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WA1 RESOURCES LTD Capital/Financing Update 2022

Oct 25, 2022

66031_rns_2022-10-25_8f4b3824-7e51-4f55-b4f8-ff5834437526.pdf

Capital/Financing Update

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ASX RELEASE
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26 OCTOBER 2022

WEST ARUNTA PROJECT

DISCOVERY OF NIOBIUM-REE MINERALISED CARBONATITE SYSTEM

Highlights

  • First drillhole at the P2 geophysical target (at the Pachpadra Prospect area) has discovered a mineralised carbonatite system

  • Significant mineralisation confirmed in drillhole PARC003 composite assays[₁] :

54m at 0.62% Nb2O5, 0.18% TREO[2] , 3.85% P2O5

from 162m within an overall interval of

142m at 0.31% Nb2O5, 0.17% TREO, 3.94% P2O5

from 74m to 216m (EOH) and ending in

2m at 1.22% Nb2O5, 0.22% TREO, 5.73% P2O5

  • Entire assayed section of the hole (74m to 216m) has highly elevated niobium (Nb), anomalous rare earth elements (REE) and phosphorus (P)

  • Samples from the top of the hole (0m to 74m) have not yet been assayed but also have potential for mineralisation

  • All single-metre splits from PARC003 will now be assayed and results from other holes are due in the coming weeks

  • Niobium is listed as a critical and strategic mineral key to global technology needs by Australia, USA, EU, Japan and India

  • Carbonatite mineral systems are important sources of niobium and REE and host all three of the world’s operating niobium mines and also Lynas Rare Earths Limited’s Mt Weld deposit

  • Only one RC hole was completed at the P2 geophysical anomaly which extends for 3 kilometres and has significant future exploration potential

WA1 Resources Ltd (ASX: WA1) ( WA1 or the Company ) is pleased to announce the first results from its maiden West Arunta Project drilling program undertaken in July.

WA1’s Managing Director, Paul Savich, commented:

“The discovery of a mineralised carbonatite system in the West Arunta is the first of its kind in the region and is a significant finding from our maiden drilling program.

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WA1 RESOURCES LTD | ABN: 51 646 878 631 | WWW.WA1.COM.AU | ASX: WA1 WA1 RESOURCES LTD | ABN: 51 646 878 631 | WWW.WA1.COM.AU | ASX: WA1 A: L2 55 CARRINGTON ST NEDLANDS WA 6009 P: +61 8 6478 7866 E: [email protected] A: 2C LOCH ST, NEDLANDS WA 6009 P: +61 8 6478 7866 E: [email protected]

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“For our first hole at P2 to have intersected high-grade niobium mineralisation that remains open and with the highest grade at the end-of-hole (2m at 1.22% Nb2O5) along with elevated rare earth elements and phosphorus, is an exciting result.

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Figure 1: P2 Schematic Cross-section Gravity anomaly image (resUC200m contours)

“To date, we have only assayed 4m composite samples commencing from 74m depth in this hole, where drilling entered fresh bedrock. With the knowledge that we are in a mineralised carbonatite system, we will assay single metre splits for the entire hole.

“The geophysical anomaly at P2 extends for approximately 3km, demonstrating the significant exploration potential of this carbonatite system. Furthermore, there are other untested anomalies within the project area, which could now represent further targets for this style of mineralisation.

“Niobium has been identified as a critical mineral by a number of countries and is a key input to future global technology needs, with ferroniobium metal (65% Nb) selling for US$45,000/t[3] . Over the coming months we will collate a comprehensive dataset from the drilling program and plan follow-up exploration activities.”

Technical Discussion

The drill program comprised seven holes for a total of 1,745 metres. Drilling provided an initial test of two target zones at the Pachpadra Prospect (P1 and P2) and the one target zone at the Sambhar Prospect (Luni).

The results provided in this announcement relate to the single reverse circulation ( RC ) hole drilled to 216 metres at P2 (PARC003). This hole was co-funded by the Western Australian Department of Mines, Industry Regulation & Safety ( DMIRS ) under the Exploration Incentive Scheme ( EIS ).

