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KINGSTON RESOURCES LIMITED — AGM Information 2019
Nov 5, 2019
65206_rns_2019-11-05_19d40879-9eca-48c6-95af-b9d11bc3ed93.pdf
AGM Information
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Misima Exploration Update
Annual General Meeting Stuart Hayward, Exploration Manager 6 November 2019
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ASX: KSN
www.kingstonresources.com.au
Disclaimer
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Forward Looking Statements
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Certain statements contained in this presentation, including information as to the future financial or operating performance of Kingston Resources Limited (“KSN”) and its projects, are forward looking statements. Such forward looking statements:
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include, among other things, statements regarding incomplete and uncertain proposals or targets, production and prices, operating costs and results, capital expenditures, and are or may be based on assumptions and estimates related to future technical, economic, market, political, social and other conditions;
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are necessarily based upon a number of estimates and assumptions that, while considered reasonable by KSN, are inherently subject to significant technical, business, economic, competitive, political and social uncertainties and contingencies; and
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involve known and unknown risks and uncertainties that could cause actual events or results to differ materially from estimated or anticipated events or results reflected in such forward looking statements.
KSN disclaims any intent or obligation to update publicly any forward looking statements, whether as a result of new information, future events or results or otherwise. The words “believe”, “expect”, “anticipate”, “indicate”, “contemplate”, “target”, “scope”, “plan”, “intends”, “continue”, “budget”, “estimate”, “may”, “will”, “schedule” and similar expressions identify forward looking statements. All forward looking statements made in this presentation are qualified by the foregoing cautionary statements. Recipients are cautioned that forward looking statements are not guarantees of future performance and accordingly investors are cautioned not to put undue reliance on forward looking statements due to the inherent uncertainty therein.
Disclaimer
No representation or warranty, express or implied, is made as to the fairness, accuracy, completeness or correctness of the information, opinions and conclusions contained in this presentation. To the maximum extent permitted by law, none of KSN, its directors, employees or agents, nor any other person accepts any liability, including, without limitation, any liability arising out of fault of negligence, for any loss arising from the use of the information contained in this presentation. In particular, no representation or warranty, express or implied is given as to the accuracy, completeness or correctness, likelihood of achievement or reasonableness or any forecasts, prospects or returns contained in this presentation nor is any obligation assumed to update such information. Such forecasts, prospects or returns are by their nature subject to significant uncertainties and contingencies.
The information contained in this presentation is for informational purposes only and does not constitute an offer to issue, or arrange to issue, securities or other financial products. The information contained in this presentation is not investment or financial product advice and is not intended to be used as the basis for making an investment decision. The presentation has been prepared without taking into account the investment objectives, financial situation or particular needs of any particular person. Before making an investment decision, you should consider, with or without the assistance of a financial adviser, whether an investment is appropriate in light of your particular investment needs, objectives and financial circumstances. Past performance is no guarantee of future performance.
Competent Persons Statement
The information in this report that relates to Exploration Results and Mineral Resources is based on information compiled by Mr Stuart Rechner BSc (Geology) MAIG, a Competent Person who is a member of the Australian Institute of Geoscientists. Mr Rechner is a Director of the Company. Mr Rechner has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity being undertaken 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 Rechner consents to the inclusion in this report of the matters based upon the information in the form and context in which it appears.
The technical and scientific disclosure of the Misima Indicated and Inferred Mineral Resource estimate has been reviewed and approved by Mr Scott Andrew McManus, a Member of the Australasian Institute of Geoscientists and a Registered Professional Geologist (Information Geoscience And Mining), and a full time employee of Skandus Pty Ltd who is a competent person as defined in the 2012 Edition of the “Australasian Code for reporting of Exploration Results, Mineral Resources and Ore Reserves” (JORC Code). Mr McManus is independent of KSN and has reviewed and approved the contents of this news release with respect to the Mineral Resource estimate.
