Talonx Resources Limited · ASX:TXR

Talonx Resources — African Mining Summit 2022

55 slides from Talonx Resources's conference presentation, Sep 21, 2022

  1. Slide 1: Kihabe/Nxuu Polymetallic Project

    Kihabe/Nxuu Polymetallic Project African Mining Summit, Botswana, September 2022 Presented by: Jacob Thamage, Resident Director Mount Burgess (Botswana) (Pty) Ltd

  2. Slide 2: Disclaimer: Forward Looking Statement

    Disclaimer : Forward Looking Statement This presentation contains forward looking statements in respect of the projects being reported on by the Company. Forward looking statements are based on beliefs, opinions, assessments and estimates based on facts and information available to management and/or

  3. Slide 3: PL43/2016 – Location

    PL43/2016 – Location

  4. Slide 4: Google Earth Image showing Kihabe and Nxuu Deposits and Gossan Anomaly

    Google Earth Image showing Kihabe and Nxuu Deposits and Gossan Anomaly

  5. Slide 5: PL 43/2016 Extension applied for

    PL 43/2016 Extension applied for: An application to extend PL 43/2016, an area covering 1,000 sq km, has recently been submitted to the Department of Mines. Maintaining the original licence area allows for potential further discoveries of minerals such as Gallium, Germanium and Vanadium Pentoxide, w

  6. Slide 6: Project Development Progress

    Project Development Progress Since being granted Prospecting Licence PL43/2016, project development has progressed. However, during the COVID pandemic, in-field operations were delayed due to restrictions imposed by both Botswana and Australia. From April 2020 to March 2022 travelling from Western A

  7. Slide 7: Work conducted during COVID

    Work conducted during COVID Restrictions during the COVID pandemic, impacting in-field operations, allowed for time to be diverted to in-depth, in-house assessment of both the main Kihabe and Nxuu, primarily Zinc, Lead, Silver, SEDEX Deposits, to determine the best way forward for the project. As th

  8. Slide 8: NXUU Deposit

    NXUU Deposit In-house assessment concluded that attention should be focused on developing the totally oxidised Nxuu Deposit first: • It presents as a low risk, shallow basin shaped Deposit, with a maximum depth of 64m to base of mineralisation. • The average depth to the base of mineralisation of 51

  9. Slide 9: Nxuu Deposit (cont’d)

    Nxuu Deposit (cont’d) • Mineralogical and Metallurgical test work conducted to date , for the purpose of maximising beneficiation within Botswana, has confirmed that: o 93% Zinc, hosted in Smithsonite and 93% Lead, hosted in Cerussite, can be recovered on site through acid leaching. o Vanadium is ho

  10. Slide 10: Nxuu Deposit (cont’d)

    Nxuu Deposit (cont’d) o 81% Vanadium Pentoxide can be recovered on site through gravity separation, then subjecting the tail to flotation using a hydroximate acid for recovery. o Both Gallium and Germanium occur in micas, which can be subject to flotation to produce a concentrate. This should then e

  11. Slide 11: NXUU DEPOSIT DRILL HOLE MAP

    NXUU DEPOSIT DRILL HOLE MAP @ Holes drilled in 2021 showing assays NORTH WEST AREA NXDD = Proposed Hole at “ mount burgess mining

  12. Slide 12: NXUU DEPOSIT SECTION

    NXUU DEPOSIT SECTION 13 135 Deg 9€0G0XN o GOXN| KALAHARI SAND. EOH wert omtege V3ERT WES: VACOT wT FE W/80'T e wEL'6 WATT Wve E 3 3 mount burgess mining

  13. Slide 13: NXUU DEPOSIT SECTION

    NXUU DEPOSIT SECTION 15 135Deg vLOGGXN KALAHARI SAND 315 Deg stad ee ‘t) V8LOT WE 64.55m mount burgess mining

