Relevant bibliographies by topics / Hydrogeology – South Africa – Transvaal

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Hydrogeology – South Africa – Transvaal'

Author: Grafiati
Published: 4 June 2021
Last updated: 17 February 2022

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Journal articles on the topic "Hydrogeology – South Africa – Transvaal"

1

Fourie, S. P. "The Transvaal, South Africa, Threatened Plants Programme." Biological Conservation 37, no. 1 (1986): 23–42. http://dx.doi.org/10.1016/0006-3207(86)90032-7.

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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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Eriksson, P. G., and C. W. Clendenin. "A review of the transvaal sequence, South Africa." Journal of African Earth Sciences (and the Middle East) 10, no. 1-2 (1990): 101–16. http://dx.doi.org/10.1016/0899-5362(90)90049-k.

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Bennett, Brett M., and Frederick J. Kruger. "Forestry in Reconstruction South Africa: Imperial Visions, Colonial Realities." Britain and the World 8, no. 2 (2015): 225–45. http://dx.doi.org/10.3366/brw.2015.0192.

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This articles analyses the establishment of state forestry programs in the Orange Free State and Transvaal following the end of the South African War/Second Anglo-Boer War (1899–1902). British imperial administrators, led by Alfred Milner, sought to reconstruct the economy of the Transvaal and Orange Free State by using personnel who had worked previously in India and Egypt rather than by drawing on local experts in the Cape Colony or Natal Colony. Colonial foresters from the Cape Colony used the opportunities provided by reconstruction to export Cape-centric ideas about forest management to t
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Coppins, B. J. "Two New Species of Micarea From South Africa." Lichenologist 31, no. 6 (1999): 559–65. http://dx.doi.org/10.1006/lich.1999.0234.

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AbstractTwo new species of Micarea are described from South Africa: M. almbornii Coppins, on loose sandstone from Stellenbosch (Western Cape) and M. endoviolascens Coppins, on damp soil from Transvaal. A note is given on Lecidea geïna Stizenb.
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Lundquist, J. E. "Fungi Associated withPinusin South Africa Part I. The Transvaal." South African Forestry Journal 138, no. 1 (1986): 1–14. http://dx.doi.org/10.1080/00382167.1986.9630036.

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Rosinski, J., and G. M. Morgan. "Ice-forming nuclei in transvaal, Republic of South Africa." Journal of Aerosol Science 19, no. 5 (1988): 531–38. http://dx.doi.org/10.1016/0021-8502(88)90205-4.

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Meyer, F. M., and L. J. Robb. "The geochemistry of black shales from the Chuniespoort Group, Transvaal Sequence, eastern Transvaal, South Africa." Economic Geology 91, no. 1 (1996): 111–21. http://dx.doi.org/10.2113/gsecongeo.91.1.111.

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Eicker, A., and Derek A. Reid. "Clathrus transvaalensis, a new species from the Transvaal South Africa." Mycological Research 94, no. 3 (1990): 422–23. http://dx.doi.org/10.1016/s0953-7562(09)80372-9.

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Klapwijk, Menno. "Minute Glass Beads from the North-Eastern Transvaal, South Africa." South African Archaeological Bulletin 46, no. 153 (1991): 34. http://dx.doi.org/10.2307/3889011.

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Dissertations / Theses on the topic "Hydrogeology – South Africa – Transvaal"

1

Foster, Michael Benedict John. "Geological control of aquifer properties of the Chuniespoort Group in the Klip River Valley and Natalspruit Basin, Transvaal." Thesis, Rhodes University, 1988. http://hdl.handle.net/10962/d1013338.

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The aquifer of the study area occupies an escarpment and low lying limestone plain, and exhibits a Vaal River type karst. The four dolomitic formations present fall into two distinct aquifer forming types; chert poor units and chert rich units. The chert poor units of the Oaktree and Lyttelton Formations were deposited in a subtidal environment and were probably dolomi tised in a migrating schizohaline environment during basin subsidence and shoreline trangression. The chert rich units of the Monte Christo and Eccles Formations were deposited in the shallow subtidal to supratidal zones and the
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Bowen, Teral Barbara. "The geochemical stratigraphy of the volcanic rocks of the Witwatersrand triad in the Klerksdorp area, Transvaal." Thesis, Rhodes University, 1985. http://hdl.handle.net/10962/d1004932.

