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

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Published: 4 June 2021

Last updated: 17 February 2022

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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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

Schutz, Christopher John. "Site relationships for Pinus patula in the Eastern Transvaal escarpment area." Thesis, University of Oxford, 1990. http://hdl.handle.net/10413/9535.

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The largest area of commercial timber plantations in southern Africa is situated along the Eastern Transvaal Drakensberg Escarpment north of Nelspruit. The site requirements of tree species in this area are poorly understood. The purpose of this study was to examine site-tree relationships in the region and the implications of such relationships for the science of forestry. Pinus patula Schiede & Deppe in Schlecht. & Cham. was selected for the study as it is the most widely planted species in the region. In Chapter 1 the geology, geomorphology, climate, soils and vegetation of the study area a

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12

Smart, Michael Charles. "Hydrogeology of the Queenstown 1:500 000 map region (Sheet 3126)." Thesis, Rhodes University, 1999. http://hdl.handle.net/10962/d1005583.

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The Groundwater characteristics of a portion of the Eastern Cape are depicted on a General Hydrogeological Map (Queenstown 3126) at 1 :500 000 scale. The purpose of the map and accompanying text is to provide a synoptic overview of the hydrogeology of the area. The "fractured and intergranular" aquifer type predominates in the more humid eastern part of the study area where the lithologies are more highly weathered whereas the fractured type predominates in the drier west. For the bulk of the area borehole yields are in the 0.5 - 2.0 ℓ/sec range. Higher yields (in the 2.0 - 5.0 ℓ/sec range) ar

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13

Adonis, Shaheeda. "The hydrochemical characteristics of groundwater in the Incomati Estuary." Thesis, University of the Western Cape, 2007. http://etd.uwc.ac.za/index.php?module=etd&action=viewtitle&id=gen8Srv25Nme4_6324_1220530108.

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<p>The focus of this work was to monitor and evaluate the hydrochemical characteristics of the groundwater in the Incomati Estuary for a period of one year. The aims of this work were to evaluate the groundwater chemistry data for any spatial and temporal variations and to evaluate the suitability of the groundwater for drinking and irrigation purposes.</p>

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14

Scoon, Roger N. "Discordant bodies of postcumulis, ultramafic rock in the upper critical zone of the Bushveld complex : iron-rich ultramafic pegmatite bodies at Amandelbult and the Driekop platiniferous ultramafic pipe." Thesis, Rhodes University, 1986. http://hdl.handle.net/10962/d1004912.

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From the abstract: In the layered sequence of the Bushveld Complex a number of distinct, but possibly genetically related groups of transgressive, postcumulus, ultramafic and mafic rock are recognised. The main part of this thesis investigates a suite of postcumulus rocks for which the name iron-rich ultramafic pegmatite is proposed. The majority of iron-rich ultramafic pegmatite bodies examined are from the upper critical zone of the layered sequence at Rustenburg Platinum Mines Amandelbult Section, in the northern sector of the western Bushveld Complex. Field relationships imply that the iro

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15

Bush, Richard Alan. "A hydrogeological assessment of the Uitenhage-Kuils River area, Cape Province, South Africa." Thesis, Rhodes University, 1987. http://hdl.handle.net/10962/d1001901.

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16

Venables, Anthony John. "A hydrogeological assessment of the Uitenhage-Coega artesian system." Thesis, Rhodes University, 1985. http://hdl.handle.net/10962/d1003815.

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The Uitenhage artesian aquifer north-west of Port Elizabeth in South Africa, is one of the few artesian groundwater systems in Southern Africa. The Uitenhage - Coega, and Kruis River areas, are the most important portions of the Uitenhage Artesian System in terms of water abstraction and water use. This study concentrates on the Uitenhage - Coega area and in particular, on the Coega Ridge where the Table Mountain Sandstone (TNS) aquifer occurs at relatively shallow depths. The investigation is aimed at assessing the geological, hydrogeological and hydrochemical characteristics of the HIS and a

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17

Field, Matthew. "The petrology and geochemistry of the upper critical zone of the Bushveld complex at the Amandelbult section of Rustenberg Platinum Mines Limited, Northwestern Transvaal, South Africa." Thesis, Rhodes University, 1987. http://hdl.handle.net/10962/d1007499.

