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Rashoop Granophyre Suite

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Journal Article
Journal: Economic Geology
Published: 01 February 1993
Economic Geology (1993) 88 (1): 27–43.
...N. J. McNaughton; P. J. Pollard; D. I. Groves; R. G. Taylor Abstract Tin mineralization at Zaaiplaats is hosted in alkali feldspar granites of the Lebowa Granite Suite which intrude the Rashoop Granophyre Suite. From the upper contact downward, the alkali feldspar granites include the marginal...
Journal Article
Published: 01 December 2004
South African Journal of Geology (2004) 107 (4): 633–652.
...R.H. Bailie; L.J. Robb Abstract Field mapping of a region in the central southeastern portion of the Bushveld Complex in an area underlain by granites of the Lebowa Granite Suite, granophyres of the Rashoop Granophyre Suite, the Rooiberg Group and Transvaal Supergroup has identified at least four...
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Journal Article
Journal: Economic Geology
Published: 01 November 1991
Economic Geology (1991) 86 (7): 1401–1433.
...P. J. Pollard; R. G. Taylor; R. P. Taylor; David I. Groves Abstract Tin with associated tungsten and rare earth element mineralization at the Zaaiplaats mine is hosted by alkali feldspar granites of the Lebowa Granite Suite which intrude granophyric granites of the Rashoop Granophyre Suite. From...
Journal Article
Published: 01 March 2020
South African Journal of Geology (2020) 123 (1): 117–128.
... and is intrusive into the Rooiberg Group, the Rashoop Granophyre Suite and the Klipkloof Granite. It is in turn intruded by the Makhutso Granite, the youngest known granite of the Lebowa Granite Suite. The Verena Granite is characterised by its coarse to very coarse-grained nature, its pinkish to reddish colours...
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Image
Schematic geological cross section across the Groenfontein tin mine from the Rashoop Granophyre Suite towards the Nebo Granite (southwest to northeast), along line A – A’ in Figure 2. Modified after Vonopartis et al. (2020).
Published: 01 March 2022
Figure 3. Schematic geological cross section across the Groenfontein tin mine from the Rashoop Granophyre Suite towards the Nebo Granite (southwest to northeast), along line A – A’ in Figure 2 . Modified after Vonopartis et al. ( 2020 ).
Image
 (a) Generalized tectonic and geological overview of the western part of the Bushveld Complex. Stratigraphic units: AI, alkaline intrusion; LGS, Lebowa Granite Suite; RGS, Rashoop Granophyre Suite; RLS, Rustenburg Layered Suite; RG, Rooiberg Group; TS, Transvaal sequence. (b) Simplified geological map of southwestern zone near Rustenburg with the location of the Impala Mine.
Published: 01 May 2004
Fig. 1.  ( a ) Generalized tectonic and geological overview of the western part of the Bushveld Complex. Stratigraphic units: AI, alkaline intrusion; LGS, Lebowa Granite Suite; RGS, Rashoop Granophyre Suite; RLS, Rustenburg Layered Suite; RG, Rooiberg Group; TS, Transvaal sequence. ( b
Journal Article
Published: 01 March 2022
South African Journal of Geology (2022) 125 (1): 45–60.
...Figure 3. Schematic geological cross section across the Groenfontein tin mine from the Rashoop Granophyre Suite towards the Nebo Granite (southwest to northeast), along line A – A’ in Figure 2 . Modified after Vonopartis et al. ( 2020 ). ...
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Journal Article
Journal: The Leading Edge
Published: 01 June 2011
The Leading Edge (2011) 30 (6): 622–638.
...Geoff Campbell Abstract The Bushveld Complex consists of three roughly coeval components, namely the Lebowa Granite Suite, the Rashoop Granophyre, and the Rustenburrg Layered Suite (RLS), the latter being the only economically important unit. The RLS underlies an area of ∼65,000 km 2...
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Journal Article
Published: 01 March 2011
South African Journal of Geology (2011) 114 (1): 1–14.
