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EASTERN RESOURCES LIMITED Capital/Financing Update 2018

Aug 27, 2018

64824_rns_2018-08-27_8ba99196-0189-4a05-b120-73a3ec8b1b91.pdf

Capital/Financing Update

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ASX Announcement –28 August 2018
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OPTION TO ACQUIRE INTEREST IN

MT COBALT CORRIDOR PROJECT

Highlights

  • Eastern Iron Limited has entered into a Call Option Agreement with Heavy Metal Exploration Pty Ltd to acquire an interest in the Mt Cobalt Corridor Project, which is a copper cobalt sulphide project in NW Queensland.

  • The project is in one of the few areas globally with a history of high grade primary cobalt production

  • Project area covers 161 sub-blocks, with a diverse geology adjacent to and extending out from known cobalt mineralisation, together with cobalt anomalism noted within the tenements.

  • Historic data has identified rock chips samples in copper (up to 5.2% Cu) and stream sediment samples anomalous in cobalt (up to 300ppm Co)

Eastern Iron Limited ACN 126 678 037 ( ASX: EFE ) ( EFE or Company ) is pleased to announce that it has on 28 August 2018 entered into a Call Option Agreement with Heavy Metal Exploration Pty Ltd ACN 163 155 913 to acquire an interest in the Mt Cobalt Corridor Project, located in the Selwyn-Mt Freda district, south of Cloncurry, NW Queensland (the “ Project ”) (Figure 1).

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Figure 1: Mt Cobalt Corridor Project EPMAs coverage.

ACN 126 678 037

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Project Summary

Location and tenures

The Project is located in NW Queensland and comprises 5 EPMAs which covers 161 sub-blocks. The EPMAs are expected to be granted in September 2018, and all have been applied for a period of 5 years. All applications are non-competitive.

EPM No. Permit Name Status Applied For
No. Sub-blocks
26690 Burnham Application 26-Oct-17
53
26715 Mt Carol Application 27-Nov-17
8
26746 Mt Carol Extended Application 2-Jan-18
9
26765 Mt Freda South Application 29-Jan-18
51
26770 Selwyn Range Application 2-Feb-18
40

Geology

The area lies within the largely Palaeo-Proterozoic Eastern Fold Belt of the Mt Isa block in NW Queensland. The area under application consists of outcrop from the Kuridala Formation which hosts a number of major deposits and mineral occurrences in the area, occurring to the west, south west and north west which include Starra (Cu,Au), Mt Dore (Cu,Au,Co), Merlin (Mo,Re), Mt Cobalt (Co,Cu,W), Swan (Cu,Au), Mt Elliott (Cu,Au) mines and The Plume (Cu,Au,Co). Dolerite is regarded as an important localiser of cobalt mineralisation at Mt Cobalt.

There are three main units in Mount Isa. These are the Western Fold Belt including Mt Isa, the Kalkadoon Leichhardt Belt and the Eastern Fold Belt that includes the three mines that produced cobalt, Mt Cobalt, Queen Sally and Success Mines. In the Eastern Fold Belt, cobalt is associated with copper. The Kuridala Formation, essentially consisting of Proterozoic metasediments such as schist, quartzite and dolerite/amphibolite conformable intrusives and its equivalent, the Soldiers Cap Group, is a major host-rock for cobalt in the area. Resources in the Eastern Fold Belt are large, particularly in the Cloncurry area, such as Las Minerale with 16,500t of cobalt, Greenmount with 11,000t of cobalt and Millennium with 4,298t cobalt. A cobalt source with high grade cobaltite ore, such as Mt Cobalt, would be the most economical resource to extract the cobalt from by flotation to produce a concentrate. Such a scenario could exist at The Plume and along the strike of the Mt Cobalt Corridor.

Previous works in the region

Previous works in the region were mainly for copper and gold. However, cobalt mineralization was identified and cobalt production of about 800t at Mt Cobalt occurred in two periods 1919 to 1943 (778 t) and 1996 to 1997 (21.5t).

At Mt Cobalt the most important rock type that hosts the mineralisation is intrusive metadolerite/amphibolite. Cobaltite veins occur in a biotite schist/shear zone near the hanging wall of the amphibolite, close to the contact with quartzite. In 1957, drill hole intercepts included 4 holes that had over 1% cobalt in the ore zone where veins were up to 80 cm wide. The deposit was drilled in the late 1990s but this information is not available.

