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KINGFISHER MINING LTD Capital/Financing Update 2023

Dec 6, 2023

65177_rns_2023-12-06_7eb72fa9-f7b5-4b36-bc1b-2174ddd2860f.pdf

Capital/Financing Update

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ASX KFM

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7 December 2023

ASX Announcement

LK1: Another Compelling Carbonatite Target

High tenor REE surface geochemistry anomalies associated with newly identified carbonatite pipe targets at the large LK1 prospect.

Highlights

  • Several large Rare Earth Elements (REE) anomalies defined at LK1 from surface geochemistry survey, with peak LREO (Light Rare Earth Oxides) value of 0.21%.

  • Anomalies coincide with the new carbonatite pipe targets delineated from the recently completed ground gravity survey and airborne magnetics.

  • Prospectivity of new carbonatite pipe targets also confirmed from highly anomalous rock chip assays, which included 0.12% and 0.10% TREO (Total Rare Earth Oxides).

  • LK1 whilst being largely undercover shares many similarities with the Company’s exciting large high grade carbonatite discovery at Mick Well, which is located 30km east of LK1.

  • Planning underway for maiden drilling at LK1 at the commencement of the 2024 field season as part of a broader drilling program which includes Mick Well.

Kingfisher Mining Limited ( ASX:KFM ) (“ Kingfisher ” or the “ Company ”) is pleased to announce the definition of exciting carbonatite targets at the large LK1 REE target in the highly prospective Gascoyne Province.

Kingfisher’s Executive Director and CEO James Farrell commented: “Our early-stage exploration at LK1 is

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----- Start of picture text -----

LK1
0.12% TREO
0.10% TREO
Legend
Carbonatite pipe target
Soil Survey: LREO (ppm)
120
----- End of picture text -----

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----- Start of picture text -----

Legend
Carbonatite pipe target
Soil Survey: LREO (ppm)
120
170
220
280
450
>1000
----- End of picture text -----

Figure 1: LK1 surface REE geochemistry and carbonatite pipe targets derived from geophysics, oblique three-dimensional view.

P +61 9481 0389 E [email protected]

W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

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progressively revealing another area of extensive carbonatite targets; a very large and exciting target that is 30km west of our well-defined high grade Mick Well Project and has all the right credentials to add a new area of discoveries to the Company’s REE portfolio.

All of our experience with on-going discoveries at Mick Well has been put into action at LK1. As we successfully applied at Mick Well, we have used the geophysics to identify dense, magnetic pipe-like features which appear very-much like carbonatite intrusion centres. We have also completed a soil geochemistry survey to help us target below the thin surficial cover that is present across the LK1 area. The soil geochemistry has revealed several REE anomalies, including a large anomaly with an outstanding peak value of 0.21% LREO that is coincident with one of our high-priority radiometric targets”.

LK1 Carbonatite Pipe Targets

Four large carbonatite pipe targets have been identified at the large-scale LK1 prospect. The carbonatite pipe targets were generated through three-dimensional modelling of the gravity and magnetics data, with areas with more dense and more magnetic rocks identified from the geophysics (Figure 2).

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0.21% LREO
Legend
0.12% TREO Carbonatite pipe target
Soil Survey: LREO (ppm)
Sample locations
120
170
220
280
0.10% TREO
450
500 m
>1000
----- End of picture text -----

Figure 2 : LK1 surface REE geochemistry and carbonatite pipe targets. The REE geochemistry has been calculated from a suite consisting of CeO2, La2O3, Nd2O3 and Pr6O11. The carbonatite pipe targets were derived from three-dimensional modelling of the combined magnetics and gravity geophysics data. Anomalous rock chip results associated with the southwestern carbonatite pipe target as well as the peak soil geochemistry value of 0.21% LREO are also shown.

P +61 9481 0389

E [email protected]

W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

==> picture [280 x 58] intentionally omitted <==

The geophysics modelling method is also the same that was applied by the Company to identify the carbonatite pipe targets at the Mick Well project (see ASX:KFM 23 October 2023), where discovery of highgrade REEs is continuing (see ASX:KFM 23 November 2023).

The two larger pipe targets are both more than 1,000m in diameter, extending from the near surface to depths of more than 1,000m below the ground surface. Surface mapping around the targets has confirmed the presence of ironstones, which have returned anomalous rock chip results of 0.12% and 0.10% TREO. The mapping, geophysics and geochemistry also indicate there are other rock types under cover which are yet to be fully identified.

LK1 Soil Geochemistry Survey

The results from soil geochemistry survey have highlighted several areas with highly anomalous REEs, including a large area with a diameter which extends for more than 2km. The anomalies are based on an LREO suite consisting of CeO2, La2O3, Nd2O3 and Pr6O11. The high magnitude surface geochemistry results which include a peak value of 0.21% TREO are spatially associated with the carbonatite pipe targets identified from the LK1 geophysical surveys (Figure 2). The broad soil anomaly in the northeast of the target area is also coincident with a circular radiometric feature, a highly significant occurrence and one of the key features recognised during the early-stage target identification at Lk1 (Figure 3).