  14. Slide 14: NXUU DEPOSIT SECTION

    NXUU DEPOSIT SECTION 16 g a | | E B/E é “| 8 Fe € ‘S€0GQXN|—~ “Wz 8 26 e 1/386 We'yy | * | | lai: Yertr & ese , gm 8 $35 A a & 96000XN 315 Deg Y/8s'0T WS 4/30 TT WO (wddgzz) widdgzt we fe Sms (wddpey) hf wddeors wddepz wz § (wasrey9)S wadeey'z est 4 5 ES 5 = al z & ES 3/29°TT Wit 1.a7m5! (wddzsp‘t)

  15. Slide 15: NXUU DEPOSIT SECTION

    NXUU DEPOSIT SECTION 17 mount burgess mining Z E a 2 a 3 a a ze aaxn + ou 2 t si no# = mua i 3/36°ST WT re | \ %O'E WT H E £€000XN = aE 58 (wad zgt‘t) ais o wiod ¢99 wz9"9 5 vag wz W/8e'or we f 6LOGAXN. f vEOCaXN t yaszr wet i 2 3 ER z ss i o SF 3 zé ‘WSLOGGXN, io a 3 a ae | a a/9o'oT we 3/30°6 9 ie

  16. Slide 16: NXUU DEPOSIT SECTION

    NXUU DEPOSIT SECTION 19 135 deg £800GXN ZOTGGXN \ (wdderr') \ \ widdgz9 W2's a widdoet wrt a10H Thea MaATIS oval NIZ [3QIXOLNAd wniavNvA) WNINVWYaD wants EOH 52.32m 5s & (weagor’z) Sig fle Bo wddtert weet £5 5 (wddzez) 12m 2,817 ppm (5,028ppm) (wddoze) widdzep wz 3/89 wigg"L mount burgess mining

  17. Slide 17: Kihabe Deposit

    Kihabe Deposit The Kihabe Deposit consists of an upper oxide zone, a transitional zone and a lower sulphide zone. Whilst attention was focused on developing the totally oxidised Nxuu Deposit first, the oxide zone of the oxide/sulphide Kihabe Deposit was assessed to confirm the content of Vanadium Pe

  18. Slide 18: Kihabe Deposit (cont’d)

    Kihabe Deposit (cont’d) Mineralogical and metallurgical test work conducted for the purpose of maximising beneficiation within Botswana confirmed that in the oxide and transitional zones: o Vanadium is hosted in the oxide mineral Descloizite, in which Vanadium Pentoxide is 1.785 times the volume of

  19. Slide 19: Kihabe Deposit (cont’d)

    Kihabe Deposit (cont’d) Mineralogical and metallurgical test work conducted to date, for the purpose of maximising beneficiation within Botswana, has confirmed that in the oxide and upper transitional zones: o 97% Zinc hosted in the oxide mineral Baileychlore, can be recovered on site through solven

  20. Slide 20: Kihabe Deposit (cont’d)

    Kihabe Deposit (cont’d) o 94% Zinc hosted in the sulphide mineral Sphalerite, within the lower transitional zone and sulphide zone can be recovered from flotation concentrates, containing 58% Zinc, transported from site to a smelter. o 84% Lead hosted in the sulphide mineral Galena, within the lower

  21. Slide 21: Kihabe Deposit (cont’d)

    Kihabe Deposit (cont’d) o 96% Silver hosted within the lower portions of the transitional zone and the sulphide zone can be recovered from flotation concentrates transported from site to a smelter. o Mineralogical and metallurgical test work still needs to be conducted on Silver in the oxide and upp

  22. Slide 22: JORC 2012 Indicated/Inferred Resource Estimate for the Kihabe Deposit

    An Indicated/Inferred Resource Estimate compliant with the 2012 JORC Code has recently been compiled for the Kihabe Deposit

  23. Slide 23: Kihabe Resource Metal Content

    KIHABE RESOURCE METAL CONTENT As can be seen, the Kihabe Indicated/Inferred Resource Estimate contains: • 321,000 tonnes of Zinc • 154,000 tonnes of Lead • 5,400,000 ounces of Silver • 10,000 tonnes of Vanadium Pentoxide