P2 is located along a major north-east trending shear and is characterised by a gravity anomaly high which is approximately 3km in length and coincides with varying levels of

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Notes 1: A ‘composite assay’ refers to the grouping of single metre samples into 4-Note 3: IS THIS REFERENCE CORRECT? Globe Metals & Mining (globem m etre combined intervals for laboratory assay, a com/niobium-markets) common industry practice utilised in RC dril ing for early-stage exploratioNote 4: Refer to Australian Strategic Meta l s Ltd’s (ASX: ASM) ASX Annou n projcem e cts nt dated 7 December 2021 and

titled “Dub b o Project Optimisation Delivers Strong Financials”, Table 9: Long Term Real Price assumptions used breviation of Total Rare Earth Oxides, representing a combined group of 17 elements (La, Ce, Pr, Nd, Pm, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Y, Sc) in the 2021 Optimisation Study

3: Globe Metals & Mining Limited, Niobium Markets – Pricing, viewed 24 October 2022 https://www.globemm.com/niobiummarkets

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magnetic anomalism. Geophysical modelling suggested a northerly dip, resulting in the decision to drill the hole with a -60 degree dip to the south. Orientation of the mineralisation (true and apparent width) is not able to be determined at this stage.

Table 1: RC Collar Location (GDA94 Zone 52)

Hole ID Target Easting Northing RL
(m)
Azimuth
(Degrees)
Dip
(Degrees)
Depth
(m)
PARC003 Pachpadra – P2 404816 7545043 401 180 -60 216

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Figure 2: Plan View of Pachpadra Drill Collar Locations

Combined gravity (resUC200m, colour) and magnetic (residual contours) anomaly images

PARC003 collared into ferruginous and mottled clays with saprock occurring from 74m. Drilling intersected a distinct carbonate rich intrusive rock from 84m, coarse grained in texture with apatite visible in hand specimen. Hematite/goethite alteration occurred for 20m from 106m.

Significant mineralisation has now been confirmed in the first P2 drillhole (PARC003) via 4m composite assays (refer to Table 2). The hole intersected elevated niobium, rare earth elements and phosphorus throughout the entire assayed portion, including:

54m at 0.62% Nb2O5, 0.18% TREO (comprising 21% Nd2O3+Pr6O11), 3.85% P2O5

within an overall interval of

142m at 0.31% Nb2O5, 0.17% TREO, 3.94% P2O5

from 74m to 216m (EOH) and ending in

2m at 1.22% Nb2O5, 0.22% TREO, 5.73% P2O5

Assay values peaked at 1.22% Nb2O5 (216m EOH), 0.43% TREO (106-110m) and 8.75% P2O5 (9094m) at varying intervals throughout the assayed section of the hole. Anomalous zinc and lead values were also noted in select intervals. Geochemical analysis was completed by ALS Laboratories in Perth.

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Figures 3-5: Top - Plan View, Middle – Cross-section, Bottom - Long-section
Schematics of gravity anomaly images (residual gravity with 2.68-2.72g/cc density shells)
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The Company will now submit the individual samples for each metre of the hole to the laboratory for assay. This will include samples from the top 74m metres of the hole, which were not included in the 4m composite samples initially submitted. Results from these samples will be reported, along with the other results from the recent drilling program, once they are received and reviewed by the Company.

Carbonatite Overview

Carbonatites are a type of igneous rock defined by their composition being rich in carbonate minerals, typically calcite or dolomite. They often occur as plugs within alkali intrusive complexes, or as dykes, sills, breccias or veins. They are generally associated with major crustal scale features in rift-related tectonic settings. Carbonatites may be mineralised with rare earth elements, niobium, phosphorus, tantalum, uranium, thorium, copper, iron, titanium, vanadium, barium, fluorine and zirconium.

The identification of a mineralised carbonatite intrusion is a significant finding for the West Arunta region, and given other intrusive bodies within the region enhances the potential for further discovery with future exploration efforts.