In the late 1990s an area south of Mt Cobalt was extensively drilled by previous explorers, as an aeromagnetic target called “The Plume”. This area was in alignment with the Mt Cobalt trend. Drilling at The Plume revealed appreciable cobalt mineralisation in several holes. Hole PLRCD-13 which in the 34m (231 – 255m) at 0.11 g/t Au, 0.54% Cu and 0.14% Co included 1m from 243m at 0.29 g/t Au,0.11% Cu and 1.92% Co. The two magnetic trends for both the Mt Cobalt copper-cobalt and Starra copper-gold areas continue south into the Burnham EPMA26690.

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Figure 2: Regional aeromagnetic imagery showing magnetic trends for both the Mt Cobalt copper-cobalt and Starra copper-gold areas continue south into the Burnham application.

EPMAs

Mt Freda South (EPMA26765): 51 sub-blocks

Mt Freda South is approximately 60km south southwest of Cloncurry in northwest Queensland, extending north east from the historic copper mining centers of Kuridala and Mt Freda.

The area consists of a diverse geology located in a north east trend extending from the copper gold historic producers of Kuridala to Mt Freda. Major structures transect the area, the most prominent is the NNW trending Cloncurry Fault which traverses through the north eastern sub blocks of the Mt Freda South EPMA. Copper-gold-cobalt anomalism occurs across the region, however the Mt Freda South EPMA is distinctly under-sampled, particularly for cobalt.

Figure 3 shows that the Mt Freda South area is characterised by diverse Proterozoic geology of the Eastern Succession of the Mt Isa Block. Most of the country rock in the area is mapped as Kuridala Group or equivalents. The Kuridala Group equivalents are hosts for the bulk of the cobalt mineral occurrences in the region including Mt Cobalt, The Plume, Mt Dore, Mobs Lease, Kuridala and Young

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Australian. Another positive feature, in a similar fashion to Mt Cobalt, is that there is a prominent large dyke-like intrusion of dolerite within the equivalents of the Kuridala Group within the Mt Freda South EPMA, particularly at the NE end. Dolerite is regarded as an important localiser of cobalt mineralisation at Mt Cobalt. The older units are intruded by a range of Meso-Proterozoic granites which are represented over several of the sub-blocks of the EPMA. Copper occurrences occur throughout the region, particularly the historic producers of Kuridala and Mt Freda. As with the other mines nearby, there is a general association in the Eastern Fold Belt of copper and cobalt.

Historic data has identified rock chips samples in copper (up to 5.2%) and stream sediment samples anomalous in cobalt (>80ppm Co up to 300ppm Co); anomalous copper (up to 500ppm Cu in streams) and gold (>10ppb Au in streams). Mafic rocks, such as intrusive dolerite are favourable host units for the cobalt mineralisation associated with copper, gold, molybdenum and tungsten in the Selwyn-Cloncurry mining districts and these occur within the Mt Freda South EPMA26765.

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Figure 3: Mt Freda South EPMA 26765 overlain on regional aeromagnetics. Prominent high magnetic ridge and spot highs ae present in most groups of sub-blocks

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Selwyn Range (EPMA26770): 40 sub-blocks

The Selwyn Range application is approximately 120km south southwest of Cloncurry. The Mt Cobalt deposit occurs within 5km of the application area and is the only historical producer of significant quantity of cobalt in the Mt Isa district.

The Selwyn Range EPMA is characterised by diverse Proterozoic geology of the Eastern Succession of the Mt Isa Block. The copper-cobalt trend of the Mt Cobalt Mine transects the sub-blocks of the EPMA. Most of the country rock in the area is mapped as Kuridala Group or equivalents which are hosts for the bulk of the cobalt mineral occurrences in the region. Another positive feature, in a similar fashion to Mt Cobalt, is that there are some large dyke-like intrusions of dolerite within the equivalents of the Kuridala Group within the Selwyn Range EPMA.

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Figure 4: Selwyn Range EPMA overlain on regional aeromagnetics.

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Mt Carol (EPMA26715): 8 sub-blocks, and Mt Carol Extended (EPMA26746): 9 sub-blocks

The Mt Carol application and Mt Carol Extended application are approximately 100km south southwest of Cloncurry in northwest Queensland, a few km to the east of the Starra Mines. Mt Cobalt is less than 5km from Mt Carol Extended.

The area has been mapped as Kuridala Group, the host geological unit for the bulk of the cobalt mineral occurrences, with high stream sediment cobalt geochemistry (80 - 300 ppm Co) occurring within and adjacent to the tenements. Prospective dolerite is a conspicuous unit within the Mt Carol Extended tenement.

