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CORAZON MINING LIMITED Regulatory Filings 2017

Feb 12, 2017

64747_rns_2017-02-12_6b9fe1e4-fca7-4dda-84fc-6c096e4fccc9.pdf

Regulatory Filings

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ASX Announcement 13[th] February

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The Manager – Company’s Announcements Australian Securities Exchange

STRONG CONDUCTORS IDENTIFIED IN DOWNHOLE EM AT FRASER LAKE COMPLEX

  • Two off-hole conductors identified by downhole electro-magnetic (EM) survey

  • Strong response of up to 10,000 siemens indicative of massive sulphide mineralisation.

  • Conductors are approximately 340m from massive sulphide intersected in recent drilling - yet to be tested with EM.

  • Follow-up ground EM is underway to fully explore the target area for additional conductors – completion expected this week.

  • Phase I drilling completed – first assays due this month.

  • Phase II drilling proposed to commence late February

Corazon Mining Limited (ASX: CZN) (“Corazon” or “the Company”) is pleased to announce the results of a downhole electro-magnetic (DHEM) geophysical survey conducted on recently completed drilling within the Fraser Lake intrusive complex (“FLC”) at the Lynn Lake Nickel-Copper-Cobalt Project in Canada.

Downhole EM Survey Results

Results from the DHEM survey of drill hole FLC-2017-002 indicates the presence of an off-hole, high CT (conductivity thickness) conductor with a strong response of more than 5,000 siemens, located 120 metres to the north-northeast of the hole (Figure 1). Anomalous conductivity starts at about 340 metres below surface and extends down to at least 480 metres. Late channel responses indicate very high CT values in excess of 10,000 siemens.

A possible second conductive body has also been observed at a shallower depth of about 250 metres down hole. The DHEM data for this feature is in the process of analysis and interpretation.

The conductors identified are approximately 340 metres from the massive sulphide identified in drill hole FLC-2017-003 (ASX announcement 6[th] February, 2017) and are likely to represent separate features. All, however, are located within the same high-chargeability IP anomaly (the Matrix HCIP feature) targeted by Corazon’s drilling and are coincidental with a > 30 m/s IP (induced polarisation) chargeability maxima within this zone.

Based on the strength of the conductive anomalies, their interpreted depth, and the depth of massive sulphide intersected in drilling, the Company has commenced a ground EM survey. This survey will - cover the full extent of the targeted high-chargeability anomaly (Figure 1 Matrix HCIP Anomaly), attempting to better define potential massive magmatic sulphides at depth within this feature.

Corazon Mining Limited | Level 1, 329 Hay Street | Subiaco 6008 | Western Australia PO Box 8187 | Subiaco East 6008 | T +61 8 6142 6366 | F +61 8 6210 1871 | [email protected]

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The ground EM survey undertaken is a Transient Electromagnetic survey utilising SQUID sensors capable of detecting massive sulphides at depths in excess of 500 metres. Data collection from this survey is expected to be completed this week.

DHEM completed on the FLC drilling utilised EMIT’s Digiatlantis B-Field BHTEM system. The Atlantis is a unique three-component borehole tool for the low-noise measurement of magnetic (B) fields in TEM, MMR and other electrical geophysical surveys or geomagnetic applications. DHEM surveys completed consisted of an in-hole loop (LoopA) and an out-hole loop (LoopB).

Although the anomalies identified from the DHEM surveys are extremely encouraging, it is recognised the FLC has numerous xenoliths of sulphidised sediments (VMS deposits and sulphidised roof pendants) that can generate strong EM conductors. Hole FLC-2017-001 targeting a VTEM conductor anomaly identified one such feature within the FLC (ASX announcement 6[th] February, 2017).

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Figure 1 Geophysical Features and Targets . Aeromagnetic Total Field image, with the main IP anomaly (Matrix HC IP), IP Survey outline and drill hole locations (FLC-2017-*). A gravity high anomaly to the south of the FLC intrusion is believed to be the source of mantle material that feed the intrusion. The main IP anomaly trends off the IP surveyed area and is in alignment with the interpreted neck/feeder zone of the intrusion.

ASX Announcement

Page | 2

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Phase 1 Drill Programme Complete

Corazon has completed its phase 1 drilling programme at FLC. This programme comprised five (5) holes for approximately 1,600 metres of core drilling, testing high priority geophysical anomalies within the FLC.

An update on the status of the drilling programme was provided in the Company’s ASX release dated 6[th] February 2017. Since that report, drill holes FLC-2017-003 and FLC-2017-005 have been completed to depths of 603 metres and 203 metres respectively.

