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Journal articles on the topic 'Geology - South Africa - Bandelierkop'

Author: Grafiati

Published: 4 June 2021

Last updated: 8 February 2022

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1

Nicoli, G., G. Stevens, J. F. Moyen, and D. Frei. "Rapid evolution from sediment to anatectic granulite in an Archean continental collision zone: the example of the Bandelierkop Formation metapelites, South Marginal Zone, Limpopo Belt, South Africa." Journal of Metamorphic Geology 33, no. 2 (2014): 177–202. http://dx.doi.org/10.1111/jmg.12116.

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2

Cairncross, Bruce. "The Witwatersrand Goldfield, South Africa." Rocks & Minerals 96, no. 4 (2021): 296–351. http://dx.doi.org/10.1080/00357529.2021.1901207.

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3

Cairncross, Bruce. "The Geological Museum, Johannesburg, South Africa." Rocks & Minerals 76, no. 2 (2001): 120–27. http://dx.doi.org/10.1080/00357520109603206.

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4

DE BEER, J. H. "Geology of Johannesburg, Republic of South Africa." Environmental & Engineering Geoscience xxiii, no. 2 (1986): 101–37. http://dx.doi.org/10.2113/gseegeosci.xxiii.2.101.

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5

Smith, Alan M. "Environmental geology, South Africa, and the South African Geological Survey." Environmental Geology and Water Sciences 18, no. 1 (1991): 1–2. http://dx.doi.org/10.1007/bf01704571.

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6

Spears, D. A., P. McL D. Duff, and P. M. Caine. "The West Waterberg tonstein, South Africa." International Journal of Coal Geology 9, no. 3 (1988): 221–33. http://dx.doi.org/10.1016/0166-5162(88)90014-6.

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7

Singh, R. G., G. A. Botha, N. P. Richards, and T. S. McCarthy. "Holocene landslides in KwaZulu-Natal, South Africa." South African Journal of Geology 111, no. 1 (2008): 39–52. http://dx.doi.org/10.2113/gssajg.111.1.39.

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8

CARTER, N. G. "Geology of Port Elizabeth, Republic of South Africa." Environmental & Engineering Geoscience xxiv, no. 4 (1987): 441–67. http://dx.doi.org/10.2113/gseegeosci.xxiv.4.441.

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9

Morton, K. L. "Hydrogeology of the Venetia Diamond Mine, South Africa." South African Journal of Geology 106, no. 2-3 (2003): 193–204. http://dx.doi.org/10.2113/106.2-3.193.

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10

Hirsch, K. K., M. Scheck-Wenderoth, D. A. Paton, and K. Bauer. "Crustal structure beneath the Orange Basin, South Africa." South African Journal of Geology 110, no. 2-3 (2007): 249–60. http://dx.doi.org/10.2113/gssajg.110.2-3.249.

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11

Greyling, M., and J. L. Van Rooy. "Hydrogeological Properties of Gypseous soils in South Africa." South African Journal of Geology 122, no. 3 (2019): 389–96. http://dx.doi.org/10.25131/sajg.122.0029.

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Abstract Gypseous soils occur in the western arid and semi-arid regions of South Africa and Namibia. These soils exhibit a complex nature and abnormal behaviour due to their gypsum content and as such they have become more prevalent in research. As these soils are finding more use in industry, an astute understanding of their hydrogeological properties and behaviour is required. Powdery gypseous soil samples collected from the Northern Cape (Geelvloer) and Western Cape (Rooiberg and R355) Provinces, as well as a prepared sample, are subject to XRD analysis, particle size distribution determination and falling-head permeability tests using both water and brine. The testing served as preliminary research to guide further studies into the topic. The prepared sample, with 19% fines, comprises 35% gypsum and 65% sand. Geelvloer samples, with 91.95% gypsum content, are comprised mostly of sand-sized particles with 45% fines. Rooiberg samples contain 75% fines with a slightly lower gypsum content of 83.25%, while R355 samples have 50% fines with 75.35% gypsum. It is generally understood that particle size distribution contributes to the hydraulic conductivity of soils, where a higher portion fines will result in a lower conductivity. In the case of gypseous soils, the solubility is of importance as well, as it may have long term effects. With the intent of evaluating the effect of the aforementioned factors on the hydraulic conductivity of gypseous soils in South Africa, the samples taken represent differences in particle size distribution and origin. Geelvloer had k-values in the order of 8.82×10-6 m/s, with the brine sample giving 9.43×10-6 m/s, while the k-values for Rooiberg and R355 were in the order of 3.90×10-6 m/s and 5.87×10-6 m/s, respectively. The brine resulted in 5.63×10-6 m/s for Rooiberg and 9.90×10-6 m/s for the R355 sample. The made sample, having less fines, had k values in the order of 2.15×10-5 m/s, and 4.19×10-5 m/s for the brine. The differences between the results are largely negligible and show that despite what is believed to influence the hydraulic conductivity, in the case of gypseous soils in South Africa, on a small scale, it remained unaffected.

