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S2 RESOURCES LTD Regulatory Filings 2019

Aug 4, 2019

65745_rns_2019-08-04_e8ff2786-64a5-4a99-9476-4e47b42fe2c9.pdf

Regulatory Filings

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Monday 5[th] August 2019

ASX Announcement

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HIGH GRADE GOLD HITS IN FIRST RECON DRILLING AT AARNIVALKEA, FINLAND

Key points

  • First phase of wide spaced reconnaissance drilling completed as an initial test of the Aarnivalkea base of till (BOT) gold anomalous trend in Finland

  • 32 shallow (~80 metre) diamond holes drilled on five broad (240-320 metre) spaced fences covering a 1,200 metre strike length

  • Confirms large new shear system hidden beneath transported glacial cover in previously unexplored district

  • Confirms gold anomalism in wide spaced holes with intersections of up to 5.5 metres @ 2.0g/t gold and 6 metres @ 5.4g/t gold (with visible gold)

  • Results received from 14 holes with 18 more awaited, so full extent and continuity not yet known

  • Rig relocated to Aakenusvaara gold prospect until remaining assay results are received, then drilling will resume at Aarnivalkea in late August

  • Additional BOT drilling has defined strike extensions to the Aarnivalkea trend and has identified a new parallel trend to the west, with end of hole values of up to 2.17g/t gold

  • Very encouraging result for first ever drilling in an entirely new concealed terrain identified by S2’s systematic greenfields exploration methodology

  • Assays also received for remaining two holes at Gwardar nickel prospect (Polar Bear, WA) indicate prospective nickel sulphide bearing lava channel, 160 metres across and open down plunge

S2 Resources Ltd (“S2” or the “Company”) advises that it has completed the first phase of reconnaissance diamond drilling at its 100% owned Aarnivalkea gold anomaly in Finland, and has received assay results for the first 14 of 32 holes drilled.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

The drilling has achieved its objective of confirming the presence of a significant shear zone system with intense hydrothermal alteration, widespread gold anomalism, and high grade gold mineralisation, with better intercepts including:

  • 10 metres @ 1.0g/t gold from 87 metres in FAVD0006

  • 5.5 metres @ 2.0 g/t gold from 42 metres, including 0.7 metres @ 6.7 g/t gold and 1 metre @ 5.3g/t gold, in FAVD0012

  • 6.0 metres @ 5.4 g/t gold from 59 metres, including 4 metres @ 7.8g/t gold in FAVD0015

These intercepts are on two lines 560 metres apart, with assay results for the intervening line of holes awaited. The results are considered highly encouraging given that this is the first phase of a broad reconnaissance program designed to confirm the presence of a shear zone, and to test for gold anomalism. The drilling is very wide spaced (fences spaced at intervals of 240-320 metres) and relatively shallow in nature (most holes 80-90 metres depth) making it particularly pleasing that both objectives have been achieved (see Figure 1).

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Figure 1. Isometric view looking northwest showing wide spaced (240-320 metre) fences of shallow (~80 metre) diamond holes and the location of the new BOT anomaly to the west of current drilling. Holes with light blue collars are those awaiting assay results.

Gold anomalism/mineralisation is mainly associated with interpreted steep easterly dipping zones of intense shearing and alteration within and at the contacts of basalts and dacitic porphyries (see Figure 2).

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

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Figure 2. Cross section showing anomalous envelopes (>0.2g/t gold) and mineralised intercepts (>1.0g/t gold) for those holes with assays received to date.

The alteration exhibits classic mesothermal lode gold characteristics including an earlier phase of ductile shearing and chlorite-sericite (potassic) alteration, a later phase of albite (sodic) alteration with brittle quartz-carbonate-(scheelite) veining, brecciation, and locally strong carbonate-silica-sulphide alteration with pyrite and/or arsenopyrite. Free gold has been observed in the most strongly mineralised intercept in hole FAVD0015 (see Figure 3).

