2014
DOI: 10.3133/sir20105090q
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Platinum-group elements in southern Africa: mineral inventory and an assessment of undiscovered mineral resources

Abstract: Box plots and comparison circles for average platinum, palladium, rhodium, and gold grade of Merensky Reef mineral resource blocks located in the eastern, northwestern, and southwestern limbs of the Bushveld Complex, South Africa ............43 29. Box plots and comparison circles for average platinum, palladium, rhodium, and gold grade of UG2 Chromitite mineral resource blocks located in the eastern, northwestern, and southwestern limbs of the Bushveld Complex, South Africa ............44 30. Map of the Meren… Show more

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Cited by 23 publications
(18 citation statements)
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“…At f c = 0.010, the cost of 2 nm of Pt is ~ 0.017 $ m -2 . In contrast, for an IrO x coatedphotoanode with a loading of 10 g m -2 (typical PEM electrolyzer loading) and with f c = 0.010, ~10 7 kg of Ir would be required to meet a 10 TW p deployment level, as compared to the estimated 10 6 kg global resource base of Ir 34. …”
mentioning
confidence: 85%
“…At f c = 0.010, the cost of 2 nm of Pt is ~ 0.017 $ m -2 . In contrast, for an IrO x coatedphotoanode with a loading of 10 g m -2 (typical PEM electrolyzer loading) and with f c = 0.010, ~10 7 kg of Ir would be required to meet a 10 TW p deployment level, as compared to the estimated 10 6 kg global resource base of Ir 34. …”
mentioning
confidence: 85%
“…Magmatic sulfide ore deposits account for some of the world's most valuable metal accumulations, currently accounting for ~56% of the world's nickel production and over 96% of supply of platinum, palladium and the other platinum group elements (Mudd and Jowitt, 2014;Zientek et al, 2014;Peck and Huminicki, 2016). They form by the accumulation of immiscible sulfide liquid that has scavenged chalcophile elements from a coexisting silicate magma, in a variety of settings:…”
Section: Introductionmentioning
confidence: 99%
“…The Rustenburg Layered Suite (RLS) of the Bushveld Complex hosts ~75% of the o ld s PGE resources i so e of the o ld s la gest magmatic sulphide deposits (Lee, 1996;Zientek et al, 2014). The RLS has been dated to 2055.91±0.26 Ma (Zeh et al, 2015) and is a series of mafic-ultramafic units, capped by the Bushveld Granites (Cawthorn, 1999;Eales and Cawthorn, 1996).…”
Section: Geological Settingmentioning
confidence: 99%