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The distribution of platinum group elements in the Insizwa Lobe, Mount Ayliff Complex, South Africa : implications for Ni-Cu-PGE Sulfide exploration in the Karoo Igneous Province

Maier Wolfgang D., Marsh J.S., Barnes Sarah-Jane et Dodd D.C.. (2002). The distribution of platinum group elements in the Insizwa Lobe, Mount Ayliff Complex, South Africa : implications for Ni-Cu-PGE Sulfide exploration in the Karoo Igneous Province. Economic Geology, 97, (6), p. 1293-1306.

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The Mount Ayliff Complex of the Eastern Cape province of South Africa is a layered intrusion of some 800 km2 surface area and up to 1,200 m thickness. On the basis of compositional similarities and spatial association, it is generally interpreted to form part of the Karoo igneous province. Similarities between the Mount Ayliff Complex and the staging chambers and feeder conduits to flood basalts that host magmatic sulfide ores elsewhere in the world suggest that the Mount Ayliff Complex may have an enhanced potential for Noril’sk-Talnakh–type massive Ni-Cu sulfide ores, an idea that is supported by the well-known sulfide occurrence at Waterfall Gorge. Here, we present major-, trace-, and noble-element data for 30 samples of cumulate rocks from a continuous 1,200 m drill core through the Insizwa lobe of the complex, as well as six samples of a footwall sill, the Taylor’s Koppie dike, that was considered a possible feeder zone to the lobe, and through a massive sulfide lens in the footwall of the lobe at Ndzongiseni. We show that most of the Insizwa cumulate rocks contain small amounts of cumulus sulfides. The sulfides, including those at Waterfall Gorge, can be explained by a model in which the sulfides were segregated from magma having chilled-margin composition. On the basis of the composition of the chilled margins, the Insizwa magma contained no entrained sulfides and was depleted in platinum group elements (PGE), although not in Cu and Ni, before emplacement. These compositional characteristics are also observed in lavas of the central Karoo igneous province and suggest only limited sulfide segregation from these magmas at depth. Our findings thus indicate relatively little potential for economic magmatic Ni-Cu-PGE sulfide deposits in the Insizwa lobe.

Type de document:Article publié dans une revue avec comité d'évaluation
Pages:p. 1293-1306
Version évaluée par les pairs:Oui
Date:Octobre 2002
Sujets:Sciences naturelles et génie > Sciences naturelles > Sciences de la terre (géologie, géographie)
Département, module, service et unité de recherche:Départements et modules > Département des sciences appliquées > Unité d'enseignement en sciences de la Terre
Mots-clés:Africa, chemical composition, composition, copper ores, Eastern Cape Province South Africa, emplacement, Insizwa Lobe, intrusions, Karoo Basin, magma chambers, magmas, major elements, metal ores, metals, Mount Ayliff Deposit, nickel ores, platinum group, platinum ores, sampling, sills, South Africa, Southern Africa, spatial distribution, spectra, thickness, trace elements, X-ray fluorescence spectra, zoning
Déposé le:10 juin 2016 15:01
Dernière modification:17 nov. 2017 00:38
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