Exploration by Other Explorers
This presentation contains information sourced from the reports of Other Explorers. References to the original reports are provided as footnotes where the information is cited in this presentation. KSN does not vouch for the accuracy of these reports. KSN has taken the decision to include this information as it is in the public domain and as we assess it to be of relevance to shareholders and investors.
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Misima Exploration Update
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Geological Framework and Prospectivity
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Key Prospects & Exploration Results
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Misima North
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Umuna East
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Quartz Mountain
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Ewatinona
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Abi
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The way forward
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Overview of Misima Mineral System
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Carbonate Base Metal Au system
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Au mineralisation
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Multiphase
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High-grade assoc. with later event
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Mineralisation is structurally controlled
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Compound structures
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WNW, NW, N-S & E-W trending structures
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Reactivated over time
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Dilatant over longer periods of time
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Reactivation of existing structures by N-S compression
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Developed in a range of lithology units (Granite, Greenstone, Structures)
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Misima Gold Project – Regional Setting
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Structure is key to definition and discovery
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Consistent structural grain across EL1747
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Complexity due to regional tectonic history
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Mineralisation associated with reactivated structures
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Opening of the Woodlark Basin (Pliocene) may induce N-S compression and subsequent dextral movement on pre-existing structures at the time of mineralisation
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Skandus 2017; Compiled by D G Jones based on Eggers (1996).
- Consistent with 4Ma-3.2Ma Age Epithermal mineralisation
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Skandus 2017; Compiled by D G Jones from Esser 1996).
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Skandus 2017; Corbett 2005
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Key Geological Criteria
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Mineral system style and key exploration vectors first described by Leach 1996 and further developed by Placer and Kingston
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Underlying mineral systems model is well established and robust
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Structure Architecture is key
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Reactivated predominantly steep dipping structures controlling high grade at Umuna
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Some flatter structures
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Competent (brittle) host
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All lithologies within the Sisa Association can act as brittle hosts
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Greenstone & granitic intrusions
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Silicified country rock
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Targeting
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Tend towards magmatic-hydrothermal + meteoric fluid interaction models for system formation • Structures passing through and adjacent to brittle host rocks
- Directly impacting targeting criteria and exploration approach
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Misima Gold Project
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Misima North
Quartz Mountain
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Location and Geography
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EL1747
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Encompasses the eastern end of Misima Island
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Core project areas
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Quartz Mountain
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Umuna
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Umuna East
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• Kulumalia
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Misima North
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Geology & Structure - Regional Interpretation
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Regional Geology and Structure
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Well established geology foundation
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Extensive mapping database
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Surface geology generally reliable with local variation between authors
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Geology by Benko used as regional scale underlay
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The structure grain of Misima Island has been described and interpreted in detail over time with framework reported by Esser 1996 being ratified by subsequent authors.
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Reconnaissance scale review of geophysics data sets reinforces the framework with a complex interplay of WNW, NW, E-W and N-S trending structures.