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Figure 3. Magnified photograph showing free gold grains and associated arsenopyrite crystals within a silicified matrix.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Meanwhile, BOT drilling undertaken concurrently with the diamond drilling has extended the Aarnivalkea anomaly to the south and has also identified a parallel trend to the west of the main trend, with a best end of hole value of 2.17g/t gold (see Figure 4).

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Figure 4. BOT anomaly with additional line to the south and a new trend to the west (at the southwest end of the anomaly).

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

The Company’s “Paana W2” exploration licence application to the west and southwest of Aarnivalkea is being fast tracked through TUKES, the Finnish Mining Authority, to enable extended BOT exploration on the southern continuation of the prospective mineralised structures (see Figure 5).

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Figure 5. Location of Aarnivalkea prospect (red diamond drillhole collars) relative to completed BOT drilling (black dots/lines), planned BOT drilling (yellow dots/lines) and fast-tracked “Paana W2” exploration licence application area (light blue outline). Additionally, S2 has sole rights to the remainder of the large Paana exploration licence application area (white outline).

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Given the broad spacing of the holes drilled to date and the number of holes with assays still awaited it is too soon to identify specific hotspots for follow up so the rig has been moved to start drilling the Aakenusvaara gold prospect. Once the remaining assays have been received the rig will commence follow up drilling which will comprise infill lines to tighten the spacing along strike, extensional lines to test the new BOT anomalies, and probe around the gold hotspots identified in phase 1.

It is anticipated that the remaining assays will be received by mid-late August and that the rig will recommence drilling at Aarnivalkea by late August. Much of the prospect is accessible year round but some parts located beneath shallow swamps may only be accessed during the winter freeze (usually December to March), so these considerations will also govern priorities.

S2’s CEO Mark Bennett said “Finland is a highly prospective but under-explored country and despite being only 25 kilometres away from Europe’s biggest gold mine, Aarnivalkea is completely unexplored, so these preliminary drilling results underpin the reason why we decided to explore there. Our next milestone is the receipt of further assays from other holes completed, and we hope to build on these results over the coming weeks through our systematic program at Aarnivalkea whilst also progressing our other emerging gold and nickel prospects elsewhere in Lapland”.

Gwardar nickel prospect, Western Australia

Results have also been received for the remaining holes recently drilled at the Gwardar nickel prospect, Polar Bear, Western Australia, where S2 holds 100% of the nickel rights on the ground previously sold to Westgold (now RNC).

Hole SPBD0360, reported on 22[nd] July 2019, intersected several zones of nickel sulphide in the centre of a Kambalda-style lava channel including 17.83 metres @ 0.75% nickel (including 0.75 metres @ 2.41% nickel and 0.68 metres @ 3.31% nickel) and 3.33 metres @ 1.38% nickel.

The two follow up holes drilled at approximately the same depth but to the north and south of SPBD0360 also intersected disseminated and narrow massive sulphides, indicating that the lava channel is nickel sulphide-bearing over a lateral width of about 160 metres, and open down plunge.

Hole SPBD0362 intersected a possible footwall embayment marking the southern edge of the lava channel approximately 80 metres to the south of the intercept in SPBD0360, containing a narrow zone of sulphides (1.22 metres @ 1.38% nickel including a narrow band of massive sulphides grading 6.16% nickel over 15 centimetres). Hole SPBD0361, drilled approximately 80 metres north of SPBD0360 intersected 5.7 metres @ 0.57% nickel (see Table 2 for details of intercepts).

Although these intercepts are not mineable grade and width, the abundance of sulphide, the size of the lava channel, and the fact that it is open down plunge are considered encouraging indications of its potential. Follow up drilling is being planned.

For further information, please contact:

Mark Bennett Anna Neuling Managing Director & CEO Executive Director & Company Secretary +61 8 6166 0240 +61 8 6166 0240

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

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Competent Persons statements

The information in this report that relates to Exploration Results from Finland is based on information compiled by Andy Thompson, who is an employee and shareholder of the Company. Mr Thompson is a member of the Australian Institute of Mining and Metallurgy (MAusIMM) and has sufficient experience of relevance to the style of mineralization and the types of deposits under consideration, and to the activities undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Thompson consents to the inclusion in this report of the matters based on information in the form and context in which it appears.

