2019
DOI: 10.1016/j.gexplo.2019.106340
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Geochemical controls on the distribution of PGE mineralisation in skarns formed during emplacement of the Platreef in the Northern limb of the Bushveld Complex, South Africa

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“…However, this definition does not help distinguish between contact-style and internal reef-style PGE mineralization that may occur at the basal and in the top parts of the Platreef, respectively, as seen in the Flatreef sequence on Turfspruit (Grobler et al 2019). In other areas of the northern limb, these two types of mineralization are superimposed and may form a thick high-grade orebody, as seen on Sandsloot where high-grade ores occur both in intrusive and metasedimentary rocks (McDonald and Holwell 2011; Klemd et al 2016;Mwenze et al 2019).…”
Section: Stratigraphy Of the Bushveld Northern Limb And Definitions Omentioning
confidence: 99%
“…However, this definition does not help distinguish between contact-style and internal reef-style PGE mineralization that may occur at the basal and in the top parts of the Platreef, respectively, as seen in the Flatreef sequence on Turfspruit (Grobler et al 2019). In other areas of the northern limb, these two types of mineralization are superimposed and may form a thick high-grade orebody, as seen on Sandsloot where high-grade ores occur both in intrusive and metasedimentary rocks (McDonald and Holwell 2011; Klemd et al 2016;Mwenze et al 2019).…”
Section: Stratigraphy Of the Bushveld Northern Limb And Definitions Omentioning
confidence: 99%