Relevant bibliographies by topics / Bushveld complex

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Academic literature on the topic 'Bushveld complex'

Author: Grafiati
Published: 4 June 2021
Last updated: 15 February 2022

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Journal articles on the topic "Bushveld complex"

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Trumbull, R. B., L. D. Ashwal, S. J. Webb, and I. V. Veksler. "Drilling through the largest magma chamber on Earth: Bushveld Igneous Complex Drilling Project (BICDP)." Scientific Drilling 19 (May 29, 2015): 33–37. http://dx.doi.org/10.5194/sd-19-33-2015.

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Abstract. A scientific drilling project in the Bushveld Igneous Complex in South Africa has been proposed to contribute to the following scientific topics of the International Continental Drilling Program (ICDP): large igneous provinces and mantle plumes, natural resources, volcanic systems and thermal regimes, and deep life. An interdisciplinary team of researchers from eight countries met in Johannesburg to exchange ideas about the scientific objectives and a drilling strategy to achieve them. The workshop identified drilling targets in each of the three main lobes of the Bushveld Complex, w
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Von Gruenewaldt, Gerhard, Martin R. Sharpe, and Christopher J. Hatton. "The Bushveld Complex; introduction and review." Economic Geology 80, no. 4 (1985): 803–12. http://dx.doi.org/10.2113/gsecongeo.80.4.803.

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Jones, M. Q. W. "Heat flow in the Bushveld Complex, South Africa: implications for upper mantle structure." South African Journal of Geology 120, no. 3 (2017): 351–70. http://dx.doi.org/10.25131/gssajg.120.3.351.

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Abstract Geothermal measurements in South Africa since 1939 have resulted in a good coverage of heat flow observations. The Archaean Kaapvaal Craton, in the central part of South Africa, is the best-studied tectonic domain, with nearly 150 heat flow measurements. The greatest density of heat flow sites is in the Witwatersrand Basin goldfields, where geothermal data are essential for determining refrigeration requirements of deep (up to 4 km) gold mines; the average heat flow is 51 ± 6mWm-2. The Bushveld Complex north of the Witwatersrand Basin is an extensive 2.06 Ga ultramafic-felsic intrusiv
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Latypov, R., S. Chistyakova, J. van der Merwe, and J. Westraat. "A note on the erosive nature of potholes in the Bushveld Complex." South African Journal of Geology 122, no. 4 (2019): 555–60. http://dx.doi.org/10.25131/sajg.122.0042.

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Abstract We describe an impressive ~55 m high outcrop from the Pilanesberg Platinum Mine open pit, located in the North-Western Bushveld Complex. The outcrop exposes the complete two-dimensional structure of three Merensky Unit potholes that cut several metres down into the underlying footwall anorthosites. The transgressive field relationships are interpreted to have resulted from thermochemical erosion of the footwall rocks by new pulses of magma replenishing the chamber and resulting in incremental growth of the Bushveld Complex.
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Ivanic, Timothy J., Oliver Nebel, John Brett, and Ruth E. Murdie. "The Windimurra Igneous Complex: an Archean Bushveld?" Geological Society, London, Special Publications 453, no. 1 (2017): 313–48. http://dx.doi.org/10.1144/sp453.1.

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Cawthorn, R. G., and N. McKenna. "The extension of the western limb, Bushveld Complex (South Africa), at Cullinan Diamond Mine." Mineralogical Magazine 70, no. 3 (2006): 241–56. http://dx.doi.org/10.1180/0026461067030328.

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AbstractMafic rocks of the Bushveld Complex at the southeastern end of the western limb, intersected in bore core from the Cullinan Diamond Mine, are described. A 260 m thick ultramafic body of orthopyroxene and chromite cumulate rocks, with mg# – 100*Mg/(Mg+Fe) – values from 77 to 84 and 0.25 to 0.5% Cr2O3 in the pyroxene, is considered to have affinity to the Critical Zone. Such an interpretation considerably extends the eastern limit of Critical Zone rocks of the western limb of the Bushveld Complex. The whole-rock composition of the lower, chilled basal contact of this body has 10% MgO and
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Bamisaiye, Oluwaseyi Adunola. "Geo-Spatial Mapping of the Western Bushveld Rustenburg Layered Suite (Rls) in South Africa." Journal of Geography and Geology 7, no. 4 (2015): 88. http://dx.doi.org/10.5539/jgg.v7n4p88.