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A B
RC01AR01
RC5
RC01AR02
RC8
MWGS2382: 0.12% TREO
Inset B
RC24
RC01AR04 Legend
Targeting
RC01AR03 RC1 300 ppm LREO contour
MWGS2666: 0.10% TREO RC18 Carbonatite targets
Soil survey extents
Historical Drilling
Rio Tinto Exploration
Barranco Resources
1 km Rock Chips
Anomalous REE results
----- End of picture text -----

Figure 3: Total magnetic intensity (A) and thorium responses coincident with anomalous REE soil geochemistry (B). Anomalous rock chips (blue boxes) and historical drill hole locations (grey boxes) described in Table 1 are also shown.

P +61 9481 0389 E [email protected] W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

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Table 1: Previous historical drilling results from the LK1 target area by Rio Tinto and Barranco (see ASX:KFM 3 April 2023).

Rio Tinto Drill Hole Pathfinder elements: highest from 2m samples1
ARC01AR01 340 ppm Ce, 195 ppm La, 1100 ppm Ba and 1150 ppm P
ARC01AR02 280 ppm Ce, 165 ppm La, 125 ppm Y, 2600 ppm Ba and 3100 ppm P
ARC01AR03 8900 ppm P
ARC01AR04 1250 ppm Ba and 1400 ppm P
Barranco Drill Hole Geology and elevated metals2
RC1 Ironstone with 7m at 0.25% Zn from 20m
RC5 Ironstone with 25m at 0.29% Zn from surface
RC8 Ironstone with 5m at 0.17% Zn from 20m
RC18 Ironstone with 30m at 0.13% Zn from 10m
RC24 Ironstone with 22m at 0.29% Zn from 1m

1 Pathfinder elements in the reporting range are associated with REE mineralisation at MW2.

2 Zinc is associated with the REE mineralisation at MW2. Drill holes not analysed for REEs.

The Carbonatite Exploration Model

The carbonatite intrusion model has a central carbonatite pipe which is comprised of multiple phases of carbonatite intrusion that is surrounded by ring dykes which form around and radial dykes which radiate out from the central intrusion (Figure 4). The carbonatite exploration model envisages alteration of the host country rock into which the carbonatites intrude, with development of sodic (Na) and potassic (K) fenites around the intrusions which often hosts the REE mineralisation (Figure 5). Figure 4: 3D schematic of a carbonatite intrusion Each part of the carbonatite system has characteristics which can be detected by modern exploration techniques, for example:

Figure 4: 3D schematic of a carbonatite intrusion[+]

  • Thorium associated with the REE mineralisation is apparent in the radiometrics.

  • Potassium fenites, the alteration which forms around carbonatites intrusions, is also apparent in the radiometrics.

  • Ferrocarbonatites have high iron content and can appear as magnetic highs in the geophysics.

  • Carbonatites typically have high density and can be distinguished from the country rocks by gravity surveys.

  • ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) remote sensing can detect various minerals and elements, including carbonates, ferrous and ferric iron as well as alumina and magnesium and can assist with of carbonatites and associated alteration.

The combination of these geophysical responses to the carbonatite geology provide a very powerful combination of exploration tools for early stage targeting and project generation.

P +61 9481 0389 E [email protected] W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

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LK1
Legend
Carbonatite
Potassic fenite
Sodic fenite
Carbonatite pipe target
REE veins/dykes
Niobium veins
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Figure 5: LK1 carbonatite pipe targets and the carbonatite associated rare earth element mineralisation model*. The model shows carbonatite intrusions and dykes, areas of potassic fenitisation as well as the late stage REE-bearing dykes and veins.

Gascoyne Exploration Program

Kingfisher is undertaking high impact and value building exploration programs targeting large-scale carbonatite targets along its 54km Chalba target corridor and its 30km long Lockier target corridor. The program will test high priority carbonatite targets across the Company’s belt-scale tenement holding, building upon the significant carbonatite discoveries, which confirmed the presence of high grade REE mineralisation along the Chalba target corridor. In addition, the Company is undertaking exploration for lithium associated with various pegmatite outcrops within its tenements at Chalby Chalby.

The exploration work planned for the 2023 field season will include:

  • Significant on-ground mapping and sampling targeting interpreted "Mt Weld style" carbonatite plugs as well as dyke mineralisation and alteration which can be used to vector towards the large-scale source of intrusions. The results will be used for drill planning of the high priority targets.

  • RC drilling to test carbonatite targets at Mick Well, Kingfisher and Arthur River.

  • Ground-based gravity at LK1 and Mick Well. The gravity survey will be used to model higher density rocks (potential mineralised carbonatites) at depth.

  • Surface geochemical survey over the large-scale high priority LK1 target at Arthur River, where mapping is restricted by deep weathering associated with the highly altered rocks and cover.