  24. Slide 24: Location of Drill Holes Containing Gallium, Germanium and Copper

    LOCATION OF DRILL HOLES CONTAINING GALLIUM, GERMANIUM AND COPPER 2 a) Oo Bae cE SH NYO yo ee 3 % » oy ek gd ee” g eN aN fo go" DRILL HOLES CONTAINING Cu - Se a "2, >? o. xe S 2. Gc (a) % PN Ue ON gi 3, Be ene [pall ro o t 7" soil Geochemical Sampling Area = =~ —= Zinc Soil Anomaly ———— Drill Hole Li

  25. Slide 25: Kihabe Deposit Long Section of the Resource Estimate

    Kihabe Deposit Long Section of the Resource Estimate for Zinc, Lead, Silver and Vanadium Pentoxide

  26. Slide 26: Section showing individual intersections within the oxide zone

    OSs Powers Saat ewe 2 Geerivee © ww swe vs SHOWING INDIVIDUAL INTERSECTIONS FOR Zn, Pb, Ag, V, (V205), Ge, Ga / WITHIN THE OXIDE ZONE ff ad of oe ~ ke ry Vy Ne, % g/ Pa s/ 6/7 152m / | “SN 7 is N SECTION / g N8 / 8 g/ TION g 8 § ORIENTA 8 ae, 8 3 60 Deg =< a =~ ‘4.40m——72.90m—. KALAHARI SAND MINERAL

  27. Slide 27: Kihabe Deposit Zone Section

    SECTION ORIENTATION KIHABE DEPOSIT ZONE 1 SECTION 8 60 Deg > 00204 KALAHARI SAND MINERALISED OXIDISED QUARTZ WACKE DFS» DEPTH FROM SURFACE ‘BHO = DOWN HOLE DEPTH mount burgess mining

  28. Slide 28: Kihabe Deposit Zone Section

    KIHABE DEPOSIT ZONE 1 SECTION 8 00203 KALAHARI SAND MINERALISED OXIDISED QUARTZ WACKE DFS = OEPTH FROM SURFACE ‘BHO = DOWN HOLE DEPTH mount burgess mining

  29. Slide 29: Kihabe Deposit Zone Section

    pai KIHABE DEPOSIT ZONE 1 SECTION 8 60 Deg > KoD202 KALAHARI SAND DFS = DEPTH FROM SURFACE ‘OND = DOWN HOLE DEPTH mount burgess mining

  30. Slide 30: Kihabe Deposit Zone Section

    aecron KIHABE DEPOSIT ZONE 1 - SECTION 8 ORIENTATION 60 Deg > KOD201 KALAHARI SAND MINERALISED OXIDISED QUARTZ WACKE FS = DEPTH FROM SURFACE OHO = DOWN HOLE DEPTH 108 mount burgess mining

  31. Slide 31: Kihabe Deposit Zone Section

    SECTION 3 ORIENTATION KIHABE DEPOSIT ZONE 1 SECTION 8 8 60 Deg > g 24m Fs, MINERALISED OXIDISED 12 WACKE 5 > a om DFS» DEPTH FROM SURFACE HO = DOWN HOLE DEPTH mount burgess mining

  32. Slide 32: Kihabe Deposit Zone Section

    SECTION ° 3 ORIENTATION KIHABE DEPOSIT ZONE 1 SECTION 8 8 60 Deg > i] KALAHARI SAND MINERALISED OXIDISED QUARTZ WACKE GERMANIUM (VANADIUM PENTOXIDE) ZINC LEAD SILVER DFS = DEPTH FROM SURFACE DHD = DOWN HOLE DEPTH pase OF OXIDATION —— pH mount burgess mining

  33. Slide 33: Kihabe Deposit Zone Section

    SECTION orientation KIHABE DEPOSIT ZONE 1 SECTION 8 KDD205 60 Deg > KALAHARI SAND MINERALISED OXIDISED QUARTZ WACKE DFS = DEPTH FROM SURFACE DHD = DOWN HOLE DEPTH mount burgess mining

