Stavely Minerals Ltd · ASX:SVY
Stavely Minerals — Mines and Wines Conference 2019
85 slides from Stavely Minerals's conference presentation, Sep 30, 2019
Slide 1: Unravelling the Gordian Knot at Thursday's Gossan
For personal use only Unravelling the Gordian Knot at Thursday’s Gossan Mines and Wines Conference 2019
Slide 2: Disclaimer
STAVELY MINERALS For personal use only Disclaimer This presentation contains only an overview of Stavely Minerals Limited (“Stavely" or the “Company”) and its activities and operations. The contents of this presentation, including matters relating to the geology and exploration potential of the Comp
Slide 3: The Evolution of Thinking: Hypothesise, Drill, Observe, Adjust
For personal use only The Evolution of Thinking: Hypothesise, Drill, Observe, Adjust
Slide 4: What clues brought us into the Stavely project?
THURSDAY’S GOSSAN For personal use only What clues brought us into the Stavely project? SNDD001 – 95m Hematite + chalcopyrite = oxidised fluid
Slide 5: What clues brought us into the Stavely project?
THURSDAY’S GOSSAN For personal use only What clues brought us into the Stavely project? SNDD001 – 95m Indications of a strongly acidic fluid = higher up in the porphyry / epithermal system = porphyry preserved
Slide 6: What clues brought us into the Stavely project?
THURSDAY’S GOSSAN For personal use only What clues brought us into the Stavely project? SNDD001 – 156m Indications of a strongly acidic fluid = higher up in the porphyry / epithermal system = porphyry preserved
Slide 7: What clues brought us into the Stavely project?
THURSDAY’S GOSSAN For personal use only What clues brought us into the Stavely project? This graphic is from our prospectus… SNDD001 – from 94.7m • 7.7m at 4.14% copper 1.08g/t gold 77g/t silver - from 154.6m • 9.5m at 2.93% copper 0.44g/t gold 42g/t silver
Slide 8: What clues brought us into the Stavely project?
THURSDAY’S GOSSAN For personal use only What clues brought us into the Stavely project? 1. Copper-gold- silver mineralisation 2. Alteration assemblage said ‘oxidised’ 3. Vuggy silica said higher up in system
Slide 9: Stavely Volcanic Belt
STAVELY VOLCANIC BELT For personal use only Located in the Grampians Stavely Zone Host sequence includes (probable) Late-Proterozoic serpentinised ultramafic and Late-Cambrian turbidites, tuffs, andesitic flows (some hyaloclastite) and dolerite, granodiorite, tonalite, diorite and dacite intrusions
Slide 10: Stavely Volcanic Belt
STAVELY VOLCANIC BELT For personal use only The Stavely Volcanic Belt is exposed or under shallow cover for about 30km south of the Grampians
Slide 11: Stavely Volcanic Belt
STAVELY VOLCANIC BELT For personal use only Stavely has the largest and most strategic tenement holding in the belt • Thursday’s Gossan porphyry • Toora West porphyry prospect • Junction porphyry • Mount Stavely porphyry • Fairview Gold prospect • Wickliffe VMS prospect • Patanga copper prospect
Slide 12: Stavely Volcanic Belt
STAVELY VOLCANIC BELT For personal use only
Slide 13: Thursday's Gossan Chalcocite Blanket
THURSDAY’S GOSSAN PORPHYRY For personal use only Thursday’s Gossan Chalcocite Blanket Inferred Mineral Resources of 28Mt at 0.4% copper1 for 110kt of contained copper 1 reported in compliance with JORC 2012, see ASX announcement 8 September 2015, subsequent Annual Reports and available from www.stav
Slide 14: For personal use only
THURSDAY’S GOSSAN PORPHYRY For personal use only 4km After Spencer, 1996
Slide 15: Pre-IPO Induced Polarisation Survey
THURSDAY’S GOSSAN PORPHYRY For personal use only Pre-IPO Induced Polarisation Survey Identified a +25mV/V chargeability anomaly in the north-central portion of the prospect with no previous drilling >80m depth. Designed 3x deep diamond drill holes to 600m to test.
Slide 16: Pre-IPO Induced Polarisation Survey
THURSDAY’S GOSSAN PORPHYRY For personal use only Pre-IPO Induced Polarisation Survey • Identified a +25mV/V chargeability anomaly in the north-central portion of the prospect with no previous drilling >80m depth. • Designed 3x deep diamond drill holes to 600m to test.