Drill hole FLC-2017-003 tested the main IP chargeable anomaly trend (the Matrix HCIP anomaly - Figure 1). Sulphide content throughout the hole graded from weakly disseminated to strongly disseminated, interstitial to matrix and massive style of mineralisation, dominated by pyrrhotite (iron sulphide), with chalcopyrite (copper) and pentlandite (nickel). Massive to semi-massive sulphide was intersected over four and a half (4.5) metres (388 to 392.5 metres downhole - ASX announcement 6[th] February, 2017) within a larger zone of approximately 25 metres of strong sulphide mineralisation.

Drill hole FLC-2017-005 (Figure 1) was drilled some distance from the main IP target, testing a coincident IP/magnetic anomaly within the Eastern Magnetic Domain on the southern side of the FLC. This hole was drilled to a depth of 203 metres and has not identified the source of the IP anomaly (which the Company believes to be deeper). The lithologies intersected include magnetite bearing gabbros, explaining the makeup of the Eastern Magnetic Zone within the FLC. The IP anomalies within this part of the FLC remain prospective, however they have a lower order of priority compared with the Matrix HCIP trend.

Next Steps

With the completion of Corazon’s initial phase of drilling at the FLC, the Company is now undertaking planning and targeting for Phase 2 Drilling, which is expected to commence later this month. Further detail on drill targets will be provided in due course.

First assay results from Phase 1 Drilling are expected to be available later this month and all assay results are on track to be received by the end of March 2017.

ASX Announcement

Page | 3

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Figure 2 – Project Location and Geology . Interpreted Geology – Emslie, R.R. and Moore, J.M. 1961. Manitoba Mines Branch, Publication 57-4. Datum UTM Zone 14 (NAD83). Lynn Lake is considered an historically significant nickel mine and remains the fourth largest nickel producing districts in Canada, despite the mine closing in 1976. The Fraser Lake Complex is twice as large as Lynn Lake and in many facets is geologically identical to Lynn Lake.

END .

For further information visit www.corazon.com.au or contact:

Brett Smith James Moses Managing Director Media and Investor Relations Corazon Mining Limited Mandate Corporate P: +61 (8) 6142 6366 M: +61 (0) 420 991 574 E: [email protected] E: [email protected]

ASX Announcement

Page | 4

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Competent Persons Statement

The information in this report that relates to Exploration Results and Targets is based on information compiled by Mr Brett Smith, B.Sc Hons (Geol), Member AusIMM, Member AIG and an employee of Corazon Mining Limited. Mr Smith has sufficient experience that is relevant to the style of mineralization and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Mr Smith consents to the inclusion in the report of the matters based on this information in the form and context in which it appears.

Canadian geologist Dr Larry Hulbert has been engaged by Corazon to manage the collation of past exploration information and the definition of new targets at Lynn Lake. Dr Hulbert has extensive knowledge of the Lynn Lake district and over 40 years’ experience in Ni-Cu-PGM exploration and research. Dr Hulbert is one of North America's foremost experts on magmatic sulphide deposits and would qualify as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”.

Dr. Hulbert has authored numerous professional papers, was the recipient of the Barlow Medal from CIM in 1993, a Robinson Distinguished Lecturer for the Geological and Mineralogical Association of Canada for 2001-2002, and in 2003 received the Earth Sciences Sector Merit Award from Natural Resources Canada.

This announcement tables results of a downhole electromagnetic (DHEM) survey completed by Discovery Int’l Geophysics Inc, (“Discovery”) based in Saskatchewan, Canada. Discovery are an accredited geophysical consultancy with extensive experience in this form of geophysical technique targeting this style of mineralisation.

The results of the BHEM survey have been audited and interpreted by the Company’s consultant geophysicist and ‘expert’, Martin St. Pierre (P. Geophysicist) from St Pierre Geoconsultant Inc., based in British Colombia, Canada.

Forward Looking Statements

This announcement contains certain statements that may constitute “forward looking statement”. Such statements are only predictions and are subject to inherent risks and uncertainties, which could cause actual values, results, performance achievements to differ materially from those expressed, implied or projected in any forward looking statements.

ASX Announcement

Page | 5

Table 1: Checklist of Assessment and Reporting Criteria

13[th] February, 2017

- - Core Drilling and Downhole EM Fraser Lake Complex Lynn Lake Project, Canada.

