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1

Walters, P. S. "English in Africa 2000 : towards a new millennium : inaugural lecture delivered at Rhodes University." Rhodes University, Grahamstown, 1988. http://hdl.handle.net/10962/d1020747.

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2

Ashton, Eugéne Mark. "The historiography of the formation of the Union of South Africa." Pretoria : [S.n.], 2010. http://upetd.up.ac.za/thesis/available/etd-03102010-183227.

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3

Lester, Alan John. "Conceptualizing social formation : producing a textbook on South Africa." Thesis, University College London (University of London), 1995. http://discovery.ucl.ac.uk/10021574/.

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The ultimate goal of the thesis is the construction of a text, appropriate for student use, on South Africa's social and spatial formation. The first part of the thesis is the most lengthy. It is a sophisticated account of South Africa's historical geography since 1652. This is written in an academic style, not for students, but for a learned readership, and contains some original insights. In itself, it represents an innovative contribution to the literature on South Africa's social development. The second part is a review of existing texts on South Africa's history and geography, written pur
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4

Moodley, Jason Anthony. "Petrogenesis of the Bysteek and Koenap Formation Migmatites, Central Namaqualand." Thesis, Rhodes University, 2013. http://hdl.handle.net/10962/d1001574.

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The Mesoproterozoic rocks of the Bysteek and Koenap Formations of the Arribees Group are exposed within a NW-SE striking antiformal structure comprised of mafic granulites and metapelitic diatexites, and a number of marble and calc-silicate rock layers. The mafic granulites of the Bysteek Formation show a typological variety of anatectic features, including nebulitic, stromatitic mesosomes, melanosomes, quartz syenitic leucocratic vein networks and syenitic pools. Melanosomes consist of hedenbergitic to diopside-rich clinopyroxene (XMg: 0.40), anorthitic plagioclase (An90), with some quartz, m
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5

Busakwe, Nolukholo Sinovuyo. "Stratigraphy and sedimentology of the Msikaba formation in KwaZulu Natal South Coast, South Africa." Thesis, University of Fort Hare, 2015. http://hdl.handle.net/10353/2501.

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The Msikaba Formation is a Late Devonian fluvial and marine succession which outcrops from Hibberdene to Port Edward along the south coast of KwaZulu-Natal Province, South Africa. The Formation is composed of brownish conglomerate at the bottom and white-greyish quartz arenite sequence in the middle and mixed quartz-arenite with feldspathic sandstone in the upper sequence. Previous studies put more emphasis on the correlation of Msikaba Formation with the Natal Group and Cape Supergroup, whereas this study revised the stratigraphy, and also put new insight on the petrography, sedimentary facie
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6

Duncan, Kenneth Foster. "A comparative study of L1 and EFL reading abilities amongst junior primary students using different reading schemes in black schools." Thesis, Rhodes University, 1995. http://hdl.handle.net/10962/d1002628.

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This thesis examines the development of children's reading skills, in both the mother tongue and English as a foreign language, during their first four years of school. It is an attempt to enter the reading world of very young learners in underdeveloped, mainly rural communities in search of practical insights into the teaching of reading in the junior primary classroom. The research focuses specifically on two approaches to reading instruction. The first is the approach traditionally used in black South African schools, characterised by teacher-centredness and rote-recall techniques. The seco
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7

Howarth, David R. "Black consciousness in South Africa : resistance and identity formation under apartheid." Thesis, University of Essex, 1995. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.520285.

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8

Tsikos, Harilaos. "The mineralogy and geochemistry of the Voëlwater banded iron-formation, Northern Cape Province." Thesis, Rhodes University, 1995. http://hdl.handle.net/10962/d1005589.

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Banded iron-formations (BIFs) are chemically precipitated sedimentary rocks in which Fe-rich bands or laminae alternate with Fe-poor ones. They formed within a specific time-span of the geological record. Their occurrence is restricted between 2.3 and 1.9 Ga, and characterises virtually all the major Precambrian-aged sedimentary basins of the world. The Precambrian Transvaal Basin in Griqualand West, South Africa, is noted for its well-developed BIF units. The Kuruman and Griquatown BIFs comprising the Asbesheuwels Subgroup (up to 1000m thick) are the best known and thickest of these. As far a
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9

Francis, Michele Louise. "Soil Formation on the Namaqualand Coastal Plain." Link to the Internet, 2008. http://hdl.handle.net/10019/806.

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10

Becker, Carl. "South African art institutions : their formation and strategy with particular reference to the question of legitimacy." Thesis, Rhodes University, 1993. http://hdl.handle.net/10962/d1007622.

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I have examined the relationship between the art institution and its social base, and the way in which legitimacy is sought and maintained under changing social circumstances. The social pattern of 'avante garde artist' vs. 'philistine public' has tended to be the context within which 20th century art has developed. The consequent disjuncture between the public art institution and its social base was subsequently accepted as the natural condition of Fine Art production. During the 1980's, two significant factors were to influence this 'natural' condition: i) The demise of 'modernism' internati
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11

Davis, Catharina Helena. "The formation of a union for salespersonnel in South Africa / C.H. Davis." Thesis, North-West University, 2009. http://hdl.handle.net/10394/4779.

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A representative body such as a trade union, workplace forum or an organisation that specifically handles disputes that may arise from unilateral decisions that are taken by employers in the billboard industry that affect the salespeople could, go a long way to improve the working conditions of these people. There is, however, no such an organisation that exists currently to protect workers in this industry. This poses the question whether salespeople in the industry would want to see the formation of such a union and whether or not they would join such a union. Another question that needs to
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12

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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13

Terracin, Matthew Theodore. "Petrography, geochemistry and origin of atypical sedimentary-igneous contact relationships at the base of the Hotazel Formation around Middelplaats, Northern Cape Province, RSA." Thesis, Rhodes University, 2014. http://hdl.handle.net/10962/d1012985.