The information in this report that relates to Exploration Results from Australia is based on information compiled by John Bartlett, who is an employee and shareholder of the Company. Mr Bartlett is a member of the Australian Institute of Mining and Metallurgy (MAusIMM) and has sufficient experience of relevance to the style of mineralization and the types of deposits under consideration, and to the activities undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Bartlett consents to the inclusion in this report of the matters based on information in the form and context in which it appears.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Hole Easting Northing RL Dip Azimuth Depth From To Width **Grade Aug/t **
FAVD0001 418381 7552400 245 -60 270 95.2 16.08 16.71 0.63 2.0
and 23.66 27.00 3.34 1.3
including 23.66 24.36 0.70 4.6
FAVD0002 418341 7552401 244 -60 270 92.8 87.00 88.00 1.00 1.7
FAVD0003 418301 7552399 244 -60 270 83.8 NSI
FAVD0004 418260 7552400 243 -60 270 80.0 21.31 22.19 0.88 1.2
and 62.77 64.19 1.42 0.7
FAVD0005 418221 7552399 243 -60 270 47.8 16.00 17.70 1.70 2.0
FAVD0006 418261 7552400 244 -60 90 100.0 87.00 97.00 10.00 1.0
including 90.00 91.00 1.00 3.6
FAVD0007 418420 7552396 246 -60 270 104.6 32.00 34.00 2.00 0.8
and 62.80 64.60 1.80 1.1
including 62.80 63.70 0.90 3.3
and 75.00 79.30 4.30 0.4
and 88.00 91.00 3.00 0.5
FAVD0008 418210 7551521 239 -60 270 80.4 25.50 27.80 2.30 0.4
and 64.00 65.00 1.00 3.0
FAVD0009* 418170 7551521 240 -60 270 71.3 NSI
FAVD0010* 418131 7551521 240 -60 270 80.6 65.00 66.00 1.00 3.4
FAVD0011* 418226 7551441 239 -60 270 81.0 66.00 69.00 3.00 0.6
FAVD0012* 418260 7551840 242 -60 270 77.4 35.00 36.05 1.05 2.0
and 42.00 47.50 5.50 2.0
including 43.41 44.13 0.72 6.7
including 46.50 47.50 1.00 5.3
and 59.90 62.00 2.10 1.6
FAVD0013* 418221 7551841 242 -60 270 77.9 65.28 67.44 2.16 1.9
FAVD0014 418178 7551841 241 -60 270 89.5 AWR
FAVD0015* 418140 7551841 241 -60 270 89.7 12.21 21.00 8.79 0.3
and 25.00 38.00 13.00 0.3
and 59.00 65.00 6.00 5.4
including 61.00 65.00 4.00 7.8
and 73.99 78.75 4.76 0.4
FAVD0016 418104 7551842 240 -60 270 89.6 AWR
FAVD0017 418380 7552160 250 -60 270 86.8 AWR
FAVD0018 418340 7552162 250 -60 270 89.8 AWR
FAVD0019 418302 7552161 249 -60 270 89.6 AWR
FAVD0020 418260 7552161 249 -60 270 89.8 AWR
FAVD0021 418221 7552163 249 -60 270 89.8 AWR
FAVD0022 418181 7552164 247 -60 270 89.6 AWR
FAVD0023 418142 7552165 247 -60 270 89.3 AWR
FAVD0024 418061 7552160 244 -60 270 98.8 AWR
FAVD0025 418002 7552162 241 -60 270 98.8 AWR
FAVD0026 418461 7552396 246 -60 270 145.9 AWR
FAVD0027 418480 7552719 243 -60 270 89.7 AWR
FAVD0028 418440 7552720 242 -60 270 89.8 AWR
FAVD0029 418401 7552721 242 -60 270 89.9 AWR
FAVD0030 418360 7552721 242 -60 270 68.9 AWR
FAVD0031 418300 7551840 242 -60 270 150.0 AWR
FPAD0001 419580 7553800 251 -60 270 83.7 AWR