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Figure 5: Location of Mt Carol and Mt Carol Extended EPMAs.

Burnham (EPMA26690): 53 sub-blocks

The Burnham application is approximately 140km south of Cloncurry. The project area contains buried aeromagnetic targets suspected of being Mid-Proterozoic Kuridala Formation and Staveley Formation; host rocks of the Starra copper-gold mines to the north; and the copper-cobalt trend of the Mt Cobalt Mine to the north northeast. These aeromagnetic ‘highs’ are also associated with the Osborne copper-gold+/-cobalt Mine, only 20 kms to the southeast. The Plume Cu-Co prospect is approx. 5kms to the tenement.

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The area is highly prospective for copper, gold, cobalt and possibly molybdenum/rhenium mineralization as this type of mineralization has been discovered and mined in rocks to the north northeast (Starra, Mt Cobalt, Merlin, Mt Dore); as well as Osborne Mine to the southeast.

The magnetic trend for both the Mt Cobalt copper-cobalt and Starra copper-gold areas continues south into the Burnham EPMA see Figure 6.

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Figure 6: Burnham EPMA 26690 and southern Mt Cobalt Corridor Tenements.

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Commercial Terms

On 28 August 2018, the Company entered into a Call Option Agreement to acquire a 25% interest in the Project (which includes EPMA 26990, EPMA 26715, EPMA 26746, EPMA 26765 and EPMA 26770 (“ Tenements ”) and all environmental approvals, authorisations, mining information, plant and equipment and other assets relating to the Tenements) owned by Heavy Metal Exploration Pty Ltd ACN 163 155 913 (“ Heavy Metal ”).

The Call Option Agreement also contemplates the Company eventually acquiring a 100% interest in the Project:

  • through meeting staged expenditure requirements under a Farm-In Agreement to be negotiated and entered into by the Company and Heavy Metal in relation to the Project (discussed further below); and

  • by the Company agreeing to enter into a Royalty Deed with Heavy Metal under which the Company will pay a royalty payment to Heavy Metal in respect of certain copper equivalent metal produced from the Tenements (discussed further below).

The Call Option Agreement contains the following key terms:

  • The Company must pay Heavy Metal a call option fee of AUD$10,000 (excluding GST) (“ Call Option Fee ”) by no later than 11 September 2018 to have an exclusive call option to acquire a 25% interest in the Project (“ Call Option ”).

  • If the Company elects to exercise the Call Option, the sale of the 25% interest in the Project is conditional on satisfaction of the following two conditions:

  • the Minister of the Department of Natural Resources and Mines in Queensland giving indicative approval for the transfer of a 25% interest in the Tenements to the Company on terms acceptable to the Company (“ Indicative Approval ”); and

  • the Farm-In Agreement and NSR Royalty Deed being in agreed form.

  • Within 10 business days after the date of receipt of Indicative Approval (“ Indicative Approval Date ”), as consideration for the acquisition of a 25% interest in the Project, the Company must:

  • pay Heavy Metal the amount that is equal to AUD$150,000 (excluding GST) less the Call Option Fee (“ Initial Acquisition Cash Payment ”); and

  • subject to shareholder and any other approvals required under the Corporations Act 2001 (Cth) and the ASX Listing Rules, issue AUD$200,000 worth of fully paid ordinary shares in the Company (“ Shares ”) of which the issue price is to be calculated on the basis of 20-day VWAP prior to the Indicative Approval Date.

  • Within 30 days after the Indicative Approval Date, the Company and Heavy Metal must negotiate the Farm-In Agreement which is expected to include the following key commercial terms:

  • Stage 1: the Company must spend a total of AUD$650,000 on the Project within the first 24 months of the commencement of the Farm-In Agreement (“Stage 1 Period”) in order to acquire an additional 35% interest in the Project.

  • Stage 2: the Company must spend an additional AUD$1,500,000 on the Project within a period of 36 months commencing on the expiry date of the Stage 1 Period in order to acquire an additional 40% interest in the Project.

  • Within 30 days after the Indicative Approval Date, the Company and Heavy Metal must also negotiate the Royalty Deed which is expected to include the following key commercial terms:

  • The Company agrees to pay a royalty payment to Heavy Metal equivalent to the value of 0.5% of net smelter return on copper equivalent metal production capped at 30,000 tonnes of copper equivalent metal produced from the Tenements.

  • The Company is not required to make the royalty payment when copper prices or the price of saleable copper equivalent metal products are at or below USD$6,000 per tonne.

