Option to acquire Karonga Lithium Project
Released
Released
Announcement PDF
ASX Announcement
ASX:DY6
3 January 2024
Option to acquire 80% of Karonga Lithium Project
HIGHLIGHTS
DY6 has secured a 6-month option to acquire an 80% interest in the Karonga Lithium
Project located in northern Malawi, a granted licence covering a total area of 39km2
The licence borders the Company’s recent exclusive prospecting license
application at Karonga (for a combined ~75km2)
Reconnaissance field work at the Karonga Lithium Project identified a number of
pegmatites of up to 500m metres in length with the potential to host lithium
mineralisation
Rock chip samples taken from the Karonga Lithium Project include visually observed
spodumene and lithium micas (lepidolite)*. Samples have been despatched for
laboratory analysis in Johannesburg
The Company is planning on undertaking a detailed geological mapping and sampling
program across the Project early in 2024
DY6 Metals Ltd (ASX: DY6) (“DY6”, the “Company”), a strategic metals explorer targeting Heavy Rare
Earths (HREE) and Niobium (Nb) in southern Malawi, is pleased to announce that it has entered into an
exclusive option to acquire an 80% interest in the Karonga Lithium Project (granted licence EPL0659)
(the Project) located in northern Malawi.
The granted licence covers ~39km2 and adjoins the Company’s recent license application at
Karonga (together, both licences cover ~75km2).
The Company’s geological team recently undertook a reconnaissance field visit at the Karonga Lithium
Project. Ten reconnaissance rock chip samples from four outcrops were collected and have been
submitted for laboratory analysis in South Africa.
The Company’s CEO, Mr Lloyd Kaiser said: “We are pleased to have reached an agreement to secure
an 80% interest in the Karonga Lithium Project in northern Malawi. The project adjoins our recently applied
for prospecting license near Karonga, adding scale potential. Importantly, field reconnaissance at the
project identified a number of pegmatites – up to 25 metres in width and 500 metres in length – with
visually observed lithium-bearing minerals. We await assay results from the reconnaissance rock chip
sampling and look forward to getting back on the ground in the coming weeks.”
+ Cautionary Statement: The Company notes that pegmatites contain varying abundances of typical LCT pegmatite non-Li-bearing minerals,
predominantly feldspar, quartz, muscovite mica (as a group also referred to as Aplite) and accessory tourmaline. Investors should note that while LCT
pegmatites are a known host for accessory lithium bearing minerals such as spodumene, it is also known that this is not a universal association. 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 pegmatite does not necessarily equate to lithium mineralisation. It is not possible to estimate the
concentration of mineralisation by visual estimation and this will be determined by chemical analysis.
Registered Office
Level 8, 99 St Georges Terrace
Perth WA 6000
P: +61 8 9486 4036
E: info@dy6metals.com
dy6metals.com
Karonga Lithium Project
Figure 1. Location map of Karonga Li Project, granted licence EPL0659, which adjoins the Company’s
recent licence application (APL0526)
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Figure 2. Topographical map of the Karonga Lithium Project
The Project is located about 440km north of the capital Lilongwe (refer Figure 2) and covers a total area
of approximately 39.27km2. The area can easily be accessed using Karonga-Chitipa M1 Road turning to
the west at Kasikisi School signpost along the M1 Road.
The Karonga area is associated with a series of 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 shales formations.
Pegmatite float material was noted in the Mwesa River which cuts NE-SW through the area. The sampling
focused on pegmatite intrusions that are traceable for up to 500m in length. In hand specimen, these
pegmatites have high percentages of albite, microcline and occasional K-feldspar with associated
muscovite and biotite micas. The pegmatites are within the basement complex as biotite schist and
gneisses with medium sized dark coloured micas. Quartz-feldspathic granulites were also observed.
Exposures of these were found with copper coatings on joints and weathered reddish brown cuprite was
observed.
Within the pegmatites, light greenish to purplish elongated feldspar-like crystals were observed, using a
hand lens and tentatively identified as spodumene*. Samples were collected and some had structures
which shows shearing effect depicting the structure of spodumene (refer Table 1).
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Figure 3 & 4: pegmatite sample and float with prismatic structures and interpreted to be spodumene
Next steps
DY6 is finalising a maiden exploration program at the Karonga Lithium Project, which will consist of
detailed geological mapping, rock chip and soil sampling. This program, anticipated to take up to 4-weeks,
will commence in January 2024.