Table 1. Details of all diamond holes completed at Paana central lease (including Aarnivalkea) in 2019 by S2. Note Holes marked with an asterisk* have preliminary results only.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Hole Easting Northing RL Dip Azimuth Depth From To Width Ni
(pct)
Cu
(pct)
SPBD0083 388748 6472647 266 -60 286 272.0 NSI
SPBD0360 388840 6472440 266 -60 268 270.0 159.00 166.00 7.00 0.47 0.04
and 183.00 200.83 17.83 0.69 0.05
including 194.53 195.28 0.75 2.41 0.08
and including 200.15 200.83 0.68 3.31 0.43
and 223.67 227.00 3.33 1.38 0.24
SPBD0361 388825 6472470 266 -60 287 290.0 248.90 254.60 5.70 0.57 0.07
SPBD0362 388870 6472400 266 -55 240 250.0 186.30 188.09 1.79 0.60 0.04
and 211.20 212.42 1.22 1.38 0.05
including 212.27 212.42 0.15 6.16 0.09

Table 2. Details of all diamond holes completed at Gwardar, Western Australia in 2019 by S2.

The following Tables are provided to ensure compliance with the JORC code (2012) edition requirements for the reporting of exploration results.

SECTION 1 SAMPLING TECHNIQUES AND DATA - FINLAND

Criteria
Sampling techniques
Drilling techniques
JORC Code explanation Commentary
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.
Base of Till (BoT) drilling is undertaken by Moreenityo Macklin
Oy of Sattanen, Finland. Holes are drilled to bedrock or blade
refusal and a 20cm sample is collected at the end of hole for
geochemical analysis and lithological logging.
Drilling is undertaken using MK Drilling of Ranua, Finland
drilling NQ2 rod size with a DDH size of 75.7mm and core size
of 50.7mm. NQ2 core samples are logged and marked up by S2
personnel. Unbiased core sample intervals were cut in half by
diamond saw with half core sent for preparation and analysis at
ALS Laboratories.
All rock grab and rock float samples are collected from outcrop
by S2 personnel and marked into sample books and a
representative portion of the sample retained. All are
forwarded for analyses by ALS Laboratories.
Include reference to measures taken to ensure
sample representivity and the appropriate
calibration of any measurement tools or systems
used
Sampling and QAQC procedures are carried out using S2
protocols as per industry best practice.
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
Diamond drilling was used to obtain core samples that have
been cut and sampled on intervals that are determined by
lithology and mineralisation.
The drill core samples are sent to ALS Laboratories for analyses
for gold and base metals. Drill core is sampled at S2’s facilities
in Kittila, Finland.
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).
Base of Till drilling is by a percussion flow through sample bit
that can collect a 20cm sample of bedrock material at the base
of glacial deposits up to 20m thick.
Diamond drilling with NQ2 wireline bit producing a 50.7mm
diameter core.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Criteria JORC Code explanation Commentary
Drill sample
recovery
Method of recording and assessing core and chip
sample recoveries and results assessed
BoT samples are visually inspected to assess if they are likely to
be a basement sample or whether the hole has failed to reach
basement due to boulders or excessive cover thickness.
Diamond Drill core recoveries are recorded by the driller and
written on core block markers. The exact recovery is then
recorded on a metre basis after core mark-up and recorded in
the database.
Measures taken to maximise sample recovery and
ensure representative nature of the samples
Sample quality is qualitatively logged on a metre basis,
recording sample condition.
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.
No relationship has been seen to exist
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.
The logging uses a standard legend developed by S2 which is
suitable for implicit wireframing. All diamond holes are
geotechnically and structurally logged.
Whether logging is qualitative or quantitative in
nature. Core (or costean, channel, etc)
photography.
All core has been photographed both dry and wet. Geological
logging of the diamond drill holes is into tough books using
standardised codes and templates. These logs are then imported
into S2’s central database
The total length and percentage of the relevant
intersections logged
All drill holes were logged in full.
Sub-sampling
techniques and
sample preparation
If core, whether cut or sawn and whether quarter,
half or all core taken.
Core sawn in half and half core taken for assay.
If non-core, whether riffled, tube sampled, rotary
split, etc and whether sampled wet or dry.
Bot samples are dried and sieved with the fine fraction
submitted for assay.
The coarse fraction is retained and logged
For all sample types, the nature, quality and
appropriateness of the sample preparation
technique.
Samples were delivered by S2 personnel to ALS Minerals
laboratory in Sodankyla, Finland, where they are crushed with
>70% <2mm (code CRU-31), split by riffle splitter (code SPL-21),
and pulverised 1000grm to 85% <75 um (code PUL-32). Crushers
and pulverizers are washed with QAQC tests undertaken (codes
CRU-QC, PUL-QC). The prepared samples are forwarded to ALS
Minerals Loughrea, Ireland, for analysis.
Quality control procedures adopted for all sub-
sampling stages to maximise representivity of
samples.
Full QAQC system in place to determine accuracy and precision
of assays
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.
For DDH’s non biased core cutting through using an orientation
line marked on core and cut to the line
Whether sample sizes are appropriate to the grain
size of the material being sampled.
Samples of appropriate size