Slide 17: First-pass Drilling
THURSDAY’S GOSSAN PORPHYRY For personal use only First-pass Drilling All 3 initial drill holes intercepted phyllic alteration at expected depths. The plan was to drill through this into the potassic zone. Hit a low-angle structure instead.
Slide 18: For personal use only
THURSDAY’S GOSSAN PORPHYRY For personal use only
Slide 19: For personal use only
THURSDAY’S GOSSAN PORPHYRY For personal use only
Slide 20: What are 'D' veins?
WHAT ARE ‘D’ VEINS? For personal use only ‘D’ veins are late- stage sulphide-rich veins with characteristic sericite alteration selvedges. They should be a ‘yellow brick road’ down to the source porphyry. After Corbett, 2012
Slide 21: Thursday's Gossan Chalcocite Blanket
THURSDAY’S GOSSAN PORPHYRY Thursday’s Gossan Chalcocite For personal use only Blanket not formed on primary low-grade porphyry copper mineralisation Two parallel zones of near-surface high-grade copper mineralisation with associated silver and gold…. These zones correspond to the near- surface expre
Slide 22: RC drilling programme targeting high-tenor zones
THURSDAY’S GOSSAN PORPHYRY For personal use only Completed 20 x drill hole RC drilling programme to target these high-tenor copper, silver and gold zones ✓ Potential for material impact on Mineral Resources update given NO silver and gold ever estimated within the Mineral Resource ✓ Help us understa
Slide 23: Thursday's Gossan RC drilling
THURSDAY’S GOSSAN PORPHYRY Thursday’s Gossan RC drilling For personal use only ➢ 24 metres at 0.64% copper and 1.2 g/t gold including: • 14 metres at 0.82% copper and 1.99 g/t gold including • 1 metre at 0.84% copper and 22.2 g/t gold ➢ 29 metres at 0.53% copper and 0.30 g/t gold to end of hole (EoH
Slide 24: Thursday's Gossan RC Drilling (north section)
THURSDAY’S GOSSAN PORPHYRY For personal use only Thursday’s Gossan RC Drilling (north section) Shallow RC drill results: ➢ 64m at 0.40% copper and 0.19g/t gold, including o 29m at 0.53% copper and 0.3g/t gold to end of hole ➢ 11m at 0.49% copper and 0.29g/t gold, and A number of RC drill holes stopp
Slide 25: Thursday's Gossan Diamond Tails (north section)
THURSDAY’S GOSSAN PORPHYRY For personal use only Thursday’s Gossan Diamond Tails (north section) RC drill holes continued / twinned with diamond drill ‘tails’. Diamond drill results: ➢ 124m at 0.31% copper and 0.12g/t gold, and ➢ 53m at 0.37% copper and 0.15g/t gold, including ▪ 23m at 0.57% copper
Slide 26: Additional diamond drill results
THURSDAY’S GOSSAN PORPHYRY For personal use only Additional diamond drill results: • 314m at 0.11% copper • 283m at 0.16% copper • 194m at 0.16% copper • 85m at 0.35% copper and 0.18g/t gold • 124m at 0.31% copper and 0.12g/t gold • 92m at 0.34% copper and 0.12g/t gold, incl • 30m at 0.50% copper an
Slide 27: Porphyry M veins
For personal use only Porphyry M veins
Slide 28: Follow-up drilling intercepting late 'D' veins in SMD015
THURSDAY’S GOSSAN PORPHYRY For personal use only Follow-up drilling continued to intercept late ‘D’ veins (transitioning to HS-style) in SMD015: ➢ 9m of 2.62% copper and 0.28g/t gold, including • 4m of 5.41% copper and 0.35g/t gold, including ▪ 1m at 14.75% copper and 0.33g/t gold ➢ 4m at 5.85% copp
Slide 29: Magnetite veins intercepted in SMD015
THURSDAY’S GOSSAN PORPHYRY Magnetite veins intercepted in SMD015 could be far more For personal use only important as a proximal indicator to mineralisation +120m intercept of classic porphyry ‘M’ veins: ➢ Typical of gold-rich porphyries ➢ Veins in this photo are similar to the E-1A ‘M’ veins at Cad
Slide 30: Magnetite veins as proximal indicator to mineralisation
THURSDAY’S GOSSAN PORPHYRY Magnetite veins intercepted in SMD015 are important as a For personal use only proximal indicator to mineralisation The veins in this photo are similar to the Cadia Ridgeway E-1B ‘M’ veins see ASX announcement 12/01/2018 and available from www.stavely.com.au