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A study of petrological and geochemical variations through the upper Critical Zone of the Bushveld Complex at Amandelbult section of R.P,M. was undertaken. The sequence at this locality may be divided into seven "units" two of which appear to be complete, possessing the sequence harzburgite-pyroxenite-norite-anorthosite. The other five Units lack basal, intermediate or upper members. Considerable lateral variations are apparent in this sequence, but these are restricted to the Lower Pseudo Reef-Merensky Reef interval, tne same portion of the succession which is affected by pothole structures.

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18

Maier, Wolfgang Derek. "Geochemical and petrological trends in the UG2-Merensky unit interval of the upper critical zone in the Western Bushveld Complex." Thesis, Rhodes University, 1992. http://hdl.handle.net/10962/d1005563.

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One of the most remarkable features of the layered sequence of the Bushveld Complex is its lateral consistency in lithology. This work has established a geochemical and lithological correlation along 170 km of strike of the interval between the UG2 chromitite and the Merensky Reef within the Upper Critical zone of the western limb of the Bushveld Complex. The correlation is based on geochemical investigations of 10 borehole intersections and lithological comparisons of more than 20 borehole intersections around the western lobe of the complex. The basic data presented include 123 whole-rock an

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19

Bartman, R. D. (Reynard Dirk). "Geology of the Palaeoproterozoic Daspoort Formation (Pretoria Group, Transvaal Supergroup), South Africa." Diss., University of Pretoria, 2013. http://hdl.handle.net/2263/42447.

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This thesis examines the geology of the Daspoort Formation (Pretoria Group, Transvaal Supergroup) of South Africa, with the accent on describing and interpreting its sedimentology. The Palaeoproterozoic Daspoort Formation (c. 2.1‐2.2 Ga) forms part of the Pretoria Group on the Kaapvaal craton. This sandstone‐ and quartzite‐dominated lithological formation covers an elliptical geographical area stretching from the Botswana border in the west to the Drakensberg escarpment in the east, with its northern limit in the Mokopane (Potgietersrus) area and Pretoria in the south; altered outliers ar

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20

Polteau, Stéphane. "Stratigraphy and geochemistry of the Makganyene formation, Transvaal supergroup, Northern Cape, South Africa." Thesis, Rhodes University, 2001. http://hdl.handle.net/10962/d1005616.

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The Makganyene Formation forms the base of the Postmasburg Group in the Transvaal Supergroup of the Northern Cape Province. The Makganyene Formation has diamictite as the main rock type, but siltstone, sandstone, shale, and iron-formations are also present. A glacial origin has been proposed in the past due to the presence of dropstones, faceted and striated pebbles. Typically, the Makganyene Formation contains banded iron-formations interbedded with clastic rocks (shale, siltstone, sandstone and diamictites) at the contact with the underlying iron-formations. This transitional zone is general

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21

Makubalo, Sisanda Sesethu. "Hydrogeochemistry of the groundwater in the Namaqualand region, South Africa : implications for surficial uranium mineralization." Diss., University of Pretoria, 2020. http://hdl.handle.net/2263/73255.

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Since the discovery of the Yeelirrie deposit in Australia in 1972, exploration for surficial uranium deposits has been supported through hydrogeochemical studies of groundwater and the calculation of the carnotite solubility index (CSI). This study aims to evaluate groundwater quality and delineate potential areas where surficial uranium mineralization (i.e. carnotite) may take place in the Namaqualand region. Surficial uranium deposits are unconsolidated soils or sediments, usually of Tertiary to Recent age. The most common surficial uranium mineral is carnotite. The study area in Namaqualand

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22

Martinelli, Giorgio Luigi. "The hydrogeology of a Karoo basalt/sandstone contact aquifer moretele II district Republic of Bophuthatswana southern Africa." Thesis, Rhodes University, 1988. http://hdl.handle.net/10962/d1001902.