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Criteria JORC Code explanation Commentary
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.
All samples were analysed by ALS Minerals Loughrea, Ireland.
BoT samples analysed for gold undergo a 25g aqua regia
digestion with ICP-MS finish (code Au-TL43). Samples analysed
for Ag, As, Bi, Ca, Cd, Cu, Fe, Hg, Mg, Mn, Mo, Ni, P, Pb, S, Sb, Tl
& Zn undergo an aqua regia digestion with ICP-AES Finish (code
ME-ICP41).
Core samples analysed for gold undergo a 50g fire assay with AA
finish (code Au-AA26). Selected samples are analysed for Ag, As,
Bi, Ca, Cd, Cu, Fe, Hg, Mg, Mn, Mo, Ni, P, Pb, S, Sb, Tl & Zn
undergo an oxidising digestion with ICP-AES Finish (code ME-
ICPORE).
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.
No geophysical tools were used to determine any element
concentrations.
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.
Full QAQC system in place including Certified Standards and
blanks of appropriate matrix and levels
Verification of
sampling and
assaying
The verification of significant intersections by
either independent or alternative company
personnel.
Andy Thompson, Country Geology Manager for S2 has
personally inspected all drill cores and rock samples.
The use of twinned holes. No twinned diamond holes have been drilled at Arnievalkea
Documentation of primary data, data entry
procedures, data verification, data storage
(physical and electronic) protocols.
Primary sampling data is collected in a set of standard Excel
templates. The information is managed by S2’s database
manager for validation and compilation into S2’s central
database.
Discuss any adjustment to assay data. No adjustments made
Location of data
points
Accuracy and quality of surveys used to locate
drillholes (collar and down-hole surveys), trenches,
mine workings and other locations used in Mineral
Resource estimation.
BoT collars were located with a handheld GPS with an accuracy
of within 3 metres.
Diamond drill collars are pegged using a Trimble DGPS to +/-
1m accuracy. Drill rigs are aligned to Grid west using Standard
Finnish National Grid ETRS-TM35FIN. The holes are downhole
surveyed using a Deviflex tool.
Specification of the grid system used. The grid system used is the Standard Finnish National Grid
ETRS-TM35FIN.
Quality and adequacy of topographic control. Elevation data for all collars is determined by a digital elevation
model derived from public domain 2m Lidar data. Topographic
control and map data is excellent.
Data spacing and
distribution
Data spacing for reporting of Exploration Results. BoT geochemical samples are drilled at 400m by 20m for initial
reconnaissance and 100m by 10m for detailed infill.
Diamond drilling is currently being drilled on 320m x 40m
spacing’s over the geochemical anomaly to scope out the
basement stratigraphy and structure and will be progressively
infilled to 80m x 40m with deeper holes as deemed appropriate.
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.
Data spacing and distribution is not sufficient at this stage to
allow the estimation of mineral resources.
Whether sample compositing has been applied. No sample compositing has been applied