... and Bushveld-age granites. Table 1. A summary of available geochronological constraints from the Bushveld Complex, Rooiberg Group and Rashoop Granophyre Suite. Rock Unit Age (Ma) Mineral Method Reference RLS = Rustenburg Layered Suite LGS = Lebowa Granite Suite...
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Image
Location map of the Pilanesberg Alkaline Province, showing the local geology including the Transvaal Supergroup (TS), with an emphasis on its strata-bound igneous units (namely the Hekpoort Formation and the Machadodorp Member), and Bushveld Complex (BC) in the Transvaal sub-basin (TB). The location of borehole BB11, close to Carletonville, is indicated by a red disc. RLS=Rustenburg Layered Suite. The other Bushveld Complex units include the Rooiberg Group, the Rashoop Granophyre and the Lebowa Granite. The Pilanesberg dyke swarm location is from Elburg and Cawthorn (2017). The inset in the lower right corner shows the Kaapvaal Craton boundaries and preserved extent of the TS mainly distributed within two sub-basins, the TB and the Griqualand West sub-basin (GWB). Compiled from 1:250000 scale South African geological maps (i.e., maps 2228, 2230, 2326, 2228, 2330, 2426, 2428, 2430, 2526, 2528, 2530, 2626, 2628, 2630).
Published: 10 November 2020
). The location of borehole BB11, close to Carletonville, is indicated by a red disc. RLS=Rustenburg Layered Suite. The other Bushveld Complex units include the Rooiberg Group, the Rashoop Granophyre and the Lebowa Granite. The Pilanesberg dyke swarm location is from Elburg and Cawthorn ( 2017 ). The inset
Image
Distribution of the outcrops of the Transvaal Supergroup with the Hekpoort Formation (2236Ma; Cornell et al., 1996) within the Transvaal sub-basin (TB). The Bushveld Complex (BC), ca. 2054 Ma (Zeh et al., 2015), units include the volcanic Rooiberg Group, and the extrusive Rashoop Granophyre and Lebowa Granite suites. The location of the Griqualand West sub-basin (GWB) and the Ongeluk Formation (2426Ma; Gumsley et al., 2017) within the Kaapvaal Craton is shown in the inset. The red rectangles along the Hekpoort outcrops represent areas corresponding to the stratigraphic columns in Figure 2; namely, southwest to northeast, the Potchefstroom syncline, the Fochville monocline and the Mooikloof monocline. The dashed rectangle shows the location of outcrops between the type locality of Hekpoort and Broederstroom towards the northeast. All compiled from 1:250000 South African geological maps (i.e., maps 2228, 2230, 2326, 2228, 2330, 2426, 2428, 2430, 2526, 2528, 2530, 2626, 2628, 2630) and literature (op. cit.).
Published: 01 December 2020
Granophyre and Lebowa Granite suites. The location of the Griqualand West sub-basin (GWB) and the Ongeluk Formation (2426Ma; Gumsley et al., 2017 ) within the Kaapvaal Craton is shown in the inset. The red rectangles along the Hekpoort outcrops represent areas corresponding to the stratigraphic columns
Image
A. Generalized geologic map of the Bushveld Complex (BC) showing the position of the Merensky reef (white dashed line) and sample location (star). Map modified from Kinnaird et al. (2005) with additional features from Webb et al. (2004) and Vorster (2003). Major faults and fault segments related to the transpressional Thabazimbi-Murchison lineament (TML) are indicated from Good and de Wit (1997). B. Cross section of the Bushveld Complex based on gravity modeling of Webb et al. (2004) at ~25°S latitude, showing the connection at depth of the eastern and western limbs of the Rustenburg Layered Suite and overlying Lebowa granites, Rashoop granophyres, and Rooiberg Group volcanics (combined into a single unit in the cross section) (adapted from Webb et al., 2004). C. Simplified stratigraphic section showing the major subdivisions of the layered mafic-ultramafic rocks (Rustenburg Layered Suite), the position of the platiniferous Merensky reef near the top of the Critical zone, and the approximate positions of major chromitite horizons (LG = Lower Group, MG = Middle Group, UG = Upper Group) in the Critical zone and major magnetite horizons in the Upper zone (MML = main magnetite layer, M = magnetite horizon) (adapted from Li et al., 2001).