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As part of a development programme in the Moretele II District, the Government of the Republic of Bophuthatswana, commissioned in 1983 the building of a dry system coal-fired power station. The lack of local surface water to cool the power station resulted in a decision to investigate the potential of the ground water resources. The resources will be required to supply an anticipated 30 year water demand. Because of the high capital investment and the importance of establishing an accurate assessement of the ground water potential there was a need for a comprehensive and detailed hydrogeologic

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23

Rafuza, Sipesihle. "Carbonate petrography and geochemistry of BIF of the Transvaal supergroup : evaluating the potential of iron carbonates as proxies for palaeoproterozoic ocean chemistry." Thesis, Rhodes University, 2015. http://hdl.handle.net/10962/d1018611.

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The subject of BIF genesis, particularly their environmental conditions and ocean chemistry at the time of deposition and their evolution through time, has been a subject of much contentiousness, generating a wealth of proposed genetic models and constant refinements thereof over the years. The prevailing paradigm within the various schools of thought, is the widespread and generally agreed upon depositional and diagenetic model(s) which advocate for BIF deposition under anoxic marine conditions. According to the prevailing models, the primary depositional environment would have involved a sea

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24

Manson, Andrew. "The Hurutshe in the Marico district of the Transvaal, 1848-1914." Doctoral thesis, University of Cape Town, 1990. http://hdl.handle.net/11427/22400.

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Bibliography: pages 284-297.<br>The Hurutshe are a Tswana-speaking chiefdom who lived in the vicinity of the Marico (Madikwe) river on the South African Highveld and emerged as an identifiable community with a distinct political structure about 350 years ago. They enjoyed periods of political and economic dominance in the mid-to late seventeenth century and again in the late eighteenth century. Following the economic and political disruptions attendant upon European commercial activities and the growth of more centralised and powerful African states in South Africa, they were propelled from th

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25

Van, Jaarsveld Floris Albertus 1922-1995. "Die Ndzundza-Ndebele en die blankes in Transvaal, 1845-1883." Thesis, Rhodes University, 1986. http://hdl.handle.net/10962/d1004379.

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In 1969 het Leonard Thompson met reg beweer dat Suid-Afrikaanse historici hulle tot op hede hoofsaaklik besig gehou het met die doen en late van 'n Blanke gemeenskap wat die land sedert 1652 oorheers het. Die Swartman was die "forgotten factor" in die geskiedenis van Suider-Afrika. Waar die Swartman die onderwerp van wetenskaplike studie was, is dit aan argeoloë, linguiste, etnoloë en fisiese en sosiale antropoloë oorgelaat. Tereg het Thompson kort hierna opgemerk: "We need to know much more about the complex process by which African chiefdoms became incorporated in white controlled politics i

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26

Latorre-Muzzio, Gina. "The influence of geological, genetic and economic factors on the ore reserve estimation of Kwaggashoek east iron ore deposit." Thesis, Rhodes University, 1993. http://hdl.handle.net/10962/d1005584.

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Tectonics plays an important role in the genesis and subsequent mlnlng development of the Kwaggashoek East ore body. Lithological key units control the effectiveness of the ore forming processes, affecting the in situ ore reserve, The Kwaggashoek East deposit is the product of primary and secondary processes. A genetic model focussed on the source, migration and deposition of iron suggests a possible original source of iron as the product of very dilute hydrothermal input into deep ocean waters, with subsequent migration through structural conduits. Supergene processes account for the upgradin

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27

Cobbing, Jude Edmund. "The Grootfontein aquifer at Mahikeng, South Africa as hydro-social system." Thesis, Nelson Mandela Metropolitan University, 2017. http://hdl.handle.net/10948/21351.