P +61 9481 0389 E [email protected] W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

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  • Surface geochemistry at Chalby Chalby to define additional lithium-bearing pegmatite drill targets.

  • Further airborne geophysics to incorporate Mooloo and North Chalba Projects to our early-stage target generation. Magnetics and radiometrics are highly effective for identifying carbonatite mineralisation.

The timeline for the planned and completed activities for 2023 for Kingfisher’s projects are shown below.

Q1 2023 Q2 2023 Q3 2023 Q4 2023
Mick Well – Kingfisher
Targetgeneration
Fieldwork,mappingand targetprogression
Ground-basedgravity
Arthur River
Targetgeneration
Fieldwork,mappingand targetprogression
Surfacegeochemistry (LK1)
RC Drilling*
Ground-basedgravity
Mooloo
Airborne magnetics and radiometrics
Fieldwork,mappingand targetprogression
Chalba
Airborne magnetics and radiometrics
Surfacegeochemistry (ChalbyChalbyLithium)
Boolaloo
Fieldwork,mappingand targetprogression
  • RC drilling to commence in early 2024 to allow time for access and heritage approvals for newly identified targets at Mick Well and LK1.

Upcoming News

  • December 2023: Further results from ongoing mapping and rock chip sampling of the high grade REE system at Mick Well.

About the Kingfisher’s Gascoyne Projects

Kingfisher’s Mick Well REE Project and Chalby Chalby Lithium Project are located in the Gascoyne region of Western Australia where the Company holds exploration licences covering 969km[2] . The tenure is prospective for carbonatite REE mineralisation similar to Hastings Technology Metals’ world-class Yangibana Deposit which includes 29.93Mt at 0.93% TREO[# ] as well as the recent Yin and C3 discoveries of Dreadnought Resources which include mineral resources of 40.82Mt at 1.03% TREO[^ ] (Figure 6). The Company’s Gascoyne tenure is also prospective for lithium-bearing Thirty Three Suite Pegmatites which hosts Delta Lithium’s Yinnetharra Project and has returned drill results of 33m at 1.9% Li2O[*] from Delta’s Malinda Prospect and rock chips results of 4.2% Li2O[+] from Delta’s Jamesons Prospect.

Kingfisher recently made discoveries of hard rock and clay rare earth elements mineralisation at Mick Well. Both styles of mineralisation are associated with carbonatites that intruded along a crustal-scale structural corridor, the Chalba Shear, which extends over a strike length of 54km within the Company’s

P +61 9481 0389 E [email protected] W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

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tenure. The Company has also identified a second structural corridor along the Lockier Shear which extends for 18km across the Company’s Mooloo Project and 12km across the Arthur River Project.

Drilling at the MW2 Prospect has intersected five parallel ferrocarbonatite lodes and associated monazite mineralisation within a 300m wide zone and has returned high-grade REE results with 5m at 2.63% TREO with 0.54% Nd2O3 + Pr6O11, 4m at 3.24% TREO with 0.54% Nd2O3 + Pr6O11, 5m at 1.54% TREO with 0.30% Nd2O3 + Pr6O11, 4m at 1.90% TREO with 0.34% Nd2O3 + Pr6O11 and 3m at 2.52% TREO with 0.41% Nd2O3 + Pr6O11. The results from the ferrocarbonatite mineralisation is 500m northwest of Kingfisher’s breakthrough REE discovery where maiden drilling returned 5m at 3.45% TREO with 0.65% Nd2O3 + Pr6O11 as well as 12m at 1.12% TREO with 0.21% Nd2O3 + Pr6O11 from a separate mineralised lode.

Kingfisher is also advancing its Chalby Chalby Lithium Project with mapping and sampling at Chalby Chalby delineating an area of 3.3km by 3km that includes multiple stacked pegmatites with a cumulative strike length of over 13km and with surface sample results up to 0.61% Li2O.

P +61 9481 0389 E [email protected] W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

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Figure 6: Location of the Mick Well Project in the Gascoyne Mineral Field showing the extents of the Durlacher Suite and Halfway Gneiss. The location of the Yangibana Deposit and Yin and Lyons Projects 100km north of Kingfisher’s projects are also shown.

P +61 9481 0389 E [email protected] W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

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This announcement has been authorised by the Board of Directors of the Company.

Ends

For further information, please contact:

Kingfisher Mining Limited

James Farrell, Executive Director Ph: +61 (08) 9481 0389 E: [email protected]

Media & Investor Enquiries

Peter Taylor, NWR Communications Ph: +61 412 036 231 E: [email protected]

About Kingfisher Mining Limited

Kingfisher Mining Limited ( ASX:KFM ) is a mineral exploration company committed to increasing value for shareholders through the acquisition, exploration and development of mineral resource projects throughout Western Australia. The Company’s tenements and tenement applications cover 1,676km[2] in the underexplored Gascoyne Mineral Fields.