Carbonatite deposits are an important source of REE and niobium production. This includes the world’s largest REE mine, Bayan Oho in Inner Mongolia, Lynas Rare Earths’ Mt Weld deposit and the world’s three major operating niobium mines.

Niobium Overview

Niobium (Nb) is a transitional metal used as a micro alloy with iron. Niobium is primarily used in the steel industry as the addition of small amounts of niobium (<1%) significantly increases the strength, decreases the weight, reduces corrosion and improves the heat resistance of steel products.

Niobium is a superconductor at very low temperatures, and as an alloy with titanium (NbTi) or tin (Nb3Sn) it produces superconducting magnets used in magnetic resonance imaging (MRI) scanners, nuclear magnetic resonance (NMR) equipment and particle accelerators such as the Large Hadron Collider at CERN. Niobium is essential for advanced technology with additional uses in gas and wind turbines, space travel, and in the manufacture of rechargeable batteries for electric vehicles.

The metal has been identified by the Australian Government and many other countries as a critical mineral, due to the concentration of supply from Brazil. There are currently three niobium producers globally: CBMM, Araxa, Brazil (66ktpa production[5] , +500Mt at 2.5% Nb2O5 resource, cost <$10/kg Nb)[4] , China Molybdenum Co., Catalao, Brazil (10ktpa production[5] , +50Mt at 1% Nb2O5 resource, cost <$10/kg Nb)[4] and Magris Resources Inc., Niobec, Canada (7ktpa production[5] , +75Mt at 0.56% Nb2O5 resource, cost <$19/kg Nb)[4] .

The main niobium product sold is in the form of ferroniobium (~65% Nb) which makes up approximately 90% of the market. Niobium prices range from US$45,000/t[3] per tonne for standard ferroniobium metal and over US$50,000/t[3] per tonne for niobium pentoxide (Nb2O5).

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Note 4: NioBay Metals, Investors – Presentations, viewed 25 October 2022 http://niobaymetals.com/wp/wp-content/uploads/2021/05/202105_Niobay_Corporate_Presentation_.pdf

5: NioCorp, Investors – Presentations, viewed 25 October 2022

https://secureservercdn.net/198.71.233.156/gx0.d43.myftpupload.com/wp-content/uploads/NioCorp_Investor_Presentation.pdf

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West Arunta Project - Overview

The West Arunta Project is located approximately 490km south of Halls Creek in WA. It comprises the Pachpadra , Sambhar and Urmia prospect areas , which are contained within a granted Exploration Licence .

Prior to WA1 acquiring the West Arunta Project in 2021, the tenement had extremely limited historical exploration for gold and copper largely in the form of reconnaissance airborne geophysics, limited ground geophysical surveys, and surface sampling. Drilling on the West Arunta Project tenement was limited to a single historic diamond hole drilled in 2010.

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Figure 6: Location of the West Arunta Project

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ENDS

For further information, please contact:

Investors

Media

Paul Savich Michael Vaughan Managing Director Fivemark Partners T: +61 8 6478 7866 T: +61 422 602 720 / +61 410 276 744 E: [email protected] E: [email protected]

Or visit our website at www.wa1.com.au

Authorised for market release by the Board of WA1.

Competent Person Statement: The information in this announcement that relates to Exploration Results is based on information compiled by Ms. Stephanie Wray who is a Member of the Australian Institute of Geoscientists. Ms. Wray is a full-time employee of WA1 Resources Ltd and has sufficient experience which is relevant to the style of mineralisation under consideration to qualify as a Competent Person as defined in the 2012 Edition of the “Australian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Ms. Wray consents to the inclusion in the announcement of the matters based on her information in the form and context in which it appears.

Forward-Looking Statements: This announcement contains forward-looking information about the Company and its operations. In certain cases, forward-looking information may be identified by such terms as "anticipates", "believes", “should”, "could", "estimates", “target”, “likely”, “plan”, "expects", "may", “intend”, "shall", "will", or "would". These statements are based on information currently available to the Company and the Company provides no assurance that actual results will meet management's expectations. Forward-looking statements are subject to risk factors associated with the Company’s business, many of which are beyond the control of the Company. It is believed that the expectations reflected in these statements are reasonable but they may be affected by a variety of variables and changes in underlying assumptions which could cause actual results or trends to differ materially from those expressed or implied in such statements. There can be no assurance that actual outcomes will not differ materially from these statements.

