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CONICO LTD Capital/Financing Update 2022

Sep 18, 2022

64678_rns_2022-09-18_31c38696-9cee-4d65-80d7-75495e9e7b06.pdf

Capital/Financing Update

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ASX Announcement

19[th] September 2022

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MESTERSVIG EXPLORATION UPDATE
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Highlights

Diamond drilling at the Mestersvig project in Greenland has concluded, with a total of 10 holes completed.

  • Eight holes have intercepted disseminated, heavily disseminated and/or matrix sulphides, including:

  • BKDD003: 3.3 metres of disseminated sulphides from 205.0 metres,

  • BKDD004: 15.5 metres of disseminated and heavily disseminated sulphides from 211.5 metres,

  • SBDD003: 4.5 metres of matrix sulphides from 134.1 metres (see Figure 1), and

  • SBDD005: 1.4 metres of heavily disseminated sulphides from 120.5 metres.

  • Zn, Pb & Cu sulphides logged in core: Consistent with mineralisation at the historic Blyklippen Mine (within the licence area) and Sortebjerg Prospect.

  • First assays: Expected within 6-8 weeks , including zinc, lead, copper, and silver.

  • Prospective horizon; Remains open along strike , with a further 9 km of un-drilled strike on the Blyklippen-hosted vein, and a further 14 km of untested mineralised quartz vein-bearing faults throughout the project area.

  • Nuldal Reconnaissance Exploration: Additional lead mineralisation at surface hosted in veins, with a massive galena outcrop up to 1 m thick.

Drill core is now in the process of being transported from Greenland to continental Europe, where it will then be sampled and submitted for assaying with results expected back within 6-8 weeks. All samples will be assayed for zinc, lead, copper and silver.

Conico Ltd ABN 49 119 057 457 Level 15, 197 St George’s Terrace Perth, WA 6000 Australia

+61 (0)8 9282 5889 @conico_ltd [email protected] @ConicoLtd www.conico.com.au conico-limited

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Mestersvig Project

Conico Limited ( ASX: CNJ ) ( Conico or the Company ) is pleased to provide an update on exploration at the 100% owned Mestersvig Project in East Greenland, where drilling concluded on 14[th] September, having commenced on 27[th] July 2022. A total of 10 diamond drill holes were completed, targeting vein-hosted Zn-Pb-Cu-Ag. Eight holes intersected zones of disseminated, heavily disseminated and/or matrix sulphides. The drill campaign was testing for extensions to the known mineralised vein system identified at Blyklippen and Sortebjerg approximately 13 km along strike from one another.

Drilling was conducted using two diamond drill rigs owned by Conico and operated by Cartwright Drilling Inc., with accommodation at an exploration camp located on site. The drill rigs and associated equipment will remain on site until the commencement of the proposed 2023 field season.

Executive Director, Guy le Page, commented :

“Mineralisation at Mestersvig is readily identifiable via visual investigation, with most holes penetrating the anticipated vein system that is known to contain zinc, lead, copper and silver mineralisation. It is pleasing to see that the mineralised vein continues along strike, proving our modelling to be correct and we await the assay results with anticipation.”

Holes that intercepted the modelled mineralised vein exhibit similar mineralisation to the historic Blyklippen Mine, consisting of vein-hosted disseminated sulphides, heavily disseminated sulphides and/or matrix sulphides (see Appendix 1), including:

  • BKDD003: 3.3 metres of disseminated sulphides from 205.0 metres,

  • BKDD004: 15.5 metres of disseminated sulphides from 211.5 metres,

  • SBDD003: 4.5 metres of matrix sulphides from 134.1 metres, and

  • SBDD005: 1.4 metres of heavily disseminated sulphides from 120.5 metres.

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Figure 1: Sulphide mineralisation in core photography (highlighted in purple) for SBDD003. See Appendices 1 & 2 for a mineralised intercept summary and the sulphide logging guide.

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NULDAL RECONNAISSANCE

Follow up reconnaissance at the Nuldal Prospect identified a mineralised vein running roughly parallel with Blyklippen, trending N-S. It contains several galena-bearing outcrops, and also hosts silver mineralisation. Two rock chip samples were taken here in 2020, grading 60.66% lead, 0.91% copper & 236 g/t silver, and 69.47% lead, 0.77% copper & 282 g/t silver (Conico ASX Announcement 8[th] December 2020). Field observations this year have found a one metre wide occurrence of massive galena with disseminated chalcopyrite in outcrop (Figure 2, and Figure 4 for location).