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Mineral system first described as CBM-Au system by Leach 1996
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Further detailed by later authors
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Umuna Fault Corridor
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M Nth
U-UE
Ewat
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Cameron 2019
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Umuna Fault Corridor
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Compound structural corridor
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Not a single structure
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Reactivation of pre-existing structures
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Retains components of all the dominant structure trends mapped across Misima
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High-grade mineralisation at Umuna occurs within reactivated and intersection of structures within the Umuna Fault Corridor
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Soil geochemistry anomalism distribution is controlled by the prevailing structure architecture
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Misima Nth and Ewatinona can be interpreted as sitting on a regional scale N-S trending lineament
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Umuna & Umuna East can also be interpreted as being controlled by a parallel N-S trending lineament
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Misima Exploration Targets
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3 main target areas (Quartz Mountain; Umuna East; Misima North)
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Advanced prospect scale work on specific targets within each area
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Target: Near surface oxide and near-surface mineralisation beneath geochemical anomalies and on mineralised structures
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Strategy: Complete target definition and testing to develop mineralisation model and target definition based on surface and drill hole geology & geochemistry
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Misima North - Ara
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Anomalous gold in soil geochemistry
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Historic workings
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Significant structures
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Misima North - Ara
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Ara/Kumauwe
Interpreted
Geology
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Work Program
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Review and compile historical data
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Surface auger geochemistry grid over wider area
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3 hand trenches across interpreted structure coincident with surface geochemistry
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10 hole drilling program to assess NW structure trend
Status
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Anomalous gold geochemistry in trenches & auger samples
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Interpreted NW trending structure/target
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Forecast drilling complete late November
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Umuna East – Diamond Drilling
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Work Program
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13 holes drilled for 1469.6m @ Oct 31[st]
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TD range from 63 to 153m
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3 holes remain in the program
Status
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Surface geology interpretation complete
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Drill holes intersect multiple narrow structures interpreted as WNW to NW trending
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Umuna East – Diamond Drilling
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Drill Hole Geology
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Drilling focussed on potential oxide resource within US$1400 pit shell
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Main trend orientated sub-parallel to Umuna trend ~ 310[o] (G) and moderate dip to NE
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Subsidiary splays orientated ~ 050[o] (G) and moderate to steeply dipping NW
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Umuna East
Umuna
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Quartz Mountain -Ewatinona
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Quartz Mountain -Ewatinona
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Highlights from the drilling include:
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20m @ 1.81g/t Au, from 78m, including 3m @ 7.48g/t Au, GDD035
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6.6m @ 1.94g/t Au, from 7.5m, and 2.0m @ 1.65g/t Au, from 31m, GDD037
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2.5m @ 1.99g/t Au, from 85m, and 8m @ 2.6 g/t Au, from 133.7m, GDD029
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3.2m @ 2.41g/t Au, from 90m, GDD030
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5.4m @ 1.51g/t Au, from 67.7m, GDD031
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1.5m @ 2.89g/t Au, from 41.3m, 7.7m @ 1.02g/t Au, from 81.3m, and 7m @ 2.24g/t Au, from 102m, and 2m @ 4.18g/t Au, from 132.2m, GDD032
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4m @ 2.17g/t, from 82m, GDD033
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2m @ 2.15g/t Au, from 92m, and 11m @ 1.40g/t Au including 3m @ 2.08g/t Au, from 122m, GDD040
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Quartz Mountain -Ewatinona
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Veins and breccia (Structures)
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Qz-Carbonate-Sphalerite-Galena +/- Pyrite
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Multistage veining
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Gold mineralisation late stage
Highlights from GDD042:
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15.7m @ 1.60g/t Au; including 7.0m @ 3.19g/t Au,
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and including 0.8m @ 8.19g/t Au
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0.5m @ 2.13g/t Au
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3.9m @ 1.86g/t Au; including 0.6m @ 8.04 g/t Au
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1.7m @ 1.46g/t Au
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Quartz Mountain – Ewatinona Geology Model
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GDD042
- Mineralisation is structurally controlled
3.9m @ 1.86g/t Au from 109.7m Incl. 0.6 @ 8g/t Au from 113m
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WNW (110[0] G)and E-W trending structures
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Subvertical to steep dipping; sub-parallel
Angled Hole @ -50[0] Veins @ 30-50[0] tca
- All primary lithologies are host rocks to mineralisation
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GDD029
- Veins and breccia zones
8m @ 2.60g.t Au from 133.7m
- Early Quartz-Pyrite
Vertical Hole
- Later Qz-carbonate-base metal sulphides
Veins @ 0-15[0] tca
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Galena + Yellow Sphalerite
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Silicification + Sericite-Illite-Pyrite alteration selvages
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Drusy to massive Qz-Cb-BMS veins within structures & stockwork zones and crackle fracture zones
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Breccia zones better developed at structure intersections
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Placer mined high grade breccia at structure intersections
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Quartz Mountain - Ewatinona
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Forward Work Program
Resource definition commencing this quarter
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Modelled structures within and outside US$1200 pit shell
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Infill and extension targets
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Phase 2 drilling program designed
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Quartz Mountain - Abi
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- GDD044 breccia unit 23.6m @ 2.91g/t Au from 7.4-
33.0m
- Not intersected by the Placer RC holes. The breccia unit could be shallow, north east dipping, and is possibly controlled by the WNW, NE dipping Abi fault.