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The Grootfontein aquifer is located about 20 km south east of Mahikeng, North West Province, South Africa, and currently supplies about 20% of Mahikeng’s water. Formed in weathered Malmani Subgroup dolomites, the aquifer contains good quality groundwater that could potentially supply more of Mahikeng’s water, as well as provide a strategic reserve of water for use during droughts. Over-abstraction of groundwater from the aquifer, mainly by irrigating farmers but also by the boreholes supplying Mahikeng, has caused the natural groundwater level to drop at a rate of about 0.4 m per year since th

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28

Kruger, Petrus Johannes. "'n Verbruikersprofiel van voetslaners in Transvaal." Thesis, 2015. http://hdl.handle.net/10210/14529.

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29

Van, Schalkwyk John Francois. "Metamorphism of ultramafic rocks during the Limpopo orogeny : evidence for the timing and significance of CO2-rich fluids." Thesis, 2014. http://hdl.handle.net/10210/11669.

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30

Davies, S. J. "The importance of browse in late dry season and early wet season diets of cattle and goats in a communal area of the Eastern Transvaal lowveld." Thesis, 1993. http://hdl.handle.net/10539/21651.

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A dissertation submitted to the Faculty of Science, University of the Witwatersrand, Johannesburg, in fulfilment of requirements for the degree of Master of Science. Johannesburg, 1991.<br>The contribution of browse and grass to the diets of cattle and goats was assessed in relation to the total biomass of woody foliage and grass available in the study area. Livestock made less use of browse during the dry season than was shown by studies conducted in the Sahel and Nylsvley, northern Transvaal. Goats fed more selectively, utilised newly flushed foliage more and fed upon a greater variety

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31

Grobler, Johannes Theodorus Wessels. "Die bestuurstaak van die provinsiale administrasieklerk in die skool." Thesis, 2014. http://hdl.handle.net/10210/9808.

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M.Ed. (Education Management)<br>The subject of this investigation is the management function of the provincial administration clerk in the school. The investigation is limited to schools within the ambit of the Transvaal Education Department and has been aimed, primarily, at determining the responsibilities and position of the administration clerk in the effective functioning of the school. As the administration office forms the nerve-centre of the school's activities and due to its staff consistence of administration clerks, a clear indication of their duties and responsibilities is an essent

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32

Pearson, Joel David. "Witchcraft management in the early twentieth century Transvaal." Thesis, 2016. http://hdl.handle.net/10539/19614.

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Towards the end of the nineteenth century, colonial governments across Africa, including South Africa, promulgated laws which aimed to prohibit the accusation of witchcraft, methods for the detection of witches and witch trials. However, while administrators saw merely superstition in witchcraft beliefs, “repugnant to the standards of civilisation”, many Africans saw an integral element of the social and spiritual order. The policing of witchcraft beliefs became a thorn in the side of colonial rule. This article brings to light some of the deeper historical complexities in policing wit

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33

Collett, David Phillip. "The archaeology of the stone walled settlements in the Eastern Transvaal, South Africa." Thesis, 2015. http://hdl.handle.net/10539/16525.

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34

Verrezen, Lucien. "Sedimentology of the Vaal Reef paleoplacer in the western portion of Vaal Reefs Mine." Thesis, 2014. http://hdl.handle.net/10210/10180.

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35

King, Pieter Hartogh. "'n Ondersoek van die slakgeassosieerde trematode parasiete in die Mooirivier, Transvaal." Thesis, 2014. http://hdl.handle.net/10210/12901.

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Pienaar, Alphonso Theofilus. "'n Liggingsanalise van blanke openbare skole in Transvaal." Thesis, 2014. http://hdl.handle.net/10210/12914.