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Figure 2: Massive galena outcropping at the Nuldal Prospect (for scale, the white marker is 12.0 cm long). For location, see Figure 4.

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BACKGROUND & TECHNICAL DISCUSSION

Local geology is dominated by Carboniferous, Permian and Triassic sediments intruded by Palaeogene dolerite sills and dykes. The area is bordered by the Palaeogene Werner Bjerge alkaline igneous complex to the south, and a major regional fault to the west, beyond which sits the Caledonian fold belt. The Mestersvig graben is the most conspicuous feature of the project area, which occurs in a 15-20 km-long anticlinal fold structure amongst widespread faulting. The graben is 4 km wide and 12 km long, with the western graben fault being the host to the Blyklippen Mine that produced 545,000 tons of ore at 9.3% lead and 9.9% zinc between 1956-1962.

Mineralisation occurs as fault controlled epithermal lead-zinc veins with accessory silver and copper. Mineralisation is hosted within quartz veins that range in thickness from 2-50 m, from surface to unknown depth. Veins are mostly associated with the border faults of the Mestersvig graben, but also occur distally and are widespread throughout the project area. Ore minerals are typically massive sphalerite and galena, with minor chalcopyrite and barite.

The Sortebjerg Prospect is situated approximately 13 km south of the Blyklippen mine and is a mineralised vein that has been subject to historic drilling. It is interpreted to be the same mineralised western graben fault that hosts the Blyklippen mine, and contains similar Zn-PbAg mineralisation, with the addition of chalcopyrite.

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Conico Ltd MEL
Conico Ltd Mel-S
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Figure 3: Location map for the Mestersvig Project, highlighting the location of the Blyklippen and Sortebjerg Prospects.

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Figure 4: Plan view of Mestersvig 2022 and historic drill collars. Red star shows the location of the 1- metre-thick massive galena outcrop. Pink diamond shows the location of 2020 rock chip sample grading 69.47% lead, 0.77% copper & 282 g/t silver.

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Figure 5: Close up view of Sortebjerg prospect showing historic drill holes with downhole assay intercepts graded by colour, and 2022 drill holes. Fault trace coincides with the mineralised vein.

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APPENDIX 1: MESTERSVIG SUMMARY LOGS - DRILL HOLE SULPHIDE MINERALISATION

Hole ID From
(m)
To
(m)
Length
(m)
Host lithology Mineralisation style
BKDD001 269.6 269.9 0.3 Quartz vein Disseminated (Sl) 5.0%
BKDD003 201.0 202.0 1.0 Quartz-feldspar vein Disseminated (Gn,Sl) 5.0%
205.0 208.3 3.3 Quartz-feldspar vein Disseminated (Gn,Sl) 5.0%
209.2 209.3 0.1 Quartz vein Matrix(Gn)25.0%
BKDD004 196.7 197.0 0.3 Quartz-feldspar vein Disseminated (Gn,Sl,Cp) 3.0%
211.5 218.4 6.9 Quartz vein Disseminated (Gn)2.0%
218.4 227.0 8.6 Quartz vein Heavily disseminated (Gn,Sl) 7.0%
230.9 231.1 0.2 Quartz vein Matrix(Cp)25.0%
BKDD005 154.5 155.1 0.6 Quartz vein Matrix(Gn)25.0%
SBDD001 78.7 79.2 0.5 Quartz vein Matrix(Gn,Sl)25.0%
79.9 80.5 0.6 Quartz vein Disseminated (Cp)2.0%
86.9 88.7 1.8 Quartz vein Disseminated (Sl) 5.0%
SBDD002 103.3 104.5 1.2 Quartz vein Heavily disseminated (Sl)10.0%
149.4 149.5 0.1 Quartz vein Heavily disseminated (Sl)10.0%
182.0 182.5 0.5 Quartz vein Disseminated (Cp)2.0%
SBDD003 134.1 138.6 4.5 Quartz vein Matrix(Sl,Cp)25.0%
140.1 140.2 0.1 Quartz vein Matrix(Sl)25.0%
142.0 142.9 0.9 Quartz vein Matrix(Sl, Cp)27.0%
161.4 162.0 0.6 Quartz vein Heavily disseminated (Sl,Cp)11.0%
SBDD005 120.5 121.9 1.4 Quartz vein Heavily disseminated (Sl)10.0%

Gn = Galena. Sl = Sphalerite. Cp = Chalcopyrite. Sulphides & metal contents are not directly correlated; Assays are required to determine metal content (e.g., Zn, Pb, Cu, Ag).