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This study lias initiated with the aim of identifying the existence of any geochemical criteria which may be used to distinguish between the various volcanic formations within the Witwatersrand triad. The Witwatersrand triad comprises three sequences: the Dominion Group at the base, the Witwatersrand Supergroup in the middle, and the Ventersdorp Supergroup at the top. It is underlain by Archaean basement rocks, and covered by rocks of the Transvaal sequence. The Dominion Group consists of the sedimentary Rhenosterspruit quartzite Formation at the base, overlain by a bimodal component of the Sy
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Riganti, Angela. "The geology and geochemistry of the north-western portion of the Usushwana Complex, South-Eastern Transvaal." Thesis, Rhodes University, 1992. http://hdl.handle.net/10962/d1005570.

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The 2.9 Ga old Usushwana Complex in the Piet Retief-Amsterdam area (south-eastern Transvaal) represents an exposed segment of a layered intrusion. It has the form of a dyke-like body elongated in a northwesterly direction, and extends to an estimated depth of 3000 -5500 m. Lithologically, the Complex consists of a cumulate succession of mafic rocks capped by granitoids and has intruded along the contact between the basement and the supracrustal sequences of the Kaapvaal Craton. Differentiation of an already contaminated gabbroic magma resulted in an ordered stratigraphic sequence comprising pr
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Crous, Stephanus Philippus. "The geology, geochemistry and stratigraphic correlations of the farm Rietfontein 70 JS on the south -eastern flank of the Dennilton Dome, Transvaal, South Africa." Thesis, Rhodes University, 1996. http://hdl.handle.net/10962/d1005572.

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The study area is located between Loskop Dam and the town of Groblersdal, on the southeastern flank of the Dennilton dome, and is underlain by lithologies of the Pretoria Group, Bushveld Complex mafics and ultramafics and acid lavas that resort under the Rooiberg felsites. Field work comprised of geological mapping, soil-, hard-rock- and stream sediment geochemistry, various geophysical techniques and diamond drilling. The rocktypes that resembles the Rustenburg Layered Suite on the farm Rietfontein 70JS is subdivided into a Mixed Zone, Critical Zone and Main Zone, on grounds of geochemical an
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Carruthers, Jane. "Game protection in the Transvaal 1846 to 1926." Thesis, University of Cape Town, 1988. http://hdl.handle.net/11427/23736.

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Faure, Kevin. "A stable isotope study of the Kaap Valley Tonalite, Barberton Mountain Land, South Africa." Master's thesis, University of Cape Town, 1989. http://hdl.handle.net/11427/15849.

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Bibliography: pages 100-109.<br>The Kaap Valley Tonalite (KVT) was a homogenous hornblende+ biotite tonalite that had been subjected to overail propylitic and potassic alteration. Petrographic studies reveal that carbonate alteration and increased proportions of hydrous minerals occur along the KVT and Barberton greenstone belt contact zone, and along major shear zones within the KVT.
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Brennan, Michael Brendan. "The genesis of ilmenite-rich heavy mineral deposits in the Bothaville/Delmas area, and an economic analysis of titanium, with particular reference to the Dwarsfontein deposit, Delmas district." Thesis, Rhodes University, 1991. http://hdl.handle.net/10962/d1005561.

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A number of ilmenite-rich heavy mineral deposits occur along the northern margin of the intracratonic Karoo basin, and are hosted by the fluvio-deltaic Middle Ecca Group. Coastal reworking of delta front sands within a regressive, microtidal shoreline may be considered as a depositional model for the development of the heavy mineral deposits. An economic analysis of titanium suggests long term positive demand, and sustained high prices for this commodity. An evaluation of the Dwarsfontein ilmenite-rich heavy mineral deposit, using available data, indicates how important it is for deposits of t
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Kriel, Lize. "'N Vergelyking tussen Colin Rae en Christoph Sonntag se weergawes van die Boer-Hananwa-oorlog van 1894." Pretoria : [S.n.], 2005. http://upetd.up.ac.za/thesis/available/etd-10192005-111653.

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Teigler, Bernd. "Mineralogy, petrology and geochemistry of the lower and lower critical zones, Northwestern Bushveld Complex." Thesis, Rhodes University, 1991. http://hdl.handle.net/10962/d1005590.

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This study of the lower part of the Rustenburg Layered Suite in the Western Bushveld Complex is based mainly on drill core samples from three localities, which are approximately 130 km apart. The NG-sequence, situated in the northwestern sector of the complex (Union Section, R.P.M.) extends from the floor of the complex to the base of the upper Critical Zone. The sequence is ca. 1800 m thick and it comprises mainly ultramafic cumulates, namely pyroxenites, olivine pyroxenites, harzburgites and dunites. Norites and anorthos ites are present only in minor proportion. Within the upper half of the
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De, Bever Johannes Nicolaas. "An overview of the early-proterozoic, auriferous Black Reef placer in the Transvaal Basin." Thesis, Rhodes University, 1997. http://hdl.handle.net/10962/d1005596.