Disclaimer: No representation or warranty, express or implied, is made by the Company that the material contained in this announcement will be achieved or proved correct. Except for statutory liability which cannot be excluded, each of the Company, its directors, officers, employees, advisors and agents expressly disclaims any responsibility for the accuracy, fairness, sufficiency or completeness of the material contained in this presentation and excludes all liability whatsoever (including in negligence) for any loss or damage which may be suffered by any person as a consequence of any information in this presentation or any effort or omission therefrom. The Company will not update or keep current the information contained in this presentation or to correct any inaccuracy or omission which may become apparent, or to furnish any person with any further information. Any opinions expressed in the presentation are subject to change without notice.

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ASX RELEASE
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Table 2: Detailed Assay Results

P2 Target RC Drilling Results – PARC003

Sample ID Depth Zn Pb P2O5 Nb2O5 Sc2O3 Y2O3 Ce2O3 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr2O3 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO
ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm %
From
To
ICP ICP XRF XRF ICP ICP ICP ICP ICP ICP ICP ICP ICP ICP ICP ICP ICP ICP ICP ICP ICP Calc
WAX03258 74
78
554
46
59800
0.18*
5
122
857
25
10
17
41
4
423
1
357
96
60
5
1
112
7
0.21
WAX03259 78
82
290
51
33200
0.05
5

99
534

26
10

17
42

4
242

1
397

110
58

5
1

78
7

0.16
WAX03261 82
86
677
118
27500
0.12*
6
123
581
23
10
12
32
4
281
1
236
64
42
4
1
108
7
0.15
WAX03262 86
90
461
150
21300
0.04

3
94
725
18
7
11
28
3
388
1
273
78
43
4
1
85
5
0.18
WAX03263 90
94
148
31
87500
0.08*
3
104
766
21
8
15
37
3
366
1
327
87
54
4
1
89
5
0.19
WAX03264 94
98
649
155
46700
0.09*
2
94
664
20
7
13
33
3
317
1
275
74
48
4
1
87
5
0.16
WAX03265 98
102
504
126
30200
0.12*
3
106
710
21
8
13
33
3
323
1
276
79
44
4
1
95
6
0.17
WAX03266 102
106
467
242
43900
0.18*
3
102
729
22
8
15
37
4
349
1
311
84
53
4
1
99
6
0.18
WAX03267 106
110
366
87
33800
0.12*
4
129
1840
28
10
21
48
4
1220
1
567
176
77
6
1
119
7
0.43
WAX03268 110
114
413
130
33700
0.07*
3
102
625
19
7
12
30
3
318
1
255
70
42
4
1
92
5
0.16
WAX03269 114
118
332
108
41500
0.08*
4
98
606
19
8
12
30
3
301
1
262
71
43
4
1
91
5
0.16
WAX03270 118
122
827
344
52900
0.10*
5
95
677
20
7
14
35
3
331
1
290
78
49
4
1
90
5
0.17
WAX03271 122
126
1435
676
46300
0.07*
4
89
629
19
7
12
31
3
306
1
268
72
44
4
1
81
5
0.16
WAX03272 126
130
1155
347
41000
0.06*
3
96
673
20
8
13
32
3
337
1
281
76
46
4
1
89
5
0.17
WAX03273 130
134
995
484
42100
0.07*
3
87
640
17
7
12
29
3
318
1
262
71
42
4
1
76
4
0.16
WAX03274 134
138
1285
540
42200
0.06*
3
96
714
20
8
13
33
3
348
1
293
80
47
4
1
88
5
0.18
WAX03275 138
142
126
35
1080
0.14