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Criteria JORC Code explanation Commentary
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.
Drillhole orientation is designed to intersect the mineralised
package of rocks and be perpendicular to shearing and
mineralisation. Structural measurements from orientated core
indicate that the main fabric and contacts are dipping steeply to
the east and hence holes collared at -60dip 270deg azimuth are
appropriate.
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 drilling at this stage is preliminary and exploratory. It is not
possible to assess if any sample bias has occurred due to drillhole
orientation at this stage.
Sample security The measures taken to ensure sample security. Chain of custody is managed by S2 personnel. Drill samples and
core is visually checked at the drill rig and then transported to
S2’s logging and cutting facilities by S2 personnel for logging,
cutting and sampling. Bagged samples are transferred to ALS
Laboratories in Sodankyla, Finland by S2 personnel.
Audits or reviews The results of any audits or reviews of sampling
techniques and data.
No audits or reviews have been conducted at this stage.

SECTION 2 REPORTING OF EXPLORATION RESULTS - FINLAND

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 Aarnivalkea prospect is located within the Paana Central
Exploration Licence. ML2018:0081
The exploration licences are 100% owned by Sakumpu
Exploration Oy, a Finnish registered 100% owned subsidiary of
S2
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.
All of the Exploration Licences are in good standing and no
known impediments exist on the tenements being actively
explored.
Exploration done by
other parties
Acknowledgment and appraisal of exploration by
other parties.
The Aarnivalkea prospect is a greenfield discovery with historic
BoT holes drilled in the region by Outukumpu not having been
assayed for gold.
Geology Deposit type, geological setting and style of
mineralisation.
The prospect is a shear zone hosted orogenic gold deposit within
the Kittila Group of the Paleoproterozoic Central Lapland
Greenstone belt.
The primary host rocks include altered and sheared basalt,
dacites and sediments
Alteration assemblages include albite, sericite, carbonate,
chlorite with disseminated pyrite, pyrrhotite and arsenopyrite.
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

down hole length and interception
depth

hole length.
Refer to sample plans in text.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Criteria JORC Code explanation Commentary
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.
All reported intersections of drilling undertaken by S2 have been
length weighted.
A nominal 0.2g/t lower cut-off is used for the reconnaissance
diamond drill intersections. No top cut has been applied.
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.
High grade intervals internal to broader zones of mineralisation
are reported as included intervals.
The assumptions used for any reporting of metal
equivalent values should be clearly stated.
None used.
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 trend of mineralisation at the targets/prospects described is
estimated to be dipping steeply to the east at approximately 75
to 80 deg.
Refer to figures in body of text.
Diagram 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.
Refer to Figures in body of text.
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 considered significant are reported.
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.
None at present
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
BoT drilling will continue where ground is accessible throughout
summer. This will initially focus immediately south and south
west of Arnievalkea where the geochemical anomaly is still
open.
Diamond drilling is currently being drilled on 320m x 40m
spacing’s over the geochemical anomaly to scope out the
basement stratigraphy and structure and will be progressively
infilled to 80m x 40m with deeper holes as deemed appropriate.
A detailed airborne magnetic survey is planned so as to
complement infill the current excellent but more regional data.
Infill gravity over the Paana tenements is also being planned.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