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Trend surface analysis (TSA) was used to investigate the structure and thickness variation pattern and to resolve trend and residual component of the structure contours and isopach maps of the Rustenburg Layered Suite (RLS) across the Bushveld Igneous Complex (BIC). The TSA technique was also employed in extracting meter scale structures from the regional structural trends. This enables small-scale structures that could only be picked through field mapping to be observed and scrupulously investigated. Variation in the structure and thickness was used in timing the development of some of the de
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Jones, MQW. "Thermophysical properties of rocks from the Bushveld Complex." Journal of the Southern African Institute of Mining and Metallurgy 115, no. 2 (2015): 153–60. http://dx.doi.org/10.17159/2411-9717/2015/v115n2a10.

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Cawthorn, R. Grant, and T. S. McCarthy. "Incompatible trace element behavior in the Bushveld Complex." Economic Geology 80, no. 4 (1985): 1016–26. http://dx.doi.org/10.2113/gsecongeo.80.4.1016.

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Maier, W. D., and B. Teigler. "A facies model for the western Bushveld Complex." Economic Geology 90, no. 8 (1995): 2343–49. http://dx.doi.org/10.2113/gsecongeo.90.8.2343.

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Dissertations / Theses on the topic "Bushveld complex"

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Everitt, Simon James. "Evolution of the UG2 unit, Bushveld Complex, South Africa : mineral composition and petrological evidence." Thesis, Rhodes University, 2013. http://hdl.handle.net/10962/d1001573.

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Several disequilibrium textures are found to occur within the hanging wall and footwall of the UG2 chromitite layer of the Bushveld Complex, South Africa. These textures include plagioclase chadacrysts found included within orthopyroxene and clinopyroxene as well as the orthopyroxenes exhibiting round crystal boundaries that appear to be resorbed. Textures found within the UG2 stratigraphy such as linear boundaries and 120° triple junctions at interfaces of adjacent plagioclase or pyroxene grains also suggest that recrystallization has taken place. The presence of both disequilibrium textures
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Curl, Edward Alexander 1972. "Parental magmas of the Bushveld Complex, South Africa." Monash University, Dept. of Earth Sciences, 2001. http://arrow.monash.edu.au/hdl/1959.1/9080.

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Gwatinetsa, Demand. "Distribution of iron-titanium oxides in the vanadiferous main magnetite seam of the upper zone : Northern limb, Bushveld complex." Thesis, Rhodes University, 2014. http://hdl.handle.net/10962/d1013281.

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The main magnetite seam of the Upper Zone of the Rustenburg Layered Suite (SACS, 1980) on the Bushveld Complex is known to host the world‘s largest vanadium bearing titaniferous iron ores. The vanadiferous titanomagnetites, contain vanadium in sufficient concentrations (1.2 - 2.2 per cent V₂O₅) to be considered as resources and vanadium has been mined historically by a number of companies among them Anglo-American, Highveld Steel and Vanadium and VanMag Resources as well as currently by Evraz Highveld Steel and Vanadium Limited of South Africa. The titanomagnetites contain iron ore in the form
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Lovegrove, Daniel Paul. "Rates and mechanisms of metamorphic processes derived from thermal aureole studies." Thesis, University of Oxford, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.249305.

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Sargeant, Fiona. "The seismic stratigraphy of the Bushveld Igneous Complex, South Africa." Thesis, University of Liverpool, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.250322.

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Twala, Mthokozisi Nkosingiphile. "Use of multispectral remote sensing data to map magnetite bodies in the Bushveld Complex, South Africa : a case study of Roossenekal, Limpopo." Diss., University of Pretoria, 2019. http://hdl.handle.net/2263/75756.