Transaction terms
DY6 has entered into a binding term sheet (BTS) with Afro Gifts Mining Limited (Afro Gifts), an
unrelated party, to acquire 80% of the Karonga Lithium Project (Project) (Acquisition). The Company
has paid Afro Gifts a non-refundable cash payment of A$25k to secure an exclusive 6-month period to
undertake due diligence of the Project.
Subject to successful due diligence, the consideration payable for the proposed Acquisition is:
•
•
•
•
$37,500 in cash on completion;
$37,500 payable in DY6 shares on completion (based on the 5-day VWAP prior to the completion
date),
DY6 to free-carry Afro Gifts 20% interest in the Project until completion of a prefeasibility study
(PFS); and
following completion of the PFS, DY6 to loan-carry Afro Gifts interest in the Project at the Australian
Bank Bill Swap rate plus 8%, to be repaid out of profits of the joint venture.
The BTS is conditional on due diligence to be conducted on Afro Gifts and the Project to the satisfaction
of the Company, any shareholder or regulatory approvals or third-party consents required by DY6 and
there being no material breach of the Afro Gifts warranties prior to completion.
The BTS also contains other terms customary for a transaction of this nature.
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Pegmatites – Information relating to observed pegmatites:
1.
The nature of the pegmatite minerals
Pegmatites observed in the area are identified by the presence of weathered quartz, some flakes
of weathered biotite, muscovite and phlogopite micas and kaolinised feldspars which forms reddish
brown colour on the ground.
The pegmatites identified were classified as zoned type with well-defined zones; wall rock,
intermediate and a core as the centre. The wall zone is made up of a fine-grained mass of quartz,
feldspar, micas and partly superficial deposit of kaolinized feldspar materials. Intermediate zone is
made up of feldspars between the core at the centre and the wall-rock zone and were made up of
matrix of medium grained quartz, feldspar and muscovite with occasional garnets. Feldspars
usually occur in large partly kaolinized crystals of micro perthite with a pinkish colour.
At the core, large quartz crystals measuring more than 5cm in width, inter-growth with pinkish
microcline to white Albite feldspars and large books of various micas types were observed.
2. Minerals observed
The minerals visually observed in the outcrops of the observed pegmatites are as follows:
• Na/Ca Feldspar
• K-Feldspar
• Quartz
• Mica – including muscovite, biotite and other mineral species
• Spodumene
• Lepidolite
3. Estimates of abundance of minerals observed
The estimates of mineral abundance may not be accurate due to the low number of reconnaissance
sampling done. Please note that the outcrops of the observed pegmatites were weathered and
therefore estimations may be inaccurate. Lab analysis will be a broad analysis for associated
elements given that lithium can be very mobile in the weathered environment.
Cautionary Statement: In relation to the disclosure of visual mineralisation, the Company cautions that visual estimates of
mineral abundance should never be considered a proxy or substitute for laboratory analysis. 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 pegmatite does not necessarily equate to
lithium mineralisation. It is not possible to estimate the concentration of mineralisation by visual estimation and this will be
determined by chemical analysis.
The Company notes that pegmatites contain varying abundances of typical LCT pegmatite non-Li-bearing minerals,
predominantly feldspar, quartz, muscovite mica (as a group also referred to as Aplite) and accessory tourmaline. Investors
should note that while LCT pegmatites are a known host for accessory lithium bearing minerals such as spodumene, it is also
known that this is not a universal association.
-ENDSThis announcement has been authorised by the Board of DY6.
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More information
Mr Lloyd Kaiser
Mr John Kay
Mr Luke Forrestal
CEO
Director & Company Secretary
Investor Relations
lloyd.kaiser@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.
Cautionary Statement
The Company notes that pegmatites contain varying abundances of typical LCT pegmatite non-Li-bearing
minerals, predominantly feldspar, quartz, muscovite mica (as a group also referred to as Aplite) and
accessory tourmaline. Investors should note that while LCT pegmatites are a known host for accessory
lithium bearing minerals such as spodumene, it is also known that this is not a universal association.
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 pegmatite does not necessarily equate to lithium mineralisation. It is
not possible to estimate the concentration of mineralisation by visual estimation and this will be
determined by chemical analysis.
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Technical References
Carter, G.S. & Bennet, J.D. (1973). The geology and mineral resources of Malawi. Bulletin Geological
Survey Malawi, 6.
Černý, P., (1991b). Rare-element granitic pegmatites, part I—Anatomy and internal evolution of pegmatite
deposits: Geoscience Canada, v. 18, no. 2.
Dill, H.G. (2007). A review of mineral resources in Malawi: with special reference to aluminium variation
in mineral deposits. Journal of Africa Earth Sciences.
Gaskell, J.L. (1973). The geology of the Mzimba area. Bulletin of Geological Survey of Malawi, 37.
