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- W2739845933 abstract "The Bushveld Complex, the largest known mafic intrusion in the world, reveals some spectacular geology, including the classic layering of dark ultramafics and light-colored anorthosite (Fig. 1). Three distinct groups of rocks make up the complex (Tankard et al., 1982), the oldest of which is the Rooiberg Group (dominated by rhyolite) and the youngest, the Lebowa Granite Suite (including a suite of granophyres). The majority of the ore deposits are, however, restricted to the intervening group of ultramaficmafic rocks, or Rustenburg Layered Suite. The Rustenburg Layered Suite is intrusive into the sedimentary rocks and subordinate volcanic rocks of the Transvaal Supergroup (ca. 2.5–2.1 Ga) and has been dated at 2.055 Ga (Scoates and Friedman, 2008). The Bushveld contains the greatest concentration of mineral wealth on the planet and includes, in addition to the platinum group element (PGE) ores, base metals (e.g., chromium, iron, tin, titanium, and vanadium) and industrial minerals (e.g., andalusite, dimension stone, and magnesite), as described by Willemse (1969) and Wilson and Anhaeusser (1988). Mining operations have spawned extensive towns and associated industrial complexes, including downstream processing plants with smelters and precious metal refineries, many of which use technology specifically designed for the Bushveld ores." @default.
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- W2739845933 date "2009-07-01" @default.
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- W2739845933 title "Discovery and Geology of the Platinum Group Element Deposits of the Bushveld Complex, South Africa" @default.
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- W2739845933 doi "https://doi.org/10.5382/segnews.2009-78.fea-02" @default.
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