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Aggeneys Mine

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The names of various inselbergs around Aggeneys. The inset shows the locality of the Aggeneys mining district within the Mesoproterozoic Namaqua-Natal mobile belt of South Africa.
Published: 01 March 2005
Figure 1. The names of various inselbergs around Aggeneys. The inset shows the locality of the Aggeneys mining district within the Mesoproterozoic Namaqua-Natal mobile belt of South Africa.
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Published: 01 October 2006
TABLE 3. VARIATION IN GARNET MnO IN TWO GARNET-RICH BEDS OF A SMALL BANDED IRON FORMATION INTERSECTED IN DIAMOND DRILL-CORE, AGGENEYS MINE, NAMAQUALAND, SOUTH AFRICA
Journal Article
Published: 01 December 2022
South African Journal of Geology (2022) 125 (3-4): 337–344.
... was likely derived from the rapidly-exhumed 1.2 to 1.0 Ga Namaqua-Natal orogenic belt on the craton’s margin that formed during Rodinia supercontinent assembly’. Figure 5. Concordia diagram for Hotson Formation schist sample DC1321 from Black Mountain mine. Two alternative age interpretations...
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Journal Article
Published: 01 March 2005
South African Journal of Geology (2005) 108 (1): 2.
... in Namibia, a new shaft and decline at Aggeneys to exploit the Broken Hill deep orebody, and the blending of ore from Swartberg and Gamsberg into the Aggeneys run of mine. As a consequence of new research results and timely reviews being presented at the Geocongress held in Windhoek during July 2002...
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Stratigraphic column at the Broken Hill Mine, Aggeneys. Due to overturning the units have names based on the structural succession found at the mine (modified after Lipson, 1990 and McClung, 2006).
Published: 01 March 2007
Figure 3. Stratigraphic column at the Broken Hill Mine, Aggeneys. Due to overturning the units have names based on the structural succession found at the mine (modified after Lipson, 1990 and McClung, 2006 ).
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Remobilisation of sulphides at the Broken Hill Mine, Aggeneys. (A) Giant crystal pegmatoidal pod of remobilized sulphide (mainly yellow chalcopyrite and grey galena) developed in the metasedimentary envelope (black magnetite quartzite). (B) Coarse-grained lenses and pods of remobilized sulphides within massive pyrrhotite ore of the LOB. Photos are available in colour at: http://web.uct.ac.za/depts/geolsci/
Published: 01 March 2005
Figure 2. Remobilisation of sulphides at the Broken Hill Mine, Aggeneys. ( A ) Giant crystal pegmatoidal pod of remobilized sulphide (mainly yellow chalcopyrite and grey galena) developed in the metasedimentary envelope (black magnetite quartzite). ( B ) Coarse-grained lenses and pods
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A. Polished thin section of diamond drill core of banded iron formation (BIF) from Broken Hill, New South Wales, showing bedded arrangement of the garnet – quartz – magnetite – apatite assemblage, and the positions of fine beds 1 and 2 containing the abundant flakes of primary chlorite (Table 1, Figs. 2–4. B. BIF, polished thin section of diamond drill-core, similar to that of Broken Hill, but from the environs of the Aggeneys mine, Namaqualand. Beds 1 and 2 of Table 3 and Figure 5 are indicated by arrows. C. Polished thin section of Broken Hill diamond drill-core showing BIF (upper quarter of photograph) and subjacent garnet–magnetite-bearing quartzofeldspathic gneiss (QFG); boundary “b” between units is shown by an arrow. Beds 1–4 of Table 4 and Figures 6–9 are indicated by numerals and arrows. D. Polished thin section of quartz – primary chlorite – muscovite – biotite – garnet – staurolite rock from diamond drill-core PJ 06, Hemlo, Ontario. Blue line indicates location of change of biotite compositions between Domains 1 and 2 of Figure 10 and Table 5.
Published: 01 October 2006
( Table 1 , Figs. 2 – 4 . B. BIF, polished thin section of diamond drill-core, similar to that of Broken Hill, but from the environs of the Aggeneys mine, Namaqualand. Beds 1 and 2 of Table 3 and Figure 5 are indicated by arrows. C. Polished thin section of Broken Hill diamond drill-core showing BIF
Journal Article
Published: 01 March 2017
South African Journal of Geology (2017) 120 (1): 153–186.
... grade metamorphism and polyphase deformation. It is the host to world class base metal sulphide resources that have been mined for more than a century. Most of these mines are no longer in production such that the Cu-Pb-Zn-Ag mines in the Aggeneys-Gamsberg Ore District (A-GOD), with a total output...
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A) Locations of the major deposits of the Aggeneys-Gamsberg ore district, near the mining town of Aggeneys. B) Location of the district in the northwest of South Africa.
