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Soutpansberg Basin

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Journal Article
Published: 07 February 2017
Geochemistry: Exploration, Environment, Analysis (2017) 17 (1): 35–41.
...Ntokozo Malaza Abstract The objective of this study was to investigate the impact of anthropogenic and natural sources of contamination on the groundwater quality of the unconfined aquifer system of the Soutpansberg Basin around Tshikondeni. Fifteen groundwater samples were collected and analysed...
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Journal Article
Published: 01 March 2015
South African Journal of Geology (2015) 118 (1): 83–90.
...A. SHABALALA; P.K. NYABEZE; Z. MANKAYI; J. OLIVIER Abstract Investigations were carried out in order to assess the groundwater chemistry of aquifers in the Soutpansberg Basin. Water samples were collected from Sagole, Tshipise, Mphephu, Dopeni and Siloam thermal springs during the winter and summer...
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Image
Map of the study area in the <b>Soutpansberg</b> <b>Basin</b>.
Published: 07 February 2017
Fig. 1. Map of the study area in the Soutpansberg Basin.
Journal Article
Published: 01 March 2016
South African Journal of Geology (2016) 119 (1): 235–242.
.... In this study we apply FA to the Soutpansberg Mountains (SM) to better characterise its extensive fracture network (most notably regional faults) covering many orders of scale, and to test whether the results mimic known geological complexities. In addition, we test whether there is any link between the fractal...
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Journal Article
Published: 01 September 2001
South African Journal of Geology (2001) 104 (3): 205–216.
... basins, represented by the Blouberg, Waterberg and Soutpansberg strata are developed regionally, and appear to have their boundaries at least partially controlled by the Palala Shear Zone. The 1400m-thick Blouberg Formation (Table 1 ) is preserved only above the Palala Shear Zone, and may have been...
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Journal Article
Published: 01 June 2006
South African Journal of Geology (2006) 109 (1-2): 139–156.
.... Cheney , E.S. and Twist , D. ( 1986 ). The Waterberg “Basin” – A reappraisal. Transactions of the Geological Society of South Africa , 89 , 353 – 360 . Cheney , E.S. , Barton , J.M. and Brandl , G. ( 1990 ). Extent and age of the Soutpansberg sequences of southern Africa...
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Journal Article
Journal: Economic Geology
Published: 01 September 2002
Economic Geology (2002) 97 (6): 1151–1166.
... are concentrated in delta distributary channel sand deposits which were forming during peak transgression in a coastal embayment of the Soutpansberg-Palapye basin. B. Manganese precipitation takes place where Mn-bearing continental run off mixes with oxygenated marine water. Precipitation is biogenically mediated...
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Journal Article
Published: 01 June 2004
South African Journal of Geology (2004) 107 (1-2): 233–254.
...-northeast, yield antipodal directions with a site mean pole at 15.6°north, 17.1°east, A 95 = 8.9°. These data are interpreted to indicate that the ~1879 to ~1872 Ma dolerites were intruded into the Waterberg Group during voluminous magmatism associated with development of the Soutpansberg rift basin. Older...
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Journal Article
Published: 01 June 1997
South African Journal of Geology (1997) 100 (2): 151–156.
...D. L. Reid; D. C. Rex; G. Brandl Abstract Jurassic basalts cap the Karoo stratigraphic sequence in the Ellisras sub-basin of the Northern Province. The 75-metre section of basalt flows, obtained from a borehole, is probably a remnant of a thicker accumulation of unknown thickness. K-Ar ages...
Journal Article
Published: 01 June 2004
South African Journal of Geology (2004) 107 (1-2): 45–58.
... imparted a mechanical anisotropy to the mantle that controlled the subsequent magmatic history of cratonic southern Africa. We furthermore suggest that four major Precambrian magmatic events: the Great Dyke, the Ventersdorp, Bushveld, and the Soutpansberg, all represent extensional failure along planes...
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Journal Article
Published: 01 June 2015
South African Journal of Geology (2015) 118 (2): 173–184.