Slide 31: SMD017
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD017 ➢ 80m interval of porphyry ‘M’ veins from 408m to 488m – below the LAS • also with early porphyry ‘A’ veins ➢ The ‘M’ veins in SMD017 display similarities to the Cadia Ridgeway barren E-1A and E-1B veins but – importantly also the E-2 laminated
Slide 32: SMD017 468m
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD017 468m The veins in this photo are similar to Cadia Ridgeway E-1A and E-1B veins and are likely barren but proximal to copper-gold mineralisation see ASX announcement 18/02/2018 and available from www.stavely.com.au
Slide 33: SMD017 470m
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD017 470m The laminated ‘M’ vein in this photo has inter-grown chalcopyrite with the magnetite and is similar to Cadia Ridgeway E-2 veins associated with the early copper-gold mineralisation event see ASX announcement 18/02/2018 and available from w
Slide 34: Where was the porphyry?
THURSDAY’S GOSSAN PORPHYRY For personal use only Where was the porphyry? • By this time, we had noticed that the LAS hosted both a late plagioclase- hornblende porphyry dyke AND copper- gold mineralised late porphyry D veins • The deeper intercepts of the ultramafic contact structure below the LAS d
Slide 35: But wait, there's more
THURSDAY’S GOSSAN PORPHYRY For personal use only But wait, there’s more - Mother Nature has had 500Ma to move the furniture around downstairs… see ASX announcement 5/09/2018 and available from www.stavely.com.au
Slide 36: SMD026
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD026 ➢ Intercepted another major structure below the LAS ➢ The north-south (NS) structure has a component of dextral strike-slip ➢ Higher grades of gold encountered (carbonate / BM-style): ➢ 1m at 5.68g/t gold west ➢ 28m at 0.21% copper and 0.27g/t
Slide 37: Drill Prospecting the NSS
THURSDAY’S GOSSAN PORPHYRY For personal use only Drill Prospecting the NSS ➢ Drilled 6 fences of 2 x holes ‘prospecting’ the NS structure looking for the hotter portion before drilling deeper ➢ SMD035 and SMD036 intercepted M veins on the western side of the NS structure ➢ Drill hole SMD041 has also
Slide 38: Structural offset on both low-angle and north-south structures
THURSDAY’S GOSSAN PORPHYRY For personal use only Structural offset on BOTH the low- angle structure AND the north- south structure The rest of the presentation will deal with a ‘composite’ cross section – it does incorporate a small amount of artistic licence to incorporate what we are seeing across
Slide 39: Composite section - key elements
THURSDAY’S GOSSAN PORPHYRY For personal use only Composite section - key elements 1. Pre-mineralisation host units are: • Sandstone/siltstone • Andesite flows • Serpentinite 2. Pre- / Syn –mineralisation intrusions include: • Quartz diorite porphyry • Micro-diorite porphyry • High-P microdiorite • D
Slide 40: Composite section - key elements
THURSDAY’S GOSSAN PORPHYRY For personal use only Composite section - key elements 4. Aplite vein-dykes and porphyry A- M veins 5. Porphyry M veins i. Magnetite ± quartz ii. Quartz with magnetite margins ± magnetite centrelines iii. Laminated M veins 6. Late dacite and lamprophyre dykes
Slide 41: SMD042 and SMD044
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD042 and SMD044 ➢ SMD042 drilled just prior to Christmas ➢ Intercepted the NS structure 225m earlier than expected ➢ Required a re-think of the structural geometries 1. The LAS was not mineralised to the north but was to the south 2. The NS structur
Slide 42: Hypothesise, Drill, Observe, Adapt
HYPOTHESISE, DRILL, OBSERVE, ADAPT For personal use only
Slide 43: New Age Relationships
For personal use only New Age Relationships
Slide 44: New Kids in Town