APPENDIX 2: FIELD GUIDE FOR THE LOGGING OF SULPHIDE MODE, TYPE, AND PERCENTAGE

Sulphide Mode Precent Range (visually estimated)
Weakly disseminated < 1%
Disseminated 1 -5 %
Heavily disseminated 5- 20 %
Matrix 20- 40 %
Net textured 20- 40 %
Semi-massive 40-80 %
Massive > 80%

*Sulphide estimates undertaken by visual observation with assays results still pending

APPENDIX 3: MESTERSVIG COLLAR LOCATION AND DETAILS

Hole ID Northing Easting Elevation Depth Dip Azimuth Comments
BKDD001 8011842 598099 337 339 m -50 238 Diamond
BKDD002 8012329 597754 432 105m -55 238 Diamond
BKDD003 8012432 597722 424 299m -55 238 Diamond
BKDD004 8012350 597735 436 263m -55 238 Diamond
BKDD005 8010206 599011 328 221 m -55 245 Diamond
SBDD001 8003147 601247 280 115m -65 240 Diamond
SBDD002 8003147 601247 280 200m -75 240 Diamond
SBDD003 8003330 601183 294 206m -60 240 Diamond
SBDD004 8003621 601013 276 200m -60 278 Diamond
SBDD005 8003418 601133 294 164 m -60 240 Diamond

Coordinates are given in WGS84 UTM Zone 26N.

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APPENDIX 4: BLYKLIPPEN DRILL TRACES

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APPENDIX 5: SORTEBJERG DRILL TRACES

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APPENDIX 6: HISTORIC SORTEBJERG COLLAR LOCATION AND DETAILS

Hole ID
BH001
BH002
BH003
BH004
BH005
BH006
BH007
BH008
BH010
BH012
BH014
BH016
SB017
SB018
SB019
Northing Easting Elevation Depth Dip Azimuth Drill Type Company Drill
**Year **
8001753 601944 255 167.4 -48 248 Diamond Nordisk Mineselskab 1952
8001801 601920 255 160.9 -45 248 Diamond Nordisk Mineselskab 1952
8001722 601875 275 66.5 -45 248 Diamond Nordisk Mineselskab 1952
8001763 601839 280 67.5 -45 248 Diamond Nordisk Mineselskab 1952
8001190 602146 149 92 -50 248 Diamond Nordisk Mineselskab 1952
8002564 601525 190 57.1 -50 248 Diamond Nordisk Mineselskab 1952
8000236 602680 30 78.3 -55 248 Diamond Nordisk Mineselskab 1952
8002520 601546 200 67.7 -50 248 Diamond Nordisk Mineselskab 1952
8002478 601575 210 82 -50 248 Diamond Nordisk Mineselskab 1952
8002433 601605 220 76.1 -50 248 Diamond Nordisk Mineselskab 1952
8002384 601628 230 74.6 -55 248 Diamond Nordisk Mineselskab 1952
8002443 601627 220 96 -65 248 Diamond Nordisk Mineselskab 1952
8002671 601451 214 47 -50 220 Diamond Ironbark ZincLtd 2011
8002671 601451 214 80 -70 220 Diamond Ironbark ZincLtd 2011
8002855 601374 245 122 -70 220 Diamond Ironbark ZincLtd 2011

APPENDIX 7: HISTORIC SORTEBJERG SIGNIFICANT INTERCEPTS

Hole ID From (m) To (m) Interval (m) Copper (%) Lead (%) Zinc (%)
BH001 40.0 45.17 5.17 1.77 12.58
BH001 132.52 133.4 0.88 0.2 21.7
BH002 122.75 124.3 1.55 0.02 15.87
BH003 13.15 14.2 1.05 7.13
BH003 21.57 22.52 0.95 0.02 7.15
BH003 52.83 55.8 2.97 0.29 1.73 11.08
BH008 33.77 34.63 0.86 0.32 9.82
BH010 40.2 41.75 1.55 0.83 7.34 18.21
BH012 46.15 49.25 3.1 3.04 8.45 12.62
BH016 91.01 91.91 0.9 5.37 0.03 1.98
SB017 8.25 10.75 2.5 0.07 0 16.1
SB018 6.4 6.9 0.5 0.06 0 11.45
SB018 21.8 22.8 1 0.02 0.22 17.95
SB019 53.8 54.8 1 0.03 0 17.33
SB019 61.8 62.1 0.3 0.11 0 5.65
SB019 84.2 84.6 0.4 0.05 0 13.35

