salt river resources ltd 24 sept16 summary geology and mineralogy
TRANSCRIPT
Salt River Resources LtdSouth Africa’s Newest Mineral Oasis
Brief summary: Geology and Mineralogy
24 September 2016
On the Edge of the Kalahari
• Salt River Resources Ltd is exploring on the southern edge of the Kalahari Desert
• Located in the metallogenically significant Namaqua Mobile Belt that hosts several world-class base metal districts
• Continuous base metal mining since 1852• The Salt River Resources “Mineral Oasis” promises
to be, together with the Gamsberg development, the next drivers of economic development in the Northern Cape region of South Africa
Namaqua Metamorphic Province
• Located in northwestern portion South Africa and southern Namibia
• Occupies a crescent-shaped body covering an area measuring 450 x 180 km
• Hosts several economically-significant base metal districts and deposits
Modified after Hartnady et al. (1985), Thomas et al. (1992; 1993) and Hanson (2003).
Namaqua Metamorphic Province
Based on structural, lithological, and geochronological differences, the NMP may be divided into four subprovinces (Kroner and Blignault, 1976):
– Kheis Subprovince– Namaqua Subprovince– Richtersveld
Subprovince– Bushmanland
Subprovince
Modified from Hartnady et al. (1985), Joubert (1986) and McClung (2006).
Deformational Events
• Folding– Comprises of four phases (Joubert, 1971)
• Faulting– Comprises two phases (Colliston and Schoch, 2002;
McClung, 2006)• Metamorphism
– Comprises four phases of greenschist- to granulite-facies metamorphism (Lipson, 1978)
Salt River Deposit
• Located about 80 km southeast of Pofadder and 80km southwest of Kakamas in the Northern Cape Province on the property Remainder of the farm Adjoining Geelvloer No. 197 (Kraandraai)
• Topography consists of a flat to slightly undulating landscape with large areas covered by sand, calcrete and scree
• Vegetation consists of low growing succulents, shrubs (i.e. drie doorn) and clumps of grass
• Besides domesticated livestock, wildlife of the property comprises jackals, bat-eared and Cape fox, rabbits/hares, mice, antelope, birds, snakes, lizards and insects.
Lovedale201
Quagga-Maag200
Hartebeesvlei199
Putsberg203
Other Mineral Occurrences
0 5 10km
Salt River Deposit
Gannapoort202
Adjoining Geelvloer
197
Graafwater198
Vaal-Kop225
Prospecting AreaMajor Gravel RoadFarm Boundaries
Salt River Deposit
Mineralised Showing
Modified after Maclaren (1988).
Styles of Mineralisation
• Base metal sulphides occur as four distinctly different styles of mineralisation– semi-massive to massive sulphide
• very fine- to fine-grained pyritic horizon– mineralised schist
• disseminated to stringer sulphides in foliated and contorted schist– stringer mineralisation in magnesium-rich altered footwall
rocks• disseminated to stringers sulphides in foliated magnesium-rich
rocks– mineralised calc-silicate gneiss
• Sulphide veins in silicified, altered and/or brecciated calc-silicate rock
Sulphide Horizons
• Three distinct, massive to disseminated, “stacked” horizons dipping approximately 25-30º to the northeast– Upper Sulphide Zone
• semi-massive to massive sulphide• 2.8m mean thickness
– Middle Sulphide Zone• stringer mineralisation in cordierite-rich footwall rocks• 2.3m mean thickness
– Lower Sulphide Zone• mineralised schist and stringer mineralisation in cordierite-rich
altered footwall rocks• 3.2m mean thickness
Upper Sulphide Zone
• Characterized by a very fine- to fine-grained, semi-massive to massive, durchbewegung-textured pyritic horizon
• Ore mineralogy consist of pyrite, sphalerite, chalcopyrite, galena ± barite, magnetite and molybdenite
• Spatially occurs throughout the deposit
py
sph
ganguepy
sphmo
gangue
Middle Sulphide Zone
• Characterized by disseminated to stringer mineralisation in foliated Mg-rich altered (quartz, cordierite, biotite/chlorite, plagioclase) gneiss
• Ore mineralogy consist of pyrite, chalcopyrite,sphalerite, galena and magnetite
• Spatially restricted to the higher-grade portions of the deposit
sph
cpy
Lower Sulphide Zone
• Characterized by disseminated to stringers of semi-massive sulphides in foliated and contorted, biotite-chlorite schist interbedded with Mg-rich altered rocks
• Ore mineralogy consist of pyrite, chalcopyrite ±sphalerite, galena andmagnetite
• Spatially restricted to the higher-grade portions of the deposit
Resource Description
• Three distinct, massive to disseminated, “stacked” horizons dipping approx. 25 - 30º to the NE.