The Company has made a number of breakthrough high grade rare earth elements discoveries in the Gascoyne region where it holds a target strike lengths of more than 54km along the Chalba mineralised corridor and more than 30km along the Lockier mineralised corridor.

To learn more please visit: www.kingfishermining.com.au

Previous ASX Announcements

ASX:KFM: High Grade Discoveries Further Expand REE Carbonatites at Mick Well 23 November 2023.

ASX:KFM: Significant Additional Carbonatites and REE Mineralisation Identified at Mick Well 14 November 2023. ASX:KFM: Broad Lithium Anomalies Identified from Chalby Chalby Soil Geochemistry Survey 26 October 2023. ASX:KFM: Gravity Survey Confirms Carbonatite Pipe Targets at Mick Well 23 October 2023.

ASX:KFM: Further High Grade REE Mineralisation Discovered at Mick Well 3 October 2023.

ASX:KFM: Multiple Stacked Lithium-Bearing Pegmatites Mapped at Chalby Chalby 11 September 2023.

ASX:KFM: Lithium-Bearing Pegmatites Confirmed at Highly Prospective Gascoyne Tenure 7 August 2023. ASX:KFM: Carbonatite Intrusions Confirmed at Large-Scale Chalba Targets 10 July 2023. ASX:KFM: Significant Exploration Program Targets Large-Scale Carbonatites 4 April 2023.

ASX:KFM: High Grade Drilling Results Confirm New MW2 REE Discovery 7 February 2023.

ASX:KFM: MW2 and MW7 Continue to Expand on Latest Surface Sample Results 23 January 2023. ASX:KFM: Assays from MW7 Confirm Another High Grade REE Discovery 29 November 2022. ASX:KFM: New REE Discoveries along Kingfisher’s 54km Target Corridor - MW7 and MW8 24 October 2022. ASX:KFM: Further Exceptional REE Results Extends MW2 Strike Length to 3km 4 October 2022. ASX:KFM: 40% REE Returned from Mick Well 30 August 2022.

ASX:KFM: Latest Drilling Returns High Grade REEs with 5m at 3.45% TREO, including 3m at 5.21% TREO 5 July 2022.

P +61 9481 0389 E [email protected] W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

ASX KFM

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ASX:KFM: Surface Assays up to 21% TREO Define a Further 800m of Outcropping Mineralisation 20 June 2022.

ASX:KFM: High Grade Rare Earths Returned from Discovery Drill Hole: 4m at 1.84% TREO, including 1m at 3.87% TREO 24 March 2022.

ASX:KFM: Significant Rare Earths Discovery: 12m at 1.12% TREO 10 January 2022.

  • ^ ASX Announcement ‘Large, High Confidence Yin Ironstone Resource – Mangaroon (100%)’. Dreadnought Resources Limited (ASX:DRE), 30 November 2023.

  • ASX Announcement ‘Drilling along 8km long Bald Hill - Fraser's trend Increases Indicated Mineral Resources by 50%’. Hastings Technology Metals Limited (ASX:HAS), 11 October 2022.

  • ASX Announcement ‘Stunning new drilling results from Yinnetharra’. Delta Lithium Limited (ASX:DLI), 23 June 2023.

    • ASX Announcement ‘Yinnetharra Lithium Project Continues to Deliver’. Red Dirt Metals Limited (ASX:RDT), 14 April 2023.

Technical Exploration Papers

    • Simandl, G.J. and Paradis, S. 2018. Carbonatites: related ore deposits, resources, footprint, and exploration methods, Applied Earth Science, 127:4, 123-152
  • Elliott, H.A.L., Wall, F., Chakhmouradian, A.R., P.R.Siegfried, Dahlgrend, S., Weatherley, S., Finch, A.A., Marks, M.A.W., Dowman, E. and Deady, F. 2018. Fenites associated with carbonatite complexes: A review. Ore Geology Reviews, Volume 93, February 2018, Pages 38-59.

Total Rare Earth Oxide Calculation

Total Rare Earths Oxides (TREO) is the sum of the oxides of the light rare earth elements lanthanum (La), cerium (Ce), praseodymium (Pr), neodymium (Nd), and samarium (Sm) and the heavy rare earth elements europium (Eu), gadolinium (Gd), terbium (Tb), dysprosium (Dy), holmium (Ho), erbium (Er), thulium (Tm), ytterbium (Yb), lutetium (Lu), and yttrium (Y).

Forward-Looking Statements

This announcement may contain forward-looking statements which involve a number of risks and uncertainties. These forward-looking statements are expressed in good faith and believed to have a reasonable basis. These statements reflect current expectations, intentions or strategies regarding the future and assumptions based on currently available information. Should one or more of the risks or uncertainties materialise, or should underlying assumptions prove incorrect, actual results may vary from the expectations, intentions and strategies described in this announcement. No obligation is assumed to update forward looking statements if these beliefs, opinions, and estimates should change or to reflect other future developments.