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Competent Persons Statement

The information contained in this report relating to exploration results relates to information compiled or reviewed by Thomas Abraham-James, a non-executive director of Conico Ltd. Mr. Abraham-James has a B.Sc Hons (Geol) and is a Chartered Professional (CPGeo) and Fellow of the Australasian Institute of Mining and Metallurgy (FAusIMM). Mr. Abraham-James has sufficient experience of relevance to the styles of mineralisation and the types of deposit under consideration, and to the activities undertaken to qualify as a Competent Person as defined in the 2012 edition of the Joint Ore Reserve Committee (JORC) “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Mr. Abraham-James consents to the inclusion in this report of the matters based on information in the form and context in which it appears.

Disclaimer

The interpretations and conclusions reached in this report are based on current geological theory and the best evidence available to the authors at the time of writing. It is the nature of all scientific conclusions that they are founded on an assessment of probabilities and, however high these probabilities might be, they make no claim for complete certainty. Any economic decisions that might be taken based on interpretations or conclusions contained in this report will therefore carry an element of risk. This report contains forward-looking statements that involve several risks and uncertainties. These forward-looking statements are expressed in good faith and believed to have a reasonable basis. These statements reflect current expectations, intentions or strategies regarding the future and assumptions based on currently available information. Should one or more of the risks or uncertainties materialise, or should underlying assumptions prove incorrect, actual results may vary from the expectations, intentions and strategies described in this report. No obligation is assumed to update forwardlooking statements if these beliefs, opinions, and estimates should change or to reflect other future developments.

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THE FOLLOWING TABLES ARE PROVIDED TO ENSURE COMPLIANCE WITH THE JORC CODE (2012 EDITION) FOR THE REPORTING OF EXPLORATION RESULTS.

MESTERSVIG PROJECT

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 (e.g.,
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 (e.g., ‘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 (e.g., submarine
nodules) may warrant disclosure of
detailed information.

Sampling
was
conducted
using
standard
industry
practices
with
diamond drilling.

Drill-holes were angled to optimally
intersect the interpreted contact with
the mineralised vein.

Mineralisation in all drill-holes has not
been quantitively determined and is
awaiting sampling and assay. The
determination in this report is qualitative,
based on visual observation made by
the on-site geologist.
Drilling
techniques

Drill type (e.g., core, reverse circulation,
open-hole hammer, rotary air blast,
auger, Bangka, sonic, etc) and details
(e.g., 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).

Wireline
diamond
drilling
using
a
75.7mm diameter drill bit and standard
tube. The core has not been orientated
but has been surveyed using a Reflex EZ-
GYRO. The drill rigs are Zinex A1 heli-
portable fly rig operated by Cartwright
Drilling Inc.
Drill
sample
recovery

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.

All drill core has been geotechnically
logged with core recovery measured
per drill core run (3m).

The drill crew was notified of the target
depth and likelihood of intersecting
sulphides,
accordingly
they
eased
pressure on the drill bit from that depth
onward to minimise the chance of core
destruction. All drill core was then
placed in trays with lids to ensure that no
core was lost during transportation from
the drill site to core logging facility. The
drill core was then reconstructed into
continuous runs by the geologist. Depths
were checked against depths indicated
on the core blocks.

It is not possible to assess whether a
relationship
exists
between
sample
recovery and grade as no assays have
been conducted to date.

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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.

All drill core has been geologically and
geotechnically logged by a qualified
geologist to a level of detail that
supports appropriate Mineral Resource
estimation,
mining
studies
and
metallurgical studies.

The logging is qualitative. All drill core
was photographed.

Logging
of
diamond
core
was
qualitative and diamond core was
photographed.

Alldrill-holeshave been loggedin full.
Sub-sampling
techniques and
sample
preparation

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.

Not applicable as no sampling has been
undertaken.
Quality of assay
data
and
laboratory tests

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
(e.g.,
standards,
blanks,
duplicates, external laboratory checks)
and whether acceptable levels of
accuracy (i.e., lack of bias) and
precision have been established.

Not applicable as no assaying has
occurred.
Verification
of
sampling
and
assaying

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.

