1-5 OF 5 RESULTS FOR

Elandskraal Complex

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2405(19)
... the history of this important ore deposit. Samples from Tau Lekoa Mine, previously known as the Vaal Reefs No. 10 Shaft Mine in the Klerksdorp goldfield, and samples from the western part of Elandskraal Mine, previously known as the Elandsrand Gold Mine in the Carletonville gold-field, were analyzed. Three...
Journal Article
Published: 01 June 2004
South African Journal of Geology (2004) 107 (1-2): 207–218.
... properties used in modelling of the Bushveld Complex profile ( Maré et al. , 2002 ; Ashwal et al. , 2003 ; James et al. , 2004 ). The value for the Elandskraal alkaline volcanic complex was calculated from major element analyses ( Frick and Walraven, 1985 ), however, only one analysis was suitably...
FIGURES | View All (6)
Journal Article
Published: 10 November 2020
South African Journal of Geology (2020) 123 (4): 597–614.
... Alkaline Province. Excluding the Elandskraal Complex ( Figure 1 ) evolved rock types such as nepheline syenites/phonolites, syenites/trachytes and carbonatites dominate the main alkaline igneous complexes of the PAP, with lesser amounts of alkaline mafic rocks ( Frick and Walraven, 1985 ; Harmer, 1999...
FIGURES | View All (9)
Series: Economic Geology, Economic Geology
Published: 01 January 2005
DOI: 10.5382/AV100.09
EISBN: 9781934969519
... than from chromite deposits. Hypotheses for the origin of PGE, Cr, and Vmineralization have been strongly influenced by observations on the Bushveld Complex that hosts well over half the world’s resources in all these commodities. Such dominance possibly impedes the development of models that might...
Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2405(17)
... ). However, the major hydrothermal event in the Witwatersrand Basin, and possibly over much of the Kaapvaal Craton, occurred at around 2050–2000 Ma. The major thermal events that affected the Witwatersrand Basin at that time include the emplacement of the Bushveld Complex and related igneous rocks...