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Books on the topic "Hydrogeology – South Africa – Transvaal"

1

Creswicke, Louis. South Africa and the Transvaal war. Publisher's Syndicate, 1993.

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2

Tyler, N. 2200Ma-Old "trace fossils" from the Transvaal Supergroup in the Transvaal. University of the Witwatersrand, 1986.

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3

Mitchell, James H. Tartan on the veld: The Transvaal Scottish, 1950₋1993. Transvaal Scottish Regimental Council, 1994.

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Hendriks, P. G. Waai, vierkleur van Transvaal. Oranjewerkers Promosies, 1991.

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Dorothea Sarah Florence Alexandra Phillips. Some South African recollections. Longmans, Green, 1989.

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Harley, M. The mineralisation at Elandshoogte Gold Mine, Eastern Transvaal, South Africa. University of the Witwatersrand, 1990.

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7

Marshall, T. R. The alluvial-diamond fields of the western Transvaal. Economic Geology Research Unit, University of the Witwatersrand, 1986.

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Marshall, T. R. The alluvial-diamond fields of the western Transvaal. Economic Geology Research Unit, University of the Witwatersrand, 1986.

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9

Funston, Malcolm. Bushveld trees: Lifeblood of the Transvaal lowveld. Fernwood Press, 1993.

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10

Sammy Marks: The uncrowned king of the Transvaal. D. Philip, 1991.

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Book chapters on the topic "Hydrogeology – South Africa – Transvaal"

1

Hofmann, Axel. "Transvaal Supergroup, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_1609.

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Hofmann, Axel. "Transvaal Supergroup, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_1609-3.

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Hofmann, Axel. "Transvaal Supergroup, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-642-27833-4_1609-4.

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Hofmann, Axel. "Transvaal Supergroup, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_1609.

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Bright, Rachel K. "The Transvaal Labour ‘Problem’ and the Chinese Solution." In Chinese Labour in South Africa, 1902–10. Palgrave Macmillan UK, 2013. http://dx.doi.org/10.1057/9781137316578_3.

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Wade, Peter, and Henk Coetzee. "Risk Assessment of Uranium in Selected Gold Mining Areas in South Africa." In Uranium, Mining and Hydrogeology. Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-87746-2_21.

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Coetzee, Henk, Nicolene van Wyk, Peter Wade, Patrich Holmstrom, Håkan Tarras-Wahlberg, and Shane Chaplin. "Migration of uranium in groundwater in three naturally occurring anomalous areas in South Africa." In Uranium, Mining and Hydrogeology. Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-87746-2_82.

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van Wyk, Nicolene, and Henk Coetzee. "The distribution of uranium in groundwater in the Bushmanland and Namaqualand areas, Northern Cape Province, South Africa." In Uranium, Mining and Hydrogeology. Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-87746-2_80.

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Winde, Frank. "Peat deposits as natural uranium filters? - First results from a case study in a dolomitic gold mining area of South Africa." In Uranium, Mining and Hydrogeology. Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-87746-2_62.

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Cole, M. M. "The vegetation over mafic and ultramafic rocks in the Transvaal Lowveld, South Africa." In The Ecology of Areas with Serpentinized Rocks. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-3722-5_13.

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Conference papers on the topic "Hydrogeology – South Africa – Transvaal"

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Dowdy, T., L. C. Kah, W. Altermann, and J. H. Alexander. "EXPLORATION OF POTENTIAL SEISMITES: ARCHEAN NAUGA FORMATION, TRANSVAAL SUPERGROUP, SOUTH AFRICA." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-345256.

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Ünsal, Tuğçe, and Kübra Yazıcı. "The Importance of Gerbera as a Cut Flower and Advances of It in Scientific Research." In International Students Science Congress. Izmir International Guest Student Association, 2021. http://dx.doi.org/10.52460/issc.2021.010.

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Gerbera, a member of the Asteraceae family, has approximately 30 species known in nature. It has spread naturally in South Africa, Africa, Madagascar, and tropical Asia. The first scientific description of gerberas is J.D. Described by Hooker. It is also known as the Transvaal Daisy or Barberton Daisy. It is the second most produced cut flower after carnation as cut flower in our country. We can divide the scientific studies conducted on the gerbera plant into four groups. Studies in general; To produce 1st quality gerbera by providing the growth of plant height, flower diameter and flower ste
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