Section 1 Sampling Techniques and Data

Criteria JORC Code explanation JORC Code explanation Commentary
Sampling Nature and quality of sampling (eg cut channels, random Drill Core Sampling
techniques chips, or specific specialised industry standard
measurement tools appropriate to the minerals under
investigation, such as down hole gamma sondes, or
Half core is sampled on the basis of geology. Minimum interval 200mm,
maximum interval sampled is 1.5m.
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
The drill core is cut using an industry standard core saw. Individual samples
are collected in labelled calico bags. Sample weights are typically between 2kg
and 5kg.
measurement tools or systems used.
Aspects of the determination of mineralisation that are
To date, no assay results have been received.
Material to the Public Report.
In cases where ‘industry standard’ work has been done this
would be relatively simple (eg ‘reverse circulation drilling Downhole Electromagnetic Survey
was used to obtain 1 m samples from which 3 kg was
pulverised to produce a 30 g charge for fire assay’). In other Details of and techniques are presented within this
cases more explanation may be required, such as where report in the section titled “Other Substantive
there is coarse gold that has inherent sampling problems. Exploration Data”.
Unusual commodities or mineralisation types (eg submarine
nodules) may warrant disclosure of detailed information.
Drilling Drill type (eg core, reverse circulation, open-hole hammer, NQ drill core is being undertaken by Vital Drilling Services using an Atlas
techniques rotary air blast, auger, Bangka, sonic, etc) and details (eg Capco CS 1000. Rod lengths are 3m (NM – Atlas Capco), with core run
core diameter, triple or standard tube, depth of diamond lengths also of 3m.
tails, face-sampling bit or other type, whether core is
oriented and if so, by what method, etc).
Depth capacity of this drill rig is approximately 700 metres.
Drill sample Method of recording and assessing core and chip sample Recovery of the core drilling is excellent (+99%).
recovery 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.

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Table 1: Checklist of Assessment and Reporting Criteria

13[th] February, 2017

- - Core Drilling and Downhole EM Fraser Lake Complex Lynn Lake Project, Canada.

Criteria JORC Code explanation JORC Code explanation Commentary
Logging Whether core and chip samples have been geologically and Core is geologically logged and tested for magnetic susceptibility &
geotechnically logged to a level of detail to support conductivity.
appropriate Mineral Resource estimation, mining studies
and metallurgical studies.
Whether logging is qualitative or quantitative in nature. Core
A hand-held XRF (Niton) is used for the purposes of assisting with mineral
identification and metal content.
(or costean, channel, etc) photography.
The total length and percentage of the relevant intersections
logged.
Sub- If core, whether cut or sawn and whether quarter, half or all Drill core is cut and typically half core is taken as a sample for analysis.
sampling
techniques
and sample
core taken.
If non-core, whether riffled, tube sampled, rotary split, etc
and whether sampled wet or dry.
Quality control measures include core duplicates (1/4 core), CANMET certified
reference materials (standards) and silica blanks.
preparation
For all sample types, the nature, quality and
appropriateness of the sample preparation technique.
Quality control procedures adopted for all sub-sampling
Samples are transported to TSL Laboratories in Saskatoon for sample
preparation, including total sample crushing and pulverising to 80% passing 75
microns.
stages to maximise representivity of samples.
Measures taken to ensure that the sampling is Sample analysis is completed by ACME Laboratories in Vancouver.
representative of the in situ material collected, including for
instance results for field duplicate/second-half sampling. Sample security is overseen by Aurora Geosciences personnel until shipment
Whether sample sizes are appropriate to the grain size of from site to the Laboratory. Shipment and transport is overseen by Corazon's
the material being sampled. Lynn Lake site manager.
Quality of The nature, quality and appropriateness of the assaying and Once sample preparation was completed by TSL Laboratories, they are
assay data laboratory procedures used and whether the technique is transported to ACME Laboratories in Vancouver for analysis. A multi-element
and considered partial or total. analysis is completed using ICP-MS with a 4 acid digest (30 gram samples). A
laboratory For geophysical tools, spectrometers, handheld XRF total of 37 elements are tested for (ACME method code AQ525).
tests instruments, etc, the parameters used in determining the
analysis including instrument make and model, reading
Both TSL and ACME are accredited Canadian laboratories.
times, calibrations factors applied and their derivation, etc. To date, no assay results have been received.
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.

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Table 1: Checklist of Assessment and Reporting Criteria

13[th] February, 2017

- - Core Drilling and Downhole EM Fraser Lake Complex Lynn Lake Project, Canada.