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.
The Gwardar prospect was sampled in four diamond drill holes,
undertaken by DDH1 Pty Ltd. Drilling is orientated in a westerly
direction, with specific azimuth modified to gain desired
separation along strike.
Sampling has been carried out by cutting and sampling half
core through areas of visible mineralisation, with sample
intervals to lithological contacts, to a maximum length of 1.2
metres.
All are forwarded for analyses by Minanalytical Laboratories
Services Australia Pty Ltd in Perth.
Include reference to measures taken to ensure
sample representivity and the appropriate
calibration of any measurement tools or systems
used
Sampling and QAQC procedures are carried out using S2
protocols as per industry best practice.
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
The diamond core is HQ and NQ2 size, sampled on geological
intervals (0.2 m to 1.2 m), cut into half (NQ2) or quarter (HQ)
core to give sample weights under 3 kg. Samples were
crushed, dried and pulverised (total prep) to produce a sub
sample for analysis by four acid digest with an ICP/OES
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).
Drilling is standard diamond coring, using either HQ triple tube
or NQ2 core diameter. The core has been orientated using a an
Ace orientation tool.
Drill sample
recovery
Method of recording and assessing core and chip
sample recoveries and results assessed
Diamond core recoveries are logged and recorded in the
database. Overall recoveries are >>95%.
Measures taken to maximise sample recovery and
ensure representative nature of the samples
Diamond core is reconstructed into continuous runs on an
angle iron cradle for orientation marking. Depths are checked
against the depth given on the core blocks and rod counts are
routinely carried out by the drillers.
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.
No relationship has been seen to exist
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.
Logging of diamond core and RC samples records lithology,
mineralogy, mineralisation, structural (DDH only), weathering,
colour and other features of the samples
logging uses a standard legend developed by S2 which is
suitable for wireframing of the basement interface.
Exploration holes are not routinely geotechnically logged but
resource holes are.
Whether logging is qualitative or quantitative in
nature. Core (or costean, channel, etc)
photography.
All core is photographed in both dry and wet form.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Criteria JORC Code explanation Commentary
The total length and percentage of the relevant
intersections logged
All drillholes were logged in full to end of hole.
Sub-sampling
techniques and
sample preparation
If core, whether cut or sawn and whether quarter,
half or all core taken.
Core was cut in half (NQ2) and quarter core (HQ) onsite using an
automatic core saw. All samples were collected from the same
side of the core.
If non-core, whether riffled, tube sampled, rotary
split, etc and whether sampled wet or dry.
No non-core sampling was completed
For all sample types, the nature, quality and
appropriateness of the sample preparation
technique.
The sample preparation follows industry best practice in sample
preparation
involving
oven
drying,
coarse
crush
and
pulverisation of entire sample to minimum of 85% passing -
75um.
Quality control procedures adopted for all sub-
sampling stages to maximise representivity of
samples.
Full QAQC system in place to determine accuracy and precision
of assays
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.
Non-biased sampling using the orientation line as a guide for
cutting with the same half used for all sampling.
No duplicate samples have been collected at this stage
Whether sample sizes are appropriate to the grain
size of the material being sampled.
The sample sizes are considered to be appropriate to correctly
represent the sought after mineralisation style
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 core samples the analytical techniques used a four acid
digest multi element suite with ICP/OES or ICP/MS finish (25
gram or 50 gram FA/AAS for precious metals).
The acids used are hydrofluoric, nitric, perchloric and
hydrochloric acids, suitable for silica based samples.
The method approaches total dissolution of most minerals.
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.
No geophysical tools were used to determine any element
concentrations.
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.
Full QAQC system in place including Certified Standards and
blanks of appropriate matrix and levels.
Verification of
sampling and
assaying
The verification of significant intersections by
either independent or alternative company
personnel.
The S2 Exploration Manager has personally inspected all
sampled core and assay results.
The use of twinned holes. No twinned holes were drilled within the main infilled anomaly.
Documentation of primary data, data entry
procedures, data verification, data storage
(physical and electronic) protocols.
Primary sampling data is collected in a set of standard Excel
templates. The information is managed by S2’s database
manager for validation and compilation into S2’s central
database.
Discuss any adjustment to assay data. No adjustments made
Location of data
points
Accuracy and quality of surveys used to locate
drillholes (collar and down-hole surveys), trenches,
mine workings and other locations used in Mineral
Resource estimation.
Drill hole collar locations were recorded using handheld Garmin
GPS. Elevation values were in AHD RL and values recorded
within the database. Expected accuracy is + or – 5 m for
easting, northing and 10m for elevation coordinates.
Downhole surveys using an Axis north-seeking gyro with
readings at surface and then every 30m downhole.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Criteria JORC Code explanation Commentary
Specification of the grid system used. The grid system is MGA_GDA94 (zone 51), local easting and
northing are in MGA.
Quality and adequacy of topographic control. Topographic surface uses handheld GPS elevation data, which is
adequate at the current stage of the project.
Data spacing and
distribution
Data spacing for reporting of Exploration Results. The nominal drillhole spacing is project specific, refer to figures
in text
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.
Data spacing, sampling technique and distribution is not
sufficient at this stage to allow the estimation of mineral
resources.
Whether sample compositing has been applied. No sample compositing has been applied.
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.
Geochemical sampling of basement interface only.
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 of diamond core is on a nominal 60 degrees to the west,
which is broadly orthogonal to the mineralisation.
Sample security The measures taken to ensure sample security. Chain of custody is managed by S2 personnel. Drill samples and
core is visually checked at the drill rig and then transported to
S2’s logging and cutting facilities on site at the S2 remote camp.
Bagged samples are transferred to Minanalytical Laboratory in
Kalgoorlie by S2 personnel.
Audits or reviews The results of any audits or reviews of sampling
techniques and data.
No audits or reviews have been conducted at this stage.

