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Gamsberg Deposit

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Journal Article
Published: 01 March 2005
South African Journal of Geology (2005) 108 (1): 35–50.
...M. Stalder; A. Rozendaal Abstract Bedded barite forms a distinct component of four Broken Hill-type deposits in the amphibolite-facies metamorphosed Bushmanland sequence of South Africa. In the Gamsberg Zn-Pb deposit, barite has been effectively fractionated from the base metal sulphide facies...
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Journal Article
Published: 01 April 2005
The Canadian Mineralogist (2005) 43 (2): 585–599.
...Marcel Stalder; Abraham Rozendaal Abstract Calderite-rich garnet and franklinite–jacobsite-rich spinel occur in amphibolite-facies hydrothermal metasedimentary rocks that stratigraphically overlie the Proterozoic Gamsberg Zn–Pb deposit, South Africa. The minerals are restricted in occurrence...
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Journal Article
Published: 01 December 2002
Mineralogical Magazine (2002) 66 (6): 915–927.
...M. Stalder; A. Rozendaal Abstract Granular aggregates of fine-grained graftonite (Fe,Mn,Ca) 3 (PO 4 ) 2 and intergrown wolfeite (Fe,Mn) 2 (PO 4 )(OH) occur in amphibolite-facies metamorphosed iron formations associated with the Gamsberg Zn-Pb deposit, South Africa. To date, these minerals were...
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Journal Article
Journal: Economic Geology
Published: 01 August 2020
Economic Geology (2020) 115 (5): 1021–1054.
... of the district and the site of active resource extension and brownfields exploration, it has been the subject of few focused studies ( Stedman, 1980 ; Strydom, 1986 ; Neufeld, 2005 ), and even fewer publications ( Ryan et al., 1986 ). Fig. 1. A) Locations of the major deposits of the Aggeneys-Gamsberg...
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Location of the Gamsberg deposit within the Aggeneys-Gamsberg ore district; N.P.=Namaqua Province (after Stalder and Rozendaal, 2004; McClung et al., 2007).
Published: 01 December 2022
Figure 1. Location of the Gamsberg deposit within the Aggeneys-Gamsberg ore district; N.P.=Namaqua Province (after Stalder and Rozendaal, 2004 ; McClung et al., 2007 ).
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a) Location of the Gamsberg deposit within the Namaqua Province, South Africa. b) Surface geology of the Gamsberg deposit.
Published: 01 April 2005
F ig . 1. a) Location of the Gamsberg deposit within the Namaqua Province, South Africa. b) Surface geology of the Gamsberg deposit.
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Surface geology of the Gamsberg deposit. The distribution of barite within the Gams Formation is indicated. Sections A-A’ and B-B’ refer to cross-sections depicted in Figure 4.
Published: 01 March 2005
Figure 3. Surface geology of the Gamsberg deposit. The distribution of barite within the Gams Formation is indicated. Sections A-A’ and B-B’ refer to cross-sections depicted in Figure 4 .
Journal Article
Published: 01 December 2022
South African Journal of Geology (2022) 125 (3-4): 323–336.
...Figure 1. Location of the Gamsberg deposit within the Aggeneys-Gamsberg ore district; N.P.=Namaqua Province (after Stalder and Rozendaal, 2004 ; McClung et al., 2007 ). ...
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(a) Lithological column through the Koeris Formation at Gamsberg (after Praekelt et al., 2006); (b) Geological map of the Gamsberg deposit (after Stalder and Rozendaal, 2004); (c) Cross-section of the Gamsberg deposit through the northern orebody (Stalder and Rozendaal, 2004). LA=lower amphibolite; UA=upper amphibolite; LS=lower metasedimentary rocks; US=upper metasedimentary rocks.
Published: 01 December 2022
Figure 2. ( a ) Lithological column through the Koeris Formation at Gamsberg (after Praekelt et al., 2006 ); ( b ) Geological map of the Gamsberg deposit (after Stalder and Rozendaal, 2004 ); ( c ) Cross-section of the Gamsberg deposit through the northern orebody ( Stalder and Rozendaal, 2004
Journal Article
Journal: Economic Geology
Published: 01 February 1989
Economic Geology (1989) 84 (1): 34–48.
... massive sulfide deposits of the central part of the Namaqua province. Whereas the Prieska deposits are related to hydrothermal action in a volcano-sedimentary sequence, no metamorphic equivalents of alteration pipes have been found at the sediment-hosted Aggeneys-Gamsberg deposits. GeoRef, Copyright...
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Lithostratigraphy and structure ofthe Gamsberg zinc deposit. This world class zinc resource is hosted by a large north-east plunging sheath fold. (Section looking north.)
Published: 01 March 2017
Figure 11. Lithostratigraphy and structure ofthe Gamsberg zinc deposit. This world class zinc resource is hosted by a large north-east plunging sheath fold. (Section looking north.)
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Figure 12.