Competent Persons Statements

The information in this report that relates to Exploration Results is based on information compiled by Mr James Farrell, a geologist and Executive Director / CEO employed by Kingfisher Mining Limited. Mr Farrell is a Member of the Australian Institute of Geoscientists and has sufficient experience that is relevant to this style of mineralisation and type of deposit under consideration and to the activity that is being reported on 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 Farrell consents to the inclusion in the report of the matters in the form and context in which it appears.

P +61 9481 0389

E [email protected]

W www.kingfishermining.com.au ABN: 96 629 675 216

Unit 2, 106 Robinson Avenue Belmont WA 6104 AUSTRALIA

Annexure 1: Rock Chip Sample Information

Sample ID Easting Northing CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO
MWGS2382 369558 7247246 446 34.4 15.8 10.1 38.4 5.8 194 1.71 184 53 43 6.45 2.17 182 13.21 1229
MWGS2666 369805 7246667 223 33.5 20.4 8.2 38.5 6.8 201 2.50 152 42 33 5.41 2.74 253 16.28 1038

Rock chips reported above a 1000ppm (0.1%) TREO cut-off grade. All sample information is parts per million (ppm).

Annexure 2: Soil Sample Information

Sample ID Easting Northing CeO2 La2O3 Nd2O3 Pr6O11 LREO Sample ID Easting Northing CeO2 La2O3 Nd2O3 Pr6O11 LREO
ARSS0001 367800 7246701 172 86 70 20 348 ARSS0182 370008 7249303 126 80 68 19 293
ARSS0022 368402 7247692 151 69 57 16 293 ARSS0183 370005 7249098 162 77 63 18 320
ARSS0025 368409 7247097 484 215 152 47 898 ARSS0204 370194 7248102 217 96 78 23 414
ARSS0027 368406 7246695 100 92 83 22 297 ARSS0211 370190 7249496 175 147 121 34 478
ARSS0038 367998 7247693 368 179 146 45 739 ARSS0212 370193 7249696 148 71 61 17 297
ARSS0044 368595 7247492 145 98 41 13 298 ARSS0218 370394 7250708 203 122 109 33 466
ARSS0049 368840 7246332 186 97 70 20 373 ARSS0224 370417 7249526 501 222 232 65 1020
ARSS0063 368600 7248496 225 104 82 24 434 ARSS0225 370410 7249306 416 67 66 19 567
ARSS0069 368996 7247896 107 87 78 22 294 ARSS0238 370409 7246709 151 65 54 15 286
ARSS0076 369210 7248510 153 74 55 16 298 ARSS0252 370590 7249301 184 88 73 21 367
ARSS0077 369203 7248306 179 98 64 20 361 ARSS0257 370591 7250300 165 78 72 19 334
ARSS0082 369208 7247310 221 74 79 21 394 ARSS0260 370797 7250897 312 47 43 12 413
ARSS0092 368994 7247110 165 66 56 16 303 ARSS0261 370809 7250698 156 85 71 20 333
ARSS0101 369391 7247103 316 136 125 34 611 ARSS0263 370810 7250296 278 124 123 36 561
ARSS0104 369405 7247702 204 95 83 23 404 ARSS0267 370804 7249502 192 89 67 21 369
ARSS0105 369392 7247895 194 95 71 21 382 ARSS0272 370990 7249497 303 121 108 31 563
ARSS0108 369397 7248501 417 182 163 47 809 ARSS0274 370992 7249895 250 144 105 31 529
ARSS0109 369387 7248717 208 99 79 23 407 ARSS0278 370993 7250711 345 174 143 42 704
ARSS0114 369601 7248305 216 131 47 19 413 ARSS0279 370996 7250906 149 78 59 17 302
ARSS0120 369604 7247090 198 95 75 22 390 ARSS0281 371194 7250691 227 32 33 9 301
ARSS0122 369597 7246700 298 141 139 36 614 ARSS0297 370806 7248107 267 141 89 27 524
ARSS0123 369601 7246494 155 83 70 19 327 ARSS0299 370810 7247703 153 70 59 16 298
ARSS0124 369798 7246492 172 69 86 22 349 ARSS0306 370990 7247695 290 179 87 28 584
ARSS0125 369596 7246296 177 91 69 20 356 ARSS0312 371391 7248492 391 91 85 24 591
ARSS0129 369798 7246699 192 79 89 24 383 ARSS0313 371390 7248690 508 98 98 27 730
ARSS0134 369790 7247697 147 138 45 15 345 ARSS0320 371402 7250900 144 85 62 17 308
ARSS0135 369796 7247895 155 66 69 19 309 ARSS0321 371601 7250905 156 78 61 18 314
ARSS0142 369793 7249299 931 453 343 102 1828 ARSS0324 371609 7250301 142 70 66 19 298
ARSS0148 369795 7250510 328 272 198 54 852 ARSS0325 371603 7250107 244 92 97 27 460
ARSS0149 369796 7250705 155 65 58 16 294 ARSS0326 371606 7249909 195 146 165 41 547
ARSS0150 369794 7250908 173 85 72 20 349 ARSS0327 371598 7249703 149 75 72 19 314
ARSS0156 369608 7249902 780 185 165 46 1176 ARSS0333 371397 7249897 364 184 211 56 815
ARSS0157 369605 7249709 303 168 105 32 608 ARSS0334 371609 7249100 300 142 124 35 600
ARSS0163 369390 7250703 188 107 101 24 420 ARSS0357 371790 7249500 169 76 67 19 332
ARSS0164 369391 7250906 148 78 66 18 310 ARSS0360 371793 7250100 130 98 75 22 326
ARSS0167 369199 7250497 180 84 76 21 360 ARSS0361 371798 7250307 147 61 57 16 281
ARSS0170 369204 7249902 401 238 218 62 918 ARSS0366 372003 7250706 157 66 55 16 295