For personal use only NEW KIDS IN TOWN
Slide 45: Thursday's Gossan Stratigraphy / Intrusive History
Thursday’s Gossan Stratigraphy / For personal use only Intrusive History ➢ Early ‘Victor’ porphyry synchronous with Bushy Creek Granodiorite and Buckeran Dolerite ➢ Then the high-phosphorous microdiorite ➢ Then the quartz diorite porphyry (QDP) ➢ QDP is cut by pyritic late porphyry D veins that must
Slide 46: Lithogeochemistry of Younger Porphyries
For personal use only Lithogeochemistry of Younger Porphyries
Slide 47: Later porphyries plot in sub-alkalic fields
THURSDAY’S GOSSAN PORPHYRY For personal use only The later set of porphyries and host units plot largely in the sub-alkalic fields with a few samples plotting just into the alkalic zone Na2O + K2O SiO2
Slide 48: Loucks' Fertility Plot
THURSDAY’S GOSSAN PORPHYRY For personal use only Loucks’ Fertility Plot The late porphyries plot well into the Cu+Au productive intrusion field
Slide 49: Loucks' Fertility Plot
THURSDAY’S GOSSAN PORPHYRY For personal use only Loucks’ Fertility Plot The late porphyries plot well into the Cu productive intrusion field - this ratio not 100% discriminant for gold-rich porphyries but many giant Cu+Au porphyries do plot in this field
Slide 50: MORB normalised spidergram
THURSDAY’S GOSSAN PORPHYRY For personal use only 1000 diorite QDP ➢ Host rocks at Thursdays Gossan have the trace monzogabbro tonalite element signature of arc magmas: enriched in dacite 100 basalt K and Pb; depleted in Ti and Nb relative to andesite microdiorite MORB LKD high P microdiorite basalt
Slide 51: V/Sc ratio maps the hydrothermal system
THURSDAY’S GOSSAN PORPHYRY For personal use only V/Sc ratio maps the hydrothermal system very well The histograms on the drill hole trace are the mag sus. M vein interval in drill hole SMD017 located below the LAS (mustard) and east of the NSS (green). The high V/Sc values (coloured hole trace) are
Slide 52: SWIR data
For personal use only SWIR data
Slide 53: Multiple alteration events complicate SWIR mineralogy
THURSDAY’S GOSSAN PORPHYRY For personal use only Multiple alteration events complicates the spatial distribution of SWIR alteration mineralogy 1. Early prograde weak K-spar alteration of the groundmass 2. Retrograde sericite / pyrite overprint 3. Prograde early dark micaceous (EDM) 3 vein 4. Prograd
Slide 54: Chlorite Composition
THURSDAY’S GOSSAN PORPHYRY For personal use only Chlorite Composition ➢ Same scene – SMD017 M vein interval ➢ Longer-wavelength chlorite absorption features reflecting iron-rich chlorites ➢ Interpreted to be higher-level and a product of a lower pH fluid
Slide 55: Illite Crystallinity
THURSDAY’S GOSSAN PORPHYRY For personal use only Illite Crystallinity ➢ Same scene – SMD017 M vein interval ➢ Lower crystallinity illite ➢ Interpreted to be higher-level and cooler
Slide 56: SWIR trends from SMD015 to SMD024
THURSDAY’S GOSSAN PORPHYRY For personal use only SWIR trends – consistent change from SMD015 / 016 above the LAS to SMD017 under the LAS to SMD024 to the north ➢ Chlorites transition from iron-rich to a mixed iron-magnesium ➢ Illite crystallinity increases ➢ Sericite absorption features move to shor
Slide 57: Sulphur Isotopes
For personal use only Sulphur Isotopes
Slide 58: Sulphur isotope analyses at Thursday's Gossan
THURSDAY’S GOSSAN PORPHYRY number of analyses use only 35 Some 220 ɗ34 sulphur samples have been 30 chalcopyrite determined at pyrite 25 Thursday’s Gossan with: For personal 20 Max 7.35‰ Min -37.69 15 Mean -1.87 10 Standard Deviation ± 4.15 Of which 65 samples returned ɗ34 5 sulphur isotope values l
Slide 59: Cadia Ridgeway sulphur isotopes
THURSDAY’S GOSSAN PORPHYRY For personal use only Cadia Ridgeway sulphur isotopes (adapted from Wilson, 2007) -3‰ ɗ34 sulphur isotope best maps out the ore zone at Cadia Ridgeway