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Mineral detection and geological mapping through conventional ground survey methods based on field observation and other geological techniques are tedious, time-consuming and expensive. Hence, the use of remote sensing in mineral detection and lithological mapping has become a generally accepted augmentative tool in exploration. With the advent of multispectral sensors (e.g. ASTER, Landsat and PlanetScope) having suitable wavelength coverage and bands in the Shortwave Infrared (SWIR) and Thermal Infrared (TIR) regions, multispectral sensors, along with common and advanced algorithms, have beco
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Koegelenberg, Corne. "Experimental evidence for sulphide magma percolation and evolution : relevant to the chromite bearing reefs of the Bushveld Complex." Thesis, Stellenbosch : Stellenbosch University, 2012. http://hdl.handle.net/10019.1/20043.

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Thesis (MSc)--Stellenbosch University, 2012.<br>ENGLISH ABSTRACT: Pt mineralization within the Bushveld Complex is strikingly focused on the chromitite reefs, despite these horizons being associated with low volumes of base metal sulphide relative to Pt grade. Partitioning of Pt (Dsil/sulp) from silicate magma into immiscible sulphide liquid appears unable to explain Pt concentrations in chromitite horizons, due to the mismatch that exists between very large R factor required and the relevant silicate rock volume. Consequently, in this experimental study we attempt to gain better insight into
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Venter, Andrew Derick. "Air quality assessment of the industrialized western Bushveld Igneous Complex / Andrew Derick Venter." Thesis, North-West University, 2011. http://hdl.handle.net/10394/8530.

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South Africa has the largest economy in Africa, with significant mining and metallurgical activities. A large fraction of the mineral assets is concentrated in the Bushveld Igneous Complex (BIC), with the western limb being the most exploited. Although the western BIC is considered to be an air pollution hotspot, inadequate air quality data currently exists for this area. To partially address this knowledge gap, a comprehensive air quality monitoring station was operated for more than two years at Marikana in the western BIC. Basic meteorological parameters, precipitation, Photosynthetic Photo
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Manyeruke, Tawanda Darlington. "Compositional and lithological variation of the Platreef on the farm Nonnenwerth, northern lobe of the Bushveld Complex implications for the origin of platinum-group elements (PGE) mineralization /." Thesis, Pretoria : [s.n.], 2008. http://upetd.up.ac.za/thesis/available/etd-01192009-164657/.

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Botha, Pieter W. S. K. "The mineralogy and geochemistry of the Rooikoppies iron-rich ultramafic pegmatite body, Karee Mine, Bushveld Complex, South Africa [electronic resource] /." Pretoria : [s.n.], 2008. http://upetd.up.ac.za/thesis/available/etd-01272009-172307/.

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Books on the topic "Bushveld complex"

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Eales, Hugh V. The Bushveld Complex: An introduction to the geology and setting of the Bushveld Complex. Council for Geoscience, 2014.

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A first introduction to the geology of the Bushveld Complex and those aspects of South African geology that relate to it. Council for Geoscience, 1999.

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Hartzer, F. J. Geology of the Transvaal Inliers in the Bushveld Complex. Pretoria:, 2000.

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Cameron, Gregory Hugh *. A geochemical investigation into the origin of the upper critical zone of the eastern Bushveld complex, South Africa. 1988.

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Book chapters on the topic "Bushveld complex"

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Cawthorn, R. Grant. "The Bushveld Complex, South Africa." In Springer Geology. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9652-1_12.

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de Beer, J. H., R. Meyer, and P. J. Hattingh. "Geoelectrical and palaeomagnetic studies on the Bushveld complex." In Proterozic Lithospheric Evolution. American Geophysical Union, 1987. http://dx.doi.org/10.1029/gd017p0191.

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Scoon, Roger N. "Skaergaard Intrusion, Greenland and Eastern Bushveld Complex, South Africa." In The Geotraveller. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-54693-9_17.

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Cawthorn, R. Grant, and Kelly L. Poulton. "Evidence for Fluid in the Footwall Beneath Potholes in the Merensky Reef of the Bushveld Complex." In Geo-Platinum 87. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-1353-0_35.

