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Showing 1 to 20 of 25 for “"Bushveld Complex"”.

  1. The 'Ins' and 'Outs' of the Bushveld Complex Upper Zone

    … geodynamic evolution of the Upper Zone of the Bushveld Complex. The Bushveld Complex is one of the few large layered intrusions in which the entire cumulate stratigraphy is preserved and well-exposed from its base to its roof. Despite this unique feature, relatively little is known about the …

    columbia-diss Repository record for The 'Ins' and 'Outs' of the Bushveld Complex Upper Zone (opens in a new tab)

  2. Geochemical characteristics and rare earth element trends of the Upper Zone in the western Bushveld Complex

    … crystallization of the Upper Zone in the western Bushveld. The geochemical characteristics of the western Bushveld Upper Zone are also briefly compared to the Upper Zone of the eastern Bushveld as exposed in the Roossenekal district. The rock types intersected by the Bierkraal 1 borehole consist …

    pretoria Repository record for Geochemical characteristics and rare earth element trends of the Upper Zone in the western Bushveld Complex (opens in a new tab)

  3. Development of the Platreef in the northern limb of the Bushveld Complex at Sandsloot, Mokopane District, South Africa

    … Layered Suite in the northern limb of the Bushveld Complex. The reef lies unconformably on a footwall (floor) sequence of Transvaal Supergroup sedimentary rocks and Archaean granite/gneiss basement, and is overlain by a hangingwall (roof) of Main Zone gabbronorites. Structural relationships …

    greenwich Repository record for Development of the Platreef in the northern limb of the Bushveld Complex at Sandsloot, Mokopane District, South Africa (opens in a new tab)

  4. An investigation into the formation of the lower Main Zone in the eastern limb of the Bushveld complex, South Africa

    The Main Zone is dominated by medium – grained, homogeneous gabbronorite, and anorthosites. The plagioclase compositions of the core is ((Na(0.227 – 0.353), K (0.012 – 0.046), Ca (0.651 – 0.777)) Al (1.630 – 1.752) Si (2.183 – 2.345) O8) and at the rim is ((Na (0.189 – 0.371), K (0.005 – 0.108), Ca …

    pretoria Repository record for An investigation into the formation of the lower Main Zone in the eastern limb of the Bushveld complex, South Africa (opens in a new tab)

  5. P-T estimates of peak Bushveld metamorphism in the eastern Bushveld complex, Limpopo Province, South Africa : constraints from P-T pseudosections

    The Bushveld Igneous Complex (BIC) is the largest layered mafic intrusion in the world and contains the largest known deposits of vanadium, chromium and Platinum group elements on the planet, as well as large deposits of iron, nickel, copper, tin and fluorite. To aid and improve our understanding …

    pretoria Repository record for P-T estimates of peak Bushveld metamorphism in the eastern Bushveld complex, Limpopo Province, South Africa : constraints from P-T pseudosections (opens in a new tab)

  6. A multi-isotopic geochemical investigation of the Lower Zone, Bushveld Complex, South Africa: implications for a crustal component for parental magmas

    … current study focuses on the Lower Zone of the Bushveld Complex, South Africa using multiple geochemical and isotopic systems to determine the origin of crustal signatures, i.e. crustal assimilation or recycled crust in the mantle source, present throughout the Rustenburg Layered Suite (RLS) …

    cape-town Repository record for A multi-isotopic geochemical investigation of the Lower Zone, Bushveld Complex, South Africa: implications for a crustal component for parental magmas (opens in a new tab)

  7. The Application of Machine Learning Methods to Portable X-Ray Fluorescence Data: A Case Study from Zwartfontein Farm, Northern Limb of the Bushveld Complex, South Africa

    … as a case study, on the Northern Limb of the Bushveld Complex of South Africa – a complex multi-commodity deposit (Ni-Cu-(Co)-PGE) comprising intricately layered mafic-ultramafic cumulate rocks overprinted by variable alteration minerals. Although pXRF provides rapid multi-elemental analysis, …

    exeter

  8. A geochemical profile through the Uitkomst Complex on the farm Slaaihoek, with special reference to the platinum-group elements and Sm-Nd isotopes

    The Uitkomst Complex is a mineralized, layered basic to ultrabasic intrusion, hosted by sedimentary rocks of the lower part of the Transvaal Supergroup. It is situated on the farms Uitkomst 541JT and Slaaihoek 540JT, about 25 km north of Badplaas and 50 km east of the eastern limb of the Bushveld

    pretoria Repository record for A geochemical profile through the Uitkomst Complex on the farm Slaaihoek, with special reference to the platinum-group elements and Sm-Nd isotopes (opens in a new tab)