  • The Company has the right to buy back the royalty from Heavy Metal for AUD$1,500,000.

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The Call Option Agreement provides that completion of the Company’s acquisition of a 25% interest in the Project (“ Completion ”) is expected to take place on the date that is 30 days after the Indicative Approval Date (or such other date as agreed by the Company and Heavy Metal in writing).

COMPETENT PERSONS STATEMENT

The information in this release that relates to Exploration Results is based on information prepared by Dr Simon Beams, a full-time employee of geological consultants Terra Search Pty Ltd who are the owners of Heavy Metal Exploration Pty Ltd.

Dr. Beams has BSc Honours and PhD degrees in geology; he is a Member of the Australasian Institute of Mining and Metallurgy (Member #107121) and a Member of the Australian Institute of Geoscientists (Member # 2689). Dr. Beams has sufficient relevant experience in respect to the style of mineralization, the type of deposit under consideration and the activity being undertaken to qualify as a Competent Person within the definition of the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (“JORC Code).

Dr. Beams consents to the inclusion in the report of the matters based on this information in the form and context in which it appears.

INVESTOR INFORMATION

Further information, previous Eastern Iron announcements and exploration updates are available at the News and Reports tab on the Company’s website –www.easterniron.com.au

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Mr Myles Fang Acting Chief Executive Officer T: 02 9906 7551 Mob: 0404 869 892

ASX: EFE

For enquiries on your shareholding or change of address please contact: Boardroom Limited, GPO Box 3993, Sydney NSW 2001, Phone: (02) 9290 960

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APPENDIX 1

JORC Code Table 1 - Mt Cobalt Corridor Project, 28 August 2018.

Section 1: Sampling Techniques and Data

Criteria JORC Code explanation Commentary
Sampling techniques
Nature and quality of sampling (e.g. cut
This report relies on data contained in
channels,
random
chips,
or
specific
reports submitted to the Queensland
specialised industry standard measurement Department of Natural Resources and
tools appropriate to the minerals under Mines as part of the Company Report
investigation, such as down hole gamma System
attaching
to
the
grant
of
sondes, or handheld XRF instruments, etc.) Exploration Permits.
These examples should not be taken as The sampling techniques, where reported,
limiting the broad meaning of sampling. used standard industry approaches. These
include:
Include reference to measures taken to
ensure
sampling
representivity
and
the
appropriate calibration of any measurement
tools or systems used.



1. -80 mesh stream sediment sampling
2. -80 mesh soil sampling
Rock chip sampling
3. Drill sampling involving splitting off a
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 1m samples from which 3kg was
pulverised to produce a 30g 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

sample of material delivered to the top of
the hole during percussion drilling (reverse
circulation & open hole percussion) to
produce a sample for assay accompanied
by geological logging of the sample.
4. Halving of drill core from diamond drilling
to produce an assay sample accompanied
by geological logging of the core.
Assaying of samples was completed by
commercial laboratory methods that were
appropriate at the time the samples were
collected. Whilst it is not possible to
determine the reliability of historical assay
results, no issues arose during compilation
In cases where ‘industry standard’ work has
been done this would be relatively simple (eg
‘reverse circulation drilling was used to obtain
and interpretation of the results that would
suggest that the assay results were not
reasonable.
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.
Drilling techniques Drill type (e.g. core, reverse circulation, open- Historical Reverse Circulation (RC), Open
hole hammer, rotary air blast, auger, Bangka, Hole
Percussion
(OH)
and
Diamond
sonic, etc.) and details (e.g. core diameter, Drilling (DD) cover almost all of the drill
triple or standard tube, depth of diamond tails, types relied on in this report.
face-sampling bit or other type, whether core
is oriented and if so, by what method, etc.)
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.


Recoveries for Percussion (RC and OH)
drill holes were not recorded.
Recoveries for diamond drill core samples
were not usually recorded for holes drilled.
No relationship is evident between sample
recovery and grade

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.