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Viljoen, Fanus, Mike Knoper, Hariharan Rajesh, Derek Rose, and Tiaan Greeff. "Application of a Field Emission Mineral Liberation Analyser to the in Situ Study of Platinum-Group Element Mineralisation in the Merensky Reef of the Bushveld Complex, South Africa." In Proceedings of the 10th International Congress for Applied Mineralogy (ICAM). Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-27682-8_91.

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Eales, H. V., and R. G. Cawthorn. "The Bushveld Complex." In Developments in Petrology. Elsevier, 1996. http://dx.doi.org/10.1016/s0167-2894(96)80008-x.

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VanTongeren, Jill A. "Mixing and Unmixing in the Bushveld Complex Magma Chamber." In Processes and Ore Deposits of Ultramafic-Mafic Magmas through Space and Time. Elsevier, 2018. http://dx.doi.org/10.1016/b978-0-12-811159-8.00005-6.

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Kinnaird, Judith A., and Iain McDonald. "The Northern Limb of the Bushveld Complex: A New Economic Frontier." In Metals, Minerals, and Society. Society of Economic Geologists (SEG), 2018. http://dx.doi.org/10.5382/sp.21.08.

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Lee, C. A. "A Review of Mineralization in the Bushveld Complex and some other Layered Intrusions." In Developments in Petrology. Elsevier, 1996. http://dx.doi.org/10.1016/s0167-2894(96)80006-6.

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Von Gruenewaldt, G., and R. E. Harmer. "Chapter 5 Tectonic Setting of Proterozoic Layered Intrusions with Special Reference to the Bushveld Complex." In Proterozoic Crustal Evolution. Elsevier, 1992. http://dx.doi.org/10.1016/s0166-2635(08)70119-1.

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Conference papers on the topic "Bushveld complex"

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Latypov, Rais, and Willem Kruger. "SOLIDIFICATION FRONTS IN MASSIVE MAGNETITITES OF THE BUSHVELD COMPLEX." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-331713.

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Coomber, S. "Gravity Inversions & FTG Analysis in the Western Bushveld Complex." In 10th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609-pdb.146.6.3.

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Letts, S., T. H. Torsvik, S. J. Webb, and L. D. Ashwal. "Palaeomagnetism of Mafic Dykes from the Eastern Bushveld Complex (South Africa)." In 8th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.144.18.

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Webb, S. J., L. D. Ashwal, T. K. Nguuri, and R. G. Cawthorn. "Geophysical constraints on the shape and emplacement of the Bushveld Complex." In 8th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.144.21.

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O.K.T. Babayeju, Mr, Prof W.J. Botha, and Prof S.A. de Waal. "Geophysical Investigation of the Marble Hall Fragment of the Bushveld Complex." In 6th SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609-pdb.221.060.

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Sepato, O. "Wavelet Analysis of Density Data from the Bushveld Complex, South Africa." In 75th EAGE Conference and Exhibition incorporating SPE EUROPEC 2013. EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20131064.

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Webb*, Susan J., Lewis D. Ashwal, Robert Trumbull, and Ilya Veksler. "ICDP Deep drilling and geophysical exploration of the Bushveld Complex, South Africa." In SEG Technical Program Expanded Abstracts 2014. Society of Exploration Geophysicists, 2014. http://dx.doi.org/10.1190/segam2014-1673.1.

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Steiner-Leach, Travis Lewis, Maureen Feineman, Sarah Penniston-Dorland, et al. "MULTIPLE SULFUR ISOTOPES IN GRANITE-HOSTED SULFIDES FROM THE BUSHVELD IGNEOUS COMPLEX." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306382.

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Compton-Jones, Charlie, Hannah Hughes, Iain McDonald, Grant Bybee, Judith Kinnaird, and Jens Andersen. "Radiogenic Isotope and Precious Metal Compositions of Orangeite Dykes Intersecting the Bushveld Complex." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.465.

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Letts, S. A., T. Torsvik, L. Aswal, and S. Webb. "New Palaeomagnetic Data from the Main and Upper Zones of the Bushveld Complex." In 68th EAGE Conference and Exhibition incorporating SPE EUROPEC 2006. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609.201402012.

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