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12

Cairncross, Bruce, Wolfgang Windisch, Henk Smit, Allan Fraser, and Jens Gutzmer. "The Vergenoeg: Gauteng Province, South Africa Fluorite Mine." Rocks & Minerals 83, no. 5 (2008): 410–21. http://dx.doi.org/10.3200/rmin.83.5.410-421.

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13

Cook, Robert B. "Diamond, Jagersfontein Mine, Free State Province, South Africa." Rocks & Minerals 75, no. 5 (2000): 344–49. http://dx.doi.org/10.1080/00357520009603092.

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14

Gibbon, Peter. "Steel, South Africa and sanctions." Minerals & Energy - Raw Materials Report 5, no. 2 (1987): 48–59. http://dx.doi.org/10.1080/14041048709409299.

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15

Bullen, W. D., R. J. Thomas, and A. McKenzie. "Gold mineralization in Natal, South Africa." Journal of African Earth Sciences 18, no. 2 (1994): 99–109. http://dx.doi.org/10.1016/0899-5362(94)90023-x.

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16

Haarhoff, J., and L. Korf. "ABA Brink: Pioneer of engineering geology in South Africa." Suid-Afrikaanse Tydskrif vir Natuurwetenskap en Tegnologie 26, no. 2 (2007): 139–50. http://dx.doi.org/10.4102/satnt.v26i2.130.

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Anthony Berrange Antill Brink – beter bekend as ABA Brink aan die lesers van sy boeke, of net Tony vir sy groot aantal kennisse en vriende – was met sy geboorte in 1927 die derde en laaste kind van Rex Brink en Georgina Antill

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17

McCourt, S., R. A. Armstrong, G. H. Grantham, and R. J. Thomas. "Geology and evolution of the Natal belt, South Africa." Journal of African Earth Sciences 46, no. 1-2 (2006): 71–92. http://dx.doi.org/10.1016/j.jafrearsci.2006.01.013.

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18

BLIGNAULT, H. J., and J. N. THERON. "RECONSTRUCTION OF THE ORDOVICIAN PAKHUIS ICE SHEET, SOUTH AFRICA." South African Journal of Geology 113, no. 3 (2010): 335–60. http://dx.doi.org/10.2113/gssajg.113.3.335.

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19

Muir, R. A., E. M. Bordy, J. S. V. Reddering, and J. H. A. Viljoen. "Lithostratigraphy of the Enon Formation (Uitenhage Group), South Africa." South African Journal of Geology 120, no. 2 (2017): 273–80. http://dx.doi.org/10.25131/gssajg.120.2.273.

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Abstract The Uitenhage Group represents the earliest deposits that filled Mesozoic rift basins in the southern Cape of South Africa during the fragmentation of the supercontinent Gondwana. The sedimentology of the Enon Formation records the development of alluvial systems that drained the region since the onset of Gondwanan rifting, and therefore plays an important role in our understanding of early landscape evolution along the southern African continental margin. The mostly coarse conglomeratic unit was deposited continuously in actively subsiding, but separated, rift basins. As a result, the deposits are diachronous between basins and display highly varied thicknesses of up to well over 2000 m.

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20

Viljoen, J. H. A., and H. C. Cawthra. "Lithostratigraphy of the Buffelskloof Formation (Uitenhage Group), South Africa." South African Journal of Geology 122, no. 1 (2019): 97–104. http://dx.doi.org/10.25131/sajg.122.0009.

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21

Hicks, N., and D. J. C. Gold. "Lithostratigraphy of the Sinqeni Formation, Pongola Supergroup, South Africa." South African Journal of Geology 123, no. 3 (2020): 399–420. http://dx.doi.org/10.25131/sajg.123.0027.

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Abstract The Mesoarchaean Sinqeni Formation forms the lowermost unit of the predominantly sedimentary Mozaan Group (Pongola Supergroup) of southern Africa. The formation comprises a dominantly arenaceous succession, which can be subdivided into four members. A laterally discontinuous gold- and uranium-bearing conglomerate package (Denny Dalton Member) is commonly developed at the base of the formation. Overlying the basal conglomerates are two significant quartz arenite packages (Dipka, and Kwaaiman Members) which are separated by a ferruginous shale package (Vlakhoek Member) that locally hosts banded-iron formation. The formation is the most extensively exposed succession of the Mozaan Group, cropping out extensively in the Hartland region, as well as in multiple inliers from Amsterdam in the Mpumalanga to Nkandla in central KwaZulu-Natal, with further exposures in Eswatini. Subeconomic gold and uranium mineralisation occur sporadically within the conglomerates of the Denny Dalton Member, and have previously been mined from multiple occurrences in the White Mfolozi, Mhlatuze and Nkandla Inliers whilst many prospecting trenches are found in the conglomerates of the Hartland and Amsterdam areas. Gold has also briefly been exploited from ferruginous shales and iron formations of the Vlakhoek Member in the Altona area. Litho-correlative equivalents of the formation comprise the Mandeva Formation (White Mfolozi Inlier), Skurwerant Formation (Amsterdam region) and Mkaya Formation (Magudu region).