  34. Slide 34: Zinc and Lead Mineralisation – Section 9900m

    Kihabe Resource – Section 9900m Zinc and Lead Mineralisation 1200m RL KALAHARI SAND 12m below surface OXIDISED 1150m RL FRESH 60m wide 1100m RL 1050m RL 1000m RL DOLOMITE QUARTZ WACKE DOLOMITE QUARTZ WACKE Zinc Model Lead Model

  35. Slide 35: Kihabe Resource – Section 10400mE

    Kihabe Resource – Section 10400mE Zinc and Lead Mineralisation 1200m RL KALAHARI 5m below surface OXIDISED 1150m RL 30m wide 1100m RL FRESH 1050m RL 1000m RL DOLOMITE QUARTZ WACKE DOLOMITE QUARTZ WACKE Zinc Model Lead Model

  36. Slide 36: Kihabe Resource – Section 11600mE

    Kihabe Resource – Section 11600mE Zinc and Lead Mineralisation 1200m RL KALAHARI 12m below surface OXIDISED 1150m RL 45m wide 1100m RL FRESH 1050m RL DOLOMITE DOLOMITE 1000m RL QUARTZ WACKE QUARTZ WACKE Zinc Model Lead Model

  37. Slide 37: Kihabe Resource – Section 11700mE

    Kihabe Resource – Section 11700mE Zinc and Lead Mineralisation 1200m RL KALAHARI 10m below surface OXIDISED 1150m RL 50m wide 1100m RL FRESH 1050m RL DOLOMITE DOLOMITE 1000m RL QUARTZ WACKE QUARTZ WACKE Zinc Model Lead Model

  38. Slide 38: Kihabe - Copper Resource

    Kihabe - Copper Resource An Initial Inferred Resource was estimated as shown below Further drilling and assaying will be required to determine the overall content of: • Copper • Gallium • Germanium

  39. Slide 39: Potential for Further Discoveries

    Potential for Further Discoveries Several other anomalies have been generated in the project area by geochemical soil sampling and assaying for Zinc, Lead, Silver and Vanadium. These all have the potential for adding to the Project’s resource base in the future. Further drilling will be required to

  40. Slide 40: The Gossan Anomaly

    The Gossan Anomaly One of these anomalies is the Gossan Anomaly, shown to contain Zinc, Lead, Silver and Vanadium. Individual selected samples also show the presence of Gallium and Germanium.

  41. Slide 41: Gossan Anomaly – Drill Hole Map highlighting Vanadium Mineralisation

    Gossan Anomaly – Drill Hole Map highlighting Vanadium Mineralisation Holes prefixed with GDD and GRC are diamond core and RC holes drilled by Mount Burgess Mining. Holes prefixed with AP are Billiton drill holes which all intersected Vanadium Mineralisation. The results cannot be reported on under c

  42. Slide 42: Gossan Anomaly – Diamond Core Hole Recoverable Vanadium Pentoxide Grades

    Gossan Anomaly – Mount Burgess Mining Diamond Core Hole Recoverable Vanadium Pentoxide Grades

  43. Slide 43: Gossan Anomaly – Diamond Core Hole Recoverable Vanadium Pentoxide Grades

    Gossan Anomaly – Mount Burgess Mining Diamond Core Hole – Recoverable Vanadium Pentoxide Grades

  44. Slide 44: Gossan Anomaly – RC Drill Holes Recoverable Vanadium Pentoxide Grades

    Gossan Anomaly – Mount Burgess Mining RC Drill Holes Recoverable Vanadium Pentoxide Grades

  45. Slide 45: Gossan Anomaly – Billiton Percussion Drill Holes

    Gossan Anomaly – Billiton Percussion Drill Holes highlighting Vanadium Mineralisation Billiton Percussion drill holes all intersected Vanadium mineralisation. All assay results for V, Zn, Pb and Ag cannot be reported on under current ASX Listing Rules as this drilling was conducted prior to the intr