Not applicable as no assaying has
occurred.
Location of data
points

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.

Drill hole collar locations are pegged
out by the supervising geologist using
handheld GPS, accurate to +/-3m. This
has been considered as sufficiently
accurate for the purposes of drillhole
accuracy.

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Criteria **JORC Code explanation ** Commentary

The drilling rigs were sighted using a
compass. Drill hole angle was set using
an inclinometer placed on the drill mast
prior to collaring the hole.

Down-hole surveying was completed at
nominal intervals using a gyro Reflex
tool, providing sufficient down hole
accuracy
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.

Not applicable as the drill holes were
targeting specific geological targets.

No sample compositing has been
applied, due to no samples having
been taken to date.
Orientation
of
data in relation
to
geological
structure

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.

Drilling was designed perpendicular to
the strike of the main mineralised
structures targeted for this program. All
reported intervals are however reported
as downhole intervals only.

No drilling orientation and/or sampling
bias have been recognised in the data
at this time.
Sample security
The measures taken to ensure sample
security.

The drill core was kept on site which is
considered remote and highly secure. It
is now in the process of being shipped in
a secure container to Longland´s core
facilityin Portugal.
Audits or reviews
The results of any audits or reviews of
sampling techniques and data.

No audits or reviews have been carried
out at this time

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SECTION 2 – REPORTING OF EXPLORATION RESULTS

(Criteria in this section apply to all succeeding sections.)

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.

The Mestersvig Project is wholly
within Mineral Exploration Licences
2020/64 & 2021/24, located on the
east coast of Greenland. They are
held 100% by Longland Resources
Ltd, a wholly owned subsidiary of
Conico Ltd.

Both Mineral Exploration Licences lie
within the Northeast Greenland
National Park.

The tenements are in good standing.
Exploration done
by other parties

Acknowledgment and appraisal of
exploration by other parties.

Historic data mentioned in this report
refers
to
exploration
and
exploitation undertaken by historic
mining and exploration companies
operating the Project from 1952 to
2011. The previous workers include
Nordisk
Mineselskab
A/S
and
Ironbark Zinc Ltd.

The historic data referenced in this
report includes diamond drilling,
surface sampling andmining.
Geology
Deposit type, geological setting and
style of mineralisation.

The type is likely that of a Mississippi
Valley Type (MVT) Pb-Zn-Ag deposit
where mineralisation has been re-
mobilised by fluids along faults.
Mineralisation is present as massive
galena-sphalerite, with associated
chalcopyrite.
Mineralisation
is
present within quartz-barite veins,
hosted
within
sandstone
and
conglomerates.
Known
mineralisation is within the fault and
vein systems associated with a
Devoniangrabensystem.
Drill hole
Information

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.

Drill hole information for the drilling
discussed in this report is listed in
Appendices 1, 3, 6 & 7.
Data
aggregation
methods

In
reporting
Exploration
Results,
weighting
averaging
techniques,
maximum and/or minimum grade
truncations (e.g., cutting of high
grades) and cut-off grades are usually
Material and should be stated.

Not applicable as no sampling or
assaying has occurred.

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Criteria **JORC Code explanation ** Commentary

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.
Relationship
between
mineralisation
widths
and
intercept lengths

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
(e.g., ‘down hole length, true width not
known’).

The geometry of the mineralisation
with respect to the drill-hole angle is
not known. All reported lengths are
in reference to down-hole length,
true width not known.
Diagrams
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.

Appropriate plans and sections
have been included in the body of
this report.
Balanced
reporting

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.

All results material and relevant to
the subject of this announcement
have been presented.
Other
substantive
exploration data

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.

Historic drill core from previous
underground and surface drilling at
Blyklippen and Sortebjerg is present
on site. The core has not been
reviewed by the Company at this
moment
in
time,
therefore
no
comment can be made as to
whether it is meaningful.

Regional aeromagnetic data was
acquired
by
the
Greenland
Government and covers the licence
area. It was flown at 400m line
spacing
and
altitude
of
approximately 300m.

In 2020, Longland Resources Ltd
acquired ground gravity data over
a portionof MEL 2020/64.
Further work
The nature and scale of planned
further work (e.g., 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.

Further work has been discussed in
the
context
of
phased
drilling
campaigns, based on the outcome
of active drilling campaigns.

For diagrams, refer to Figures 3, 4 &
5.

18 Conico Ltd ASX: CNJ F:BDD