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Olivier, Jana. "Hail in the Transvaal : some geographical and climatological aspects." Thesis, 2014. http://hdl.handle.net/10210/11151.

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M.Sc. (Geography)<br>Hailstorms are well-known phenomena in the summer rainfall region of southern Africa where they cause extensive damage - especially in the agricultural sector. This thesis examines the geography and climatology of hail in the Transvaal. It deals with three main issues, namely a) the spatial and temporal characteristics of hail days (HDs); b) rainfall and atmospheric conditions prevailing during hail events; and c) the geography of hail damage as it pertains to maize. In the Transvaal, hail day frequency (HDF) increases with altitude and latitude in a non-linear (exponentia

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38

Crisp, Nicholas Gilmour. "Regionalisation Of Hospital Infrastructure In The Eastern Transvaal Area." Thesis, 1991. https://hdl.handle.net/10539/24294.

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A Dissertation Submitted to the Faculty of Medicine University of the Witwatersrand, Johannesburg for the Degree of Master of Medicine (Community Health)<br>The extremely complex fragmentation of health services in the greater South Africa has lead to confusion, duplication and uncoordinated planning. This study assesses the hospital component of the health services in one discrete geographical area where service responsibilities are particularly complex. Each of the hospitals identified within the study area was visited and, after a short conducted tour, detailed information was obtain

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39

Meijer, Engelbert Johan. "Netwerkbeplanning van die riviervloeimeetstasienetwerk in die Oos-Transvaal." Diss., 1994. http://hdl.handle.net/10500/17430.

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Text in Afrikaans<br>Water is in 'n relatief droe land soos Suid-Afrika van uiterste belang. Daar is 'n groot behoefte aan inligting oor die potensieel verbruikbare waterbronne. Hierin word voorsien deur 'n netwerk van riviervloeimeetstasies. Met veranderende ekonomiese toestande word die effektiwiteit van die netwerk van al hoe groter belang. Dit is hier waar netwerkbeplanning 'n aktiewe rol begin speel. As gevolg van die groot variasie in die aard van die opvanggebiede in Suid-Afrika, en die feit dat daar 'n bestaande netwerk is, is dit nodig dat netwerkbeplanning stapsgewys benader word.

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Swart, Quentin Dax. "Carbonate rocks of the Paleoproterozoic Pretoria and Postmasburg Groups, Transvaal Supergroup." Thesis, 2012. http://hdl.handle.net/10210/6946.

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M.Sc.<br>Certain carbonate bearing formations in the Paleoproterozoic Pretoria Group and its Griqualand West equivalent exhibit remarkable geochemical and stable isotopic signatures. The 8'3Ccarb isotopic signatures from the Duitschland and Silverton Formations exhibit large positive excursions, which seemingly coincide with a significant increase in atmospheric oxygen between 2.4 and 2.0 Ga. The Duitschland Formation with its distinctive basal unconformity is composed primarily of limestone and dolomite units, interbedded with two compositionally different shale units and quartzite. Toward th

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41

Raath, Schalk Petrus. "Die houding van onderwysers in Transvaal teenoor die omgewing en omgewingsopvoeding." Thesis, 2014. http://hdl.handle.net/10210/11485.

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Von, Bredow Sigrid. "Quantifying evaporation on the surface of slimes dams in the southeastern part of the North West Province." Thesis, 2014. http://hdl.handle.net/10210/10240.

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M.A. (Geography and Environmental Management)<br>Water can be regarded as a scarce commodity in South Africa and one cannot rely solely on the discovery of new water resources to meet the ever increasing demands. Water is arguably the most precious resource in South Africa and its proper management in all spheres of activity is imperative ( Middleton and Stern,1987 ). This is no different in the mining industry where a primary consumptive use of water is in the tailings dams and associated return water. Restricted implementation of Government water plans and a series of droughts has forced use

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Stols, Helene Elizabeth. "Die behandelingsbelewenis van psigiatriese pasiënte in 'n privaat kliniek." Thesis, 2014. http://hdl.handle.net/10210/11338.

