or reviews have been undertaken by DY6 Metals staff.
Section 2 Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)
Criteria
JORC Code explanation
Commentary
Mineral
tenement and
• Type, reference name/number, location and ownership including
agreements or material issues with third parties such as joint
• New Granted Exploration Licence No EL0782/24 for Karonga.
Licence is wholly owned by DY6 Metals Ltd through Malawian vehicle
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Criteria
JORC Code explanation
land tenure
status
ventures, partnerships, overriding royalties, native title interests,
historical sites, wilderness or national park and environmental
settings.
• The security of the tenure held at the time of reporting along with any
known impediments to obtaining a licence to operate in the area.
• Acknowledgment and appraisal of exploration by other parties.
Exploration
done by other
parties
Geology
Drill hole
Information
• Deposit type, geological setting and style of mineralisation.
• A summary of all information material to the understanding of the
exploration results including a tabulation of the following information
for all Material drill holes:
o easting and northing of the drill hole collar
o elevation or RL (Reduced Level – elevation above sea level in
metres) of the drill hole collar
o dip and azimuth of the hole
o down hole length and interception depth
o hole length.
• If the exclusion of this information is justified on the basis that the
Commentary
Green Exploration Ltd (GEL).
• No known impediments to jeopardise licence to operate.
• The tenement area has been prospected and intermittently mined by
artisanal miners in other areas for other commodities especially
gemstones.
•
On a regional scale, the Karonga area is associated with a series of
NW-SE and N-S trending ridges with metamorphic Basement complex
rocks commonly identified as windows within the Karroo System which
overlies the basement. The Karroo System units are typically
sandstones with carbonaceous shale formations.
•
On a local scale, the licence area is comprised of a suite of quartzite
rocks, pegmatitic rocks and amphibole gneisses that intrude into the
basement gneissic rocks forming the wall rock of the project area. The
lithologies have a general NW-SE trend and are dipping west / southwest at very steep angles ranging from 600 to 850.
•
Disseminated mineralisation style observed in malachite, azurite and
sulphides. The presence of base metals and other related metal
mineralisation is evident in the pegmatitic rocks and quartz zones
(quartzite) group. The quartzite unit have clear malachite and azurite
coexisting with sulphides minerals indicating the presence of copper
and other base metals.
• No drilling undertaken and therefore no drillhole information is being
reported.
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Criteria
Data
aggregation
methods
JORC Code explanation
•
•
•
Relationship
between
mineralisation
widths and
intercept
lengths
•
Diagrams
•
Balanced
reporting
•
Other
substantive
exploration
data
•
Further work
•
•
•
•
information is not Material and this exclusion does not detract from
the understanding of the report, the Competent Person should clearly
explain why this is the case.
In reporting Exploration Results, weighting averaging techniques,
maximum and/or minimum grade truncations (eg cutting of high
grades) and cut-off grades are usually Material and should be stated.
Where aggregate intercepts incorporate short lengths of high grade
results and longer lengths of low grade results, the procedure used
for such aggregation should be stated and some typical examples of
such aggregations should be shown in detail.
The assumptions used for any reporting of metal equivalent values
should be clearly stated.
These relationships are particularly important in the reporting of
Exploration Results.
If the geometry of the mineralisation with respect to the drill hole
angle is known, its nature should be reported.
If it is not known and only the down hole lengths are reported, there
should be a clear statement to this effect (eg ‘down hole length, true
width not known’).
Appropriate maps and sections (with scales) and tabulations of
intercepts should be included for any significant discovery being
reported These should include, but not be limited to a plan view of
drill hole collar locations and appropriate sectional views.
Where comprehensive reporting of all Exploration Results is not
practicable, representative reporting of both low and high grades
and/or widths should be practiced to avoid misleading reporting of
Exploration Results.
Other exploration data, if meaningful and material, should be reported
including (but not limited to): geological observations; geophysical
survey results; geochemical survey results; bulk samples – size and
method of treatment; metallurgical test results; bulk density,
groundwater, geotechnical and rock characteristics; potential
deleterious or contaminating substances.
The nature and scale of planned further work (eg tests for lateral
extensions or depth extensions or large-scale step-out drilling).
Diagrams clearly highlighting the areas of possible extensions,
Commentary
• No data aggregation methods are being used.
• No drilling undertaken and therefore no mineralisation widths have
been reported
• Location maps of project and samples taken are within the release
with location details contained.
• The reporting of exploration results is considered balanced by the
competent person. The locations of samples are included in this
release.
• Regional airborne magnetic data from the government has been used
for target generation and is included within the release.
• Reprocessed historical hyperspectral Sentinel-2 NVIR and SWIR
satellite data has been used for target generation and is included
within the release.
• Geochemical analysis of the four collected samples at SGS
laboratory in South Africa to verify and validate the results obtained
from the pXRF machine.
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Criteria
JORC Code explanation
including the main geological interpretations and future drilling areas,
provided this information is not commercially sensitive.
Commentary
• Detailed geochemical sampling and geological mapping
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