• Ore zones average 3m in thickness• Ore mineralogy consist of pyrite (FeS2),
sphalerite (ZnS), chalcopyrite (CuFeS2), galena (PbS) ± barite (BaSO4), magnetite (Fe3O4) and molybdenite (MoS)
Resource Confirmation
• 20,179m of resource drilling– Widely-spaced diamond boreholes of 14,439m
and 2,292m of percussion drilling by previous exploration companies
– 3,448m of closely-spaced diamond drilling by SRR• Assay data analysed by two internationally
accredited laboratories
Potential Mineralization
23.3 Mt @ 1.5% Zn, 0.7% Pb, 0.4% Cu, 21 g/t Ag & 1.0 g/t Au
Total Mineral Resource
Measured Resources9.97 Mt @ 1.8% Zn, 0.5% Cu, 0.6% Pb, 21 g/t Ag & 0.5 g/t Au
Indicated Resources14.13 Mt @ 1.8% Zn, 0.7%
Cu, 0.4% Pb, 19 g/t Ag & 0.7 g/t Au
Total Mineral Resource atSalt River
Project: 47.4 Mt at 1% Zn threshold
Salt River West Occurrences
Soutputs Noord Occurrence
Comparison – Black Mountain
• Poly-metallic base metal mine in Northern Cape Province • Produces 168kt of concentrate per annum• Shallow ore bodies depleted• Currently mining Broken Hill Deeps ore body to depth of 1900m• Salt River Resources planning to produce 30kt concentrate
initially increasing to 90.5kt concentrate per year• Current mineral resource only estimated from surface to 500m
depth, but remains open at depth and to the west• Mineralised intercepts encountered up to 1300m down dip to the
north
Management Team
1. Jeff Rapoo – Chairman– 45 years relevant experience in finance
and mining2. Marius Welthagen – Managing
Director– 26 years relevant mining experience
3. Joe Rachidi – Director: Legal– 25 years relevant experience
4. Prof David Reid – Director: Geology– 30 years relevant in the Namaqualand
Mobile Belt5. Eben van Tonder
– 15 years experience as Technical Manager 1
23 5
4
Project Development
Project Definition
Geological studies
Mineral Rights
Salt River Base Mineral Project
FeasibilityDrilling
ProvenResources
Bankable feasibility
Project development phases
Resource definition
ConfirmationDrilling
MeasuredResources
RaiseCapital
EstablishMiningOperation
Production
Phase 2 Phase 3Phase 1
Bankable Feasibility
One year to completion of DFS
Exploration drilling to indicated to measured resource
Concentrate marketing and completion of DFS
Bulk sampling incline
Metallurgical testing
Pilot plant and mine planning
Disclaimer
• This presentation is directed at individuals having professional investment management experience.
• No representation or warranty is given or implied by Thabex Limited or Salt River Resources Limited or their directors as to the accuracy or completeness of the information or opinions contained herein and no liability is accepted for any such information or opinions.
• The presentation may contain certain forward looking statements that are subject to certain risks and uncertainties, e.g. the company’s plans, goals and prospects. Actual results may differ materially.
• This presentation does not constitute an offer to purchase, sell, issue or subscribe for shares in Thabex Limited or Salt River Resources Limited.