1
73
70
13
6
4
12
2
27
-
36
9
10
2
1
68
4
0.03
WAX03276 142
146
44
23
530
0.24

2
68
121
14
5
5
16
2
57
-
58
14
14
3
-
64
3
0.04
WAX03277 146
150
207
53
30100
0.27*
3
93
613
19
7
12
31
3
277
1
239
69
40
4
1
86
5
0.15
WAX03278 150
154
92
36
59800
0.25*
4
100
737
21
8
14
36
3
319
1
299
84
50
4
1
94
5
0.18
WAX03279 154
158
101
47
55000
0.23*
6
91
692
20
8
14
34
3
299
1
290
79
48
4
1
87
5
0.17
WAX03281 158
162
99
28
47000
0.14*
5
87
678
19
7
12
32
3
305
1
283
78
44
4
1
84
5
0.16
WAX03282 162
166
1585
711
44000
0.56
5
80
693
18
7
13
31
3
276
1
283
77
44
4
1
80
4
0.16
WAX03283 166
170
2180
711
31100
0.62
2
81
712
18
7
12
29
3
293
1
268
74
42
4
1
82
5
0.16
WAX03284 170
174
460
162
31600
0.58
2
83
757
19
7
12
30
3
318
1
278
78
42
4
1
82
5
0.17
WAX03285 174
178
211
72
42700
0.62
3
85
760
17
7
12
30
3
313
1
290
81
46
4
1
82
5
0.17
WAX03286 178
182
1010
553
50600
0.57
3
77
767
17
6
12
31
3
313
1
302
83
46
4
1
79
4
0.17
WAX03287 182
186
2040
1245
66500
0.60
3
91
903
20
7
14
35
3
359
1
349
96
51
4
1
89
5
0.20
WAX03288 186
190
1350
707
34100
0.73
3
84
816
19
7
13
31
3
332
1
299
85
46
4
1
85
5
0.18
WAX03289 190
194
1230
629
38700
0.81
2
92
763
18
7
12
31
3
323
1
295
83
47
4
1
86
5
0.18
WAX03290 194
198
1490
628
38200
0.91
2
98
819
20
8
13
33
3
341
1
310
87
48
4
1
93
6
0.19
WAX03291 198
202
624
237
25900
0.58
2
84
766
19
8
12
30
3
360
1
286
81
44
4
1
91
6
0.18
WAX03292 202
206
1140
508
29100
0.36*
3
85
713
17
7
12
29
3
331
1
273
76
43
4
1
85
5
0.17
WAX03293 206
210
1025
400
37100
0.36*
2
92
732
19
8
14
32
3
345
1
289
80
45
4
1
89
5
0.18
WAX03294 210
214
593
251
22100*
0.41
2
93
729
21
9
12
33
4
334
1
292
81
46
4
1
105
7
0.18
WAX03295 214
216
1145
412
57300
1.22
2
100
943
23
9
15
39
4
409
1
371
105
56
5
1
107
7
0.22

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* WAX03258, WAX03261 – WAX03281 – Reported Nb values were analysed via lithium borate fusion (ALS LabCode - ME-MS85). These intervals did not trigger the requirement for XRF determination. *** WAX03292 & WAX03293 – Samples are currently undergoing XRF analysis, the values reported in Table 2 represent the upper detection limit value associated with method ME-MS85 (>3600ppm).

* WAX03259 – All reported elements were analysed via 4 acid digest (ALS Lab Code – ME-MS61r), except for P2O5 which triggered the upper detection limit. Overlimit P2O5 analysis was completed via ALS lab code P- OG62 *** WAX03262, WAX03275, WAX03276 & WAX03294, reported P2O5 analysis completed via ALS Lab Code – ME-MS61r, results did not trigger the requirement for overlimit analysis.

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ASX RELEASE
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About WA1

WA1 Resources Ltd is based in Perth, Western Australia and was admitted to the official list of the Australian Securities Exchange (ASX) in February 2022. WA1’s shares are traded under the code WA1.

WA1’s objective is to discover a Tier 1 deposit in Western Australia’s under explored regions and create value for all stakeholders. We believe we can have a positive impact on the remote communities within the lands on which we operate. We will execute our exploration using a proven leadership team which has a successful track record of exploring in WA’s most remote regions.