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22

Campbell, Geoff. "Exploration geophysics of the Bushveld Complex in South Africa." Leading Edge 30, no. 6 (2011): 622–38. http://dx.doi.org/10.1190/1.3599148.

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23

Perritt, Sam, and Mike Roberts. "Flexural-slip structures in the Bushveld Complex, South Africa?" Journal of Structural Geology 29, no. 9 (2007): 1422–29. http://dx.doi.org/10.1016/j.jsg.2007.06.008.

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24

Gutzmer, Jens, and Bruce Cairncross. "Spectacular Minerals from the Kalahari Manganese Field, South Africa." Rocks & Minerals 77, no. 2 (2002): 94–107. http://dx.doi.org/10.1080/00357529.2002.9926665.

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25

O'Regan, Hannah J., and Christine Steininger. "Felidae from Cooper's Cave, South Africa (Mammalia: Carnivora)." Geodiversitas 39, no. 2 (2017): 315–32. http://dx.doi.org/10.5252/g2017n2a8.

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26

Wälde, Thomas. "Mining law reform in South Africa." Minerals & Energy - Raw Materials Report 17, no. 4 (2002): 10–17. http://dx.doi.org/10.1080/14041040209362577.

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27

Midzi, Vunganai, B. Manzunzu, T. Mulabisana, B. S. Zulu, T. Pule, and S. Myendeki. "Probabilistic seismic hazard maps for South Africa." Journal of African Earth Sciences 162 (February 2020): 103689. http://dx.doi.org/10.1016/j.jafrearsci.2019.103689.

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28

Catuneanu, O., H. Wopfner, P. G. Eriksson, et al. "The Karoo basins of south-central Africa." Journal of African Earth Sciences 43, no. 1-3 (2005): 211–53. http://dx.doi.org/10.1016/j.jafrearsci.2005.07.007.

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29

Shone, R. W., and P. W. K. Booth. "The Cape Basin, South Africa: A review." Journal of African Earth Sciences 43, no. 1-3 (2005): 196–210. http://dx.doi.org/10.1016/j.jafrearsci.2005.07.013.

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30

Cornell, D. H., and R. J. Thomas. "Age and tectonic significance of the Banana Beach Gneiss, KwaZulu-Natal South Coast, South Africa." South African Journal of Geology 109, no. 3 (2006): 335–40. http://dx.doi.org/10.2113/gssajg.109.3.335.

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31

STANLEY, G. G. "Gold Extraction Plant Practice in South Africa." Mineral Processing and Extractive Metallurgy Review 6, no. 1-4 (1990): 191–216. http://dx.doi.org/10.1080/08827509008952661.

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32

Weinert, C. H. SW. "Yugawaralite in the Letaba Formation, northeastern KwaZulu--Natal, South Africa." South African Journal of Geology 103, no. 1 (2000): 69–73. http://dx.doi.org/10.2113/103.1.69.

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33

Reid, D. L. "Research on Proterozoic zinc deposits in Namibia and South Africa." South African Journal of Geology 108, no. 1 (2005): 2. http://dx.doi.org/10.2113/108.1.2.

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34

Brauer, B., T. Ryberg, and A. S. Lindeque. "Shallow seismic velocity structure of the Karoo Basin, South Africa." South African Journal of Geology 110, no. 2-3 (2007): 439–48. http://dx.doi.org/10.2113/gssajg.110.2-3.439.

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35

Cairncross, B., and T. S. McCarthy. "A Geological Investigation of Klippan in Mpumalanga Province, South Africa." South African Journal of Geology 111, no. 4 (2008): 421–28. http://dx.doi.org/10.2113/gssajg.111.4.421.

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36

Arima, M., and S. T. Johnston. "Crustal Evolution of the Tugela Terrane, Natal Belt, South Africa." Gondwana Research 4, no. 4 (2001): 563–64. http://dx.doi.org/10.1016/s1342-937x(05)70367-1.

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37

Jonker, B., and T. Abiye. "Groundwater potential of the eastern Kalahari region of South Africa." South African Journal of Geology 120, no. 3 (2017): 385–402. http://dx.doi.org/10.25131/gssajg.120.3.385.