Forward Plan: Follow-up GDD044
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Steep dipping mineralised zones interpreted from drill hole and mapping
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3 hole concept follow-up program
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Quartz Mountain - Abi
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Abi Mineralised Structure Modelling
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Placer holes & GDD041, GDD043 & GDD044 assays
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Same mineralisation trend parameters as Ewatinona
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Resolving onto stacked steep dipping structures
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Initial testing with GDD044 follow-up drilling
Forward Plan
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Hand trenches across projections of interpreted mineralised trends
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Reopen access to Placer RC holes
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Develop structure and mineralisation model/targets
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Design and plan DDH
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Misima Gold Project – Exploration Work Plan
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➢ Drilling and Geology/Resource Modelling
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Consolidation & review after each drill program
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Complete Phase1 Umuna East drilling
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Complete Phase 1 Misima North - Ara drilling
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Stage 2 Resource definition drilling Ewatinona
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Drill follow-up of GDD044 (Abi Prospect)
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Review Umuna resource/reserve opportunities
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Review Kulumalia geology and model
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➢ Maintain 2 drill rigs testing a portfolio of resource definition and advanced targets into 2020
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➢ Ewatinona and other mineral resource models H1 2020
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➢ Mining studies to commence from mid-2020
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Appendix: Misima Resource
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▪ November 2017, JORC 2012 Resource of 82.3Mt at 1.1 g/t for 2.8Moz[1]
| Deposit | Material | Resource | Cutoff | Tonnes | Gold | Silver | Au Moz | Ag Moz |
|---|---|---|---|---|---|---|---|---|
| Category | (g/t Au) | (Mt) | (g/t Au) | (g/t Ag) | ||||
| Umuna | Sub-total | Indicated | 0.5 | 37.2 | 1.1 | 4.9 | 1.3 | 5.8 |
| Inferred | 0.5 | 38.4 | 1.0 | 6.1 | 1.3 | 7.5 | ||
| Total | Combined | 75.7 | 1.1 | 5.5 | 2.6 | 13.3 | ||
| Ewatinona | Oxide | Inferred | 0.5 | 1.0 | 0.9 | 3.4 | 0.03 | 0.1 |
| Primary | Inferred | 0.5 | 5.6 | 1.0 | 3.1 | 0.2 | 0.6 | |
| Sub-total | Inferred | 6.6 | 1.0 | 3.2 | 0.22 | 0.7 | ||
| Misima Total | Indicated | 37.2 | 1.1 | 4.9 | 1.3 | 5.8 | ||
| Inferred | 45.0 | 1.0 | 5.6 | 1.5 | 8.1 | |||
| Total Mineral Resource | 82.3 | 1.1 | 5.3 | 2.8 | 13.9 |
▪ Potential to be a large scale open pit
| Cut Off (g/t) 0.3 0.4 0.5 0.6 0.7 0.8 0.9 |
Tonnes (Mt) | Au g/t | Au Moz |
|---|---|---|---|
| 157.5 | 0.7 | 3.7 | |
| 111.3 | 0.9 | 3.2 | |
| 82.3 | 1.1 | 2.8 | |
| 62.8 | 1.2 | 2.5 | |
| 49.5 | 1.4 | 2.2 | |
| 39.9 | 1.5 | 2.0 | |
| 32.8 | 1.7 | 1.8 |
Umuna grade-tonnage curve
1 KSN.ASX announcement 27[th ] November 2017, https://www.asx.com.au/asxpdf/20171127/pdf/43plq8fmmz5dq0.pdf, cut off grade 0.5 g/t, USD1200/oz Au & USD 16/oz Ag
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