Licence Details
Tenement No.
EPL0659
Tenement Holder
Afro Gifts Mining Limited
Size (km2)
39.27
Grant Date
22/04/2022
Expiry Date
21/04/2025
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Table 1 – Sample Outcrop Locations and Details for Karonga Lithium Project
Outcrop ID
25KAW001A
Sample
ID
Eastings
(UTM,
Zones
36S)
590016
25KAW001B
S01,
S02,
S03,
S04,
GS1
S05,
S06
S07
25KAW001B
25KAW001B
Northings
(UTM, Zones 36S)
8886992
Outcrop/
Boulder/
Float
Outcrop
Rock Type
Pegmatite
Grain
Size
(cm)
Quartz
(%)
2-5
3 - 40
590064
8887068
Outcrop
Pegmatite
1
45 - 60
590078
8887107
Outcrop
Pegmatite
1-2
30 - 60
S08A
590078
8887107
Outcrop
Pegmatite
1-2
20 - 40
25KAW001B
S08B
590078
8887107
Outcrop
Pegmatite
1-2
30 - 60
25KAW001B
GS2
590064
8887068
Float
Pegmatite
4
25
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Ca/N
a
Feld
spar
(%)
K
Feld
spar
(%)
Mica
Other
Minerals
(%)
(%)
45 94
3–
10
430
0–1
15 45
15 60
10 50
15 60
60
4
0
4
5–
20
5 -20
10
5-20
0
4
5-20
0
1
4
0
Spodumene
%
1-5%
0
0-1%
0–1%
1–5%
5–10%
5-10%
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.
• 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
• Reconnaissance random rock chip samples have been collected
intermittently from exposures within the region.
• These are hoped to be representative of the styles of pegmatites
intrusives within the area.
• The samples will not be representative of any mineralisation
potentially within the pegmatites.
Drilling
techniques
Drill sample
recovery
Logging
9
• No drilling is being reported
• No drilling is being reported
• No drilling is being reported
Criteria
Sub-sampling
techniques
and sample
preparation
Quality of
assay data
and
laboratory
tests
Verification of
sampling and
assaying
Location of
data points
JORC Code explanation
Commentary
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 verification of significant intersections by either independent or
alternative company personnel.
• The use of twinned holes.
• 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.
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• No sub-sampling has been undertaken
• Portion of the reconnaissance samples are being prepared for
petrographic study with the balance to be dispatched to a commercial
laboratory for 4 acid ICP analysis.
• No drilling being reported
• All locations determined by handheld GPS using WGS 84 datum in
Zone 36S.
Criteria
JORC Code explanation
Commentary
Data spacing
and
distribution
• 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.
• Sample type and spacing are not designed to be used in an MRE.
• No compositing has been applied.
• The results of any audits or reviews of sampling techniques and data.
• No audits or reviews have been undertaken by DY6 Metals staff.
Orientation of
data in
relation to
geological
structure
Sample
security
Audits or
reviews
• Sampling was of a reconnaissance nature only and was designed to
achieve unbiased sampling.
• No drilling being reported.
• Samples were bagged in the field and delivered to the Malawi
Geological Survey by DY6 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
land tenure
status
• Type, reference name/number, location and ownership including
agreements or material issues with third parties such as joint
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.
• The Exploration Licence is owned 100% by Afro Gifts Mining Limited.
• Deposit type, geological setting and style of mineralisation.
• The project area occurs within orthogneisses, schist and granulite
units in the Mesoproterozoic Irumide orogenic belt that extends from
around Lundazi in eastern Zambia into Malawi; this belt hosts several
Exploration
done by other
parties
Geology
11
• The tenement areas have been prospected and intermittently mined
by artisanal miners.
Criteria
JORC Code explanation
Commentary
granitic pegmatite swarms which are mined for gemstones including
beryl varieties and other related metal deposit types.
Drill hole
Information
Data
aggregation
methods
Relationship
between
mineralisation
widths and
intercept
lengths
Diagrams
Balanced
reporting
• 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
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
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• No drilling is being reported.
• No aggregation methods are being used.
• No mineralisation widths have been reported
• Location maps of projects are within the release with relevant
exploration contained.
• The reporting of exploration results is considered balanced by the
competent person. The locations of samples are included in this
release.
Criteria
Other
substantive
exploration
data
Further work
JORC Code explanation
Commentary
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,
including the main geological interpretations and future drilling areas,
provided this information is not commercially sensitive.
13
• No other exploration to report
• Further surface sampling, mapping and drilling of potential targets
once tenure is granted.
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