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Unit 2, 106 Robinson Avenue P +61 9481 0389 Belmont WA 6104 AUSTRALIA E [email protected] ABN: 96 629 675 216 W www.kingfishermining.com.au

Investor Centre

Sample ID Easting Northing CeO2 La2O3 Nd2O3 Pr6O11 LREO Sample ID Easting Northing CeO2 La2O3 Nd2O3 Pr6O11 LREO
ARSS0368 372004 7250295 180 57 51 14 302 ARSS0425 372806 7250505 142 126 100 28 397
ARSS0374 372013 7249115 206 87 80 22 394 ARSS0427 372824 7250106 190 90 70 20 371
ARSS0387 372194 7249305 207 96 97 25 425 ARSS0428 372810 7249910 167 76 62 18 323
ARSS0388 372197 7249502 165 70 58 17 309 ARSS0432 372801 7249107 259 153 146 40 598
ARSS0389 372190 7249699 234 103 91 26 453 ARSS0434 372808 7248711 1157 438 388 113 2097
ARSS0391 372198 7250100 236 120 114 32 502 ARSS0437 372995 7248904 274 137 117 33 561
ARSS0395 372196 7250892 156 79 62 18 315 ARSS0439 373008 7249292 171 87 76 21 355
ARSS0396 372401 7250700 181 94 72 20 367 ARSS0440 372991 7249498 263 127 108 31 529
ARSS0399 372402 7250095 282 127 112 32 552 ARSS0442 373001 7249904 254 102 96 27 480
ARSS0400 372410 7249896 245 110 100 29 484 ARSS0445 373002 7250499 131 99 73 20 323
ARSS0401 372402 7249698 170 79 66 19 333 ARSS0447 372997 7250908 207 91 71 21 390
ARSS0402 372404 7249508 301 265 251 70 887 ARSS0448 373196 7250907 174 82 67 19 342
ARSS0403 372395 7249308 304 167 128 37 636 ARSS0452 373399 7250898 154 76 56 16 303
ARSS0404 372401 7249110 147 99 81 22 348 ARSS0454 373610 7250709 250 107 92 26 475
ARSS0406 372408 7248706 270 137 124 36 566 ARSS0455 373610 7250503 218 104 90 26 437
ARSS0407 372397 7248506 159 70 72 20 321 ARSS0460 373206 7249906 219 111 89 26 444
ARSS0409 372590 7248504 274 56 53 15 398 ARSS0461 373205 7249698 120 114 90 25 348
ARSS0410 372590 7248702 165 79 67 19 330 ARSS0465 373209 7248890 182 72 62 18 334
ARSS0411 372590 7248901 178 106 95 25 404 ARSS0466 373203 7248710 263 77 77 21 438
ARSS0412 372597 7249102 427 184 143 41 794 ARSS0469 373395 7249308 291 181 154 46 672
ARSS0413 372610 7249294 186 181 180 44 591 ARSS0470 373391 7249502 197 94 80 23 393
ARSS0414 372590 7249496 168 87 78 21 355 ARSS0471 373397 7249700 115 109 92 26 342
ARSS0417 372592 7250098 141 74 65 18 298 ARSS0472 373398 7249903 251 57 57 16 381
ARSS0418 372594 7250298 154 83 67 19 323 ARSS0473 373393 7250126 151 65 60 17 293
ARSS0419 372590 7250501 267 111 84 24 486 ARSS0476 373601 7249902 344 14 14 3 375
ARSS0422 372399 7250896 266 46 45 13 369 ARSS0479 373592 7249306 569 64 57 16 707

LREO is calculated from CeO2, La2O3, Nd2O3 and Pr6O11. Soil samples reported above a 288ppm LREO cut-off grade. All sample information is parts per million (ppm).