Forward-Looking Statements

This ASX Release may contain certain “forward-looking statements” which may be based on forward-looking information that are subject to a number of known and unknown risks, uncertainties, and other factors that may cause actual results to differ materially from those presented here. Where the Company expresses or implies an expectation or belief as to future events or results, such expectation or belief is expressed in good faith and believed to have a reasonable basis. For a more detailed discussion of such risks and other factors, see the Company’s Prospectus and Annual Reports, as well as the Company’s other ASX Releases. Readers should not place undue reliance on forward-looking information. The Company does not undertake any obligation to release publicly any revisions to any forward-looking statement to reflect events or circumstances after the date of this ASX Release, or to reflect the occurrence of unanticipated events, except as may be required under applicable securities laws.

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WA1 RESOURCES LTD | ABN: 51 646 878 631 | WWW.WA1.COM.AU | ASX: WA1 WA1 RESOURCES LTD | ABN: 51 646 878 631 | WWW.WA1.COM.AU | ASX: WA1 A: L2 55 CARRINGTON ST NEDLANDS WA 6009 P: +61 8 6478 7866 E: [email protected] A: 2C LOCH ST, NEDLANDS WA 6009 P: +61 8 6478 7866 E: [email protected]

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JORC Code, 2012 Edition – Table 1

Section 1 Sampling Techniques and Data

Criteria Commentary
Sampling techniques
All geological information referred to in this ASX Announcement
was derived from Reverse Circulation drill chips.

From every metre drilled a 2-3kg sample (split) was sub-sampled
into a calico bag via the rig mounted cone splitter. The 1m single
splits were placed in storage pending submission to lab for
submission if the 4m composite sample returned anomalism.

A 4m composite sample was then collected using an aluminium
scoop to sub sample each spoil pile located on the ground
adjacent to the rig. Average sample weights are about 2-2.5kg.
Comments on the mineralisation have been limited to the
observations of the major mineral(s) apparent in the RC chips. 5
samples from PARC003 have been sent for petrographic analysis,
this analysis will aid mineral identification.

Geochemical analysis has determined the presence of a calcio
carbonatite at P2. Geochemical analysis has highlighted the
presence of Niobium and other Light Rare Earth Elements.

The drill chips are from a range of altered and non-altered rocks in
transitional and primary zones from 74m downhole. The initial
74m of sediment and clay were not composite sampled. However,
the original metre splits will be submitted to gain a representative
view from drill hole intersections.

Samples have been sent to the laboratory for assay and will further
inform geological understanding and interpretation.

Petrographic analysis is underway to understand the mineralogy.

Laboratory Analysis - Samples were initially submitted for 4 acid
digest 61 element suite with REE’s - ALS method - ME-MS61r.
Samples that triggered the upper detection limit for Ce
(>500ppm) and Nb (>500ppm) underwent overlimit analysis via
lithium borate fusion (ME-MS85), where Nb triggered the upper
detection limit (>5000ppm) XRF was used for the final
determination via ALS method ME-XRF30. The phosphorus
overlimit method used was P -OG62.

4m composites were submitted for analysis while the 1m splits
directly from the rig sample cyclone were placed into storage. The
1m splits will be assayed.

4m composite sampling was completed from spoil piles with
samples submitted to the laboratory determined by the site
geologist.

All 4m samples from 74m to EOH were submitted to ALS
Laboratories in Perth for analysis by 4 acid digestion with MS/ICP
finish (ALS Code ME-MS61r).

Where the over-limits were triggered, further analysis was
completed via lithium borate fusion, a method of complete
digestion (ALS Method ME-MS85), where over limits values were
further triggered samples underwent XRF determination (ALS
Method ME-XRF30)

All samples were initially analysed via ME-MS61r, however, upon
internal review ALS advised that several samples reporting Nb
values were under reported due to the partial 4- acid digest and
the suspected variable mineralogy of the Niobium occurrence. All
1m splits will be analysed via lithium borate fusion and XRF, both
are methods suitable for Niobium and REE analysis.