Published: 01 August 2020
Fig. 1. A) Locations of the major deposits of the Aggeneys-Gamsberg ore district, near the mining town of Aggeneys. B) Location of the district in the northwest of South Africa.
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U-Pb concordia diagram for zircons from the Shaft Schist (sample ALP 136) from the Broken Hill Mine, Aggeneys.
Published: 01 March 2007
Figure 13. U-Pb concordia diagram for zircons from the Shaft Schist (sample ALP 136) from the Broken Hill Mine, Aggeneys.
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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Journal Article
Published: 01 March 2005
South African Journal of Geology (2005) 108 (1): 51–70.
...Figure 1. The names of various inselbergs around Aggeneys. The inset shows the locality of the Aggeneys mining district within the Mesoproterozoic Namaqua-Natal mobile belt of South Africa. ...
FIGURES | View All (8)
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U-Pb concordia diagram for zircons from Namies Schist (ALP 39) from the Broken Hill Mine, Aggeneys. The inset shows a histogram of 207Pb/206Pb ages for this sample.
Published: 01 March 2007
Figure 9. U-Pb concordia diagram for zircons from Namies Schist (ALP 39) from the Broken Hill Mine, Aggeneys. The inset shows a histogram of 207 Pb/ 206 Pb ages for this sample.
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U-Pb concordia diagram for zircons from Dark Quartzite (sample ALP 42) from the Broken Hill Mine, Aggeneys. The inset shows a histogram of 207Pb/206Pb ages for this sample.
Published: 01 March 2007
Figure 10. U-Pb concordia diagram for zircons from Dark Quartzite (sample ALP 42) from the Broken Hill Mine, Aggeneys. The inset shows a histogram of 207 Pb/ 206 Pb ages for this sample.
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U-Pb concordia diagrams for zircons from the Ore Schist Formation Garnet Quartzite (sample ALP 114) from the Broken Hill Mine, Aggeneys. (a) shows the older ages of the cores with (b) showing the younger ages of the low Th and Th/U overgrowths.
Published: 01 March 2007
Figure 12. U-Pb concordia diagrams for zircons from the Ore Schist Formation Garnet Quartzite (sample ALP 114) from the Broken Hill Mine, Aggeneys. (a) shows the older ages of the cores with (b) showing the younger ages of the low Th and Th/U overgrowths.
Journal Article
Published: 01 March 2025
South African Journal of Geology (2025) 128 (1): 91–114.
...W.J. Nel; W.P. Colliston Abstract Most of the deformed amphibolite-grade lithological units of the eastern Aggeneys Terrane are traditionally regarded as correlatives of the Wortel Formation of the Aggeneys Subgroup in the Bushmanland Group. Recent structural-stratigraphic mapping in the eastern...
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Journal Article
Published: 01 March 2007
South African Journal of Geology (2007) 110 (1): 59–86.
...Figure 3. Stratigraphic column at the Broken Hill Mine, Aggeneys. Due to overturning the units have names based on the structural succession found at the mine (modified after Lipson, 1990 and McClung, 2006 ). ...
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Journal Article
Published: 01 March 2005
South African Journal of Geology (2005) 108 (1): 3–4.
... was associated with a quartzite unit that outcropped intermittently on farms between Springbok and Aggeneys. It also played an important role in the mineralisation in the O’kiep Copper Company’s mines. Gossan samples at Aggeneys returned as much as 4.8% Cu, 6.8% Pb and 0.15% Zn. During the field work...
Journal Article
Published: 01 March 2008
South African Journal of Geology (2008) 111 (1): 112–113.
... to the Broken Hill Mine. Consequently we used Lipson’s (1990) terminology as this was/is used at the mine and related directly to the succession there ( Bailie et al ., 2007a , pp. 62–63). We noted (in the abstract and summary, p. 83) that the ages obtained relate to the Bushmanland Group in the Aggeneys...
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Major element plots for the Bushmanland Group metasediments at the Broken Hill Mine, Aggeneys. (a) TiO2 vs. SiO2. (b) Al2O3 vs. SiO2. (c) Al2O3 vs. SiO2 for the Shaft Schist from various boreholes at the Broken Hill Mine. (d) TiO2 vs. Al2O3. (e) A-CN-K ternary plot (after Nesbitt and Young, 1984; 1989). (f) K2O-MgO-Na2O ternary plot illustrating the K-enrichment and Na-depletion of the metasediments.
Published: 01 March 2007
Figure 4. Major element plots for the Bushmanland Group metasediments at the Broken Hill Mine, Aggeneys. ( a ) TiO 2 vs. SiO 2 . ( b ) Al 2 O 3 vs. SiO 2 . ( c ) Al 2 O 3 vs. SiO 2 for the Shaft Schist from various boreholes at the Broken Hill Mine. ( d ) TiO 2 vs. Al 2 O 3 . ( e ) A-CN-K