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Limpopo province

Sadiki, P. and Ramutsmdela, M. (2002). Peri-urban transformation in South Africa Experiences from Limpopo province. Geojournal 57, 75-81. [Pg.245]

Dallaire R, Dewailly E, Pereg D et al (2(K)9) Thyroid function and plasma concentrations of polyhalogenated compounds in Inuit adults. Environ Health Perspect 117 1380-1386 Damerud PO, Aune M, Larsson L et al (2011) Levels of brominated flame retardants and other persistent organic pollutants in breast milk samples from Limpopo province. South Africa. Sci Total Environ 409 4048 053... [Pg.87]

The morama bean is an underutilized leguminous oilseed native to the Kalahari Desert and neighboring sandy regions of Botswana, Namibia, and South Africa (Limpopo, North-West, Gauteng, and Northern Cape provinces), and forms part of the diet of the indigenous population in these countries. It is also known as gemsbok bean. [Pg.188]

Fig. 1. Map showing station locations, topography and principal geological provinces in the region of study within southern Africa, Fifty-five broadband (REFTEK/STS-2) stations were installed in April 1997 in South Africa, Botswana and Zimbabwe. Stations in light blue were redeployed in April 1998 to sites indicated in yellow. A total of 82 sites were occupied over the two year deployment. In addition, three global seismic network broadband stations (white triangles) are located in the region and their data incorporated in the analysis. The array extends from the Cape Fold Belt in the south, through the Proterozoic Namaqua-Natal Mobile Belt, across the Kaapvaal Craton and Bushveld Province, through the Archaean Limpopo Mobile Belt and into the Zimbabwe Craton. On the west, the array covers part of the Kheis and Okwa Proterozoic Fold and Thrust Belts of Botswana and western South Africa. To the east, the array extends into the Early Archaean Barberton terrane, near the NW border with Swaziland. Published in James et al., GRL28, 2001, fig. 1. Fig. 1. Map showing station locations, topography and principal geological provinces in the region of study within southern Africa, Fifty-five broadband (REFTEK/STS-2) stations were installed in April 1997 in South Africa, Botswana and Zimbabwe. Stations in light blue were redeployed in April 1998 to sites indicated in yellow. A total of 82 sites were occupied over the two year deployment. In addition, three global seismic network broadband stations (white triangles) are located in the region and their data incorporated in the analysis. The array extends from the Cape Fold Belt in the south, through the Proterozoic Namaqua-Natal Mobile Belt, across the Kaapvaal Craton and Bushveld Province, through the Archaean Limpopo Mobile Belt and into the Zimbabwe Craton. On the west, the array covers part of the Kheis and Okwa Proterozoic Fold and Thrust Belts of Botswana and western South Africa. To the east, the array extends into the Early Archaean Barberton terrane, near the NW border with Swaziland. Published in James et al., GRL28, 2001, fig. 1.
REE content [in ppm (wt)] of high-grade metasedimentary rocks from the Archean Limpopo Belt and Kapuskasing Structural Province. (From Taylor et al. 1986.)... [Pg.522]


See other pages where Limpopo province is mentioned: [Pg.345]    [Pg.191]    [Pg.24]    [Pg.149]    [Pg.345]    [Pg.191]    [Pg.24]    [Pg.149]    [Pg.12]    [Pg.12]    [Pg.41]    [Pg.201]   
See also in sourсe #XX -- [ Pg.24 ]




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