Slide 60: Lighter S isotopes associated with later porphyries
THURSDAY’S GOSSAN PORPHYRY For personal use only Lighter S isotopes associated with the later porphyries Interpreted to reflect: 1. Proximity to the magmatic source 2. The strongly oxidised fluid responsible for mineralisation 3. Given we are not yet in the ‘core’ potassic alteration / mineralisatio
Slide 61: The Penny Drops
For personal use only The Penny Drops
Slide 62: SMD042 and SMD044
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD042 and SMD044 ➢ SMD042 drilled just prior to Christmas ➢ Intercepted the NS structure 225m earlier than expected ➢ Required a re-think of the structural geometries 1. The LAS was not mineralised to the north but was to the south 2. The NS structur
Slide 63: SMD044
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD044 ➢ Large low-grade intercept of 952m at 0.23% copper – reflects a very large system ➢ Included 70m of chalcopyrite mineralisation – 70m at 0.51% copper including: • 10m at 2.43% copper and 0.30g/t gold ➢ Intercepted another interval of chalcopyr
Slide 64: SMD044
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD044 Silica-pyrite mineralisation cut by bornite-chalcocite at 924.3m see ASX announcement 18/02/2019 and available from www.stavely.com.au
Slide 65: SMD044W1
THURSDAY’S GOSSAN PORPHYRY For personal use only SMD044W1 ➢ Large low-grade intercept of 393m at 0.32% copper ➢ Intercepted another interval of chalcopyrite- bornite-chalcocite-covellite mineralisation: • 18m at 3.62% copper, 0.28g/t gold and 15g/t silver, including o 7m at 7.74% copper, 0.46g/t gol
Slide 66: SMD044W1
STAVELY MINERALS For personal use only SMD044W1 392m at 0.32% copper incl. • 18m at 3.62% Cu, 0.28g/t Au and 15g/t Photo 1. Pyrite vein with bornite-covellite-chalcocite(+-digenite) veining at 859.0m in Ag, including: SMD044W1. • 7m at 7.74% Cu, 0.46g/t Au and 32g/t Ag, including: • 2m at 15.7% Cu,
Slide 67: Copper Lode Splay (CLS)
THURSDAY’S GOSSAN PORPHYRY For personal use only Copper Lode Splay (CLS) Intercepted in a couple of shallower holes: ➢ STRC019D – 3m at 2.65% copper and 1.17g/t gold ➢ SMD015 - 9m of 2.62% copper and 0.28g/t gold from 248m, including • 4m of 5.41% copper and 0.35g/t gold, including ▪ 1m at 14.75% co
Slide 68: Copper lode-style mineralisation from 542.5m in SMD032
THURSDAY’S GOSSAN PORPHYRY For personal use only Copper Lode-style (think Magma Mine veins) pyrite-chalcopyrite-bornite-covellite-chalcocite mineralisation from 542.5m in SMD032 – note the chalcocite occurs as late network veins within the more massive sulphides see ASX announcement 18/12/2018 and a
Slide 69: Copper Lode Splay
THURSDAY’S GOSSAN PORPHYRY For personal use only Copper Lode Splay These structures are very important: • They are a genuine exploration target in their own right – high grade, intercepted over 400m vertically and ~500m along strike – an analogy would be the Magma Mine, Superior Arizona or the veins
Slide 70: Magma Mine and the Resolution Porphyry
MAGMA MINE AND THE RESOLUTION PORPHYRY For personal use only Magma Mine and the Resolution Porphyry Can follow the Magma copper lode veins to the Resolution copper porphyry: 1.8Bt at 1.53% copper (Rio Tinto, 2018)
Slide 71: For personal use only
Off section mineral Zonation sphalerite -Ag lower sulphidation bornite tennantite digenite enargite chalcopyrite | _ Magma Mine No 9 shaft surface 1 replacement deposit pyrite bornite chalcocite digenite + covellite enargite chalcocite-bornite bornite-chalcocite digenite pyrite-chalcopyrite quartz A
Slide 72: Magma Vein Long Section
For personal use only MAGMA VEIN LONG SECTION Sulphides are zoned from arsenical copper sulphides typical of high-sulphidation mineralisation through intermediate sulphidation to low sulphidation. Gold has an affinity with the distribution of bornite.