SECTION 2 REPORTING OF EXPLORATION RESULTS – GWARDAR, WA

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 Gwardar prospect is located on tenement M63/230 owned
by Polar Metals Pty Ltd (a wholly owned subsidiary of Royal
Nickel Corp) and is part of the Polar Bear Project. S2 retains
rights to nickel mineralisation within the Polar Bear project.
M63/230 is located within the Ngadju Native Title Claim
(WC99/002).
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.
All of the Exploration Licences are in good standing and no
known impediments exist on the tenements being actively
explored.
Exploration done by
other parties
Acknowledgment and appraisal of exploration by
other parties.
Historical drilling by Anaconda Nickel Ltd drilled a number of
diamond and percussion drill holes along the interpreted
ultramafic basal contact. Collar locations from historical drill
holes have not been field verified.
INCO conducted a reconnaissance small loop Slingram type EM
survey. Six diamond holes were drilled (none at Gwardar).
Sirius Resources undertook MLEM and RC and diamond drilling
along the Taipan – Gwardar trend, with a total of one diamond
hole and six RC holes within the Gwardar prospect.
The collar locations for all INCO and Sirius drill holes have been
verified by S2 personnel.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Criteria JORC Code explanation Commentary
Geology Deposit type, geological setting and style of
mineralisation.
The geology at Polar Bear is dominated by complexly deformed
Achaean greenstone assemblages of the Norseman-Wiluna
Greenstone Belt which have been metamorphosed to upper
greenschist facies.
The Eudyne Mafic Sequence (EMS) consists of tightly folded
ultramafic and mafic intrusives and extrusives with minor
interflow sediments. The rocks are frequently talc-carbonate
altered and moderately well foliated. The ultramafic rocks are
typically komatiites and komatiitic basalt.
The deposit style sought after is analogous to Kambalda-style
nickel copper sulphide deposits.
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

down hole length and interception
depth

hole length.
Refer to sample plans in text.
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.
Reported assay results for diamond drilling have been length
and bulk density weighted. Intervals have been calculated using
a 0.4% nickel lower cut-off, with maximum of 2m internal
dilution.
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.
Individual sample intervals vary between 0.2 and 1.2 metres,
selected based on lithological contacts.
The assumptions used for any reporting of metal
equivalent values should be clearly stated.
No reporting of metal equivalent has been used.
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 trend of mineralisation at the prospects described is broadly
NNW, dipping at approximately 60 degrees to the ENE. RC and
Diamond drilling has been used to determine this.
Refer to figures in body of text.
Diagram 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.
Refer to Figures in body of text.
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 considered significant are reported.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au

Criteria JORC Code explanation Commentary
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.
No other exploration data present.
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
Detailed processing and modelling of DHEM data. Additional
diamond drilling to test down-dip of the existing drilling.

4/24 Parkland Road, Osborne Park, WA 6017, Australia. PO Box 1209, Osborne Park, WA 6916, Australia ABN 18 606 128 090 T +61 8 6166 0240 F 61 8 6270 5410 E [email protected] W www.s2resources.com.au