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Criteria JORC Code explanation JORC Code explanation Commentary
Logging Whether core and chip samples have been Geological logging of most of the drill holes
geologically and geotechnically logged to a is available in the Company Report
level of detail to support appropriate Mineral System. No geotechnical logs have been
Resource estimation, mining studies and reported and it is assumed that these were
metallurgical studies not done. Diamond drill hole logs usually
include some structural data.
Whether logging is qualitative or quantitative The logging is generally of a qualitative
in nature. Core (or costean, channel etc.) nature. No core or chip photography is
photography. available in the reports.
The total length and percentage of the For the logs available, logging of all
relevant intersections logged. material has been completed.
Sub-sampling If core, whether cut or sawn and whether As reported above, it is reported that
techniques and quarter, half or all core taken. diamond drill core has been halved as is
sample preparation If non-core, whether riffled, tube sampled, standard practice for most explorers.
rotary split, etc. and whether sampled wet Details of the approach taken for sampling
or dry. of RC drill holes are not available.
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.
Quality of assay data
The nature, quality and appropriateness As reported above, assaying of samples
and laboratory tests of
the
assaying
and
laboratory
was completed by commercial laboratory
procedures
used
and
whether
the
methods that were appropriate at the time
technique is considered partial or total. the samples were collected.
For geophysical tools, spectrometers,
handheld XRF instruments, etc. the Assay data submitted with the reports
parameters used in determining the include some duplicate assaying. It is
analysis including instrument make and unknown in detail what quality control
model, reading times, calibration factors procedures were adopted.
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. _
Verification of The
verification
of
significant
The tenements are still in application stage
sampling and intersections by either independent or and Heavy Metal have not yet undertaken
assaying alternative company personnel. any exploration on the ground.


The use of twinned holes.
Documentation of primary data, data
entry procedures, data verifications, data
storage
(physical
and
electronic)
protocols.
Discuss any adjustment to assay data.
It is evident that most of the historical drill
hole data was captured on paper and
stored on paper. The compilation of that
data in digital form has been overseen by
the competent person with plotting of
surface geochemical and drill data on both
plans and sections in digital form.
No adjustments have been made to
historical sample assay data as there was
no apparent reason for such adjustments.

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Criteria JORC Code explanation JORC Code explanation Commentary
Location of data Accuracy and quality of surveys used to Historical data was often collected on local
points locate drill holes (collar and down-hole grids. Data has been compiled using the
surveys), trenches, mine workings and other appropriate local grid coordinates and grid
locations
used
in
Mineral
Resource
translations have been used to convert
estimation. from one grid to another and to convert
coordinates to MGA coordinates where
required. In the absence of a suitable RL
datum for the area, the SRTM DTM over
the area has been used for height control
and plotting of sections. As Heavy Metal
progresses work in the area it is expected
that a more formal height datum will be
established for the area.
Specification of the grid system used. The area lies within UTM Zone 54, GDA94
datum.
Quality and adequacy of topographic control.
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)

Regional and prospect scale surface
geochemical data spacing is variable.
The
regional
exploration
data
and
prospects within Heavy Metal’s Mt Cobalt
Corridor project area are at an early
exploration stage and no resources have
been estimated for the area.
and classifications applied.
Whether sample compositing has been
applied.
Orientation of data in Whether the orientation of sampling Historical soil grids have been laid out
relation to geological achieves unbiased sampling of possible bearing in mind the general structural
structure structures and the extent to which this is grain in the area. More recent regional
known, considering the deposit type. drilling has been on a grid pattern based
If
the
relationship
between
drilling
on AMG or MGA coordinates. Further
orientation and the orientation of key interpretation
of
the
orientation
of
mineralised structures is considered to mineralized
zones
might
require
a
have introduced a sampling bias, this different orientation of soil grids and drill
should be assessed and reported if holes in future.
material.
Sample security The measures taken to ensure sample No samples are apparently available from the
security. historical sampling undertaken.
Audits or reviews The results of any audits or reviews of No audits or reviews of the sampling
sampling techniques and data. techniques and data have been undertaken at
this time.

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Section 2: Reporting of Exploration Results

Criteria
JORC Code explanation
Commentary
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
and
environmental settings.
The security of the tenure held at the
time of reporting along with any known
impediments to obtaining a license to
operate in the area.

The area reported on lies within the
following
Exploration
Permit
for
Minerals Application areas s, applied
for byHeavyMetal.
EPMA #
26690
Burnham
26715
Mt Carol
26746
Mt Carol Extended
26765
Mt Freda South
26770
Selwyn Range
Heavy Metal is in the process of
notifications to land holders and
native title parties to allow access to
the ground.
Exploration done by
other parties
Acknowledgement
and
appraisal
of
exploration by other parties.