... and the Central Zone of the Limpopo Mobile Belt (LMB) either 2.65 Ga or 2.0 Ga. Bordering the basin in the north is the Beit-Bridge Complex which is composed of arnothosites, gabbros, serpentinites and gneiss, while in the south, it is the volcano-sedimentary Soutpansberg Group ( Figure 1 ). The deposition...
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Journal Article
Published: 01 March 2019
South African Journal of Geology (2019) 122 (1): 1–16.
...N. Barbolini; V. Nxumalo; N. Wagner; J. Kramers; C. Vorster; B. Cairncross; M.K. Bamford Abstract Strata of the Springbok Flats, Ellisras and Tshipise (Soutpansberg-Pafuri) basins of South Africa are considered to have been deposited contemporaneously with those of the main Karoo Basin (MKB...
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Journal Article
Published: 01 June 2004
South African Journal of Geology (2004) 107 (1-2): 13–32.
... which the younger domains were accreted during formation of the Kaapvaal Craton. By ~3 Ga the lithosphere was sufficiently rigid to support development of the Dominion, Witwatersrand and Pongola sedimentary basins, followed by extensive volcanism during the Ventersdorp and concomitant granitoid activity...
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Image
( A ) Distribution of Karoo <b>basins</b> in southern Africa and ( B ) lithostrati...
Published: 01 March 2019
Figure 1. ( A ) Distribution of Karoo basins in southern Africa and ( B ) lithostratigraphic correlation of the main Karoo Basin (MKB), Springbok Flats Basin (SFB), Ellisras, and Tshipise (Soutpansberg-Pafuri) basins in South Africa (after Johnson et al., 1996, 2006 ; Catuneanu et al., 2005 ).
Image
A geographical map with rivers, showing the location of thermal springs and...
Published: 01 March 2015
Figure 1 A geographical map with rivers, showing the location of thermal springs and the outline of the Soutpansberg basin located in the northern part of South Africa.
Series: Geological Society, London, Memoirs
Published: 01 January 2015
DOI: 10.1144/M43.2
EISBN: 9781862397194
... ) possibly also playing a role. Intrusion of the c. 2.5 Ga Bushveld Complex in central-north Kaapvaal terminated Transvaal deposition and was succeeded by complex rifted basins around the intrusion, accommodating continental deposits of the Waterberg (Fig. 2.8 a) and Soutpansberg Groups ( c. 2.05–1.7 Ga...
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Journal Article
Published: 01 December 2014
South African Journal of Geology (2014) 117 (2): 193–210.
... the main Karoo Basin led to the formation of a retroarc foreland system. The smaller coalfields in the northern part of south Africa, including the Waterberg, Soutpansberg and Tuli Coalfields, were interpreted as having been deposited in back-bulge basins tectonically related to the main Karoo Basin...
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Journal Article
Published: 01 March 2002
South African Journal of Geology (2002) 105 (1): 51–66.
...Emese M. Bordy; Octavian Catuneanu Abstract The sedimentary rocks of the Karoo Supergroup in the Tuli Basin (South Africa) may be grouped into four stratigraphic units: the Basal, Middle and Upper units, and the Clarens Formation. This paper presents the findings of the sedimentological...
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Journal Article
Published: 01 December 2013
South African Journal of Geology (2013) 116 (2): 323–345.
... ) coalfields formed within a larger intracratonic trough (defined largely by the Proterozoic Soutpansberg-Waterberg basins) and were subjected to tectonic/structural reactivation during Permian to early Triassic times ( Arnot and Williams, 2007 , p.7-1). Several structural lineaments in the basement rocks...
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Journal Article
Published: 01 March 2019
South African Journal of Geology (2019) 122 (1): 79–96.
...T. Andersen; M.A. Elburg; H.S. Van Niekerk Abstract Laser-ablation ICPMS U-Pb and Lu-Hf isotope data on detrital zircon in sandstone from the Palaeoproterozoic Waterberg Group in the Waterberg and Nylstroom basins of northeastern South Africa contain a dominant Palaeoproterozoic (2000 to 2150 Ma...
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