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Attachment 1: JORC Code, 2012 Edition – Table 1

Section 1 Sampling Techniques and Data

Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Sampling Nature and quality of sampling (eg cut channels, random chips, or specific Rock chip samples were taken as individual rocks representing an outcrop
techniques specialised industry standard measurement tools appropriate to the minerals to give an indication of possible grades and widths that can be expected
under investigation, such as down hole gamma sondes, or handheld XRF from drilling. Individual rock samples can be biased towards higher grade
instruments, etc). These examples should not be taken as limiting the broad mineralisation.
meaning of sampling. Rock chip samples were typically between 1 and 2 kg. The entire sample
Include reference to measures taken to ensure sample representivity and the received by the laboratory was crushed and pulverised to 85% passing 75
appropriate calibration of any measurement tools or systems used. micron.
Aspects of the determination of mineralisation that are Material to the Public A duplicate sample of between 0.1 and 0.2 kg was retained by the
Report. Company for some of the samples reported.
In cases where ‘industry standard’ work has been done this would be relatively Soil samples were collected on a nominal 200m by 200m grid, the entire
simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from sample retained for analysis.
which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other The soil samples were placed in prenumbered sample bags, and packed
cases more explanation may be required, such as where there is coarse gold in sample boxes for transport to the laboratory.
that has inherent sampling problems. Unusual commodities or mineralisation The LK1 gravity survey was completed using a CG5 Autograv gravity meter.
types (eg submarine nodules) may warrant disclosure of detailed information. The station locations were recorded using a CHCi70+ GNSS survey system.
The expected accuracy of the gravity survey is better than 0.02 mGal with
station location accuracy being +/- 0.02m.
The LK1 gravity survey includes 1210 stations and covers an area of 39km2.
The survey was completed on a 200m by 200m grid, with infilling to 100m
by 100m centres in high priority areas.
Drilling Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, No new drilling results are included in this report.
techniques auger, Bangka, sonic, etc) and details (eg 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). _
Drill sample Method of recording and assessing core and chip sample recoveries and No new drilling results are included in this report.
recovery 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.
Logging Whether core and chip samples have been geologically and geotechnically No new drilling results are included in this report.
logged to a level of detail to support appropriate Mineral Resource estimation,
mining studies and metallurgical studies.

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Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Whether logging is qualitative or quantitative in nature. Core (or costean,
channel, etc) photography.
The total length andpercentage of the relevant intersections logged.
Sub-sampling If core, whether cut or sawn and whether quarter, half or all core taken. The entire sample received by the laboratory was crushed and pulverised
techniques If non-core, whether riffled, tube sampled, rotary split, etc and whether to 85% passing 75 micron.
and sample sampled wet or dry.
preparation For all sample types, the nature, quality and appropriateness of the sample
preparation technique.
Quality control procedures adopted for all sub-sampling stages to maximise
representivity of samples.
Measures taken to ensure that the sampling is representative of the in situ
material collected, including for instance results for field duplicate/second-half
sampling.
Whether sample sizes are appropriate to the grain size of the material being
sampled.
Quality of The nature, quality and appropriateness of the assaying and laboratory Samples were analysed by Intertek Genalysis in Perth. The sample analysis
assay data procedures used and whether the technique is considered partial or total. uses a sodium peroxide fusion with an Inductively Coupled Plasma Mass
and laboratory
For geophysical tools, spectrometers, handheld XRF instruments, etc, the Spectrometry and Inductively Coupled Plasma (ICP) Mass Spectrometry
tests parameters used in determining the analysis including instrument make and (MS) and Optical Emission Spectrometry (OES) finish.
model, reading times, calibrations factors applied and their derivation, etc. The quality of the gravity data was monitored during the survey by the
Nature of quality control procedures adopted (eg standards, blanks, contractor. Any stations that did not conform with the quoted
duplicates, external laboratory checks) and whether acceptable levels of specifications were repeated. A daily report which included the QC was
accuracy (ie lack of bias) and precision have been established. provided to Kingfisher for monitoring.
Verification of The verification of significant intersections by either independent or alternative Independent checks or field duplicates were not conducted for rock chips
sampling and company personnel. and are not considered necessary for that type of sample.
assaying The use of twinned holes.
Documentation of primary data, data entry procedures, data verification, data
storage (physical and electronic) protocols.
Discuss any adjustment to assay data.
Location of Accuracy and quality of surveys used to locate drill holes (collar and down- Rock chip and soil sample locations were surveyed using a handheld GPS
data points hole surveys), trenches, mine workings and other locations used in Mineral using the UTM coordinate system, with an accuracy of +/-5m.
Resource estimation. Gravity survey station locations were recorded using a CHCi70+ GNSS
Specification of the grid system used. survey tool with accuracy of +/- 0.02m.
Quality and adequacy of topographic control.