Published: 01 May 2008
of the Rustenburg Layered Suite and overlying Lebowa granites, Rashoop granophyres, and Rooiberg Group volcanics (combined into a single unit in the cross section) (adapted from Webb et al., 2004 ). C. Simplified stratigraphic section showing the major subdivisions of the layered mafic-ultramafic rocks (Rustenburg
Journal Article
Published: 01 December 2024
South African Journal of Geology (2024) 127 (4): 731–748.
... by younger sedimentary rocks. Stratigraphically, the Bushveld Complex is broken into the mafic Rustenburg Layered Suite and acidic Lebowa Granite, Rashoop Granophyre, and Rooiberg Volcanic suites (Figure 1). The Rustenburg Layered Suite in turn is divided into the Upper, Main, Critical, Lower, and Marginal...
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Journal Article
Journal: Geology
Published: 01 June 2012
Geology (2012) 40 (6): 491–494.
... and a buoyant Si-rich magma to form the upper part of the sequence is best able to explain the observations. In addition, the phases in the upper siliceous cap of the Bushveld Complex are in major and trace element equilibrium with portions of the overlying Rooiberg rhyolites and/or Rashoop granophyres...
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Journal Article
Journal: Economic Geology
Published: 01 May 2008
Economic Geology (2008) 103 (3): 465–471.
... of the Rustenburg Layered Suite and overlying Lebowa granites, Rashoop granophyres, and Rooiberg Group volcanics (combined into a single unit in the cross section) (adapted from Webb et al., 2004 ). C. Simplified stratigraphic section showing the major subdivisions of the layered mafic-ultramafic rocks (Rustenburg...
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Journal Article
Published: 01 September 2004
South African Journal of Geology (2004) 107 (3): 413–430.
..., and sills of the Rashoop Granophyre Suite. The granites post-date a 7 to 8km thick layered mafic and ultramafic Layered Suite (Figure 1 ), as shown by granite feeder dykes that cut the Layered Suite in the eastern limb of the Complex ( e.g. Hammerbeck, 1970 ; Walraven and Hattingh, 1993 ) and xenoliths...
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Journal Article
Published: 01 June 2000
South African Journal of Geology (2000) 103 (2): 120–127.
... ( Walraven, 1981 ; Eales and Cawthorn, 1996 ). Regional-scale RLS—country rock concordance is demonstrated by the similarity of dips (Figure 2 ). The roof of the complex is composed of Rooiberg Group rhyolites and granophyres of the Rashoop Granophyre Suite ( SACS, 1980 ; Eales and Cawthorn, 1996...
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Journal Article
Published: 01 October 2016
Mineralogical Magazine (2016) 80 (6): 1041–1053.
... is capped by the Rashoop Granophyre Suite. For detailed insights into the geology, stratigraphy and mineralization of the RLS, the reader is referred to Eales and Cawthorn (1996) , Lee (1996) , Cawthorn et al. (2005) , Kruger (2005) , Naldrett et al. (2011) and Maier et al. (2013) . Fig...
FIGURES
Journal Article
Published: 01 December 2023
South African Journal of Geology (2023) 126 (4): 425–450.
... ( Eriksson et al., 2006 ). We also do not recognise the Rashoop Granophyre Suite as a discrete entity as this is a misguided attempt by SACS ( 1980 ) at conflating granophyres of the Rooiberg Group and of the Lebowa Granite Suite into a single group. (They have different origins and different ages...
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Journal Article
Published: 26 September 2024
The Canadian Journal of Mineralogy and Petrology (2024) 62 (5): 713–730.
... (PGE), vanadium, and fluorite ( Anhaeusser & Maske 1986 , Wilson & Anhaeusser 1998 , Johnson et al. 2006 ). It is stratigraphically subdivided into the Rustenburg Layered Suite, the Rashoop Granophyre Suite, and the Lebowa Granite Suite (LGS) ( Walraven & Hattingh 1993 , Walraven et...
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