Criteria JORC Code explanation JORC Code explanation Commentary
Verification The verification of significant intersections by either Drilling is being managed by experienced geological personnel from Aurora
of sampling independent or alternative company personnel. Geosciences and overseen by Corazon’s consultant and nickel sulphide expert
and The use of twinned holes. Dr Larry Hulbert.
assaying Documentation of primary data, data entry procedures, data
verification, data storage (physical and electronic) protocols.
To date, no assay results have been received.
Discuss any adjustment to assay data.
Location of Accuracy and quality of surveys used to locate drill holes Drill holes were positioned using a hand-held Trimble GEOXH GPS and Reflex
data points (collar and down-hole surveys), trenches, mine workings Northfinder APS.
and other locations used in Mineral Resource estimation.
Specification of the grid system used.
The survey data is recorded in real-world grid system NAD 83 Zone 14.
Quality and adequacy of topographic control.
Data spacing Data spacing for reporting of Exploration Results. Drill holes are widely space and targeted at individual geophysical anomalies.
and
distribution
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
This exploration is reconnaissance in nature and as such will not result in the
immediate definition of a mineral resource estimation.
estimation procedure(s) and classifications applied.
Whether sample compositing has been applied.
Orientation Whether the orientation of sampling achieves unbiased Drill holes are widely space and targeted at individual geophysical anomalies.
of data in
relation to
sampling of possible structures and the extent to which this
is known, considering the deposit type.
Azimuths and dips are variable, dependent on the targets being tested.
geological If the relationship between the drilling orientation and the No bias for the sampling has been established.
structure orientation of key mineralised structures is considered to
have introduced a sampling bias, this should be assessed
and reported if material.
Sample The measures taken to ensure sample security. Sample security is overseen by Aurora Geosciences personnel until shipment to
security the Laboratory.
Individual samples are collected in calico bags, before being bundled together
into sealed in large PVC bags and sealed with security tags for transport to the
laboratory.
Shipment and transport of the samples to TSL Laboratories is overseen by

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Table 1: Checklist of Assessment and Reporting Criteria

13[th] February, 2017

- - Core Drilling and Downhole EM Fraser Lake Complex Lynn Lake Project, Canada.

Criteria JORC Code explanation JORC Code explanation Commentary
Corazon’s Lynn Lake site manager.
Audits or The results of any audits or reviews of sampling techniques To date, no assay results have been received. As such no audits or reviews
reviews and data. have been conducted.

Section 2 Reporting of Exploration Results

(Criteria listed in the preceding section also apply to this section.)

Criteria JORC Code explanation JORC Code explanation Commentary
Mineral Type, reference name/number, location and ownership The Fraser Lake Complex (FLC) is predominantly covered in an agreement
tenement including agreements or material issues with third parties between Mr Peter Dunlop and Corazon Mining Limited whereby Corazon has
and land such as joint ventures, partnerships, overriding royalties, the option to acquire 100% of the project by meeting certain conditions. This
tenure status native title interests, historical sites, wilderness or national agreement was originally announced within a Company ASX announcement
park and environmental settings. dated 18 May 2010, with the most recent amendments to this agreement
The security of the tenure held at the time of reporting along presented in a Company ASX announcement dated 29 July 2015.
with any known impediments to obtaining a licence to
operate in the area.
The tenure includes multiple Mineral Claims as defined by the Provincial
Government of Manitoba. All claims are currently in good standing.
Corazon Mining works closely with First Nation groups and several government
organizations responsible for mining and the environment. Work Permits are
currently in place for the FLC and covers activities such as ground geophysics
and land-based drilling.
Exploration Acknowledgment and appraisal of exploration by other Where exploration has been completed by other parties, those parties have
done by parties. been referenced in this document or within previous ASX announcements by
other parties the Company. In particular refer to CZN ASX announcement dated 11 April
2016.
Geology Deposit type, geological setting and style of mineralisation. Magmatic nickel-copper-cobalt sulphide deposits associated within
mafic/ultramafic intrusive rock (gabbro related).
Volcanogenic massive sulphide (VMS) deposits. Zinc dominant +/- lead,
copper, silver and gold.

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Table 1: Checklist of Assessment and Reporting Criteria

13[th] February, 2017

- - Core Drilling and Downhole EM Fraser Lake Complex Lynn Lake Project, Canada.