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Criteria Commentary
Drilling techniques
Reverse Circulation (RC) drilling was completed at all holes to a
diameter of 114mm.
Drill sample recovery
Sample recoveries are visually estimated for each metre with poor
or wet samples recorded in sample log sheets.

The sample cyclone was routinely cleaned at the end of each 6m
rod and when deemed necessary.

No relationship has been determined between sample recovery
and the mineralisation returned.
Logging
Geological logging of drill holes was done on a visual basis with
logging including lithology, mineralogy, texture, deformation,
alteration, mineralisation, veining, colour and weathering.

Logging of drill chips is qualitative and based on the presentation
of representative chips retained for all 1m sample intervals in the
chip trays.

All drill holes were logged in their entirety.
Sub-sampling
techniques and sample
preparation
RC Drilling

From every metre drilled, a 2-3kg sample was sub-sampled into a
calico bag via the drill rig cyclone splitter.

QAQC in the form of CRMs (OREAS Standards) were inserted at a
rate of 1:50 samples.

4m composite sampling was completed from spoil piles with
samples submitted to the laboratory determined by the site
geologist.

Samples were submitted to ALS Laboratories (Perth) where they
are dried, pulverised and analysed for multi-element
determination via 4-acid digestion with MS/ICP finish (ALS Code
ME-MS61r).

Over-limit assays were completed via Lithium Borate Fusion ALS
Method ME-MS85), where the upper detection limit was exceeded
XRF determinations were completed via ALS Method ME-XRF30

Table 2 notes where method ME-XRF30 was used and reported.

All samples were initially analysed via ME-MS61r, however, the
partial digest failed to liberate all contained Nb. Where the upper
detection limit for Nb was triggered, samples underwent lithium
borate fusion a total digest which highlighted discrepancies
between the results of the partial and total digestion methods.
The Nb did not dissolve fully in the partial digest due to the
suspected variable mineralogy of the Niobium. This resulted in
initial under-reporting, samples have since been analysed via
lithium borate fusion. All 1m splits will be analysed via lithium
borate fusion with XRF determination where required, both are
methods suitable for Niobium and REE analysis. Nb assays
>500ppm underwent lithium borate fusion analysis and samples
>5000ppm had XRF determinations via ME-XRF30
Quality of assay data
and laboratory tests

A 4- acid digest was initially considered an appropriate method of
sample analysis. However, the partial digest failed to liberate all
contained Niobium (Nb), Consequently overlimit analysis was
completed on samples with elevated Ce and Nb via Lithium
Borate fusion, which is considered a total digest. Additional
overlimit analysis was required on Nb via Method ME-XRF30. The
phosphorus overlimit used was P-OG62.

Standard laboratory QAQC was undertaken and monitored by the
laboratory and then by WA1 upon receipt of assay results.

Company standards were inserted and analysed as part of the ME-
MS61r suite. No standards were inserted into the ME-MS85 and

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Criteria Commentary
ME-XRF30 sequences as samples were not analysed via these
methods en masse. Instead, for the lithium borate fusion and the
ME-XRF methods, the laboratory standards have been reviewed by
the company and have passed internal ALS QAQC checks.

Lab QAQC protocol for XRF analysis includes, a quartz blank at the
beginning of every run, whilst the XRF is calibrated using internal
lab standards.
Verification of sampling
and assaying

Drill chips have been viewed and assessed by WA1’s Exploration
Manager for mineralogy and alteration.

Independent petrographic analysis of selected drill chips is being
undertaken by A&A Crawford Geological Research Consultants Pty
Ltd.

Portable XRF readings were taken in the field to aid interpretation.

Logging and sampling was completed manually in the field and
then recorded directly into a digital logging system.

No twinned holes have been drilled at this time.

No adjustments to any assay data have been undertaken.
Location of data points
Drill hole collars were surveyed and recorded using a DGPS.

All co-ordinates are provided in the MGA94 UTM Zone 52 co-
ordinate system with an estimated accuracy of +/-5m.