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M.Cur. (Psychiatric Nursing)<br>With modern psychiatric treatment, patients usually come into contact with as many as six different team members. These team members have their own particular treatment plans for patients. This has prompted the question: "How do patients experience their treatment by the interprofessional health team?" The aims of this study are as follows: • To explore psychiatric patients' experiences of their treatment by the interprofessional health team in a particular private psychiatric clinic. • To set basic guidelines which will promote the optimisation of treatment of

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"Die geologie van die Krokodilrivierfragment, Transvaal." Thesis, 2014. http://hdl.handle.net/10210/13109.

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Coetzee, Eugene Marco. "'n Elektroforetiese ondersoek van verskeie reenboogforelbevolkings in Transvaal." Thesis, 2014. http://hdl.handle.net/10210/9331.

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Leurs, Gondanette. "Implikasies van enkele modelle van skoolhoofskap in Transvaal." Thesis, 2014. http://hdl.handle.net/10210/11568.

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M. Ed. (Educational Management)<br>School principals are primarily.concerned with education and the effective management of the school entrusted to them. Every principal is given a task to do when he is appointed to or at a school. How successfully he accomplishes his task, and the support that he receives, is highlighted in this study. The principal is a leader who has to perform a complex number of tasks. He works with both adults and children and as a result the method and style of leadership and management is of great importance. The recognition of the principal as leader in the field of i

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"Alteration and gold mineralisation in the Roodepoort Goldfield, Pietersburg Granite-Greenstone Terrane." Thesis, 2014. http://hdl.handle.net/10210/12896.

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Crous, Jacobus Jooste. "Faktore wat huweliksmaatseleksie beinvloed : 'n vergelyking tussen eerste en tweede huwelike." Thesis, 2014. http://hdl.handle.net/10210/12287.

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M.A. (Clinical Psychology)<br>The overall aim of this study is to establish whether theories on mate selection apply more to first than to subsequent marriages. In the case of subsequent marriages synthesis of the hypotheses is made more difficult by the lack of available research results on the role of internal factors involved in mate selection. It is reasonable to assume differences between first and subsequent marriages in terms of factors that play a significant role in mate selection. Several theories on mate selection have evolved since the formulation of psycho-analytical theory. Initi

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Moore, J. M., H. Tsikos, and S. Polteau. "Deconstructing the Transvaal Supergroup, South Africa: implications for Palaeoproterozoic palaeoclimate models." 2001. http://eprints.ru.ac.za/446/1/Deconstructing_the_Transvaal_Supergroup%2C_South_Africa_-_implications_for_Palaeoproterozoic.pdf.

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Current correlations between the Pretoria and Postmasburg Groups of the Transvaal Supergroup are shown to be invalid. The Postmasburg Group is also demonstrated to be broadly conformable with the underlying Ghaap Group and therefore considerably older (~2.4 Ga) than previously supposed. The new stratigraphy documents an extensive (100 Ma) and continuous cold-climate episode with a glacial maximum at the Makganyene Formation diamictite. Iron formations of the underlying Asbesheuwels and Koegas Subgroups and overlying Hotazel Formation have similar origins, related, respectively, to the onset an

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Sibeko, Catherine Rejoice. "Psychiatric nurses' communication with psychiatric patients." Thesis, 2014. http://hdl.handle.net/10210/10416.

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M.Cur. (Psychiatric Nursing)<br>The psychiatric nurse, as a member of the multiprofessional mental health team, utilises a goal directed approach to assist the psychiatric patient to mobilise resources to promote, restore and maintain his mental health as an integral part of his quest for wholeness. This goal directed approach is the nursing process which comprises assessment, planning, implementing and evaluation. All four steps of the nursing process and the nurse's interaction wi th the patient are dependent upon therapeutic communication between the nurse and the patient to elicit the nece

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