Slide 73: Butte Montana Composite Plan / Section
BUTTE MONTANA COMPOSITE PLAN / SECTION For personal use only Bute Montana sulphide zonation Sulphides are zoned from arsenical copper sulphides typical of high-sulphidation mineralisation through intermediate sulphidation to low sulphidation. Gold has an affinity with the distribution of bornite.
Slide 74: Stavely Project schematic cross sections
641 297m 5B 727mN (641. 680mE SAI S7mE Fo “a, 586 727mN 641 BBE 641 87mE sue [1 Quattz Dovite = wa Dace I peaboroes Lb Micro-diorite (Ey Hig masnestum — Sandtone,sittonc, aides TD Seventnite [EJ Advanced arginic [] Aceittic [] Propytitic [Ey Ponte [EJ strong pryite [Ey sodic ~A00m 3. a 1 oV stavety
Slide 75: Thursday's Gossan sulphide zonation
For personal use only THURSDAY’S GOSSAN Sulphide zonation • Early massive pyrite then brecciated and filled with later copper sulphides. • Sulphides are zoned from deeper arsenical copper sulphides typical of high- sulphidation mineralisation through intermediate sulphidation to low sulphidation. •
Slide 76: Structural control to high grade copper, gold and silver
For personal use only THURSDAY’S GOSSAN Structural control to high grade copper ± gold and silver mineralisation • Three major structures (that we know of…) - • The north-south structure (NSS) • The copper lode splay (CLS) • The ultramafic contact fault (UCF)
Slide 77: Structural control to high grade copper-gold-silver mineralisation
For personal use only THURSDAY’S GOSSAN Structural control to high grade copper-gold-silver mineralisation • Three major structures (that we know of…) - • The north-south structure (NSS) • The copper lode splay (CLS) • The ultramafic contact fault (UCF)
Slide 78: Extremely high grades on the ultramafic contact
For personal use only THURSDAY’S GOSSAN Extremely high grades on the ultramafic contact • The ultramafic has been serpentinised during metamorphism • Abundant magnetite – possible reaction with fluids enhancing grade • Low pH – dissolves the serpentinite and deposits nickel and cobalt
Slide 79: SMD050
THURSDAY’S GOSSAN For personal use only SMD050 (BTW it only took us 50 drill holes to get here…) • 32m at 5.88% copper, 1.00g/t gold and 58g/t silver, from 62m drill depth including • 12m at 14.3% copper, 2.26g/t gold and 145g/t silver from 82m, including • 2m at 40% copper, 3.00g/t gold and 517g/t
Slide 80: Extremely high grades on the ultramafic contact
For personal use only THURSDAY’S GOSSAN Extremely high grades on the ultramafic contact • The ultramafic has been serpentinised during metamorphism • Abundant magnetite – possible reaction with fluids enhancing grade • Low pH – dissolves the serpentinite and deposits nickel and cobalt
Slide 81: Other Opportunities - Junction
OTHER OPPORTUNITIES - JUNCTION 1 For personal use only Aircore hole TGAC078 • 57m at 2.43% copper and 22g/t silver to EoH • 6m at 0.16g/t gold
Slide 82: Conclusion
For personal use only Conclusion
Slide 83: Take Away Messages
TAKE AWAY MESSAGES For personal use only 1. Stavely has demonstrated that there are multiple porphyry phases at Thursday’s Gossan 2. Hosts structurally-controlled high-grade lode-style copper-gold-silver mineralisation similar to Magma, Arizona and Butte, Montana 3. Lots of ‘room to move’ – early da
Slide 84: Tips for Success
TIPS FOR SUCCESS For personal use only 1. Hypothesise, Drill, Observe, Adapt 2. Build a diverse team – its an impediment to progress if all are thinking the same way 3. Choose you consultants carefully, get them involved early and bring them along with you 4. Collect your data systematically and use
Slide 85: Thank You
STAVELY MINERALS For personal use only Thank You Contact Us: Stavely Minerals Limited Level 1, 168 Stirling Highway Nedlands WA 6009 www.stavely.com.au info@stavely.com.au Ph: 08 9287 7630 The information in this presentation is extracted from information available to view on www.stavely.com.au. The