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The Bushveld complex A quick presentation
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The Bushveld Complex, South Africa
The biggest: km x 9 km The Red Granite intruded Ma afterwards Figure Simplified geologic Map and cross section of the Bushveld complex. After Willemse (1964), Wager and Brown (1968), and Irvine et al. (1983).
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Bushveld Complex The World’s Biggest Layered Igneous Intrusion
Floor LZ LCZ UCZ MZ UZ Panorama of the Olifants River Valley, NE Bushveld Jodie’s lecture
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Jodie’s lecture
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Intrusive sill of Bushveld dolerite in Transvaal sequence
Near Burgersfort
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Lower zone Peridotites/pyroxenites
(Jagdlust, Burgersfort-Polokwane Road)
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Lower zone Peridotites/pyroxenites
(Jagdlust, Burgersfort-Polokwane Road)
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The critical zone overlooking the lower zone (left)
(Burgersfort-Polokwane Road)
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Different pyroxenite types, Critical zone
(Mandaagshoek, near Burgersfort)
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Norite and anorthosite, Critical zone
(Mandaagshoek, near Burgersfort)
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Layered anorthosite, Critical zone
(Tweefontein, Lydenburg-Burgersfort area)
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Anorthosite and chromitite, Critical zone
(Dwars River, Lydenburg-Burgersfort area)
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UG3 Chromitite, Critical zone
(Mandaagshoek, near Burgersfort)
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Massive black gabbros (« Belfast black »), Main zone
(Near Stoffberg, Belfast area)
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Modal layering in gabbros, Main zone
(Lydenburg-Burgersfort area)
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Gabbros and magnetite (Main Magnetite Layer), Upper zone
(Magnet Heights)
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Upper zone gabbronorite
(Magnet Heights)
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Main magnetite layer, Upper zone
(Magnet Heights)
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In-situ differentiation
Or successive magma batches?
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Isotopic evolution ISr(2.05 Ga)
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