  9. An electrochemical investigation of platinum group minerals

    The Bushveld complex is the largest ore body in the world hosting platinum group elements (PGEs). It is a stratified orebody with three major reefs namely, the Merensky reef, UG2 reef and the Platreef. Platinum and palladium are the most abundant PGEs found in the Bushveld complex. They occur in …

    cape-town Repository record for An electrochemical investigation of platinum group minerals (opens in a new tab)

  10. Surface characterisation and flotation behaviour of the platinum and palladium arsenide, telluride and sulphide mineral species

    … Platreef is located in the northern limb of the Bushveld Complex of South Africa. This reef consists of a complex assemblage of rock types, with pyroxenites, serpentinites and calcsilicates being the most abundant. The predominant PGMs are the tellurides, arsenides, alloys and sulphides. The Pt …

    cape-town Repository record for Surface characterisation and flotation behaviour of the platinum and palladium arsenide, telluride and sulphide mineral species (opens in a new tab)

  11. The oxygen, carbon & hydrogen isotope geochemistry of the Phalaborwa Complex, South Africa

    The 2060 ± 2 Ma Phalaborwa Complex is a pipe-like ultramafic to carbonatite intrusion formed from multiple magma pulses. This produced a main pipe of pyroxenite, carbonatite and foskorite (olivineapatite-magnetite-calcite) and many smaller syenite plugs around the pipe. The complex is the oldest …

    cape-town Repository record for The oxygen, carbon & hydrogen isotope geochemistry of the Phalaborwa Complex, South Africa (opens in a new tab)

  12. In situ mineral geochemistry as a guide to ore-forming processes

    … Cu-Au deposits. These studies revealed complex chemical zonation, providing a detailed record of cryptic fluid chemistry and depositional processes. A distinct isotopic signature and residual metastable silica hydrates in quartz microcrystals from the El Indio deposit, Chile provided the …

    aus-cath Repository record for In situ mineral geochemistry as a guide to ore-forming processes (opens in a new tab)

  13. In situ mineral geochemistry as a guide to ore-forming processes

    … Cu-Au deposits. These studies revealed complex chemical zonation, providing a detailed record of cryptic fluid chemistry and depositional processes. A distinct isotopic signature and residual metastable silica hydrates in quartz microcrystals from the El Indio deposit, Chile provided the …

    anu Repository record for In situ mineral geochemistry as a guide to ore-forming processes (opens in a new tab)

  14. Investigation of the surface properties of gangue minerals in PGM bearing ores

    … associated sulphides by froth flotation from the Bushveld Igneous Complex is complicated by the presence of naturally floatable gangue minerals such as talc. Although talc is present in small quantities it has a disproportionate effect on concentrate grade by enhancing froth stability and …

    cape-town Repository record for Investigation of the surface properties of gangue minerals in PGM bearing ores (opens in a new tab)

  15. An investigation into chemical factors that affect the behaviour of Gangue minerals in the flotation of PGM ores

    … of Platinum Group Elements (PGE) from the Bushveld Complex in South Africa. This process aims to optimise the recovery of valuable PGE and sulphide minerals and the rejection of unwanted gangue minerals. The major reefs are exploited in South Africa i.e. Merensky reef and UG-2 reef. Gangue …

    cape-town Repository record for An investigation into chemical factors that affect the behaviour of Gangue minerals in the flotation of PGM ores (opens in a new tab)

  16. A quality control model for the development of high-confidence flotation test data

    … test data for the Merensky ore type found in the Bushveld complex of South Africa. The complex nature of the platinum-group element (PGE) deportment in this ore renders the normally-practiced procedures inappropriate for this particular testwork. A more robust and thorough procedure is necessary …

    cape-town Repository record for A quality control model for the development of high-confidence flotation test data (opens in a new tab)

  17. Application of the 190Pt-186Os isotope decay system to dating platinum-group minerals

    … well constrained situations. The age of the Bushveld Complex has been measured using various radioisotope chronometers which yield ages ranging from 1921 – 2165 Ma, although an age of 2054 Ma is widely accepted. We present an accurate isochron age of 2012 ± 47 Ma (2σ, n = 50, MSWD = 1.19) for …

    durham Repository record for Application of the 190Pt-186Os isotope decay system to dating platinum-group minerals (opens in a new tab)

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