All of the data utilised in this report
has been completed and reported
under the Company Report System
applying
to
granted
Exploration
Permits
for
Minerals
by
the
Queensland Department of Natural
Resources and Mines.
However, compilation in digital form
and interpretation of the results of
that work in digital form has been
overseen by the Competent Person.
Geology
Deposit type, geological setting and style
of mineralisation.
Various mineralisation styles are present
in the Eastern Succession area of the Mt
Isa Block. Copper – Gold- Cobalt
mineralisation is present throughout the
region
hosted
in
Proterozoic
sedimentary,
ironstone,
amphibolite,
dolerite and granitic rock packages.
These deposits are primarily localised
along structures. Intrusive drivers of this
mineralisation
can
be
evident,
but
elsewhere the origin of the hydrothermal
fluid is unknown. Ideas and interpretation
of mineralisation within the Mt Cobalt
Corridor area could change after Heavy
Metal complete their own field work and
interpretation of the results of that work.
Historical mapping has been completed
by BMR/GSQ, Placer, MIM, Cyprus,
Arimco, BHP/Utah and others.
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:

Easting and northing of the drill hole
collar

Elevation or RL (Reduced Level –
elevation above sea level in metres)
of the drill hole collar

Dip and azimuth of the hole
Drilling to date in the Mt Cobalt Corridor
has been sparse in nature and almost
exclusively
shallow
bedrock
drilling.
There are no significant base or precious
metal intersections reported.

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Criteria JORC Code explanation Commentary Commentary
Drill hole information

Down hole length and interception
(cont.) depth

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.
Data aggregation In
reporting
Exploration
Results,

No cut-offs have been applied in
methods weighting
averaging
techniques,
reporting
of
the
soil,
stream
maximum
and/or
minimum
grade
sediment, rock chip and bedrock
truncations (e.g. cutting of high grades) sampling exploration results.
and cut-off grades are usually Material
and should be stated.
Where aggregate intercepts incorporate
No aggregate intercepts have been
short lengths of high grade results and applied in reporting of the soil
longer lengths of low grade results, the sampling exploration results.
procedure used for such aggregation
should be stated and some typical
examples of such aggregations be
shown in detail
The assumptions used for any reporting
No metal equivalents have been
of metal equivalent values should be used in reporting.
clearly stated.
Relationship between

The relationships are particularly

No
‘true widths’ are reported as this
mineralisation widths
important
in
the
reporting
of

depends on a long and comprehensive
and intercept lengths
Exploration Results.
process of interpreting the orientation

If the geometry of the mineralisation

and
nature
of
the
mineralisation
with respect to the drill hole angle is
intersected. This will probably take quite
known, its nature should be reported
some time to complete properly.

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).
Diagrams Appropriate maps and sections (with
Plotting of historic exploration
results
scale) and tabulations of intercepts
with MGA coordinates of surface
stream
should be included for any significant
sediment, soil and rock chip data has
discovery being reported. These should
been regional in nature. Drilling within
include, but not be limited to a plan view
the
EPMA area has not been sufficiently
of
drill
hole
collar
locations
and

dense to plot cross sections.
appropriate sectional views.
Balanced reporting Where comprehensive reporting of all
All
complied sample results appear on
Exploration Results is not practicable,
the
regional geochemical plots.
representative reporting of both low and
high grades and/or widths should be
practised to avoid misleading reporting of
Exploration Results.

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Criteria JORC Code explanation Commentary Commentary
Other substantive Other exploration data, if meaningful and The
results
reported
here
are
exploration data material, should be reported including regional in nature. More sampling is
(but
not
limited
to):
geological
required to fully understand the
observations; geophysical survey results; relationship to mineralisation.
geochemical
survey
results;
bulk
The Heavy Meat exploration team
samples – size and method of treatment; has considerable experience in the
metallurgical test results; bulk density, area and identified the potential
groundwater,
geotechnical
and
rock
locations of cobalt mineralisation
characteristics; potential deleterious or
contaminating substances.
Further work The nature and scale of planned further Proposed further work includes field
work (e.g. test for lateral extensions or work to delineate the distribution of
depth extensions or large-scale step-out copper-gold cobalt mineralisation.
drilling). Particular methods to determine the
potential for mineralisation would
include regional stream sediment
sampling, soil sampling, regional
rock chip sampling, bedrock drilling,
ground magnetics and targeted drill
testing. This work will be carried out
once tenements are granted and
access requirements to the area
have been finalized.
Diagrams clearly highlighting the areas Not yet determined, waiting until
of possible extensions, including the ground truthing can occur after
main
geological
interpretations
and
EPMAs are granted.
future
drilling
areas,
provided
this
information is not commercially sensitive.

15