Criteria
JORC Code explanation
Commentary
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 Survey Data
Hole ID
East
North
RL
Dip
Azim
Depth
(m)
FLC-2017-01
370646
6295799
354
-60
020
83
FLC-2017-02
370915
6296179
359
-86
334
605
FLC-2017-03
370735
6296079
348
-87
334
603
FLC-2017-04
371423
6295986
351
-86
156
107
FLC-2017-05
372382
6295787
362
-86
156
203
Survey data presented in real-world grid system NAD 83 Zone 14
Data
aggregation
methods

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.
No data aggregation has been reported in this announcement.
Relationship
between
mineralisatio
n 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 (eg
‘down hole length, true width not known’).
Typical Lynn Lake Ni-Cu-Co Magmatic Sulphide Deposits
Known nickel-copper-cobalt magmatic sulphide deposits in the Lynn Lake
Mining Centre are typically “pipe-like” in form, averaging between 80m and
120m in strike, 30m to 60m in width and with vertical extents of 100’s of
metres. The historically mined deposits in the Lynn Lake area have been
developed to a maximum depth of approximately 1,100 metres.
Multiple sulphide pipe-like deposits have been identified and mined in the Lynn
Lake area.

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Table 1: Checklist of Assessment and Reporting Criteria

13[th] February, 2017

- - Core Drilling and Downhole EM Fraser Lake Complex Lynn Lake Project, Canada.

Criteria JORC Code explanation JORC Code explanation Commentary
Diagrams Appropriate maps and sections (with scales) and tabulations Appropriate diagrams have been included in the announcement.
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.
Balanced Where comprehensive reporting of all Exploration Results is This report tables early findings with respect to core drilling currently being
reporting not practicable, representative reporting of both low and undertake within the FLC at Lynn Lake.
high grades and/or widths should be practiced to avoid
misleading reporting of Exploration Results.
Other Other exploration data, if meaningful and material, should be The announcement contains results of current and past exploration programs
substantive reported including (but not limited to): geological including surface sampling, drilling, geophysics and geological mapping.
exploration observations; geophysical survey results; geochemical
data survey results; bulk samples – size and method of Information regarding this work has been referenced in this document or within
treatment; metallurgical test results; bulk density, previous ASX announcements by the Company.
groundwater, geotechnical and rock characteristics;
potential deleterious or contaminating substances. Downhole Electromagnetic Survey
This announcement tables results of an BHEM survey completed on drilling
reported within. This work was completed by Discovery Int’l Geophysics Inc,
based in Saskatchewan, Canada. Discovery are an accredited geophysical
consultancy with extensive experience in this form of geophysical technique
targeting this style of mineralisation.
The results of the BHEM survey have been audited and interpreted by the
Company’s consultant geophysicist and ‘expert’, Martin St. Pierre (P.
Geophysicist) from St Pierre Geoconsultant Inc., based in British Colombia,
Canada.
Downhole EM (DHEM) has been completed on the FLC drilling utilizing EMIT’s
Digiatlantis B-Field BHTEM system.
The Atlantis is a unique 3-component
borehole tool for the low-noise measurement of magnetic (B) fields in TEM, MMR
and other electrical geophysical surveys or geomagnetic applications. DHEM
surveys completed consisted of an in-hole loop (LoopA) and an out-hole loop
(LoopB).

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Table 1: Checklist of Assessment and Reporting Criteria

13[th] February, 2017

- - Core Drilling and Downhole EM Fraser Lake Complex Lynn Lake Project, Canada.

Criteria JORC Code explanation JORC Code explanation Commentary
Geophysical equipment consisted of an EMIT DigiAtlantis 3D simultaneous B-
Field BHTEM system; a Geonics BH43-3D dB/dt sequential system, Monex
Geoscope TerraTx-50 Transmitter, Geonics EM-57/67 4.5kW TEM transmitter,
portable generators; down-hole running gear and wire-loops.
Two loops are used per drill hole with transmitter current of 25 to 40 Amps.
The loops have been designed to test the full depth of the drill holes
(approximately) and utilize existing cut lines (completed for the IP geophysical
survey).
Further work The nature and scale of planned further work (eg tests for Results of the BHEM completed will be used to target additional drilling within
lateral extensions or depth extensions or large-scale step- the FLC prospect.
out drilling).
Diagrams clearly highlighting the areas of possible
extensions, including the main geological interpretations and
Assay results from drilling completed at the FLC are expected prior to the end
of March, 2017.
future drilling areas, provided this information is not Extension of the IP geophysics coverage further to the west, covering the
commercially sensitive. interpreted feeder-zone (neck) of the FLC intrusion, is proposed. Due to
access issues, this work will need to be completed this winter.

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