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Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Data spacing Data spacing for reporting of Exploration Results. No new drilling results are included in this report.
and Whether the data spacing and distribution is sufficient to establish the degree
distribution of geological and grade continuity appropriate for the Mineral Resource and
Ore Reserve estimation procedure(s) and classifications applied.
Whether sample compositing has been applied.
Orientation of Whether the orientation of sampling achieves unbiased sampling of possible Rock chip samples are collected to represent the outcrop.
data in structures and the extent to which this is known, considering the deposit type. The nature of the surface outcrops of mineralisation appears to be similar
relation to If the relationship between the drilling orientation and the orientation of key to the mineralisation intersected in drilling, where the interpreted
geological mineralised structures is considered to have introduced a sampling bias, this orientation indicates a true width for the mineralised zone of between 3m
structure should be assessed and reported if material. and 5m.
Sample The measures taken to ensure sample security. Samples were given individual samples numbers for tracking.
security The sample chain of custody was overseen by the Company’s geologists.
Samples were transported to the laboratory in Perth sealed bulka bags.
The digital gravity data is stored in a secure portal be the by the
contractor. Access to the digital portal is provided to the Company and its
consultants.
Audits or The results of any audits or reviews of sampling techniques and data. The sampling techniques and analytical data are monitored by the
reviews Company’s geologists.
External audits of the data have not been completed.
The gravity data was reviewed by external geophysical consultants Mira
Geoscience to evaluate the validity of the data and model the results.

Section 2 Reporting of Exploration Results

Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Mineral tenement
Type, reference name/number, location and ownership including The project area is located 80km northeast of the Gascoyne Junction and
and land tenure agreements or material issues with third parties such as joint ventures, 230km east of Carnarvon.
status partnerships, overriding royalties, native title interests, historical sites, The project includes 12 granted Exploration Licences, E09/2242, E09/2349,
wilderness or national park and environmental settings. E09/2319, E09/2320, E09/2481, E09/2494, E09/2495, E09/2653, E09/2654,
The security of the tenure held at the time of reporting along with any E09/2655, E09/2660 and E09/2661.
known impediments to obtaining a licence to operate in the area. The tenements are held by Kingfisher Mining Ltd.
The tenements lie within Native Title Determined Areas of the Wajarri
Yamatji People and Gnulli People.
All the tenements are in good standing with no known impediments.

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Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Exploration done Acknowledgment and appraisal of exploration by other parties. No previous systematic exploration for carbonatite-associated
by other parties mineralisation had been previously completed.
Exploration for base metals at Kingfisher undertaken was by Pasminco Ltd
in 1994, Mt Phillips Exploration Pty Ltd in 2006 and WCP Resources in 2007.
Exploration for base metals at Mick Well was completed by Helix
Resources Ltd in 1994, WA Exploration Services Pty Ltd in 1996, Mt Phillips
Exploration Pty Ltd in 2006 and WCP Resources in 2007.
Geology Deposit type, geological setting and style of mineralisation. The Company’s tenements in the Gascoyne Mineral Field are prospective
for rare earth mineralisation associated with carbonatite intrusions and
associated fenitic alteration.
The geological models were generated from three-dimensional inversion
models of the total magnetic intensity and gravity data using thresholds
of 0.009 mgal and 0.02 g/cc.
Drill hole A summary of all information material to the understanding of the No new drilling results are included in this report.
Information 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.
Data aggregation
In reporting Exploration Results, weighting averaging techniques, maximum No new drilling results are included in this report and no data aggregation
methods and/or minimum grade truncations (eg cutting of high grades) and cut-off has been applied.
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.

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Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Relationship These relationships are particularly important in the reporting of Exploration No new drilling results are included in this report.
between Results. True width is obscured by thin cover and appears to be similar to intervals
mineralisation If the geometry of the mineralisation with respect to the drill hole angle is intersected in drilling, 3 to 5m.
widths and known, its nature should be reported.
intercept lengths 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’). _
Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts A map showing relevant data has been included in the report.
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 not practicable, All rock chip samples of REE mineralisation have been reported. The
reporting representative reporting of both low and high grades and/or widths should reported sample batches also included some samples collected as part
be practiced to avoid misleading reporting of Exploration Results. of ongoing evaluation of the geology of the area.
A mask was applied to soil survey data to remove samples of transported
cover (~5% of data) prior to use in modelling and interpretation. Masking
of transported cover samples is considered to be standard practice for
assessing surface geochemical anomalies.
Other Other exploration data, if meaningful and material, should be reported All of the relevant historical exploration data has been included in this
substantive including (but not limited to): geological observations; geophysical survey report.
exploration data results; geochemical survey results; bulk samples – size and method of All historical exploration information is available via WAMEX.
treatment; metallurgical test results; bulk density, groundwater,
geotechnical and rock characteristics; potential deleterious or
contaminating substances.
Further work The nature and scale of planned further work (eg tests for lateral extensions On-going exploration in the area is a high priority for the Company.
or depth extensions or large-scale step-out drilling). Exploration to include target-scale acquisition of geochemistry and
Diagrams clearly highlighting the areas of possible extensions, including the geophysics data to define the extents of carbonatites, mapping and rock
main geological interpretations and future drilling areas, provided this chip sampling as well as additional RC drilling.
information is not commercially sensitive.

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