Azimuth and dip of the drill hole was recorded after completion of
the hole using a gyro. A reading was taken every 50m with an
accuracy of +/-1 degree azimuth and +/-0.3 degree dip.
Data spacing and
distribution

See drill hole table for hole position and details.

Data spacing at this stage is not suitable for Mineral Resource
Estimation.
Orientation of data in
relation to geological
structure

The orientation of mineralisation is unconstrained with only a
single hole having been drilled into the target.

See drill hole table for hole details and the text of this
announcement for discussion regarding the decision to angle the
hole to the south.

Drill holes were designed based on observations from modelled
geophysical data.

True and apparent widths have not been interpreted from the
available data.

No sample bias is known at this time.
Sample security
Sample security is not considered a significant risk with WA1 staff
present during collection.

All geochemical samples were collected, bagged and sealed by
WA1 staff, and delivered to Port Hedland for haulage directly to
ALS Laboratories in Perth.

1m splits are stored in a secure location.
Audits or reviews
The program is reviewed on an ongoing basis by senior WA1 staff.

Section 2 Reporting of Exploration Results

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

Criteria Commentary
Mineral tenement and
land tenure status

The West Arunta Project comprises one granted Exploration
Licence (E80/5173) and four Exploration Licence Applications.

All work completed and reported in this ASX Announcement was
completed on E80/5173 which is 100% owned by WA1 Resources
Ltd.

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Criteria Commentary
Exploration done by
other parties

The West Arunta Project has had limited historic work completed
within the Project area with the broader area having exploration
focused on gold, base metals, diamonds and potash.

Significant previous explorers of the Project area include Beadell
Resources and Meteoric Resources. Only one drill hole (RDD01)
has been completed within the tenement area by Meteoric in
2009, and more recently a second hole proximate to the Project by
Encounter Resources Ltd in 2020.

Most of the historic work was focused on the Urmia and Sambhar
Prospects with historic exploration (other than RDD01) being
limited to geophysical surveys and surface sampling.

Historical exploration reports are referenced within the WA1
Resources Ltd Prospectus dated 29 November 2021 which was
released by ASX on 4 February 2022.
Geology
The West Arunta Project is located within the West Arunta
Orogen, representing the western-most part of the Arunta Orogen
which straddles the Western Australia-Northern Territory border.

Outcrop in the area is generally poor, with bedrock largely covered
by Tertiary sand dunes and spinifex country of the Gibson Desert.
As a result, geological studies in the area have been limited, and a
broader understanding of the geological setting is interpreted
from early mapping as presented on the MacDonald (Wells, 1968)
and Webb (Blake, 1977 (First Edition) and Spaggiari et al., 2016
(Second Edition)) 1:250k scale geological map sheets.

The West Arunta Orogen is considered to be the portion of the
Arunta Orogen commencing at, and west of, the Western
Australia-Northern Territory border. It is characterised by the
dominant west-north-west trending Central Australian Suture,
which defines the boundary between the Aileron Province to the
north and the Warumpi Province to the south.

The broader Arunta Orogen itself includes both basement and
overlying basin sequences, with a complex stratigraphic, structural
and metamorphic history extending from the Paleoproterozoic to
the Paleozoic (Joly et al., 2013).
Drill hole Information
Refer to Table 1 for drill hole details.
Data aggregation
methods

Significant intercepts are weight averaged by length.

No metal equivalents have been reported.
Relationship between
mineralisation widths
and intercept lengths

The true thickness of the mineralisation intersected in the drill
hole is not currently able to be calculated due to limited data.
Diagrams
Refer to Figures provided within this ASX Announcement.
Balanced reporting
All meaningful information has been included in the body of the
text.
Other substantive
exploration data

All material data and information has been included in the body of
this ASX Announcement.

No metallurgical assessments have been completed.
Further work
Further interpretation of drill data and assay results will be
completed over the coming months, including detailed
petrographic analysis.

Additional geophysical surveys are planned to be completed to aid
interpretation and future work programs.

1m split samples will be assayed for intervals of interest.

Additional exploration drilling will be planned.

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