  46. Slide 46: Worldwide Demand for Metals – Gallium

    Worldwide Demand for Metals of the Kihabe -Nxuu Polymetallic Deposits GALLIUM Gallium, a soft metallic element, is currently used for semi- conductors, blue ray technology, light emitting diodes (LEDs), pressure sensors for touch switches, as an additive to produce low melting-point alloys and in mo

  47. Slide 47: Worldwide Demand for Metals – Gallium (cont’d)

    Worldwide Demand for Metals of the Kihabe -Nxuu Polymetallic Deposits GALLIUM (cont’d) The Fraunhofer Institute System and Innovation Research, expects that by 2030, the worldwide demand for Gallium will be six times higher than the current production rate of around 720 tonnes per annum.

  48. Slide 48: Worldwide Demand for Metals – Germanium

    Worldwide Demand for Metals of the Kihabe -Nxuu Polymetallic Deposits GERMANIUM Germanium is used in fibre optics, infra-red optics, high brightness LEDs used in automobile head lights and in semi-conductors for transistors in thousands of electronic applications. Recently declared as a strategic me

  49. Slide 49: Worldwide Demand for Metals – Vanadium Pentoxide

    Worldwide Demand for Metals of the Kihabe -Nxuu Polymetallic Deposits VANADIUM PENTOXIDE (V2O5 ) V2O5 is a key component for a clean energy future and future energy storage requirements. Given a recent push to replace petrol and diesel with electric power, V2O5 has an exceptionally important part in

  50. Slide 50: Worldwide Demand for Metals – Zinc

    Worldwide Demand for Metals of the Kihabe -Nxuu Polymetallic Deposits ZINC Zinc, which in February 2022 was added to the list of critical minerals by the U.S. Geological Survey, Department of the Interior, has primarily been used for generations in zinc plating for corrosion resistance as with galva

  51. Slide 51: Worldwide Demand for Metals – Zinc (cont’d)

    Worldwide Demand for Metals of the Kihabe -Nxuu Polymetallic Deposits ZINC (cont’d) In September 2021, researchers from the University College of London published a paper on new Zinc based batteries that can be charged directly by light. Vanadium dioxide (VO2) is used as a photocathode for Zinc-ion

  52. Slide 52: Worldwide Demand for Metals – Lead

    Worldwide Demand for Metals of the Kihabe -Nxuu Polymetallic Deposits LEAD Lead, which is corrosion free, is used for lead-acid car batteries, roofing, radiation protection, solders, ammunition and weights. Large-format lead-acid batteries, often referred to as battery banks, are used as storage fac

  53. Slide 53: Worldwide Demand for Metals – Silver

    Worldwide Demand for Metals of the Kihabe -Nxuu Polymetallic Deposits SILVER Silver has primarily been used for generations for the manufacture of jewellery and domestic utensils. It is currently used as a significant material for alternative energy generation in the manufacture of photovoltaic pane

  54. Slide 54: Corporate Details

    Corporate Details Listed on ASX since 1985 ASX Code MTB Shares on Issue 859,171,119 (as at 30 June 2022) Directors Joint Company Secretaries Nigel Raymond Forrester, FCA Jan Forrester Harry Warries, MS Mine Eng., FAusIMM Serene Chau, CPA Robert Brougham, FAusIMM, BSc Karen Clark Registered Office 8/

  55. Slide 55: Wholly owned Subsidiary Mount Burgess (Botswana) Directors

    Wholly owned Subsidiary Mount Burgess (Botswana) (Proprietary) Limited Directors Jacob Thamage, BSc Mine Eng, MBA Nigel Raymond Forrester, FCA Jan Forrester Serene Chau, CPA Company Secretary Kingsway (Pty) Ltd Registered Office C/O BDO Spencer Steward 39a Gaborone International Commerce Park Gaboro

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