Published: 01 March 2017
Figure 12. (a) The Gamsberg zinc deposit is the type area of the Gams Member, its distribution is shown in a simplified geological map of the Gamsberg basin. The position ofthe main ore bodies are indicated as well as the perimeters ofthe planned open cast mine ( Table 1 ). (b) Verticaland
Journal Article
Published: 01 March 2017
South African Journal of Geology (2017) 120 (1): 153–186.
...Figure 11. Lithostratigraphy and structure ofthe Gamsberg zinc deposit. This world class zinc resource is hosted by a large north-east plunging sheath fold. (Section looking north.) ...
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Schematic section showing the distribution of hydrothermal facies at Gamsberg. The B unit is best developed at Gamsberg North, but thins out rapidly towards the eastern barite deposit. Massive barite and interbedded Fe- and Ba-rich metachert at Gamsberg East can be correlated with more Fe- and Mn-rich silicate and silicate-carbonate facies sediments at Gamsberg North.
Published: 01 March 2005
Figure 5. Schematic section showing the distribution of hydrothermal facies at Gamsberg. The B unit is best developed at Gamsberg North, but thins out rapidly towards the eastern barite deposit. Massive barite and interbedded Fe- and Ba-rich metachert at Gamsberg East can be correlated with more
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(a) Location of the Aggeneys-Gamsberg ore district within the Namaqua Province. (b) Geological map of the Aggeneys-Gamsberg ore district showing the position of the four major base metal deposits.
Published: 01 March 2005
Figure 1. ( a ) Location of the Aggeneys-Gamsberg ore district within the Namaqua Province. ( b ) Geological map of the Aggeneys-Gamsberg ore district showing the position of the four major base metal deposits.
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(a) Regional setting of the Aggeneys-Gamsberg Ore District in the Namaqua Sector of Namaqua-Natal Metamorphic Province, (b) General view of the A-GOD from the west. Broken Hill-Deeps operations in theforeground and the village ofAggeneys and Gamsberg zinc deposit in the far distance (Photography Arnand vanHeerden, with permission).
Published: 01 March 2017
Figure 9. (a) Regional setting of the Aggeneys-Gamsberg Ore District in the Namaqua Sector of Namaqua-Natal Metamorphic Province, (b) General view of the A-GOD from the west. Broken Hill-Deeps operations in theforeground and the village ofAggeneys and Gamsberg zinc deposit in the far distance
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Schematic illustration ofthe depositional environment ofthe deposits of the A-GOD showing the different settings of the Gamsberg. Broken Hill-Deeps and Swartberg deposits within a continental and tensional tectonic regime. Pelitic ores are the equivalent of organic-rich shales (orange) and are associated with chemogenic ores (black). Gamsberg is interpreted as distal ore with respect to the main fault related feeders compared to the proximal ores of Broken Hill-Deeps and Swartberg. The heat source is a deep-seated basaltic magma which extruded after deposition ofthe Gams Member (Stalder, 2004; Stalder and Rozendaal2004b).
Published: 01 March 2017
Figure 19. Schematic illustration ofthe depositional environment ofthe deposits of the A-GOD showing the different settings of the Gamsberg. Broken Hill-Deeps and Swartberg deposits within a continental and tensional tectonic regime. Pelitic ores are the equivalent of organic-rich shales (orange
Journal Article
Published: 01 March 2016
South African Journal of Geology (2016) 119 (1): 63–76.
...), which is an Environmental Mapping and Analysis Program. The Aggeneys Cu-Pb-Zn deposit, situated in the arid north western part of South Africa, represents a unique field laboratory for testing these new tools. Here spaceborne hyperspectral data covering the Swartberg, Big Syncline and Gamsberg area were...
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(A) The location (Google Earth) and simplified geology (adapted from Rozendaal et al., 2017) of the four polymetallic deposits of the Gamsberg-Aggeneys Ore District, namely Broken Hill, Swartberg (Black Mountain), Gamsberg, and Big Syncline. (B) The area of the black rectangle in Figure 1A showing the location of the drill cores drilled during the 2015 to 2019 drilling campaign at Big Syncline, with the drill cores that were sampled for this study highlighted in three different colours (map provided by Vedanta Plc). Coordinates are given in the format of the South African Coordinate Reference System, which is based on the World Geodetic System 1984 ellipsoid, utilising a central meridian of 19°E and a latitude of origin of 0°.
Published: 01 March 2024
Figure 1. ( A ) The location (Google Earth) and simplified geology (adapted from Rozendaal et al., 2017 ) of the four polymetallic deposits of the Gamsberg-Aggeneys Ore District, namely Broken Hill, Swartberg (Black Mountain), Gamsberg, and Big Syncline. ( B ) The area of the black rectangle
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Location of the four major base metal deposits in the Aggeneys-Gamsberg ore district.
Published: 01 December 2002
F ig . 1. Location of the four major base metal deposits in the Aggeneys-Gamsberg ore district.