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Abstract An integrated approach involving geological, borehole data, hydrogeochemical and environmental isotope analyses was used to determine the groundwater potential of the eastern Kalahari region of South Africa, an area to the west of Mahikeng that stretches northward from the Orange River into Botswana. The total groundwater resource potential for the eastern Kalahari region of South Africa is estimated at 10127 Mm3/a, with the Kalahari Group aquifer showing the greatest potential, comprising 51% of the total resource. The storage capacity of the Kalahari Group aquifer (7130 Mm3) is also impressive, estimated to be more than twice that of the dolomite aquifer (2728 Mm3). Despite having such great potential, the aquifer is not actively recharged and is often associated with very saline water that is not suitable for human and livestock consumption. The limestone and dolomite aquifers of the Campbell Rand Subgroup, as well as the weathered granitic rocks of the Archaean basement, are considered as the most prospective water bearing formations, with a groundwater resource potential estimate of 1981 Mm3/a and 1845 Mm3/a, respectively. Aquifers with the least potential in the project area comprise the fractured basement rocks of the Kraaipan - Amalia greenstone belt, with a groundwater resource potential of 26 Mm3/a, and the fractured sedimentary rocks of the Asbestos Hills Subgroup, with a groundwater resource potential of 108 Mm3/a. The calculated groundwater storage and resource potential in the eastern Kalahari region of South Africa satisfies a large proportion of the water demand in the region.

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38

Buick, I. S., R. Uken, R. L. Gibson та T. Wallmach. "High-δ13C Paleoproterozoic carbonates from the Transvaal Supergroup, South Africa". Geology 26, № 10 (1998): 875. http://dx.doi.org/10.1130/0091-7613(1998)026<0875:hcpcft>2.3.co;2.

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39

ENGLAND, G. L., B. RASMUSSEN, B. KRAPEZ, and D. I. GROVES. "Archaean oil migration in the Witwatersrand Basin of South Africa." Journal of the Geological Society 159, no. 2 (2002): 189–201. http://dx.doi.org/10.1144/0016-764900-197.

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40

SEPPÄLÄ, MATTI. "Evolution of landforms in South Africa." Boreas 9, no. 4 (2008): 320. http://dx.doi.org/10.1111/j.1502-3885.1980.tb00712.x.

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41

Nyoni, Marco, and Bishop John. "Geophysical surveys at the Nkomati Mine, Mpumalanga, South Africa." Exploration Geophysics 31, no. 3 (2000): 521–30. http://dx.doi.org/10.1071/eg00521.

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42

Cherry, Michael. "Geology hits rich vein as South Africa boosts science spending." Nature 380, no. 6573 (1996): 371. http://dx.doi.org/10.1038/380371a0.

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43

Reimold, W. U., and R. L. Gibson. "Geology and evolution of the Vredefort impact structure, South Africa." Journal of African Earth Sciences 23, no. 2 (1996): 125–62. http://dx.doi.org/10.1016/s0899-5362(96)00059-0.

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44

Konopásek, Jiří, Jiří Sláma, and Jan Košler. "Linking the basement geology along the Africa-South America coasts in the South Atlantic." Precambrian Research 280 (July 2016): 221–30. http://dx.doi.org/10.1016/j.precamres.2016.05.011.

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45

Lepper, Ian, and Peter Robbins. "Gold and international sanctions against South Africa." Minerals & Energy - Raw Materials Report 6, no. 1 (1988): 6–13. http://dx.doi.org/10.1080/14041048809409324.

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46

Jourdan, Paul. "Mining industry in a democratic South Africa." Minerals & Energy - Raw Materials Report 9, no. 4 (1993): 20–23. http://dx.doi.org/10.1080/14041049309408518.

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47

Dansereau, Suzanne. "Mine migrancy in Zimbabwe and South Africa." Minerals & Energy - Raw Materials Report 10, no. 4 (1994): 25–39. http://dx.doi.org/10.1080/14041049409409399.

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48

Gutzmer, J. "Asbestiform manjiroite and todorokite from the Kalahari manganese field, South Africa." South African Journal of Geology 103, no. 3-4 (2000): 163–74. http://dx.doi.org/10.2113/1030163.

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49

Moore, A. E. "Drainage evolution in south-central Africa since the breakup of Gondwana." South African Journal of Geology 104, no. 1 (2001): 47–68. http://dx.doi.org/10.2113/104.1.47.

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50

Kalbskopf, S. P. "The Zandrivier Deposit, Pietersburg Green Belt, South Africa: an Auriferous Tourmalinite." South African Journal of Geology 106, no. 4 (2003): 361–74. http://dx.doi.org/10.2113/106.4.361.

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