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In the Middelplaats mine area of the Kalahari manganese field, two drill holes (MP53 and MP54) intersected anomalously high-grade manganese ore sitting stratigraphically just above an igneous body (likely a dike or sill). Manganese ore located within approximate 5 meters of the contact with the underlying igneous rocks has been substantially metasomatically upgraded from 25 percent manganese, to over 40 percent whilst the dominant manganese species within the ore has been altered to hausmannite. This report demonstrates the metasomatic alteration is related to devolatilization (removal and/or
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14

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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Frost, Susan. "Early Cretaceous alluvial palaeosols (Kirkwood formation, Algoa Basin, South Africa) and their palaeoenvironmental and palaeoclimatological significance." Thesis, Rhodes University, 1996. http://hdl.handle.net/10962/d1005551.

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The Kirkwood Formation in the Bushman's River area of the Algoa Basin is characterised by a number of fining-upward cycles. These have been interpreted as indicating deposition in a dynamic aggrading meandering river system with the channel deposits (conglomerates grading upwards into sandstones) fining upward into the overbank deposits (mudrocks). Channel, channel-margin and overbank deposits were recognised. The three mudrock sequences logged comprise compound pedofacies sequences of multistorey, simple and cumulative palaeosols. Distinctive palaeopedological features, such as root traces an
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Browning, Claire. "A preliminary investigation and photographic atlas of nodules found in the Bokkelveld group (Gydo formation), Steytlerville district, South Africa." Thesis, Nelson Mandela Metropolitan University, 2009. http://hdl.handle.net/10948/927.

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Nodules within the lower Bokkeveld shales often contain well-preserved invertebrate fossil material. The aim of this study was to describe some characteristics seen at various scales (macro-, micro- and ultra -) within nodules that might contribute to an understanding of aspects of nodule formation and the reasons for the excellent preservation of the fossil material within these nodules. Detailed, high quality macro-photographs were taken of sliced and whole nodule surfaces and a catalogue was produced to tentatively identify fossils present and illustrate the variations seen within nodules.
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17

Bank, Leslie John. "Traders and taximen in Qwaqwa : a study of class formation in a South African homeland." Master's thesis, University of Cape Town, 1988. http://hdl.handle.net/11427/22544.

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Bibliography: pages 229-245.<br>This thesis is centred around the experiences of traders and taximen in Qwaqwa, the smallest of South Africa's 'homelands'. It aims to investigate the extent to which small-scale entrepreneurs of various kinds can be seen to be participating in processes of class formation within the homeland. The focus adopted directs attention away from the issue of poverty which has dominated rural research over the past decade. The thesis also seeks to contribute to existing studies of class formation in the homelands, which address the problem from the perspective of 'state
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18

Meyer, Ferdinand. "Model closure and price formation under switching grain market regimes in South Africa." Thesis, Pretoria : [s.n.], 2006. http://upetd.up.ac.za/thesis/available/etd-12082006-105715.

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Thesis (D.Phil.(Agricultural Economics, Extension, and Rural Development))--University of Pretoria, 2006.<br>Includes summary. Includes bibliographical references. Available on the Internet via the World Wide Web.
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19

Schröder, Marian. "A case study : identity formation in a cross-racial adoptee in South Africa." University of the Western Cape, 2015. http://hdl.handle.net/11394/4697.

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Magister Psychologiae - MPsych<br>Due to the history of Apartheid in South Africa, cross-racial adoption is a fairly recent practice which was only legalised when the law was amended in 1991 so that prospective parents were allowed to adopt a child from a different race to them. As the consequences of the past linger, the most common form of cross-racial adoption is White parents adopting Black children. Studies on cross-racial adoption have been extensively conducted internationally, but research in South Africa is sparse. In this research study an explorative case study of a cross-racially a
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20

Susela, Zamampondo. "Stratigraphy and sedimentology of the Mzamba formation in the Eastern Cape, South Africa." Thesis, University of Fort Hare, 2014. http://hdl.handle.net/10353/d1019807.

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This research project is aimed at providing new information to the stratigraphy, sedimentology, palaeontology and diagenesis of the Mzamba Formation. The study area is located at the south of Port Edward, Eastern Cape. The methodologies employed in this study include field geological investigation and sampling, stratigraphic measurement and logging, thin-section microscope study, powder samples of XRD analysis, and SEM-EDX analysis of rock textures and mineral compositions. The stratigraphy of the Mzamba Formation can be divided into three newly established members, i.e. the Lower Conglomerate
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21

Bradlow, Muhammad 'Adil. "Imperialism, state formation and the establishment of a Muslim community at the Cape of Good Hope, 1770-1840 : a study in urban resistance." Master's thesis, University of Cape Town, 1988. http://hdl.handle.net/11427/17069.

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Includes bibliography.<br>One of the most significant and yet least studied developments of late eighteenth and early nineteenth century Cape Town is the emergence and growth of a muslim community. So dramatic was this process, that by the end of the period of slavery, well over two thirds of the town's non-European population were considered to be members of this community. Yet this process has largely been regarded, in such studies as do exist, as one of only marginal significance to the unfolding pattern of struggles that characterise this turbulent and brutal period of Cape Town's history.
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22

Oghenekome, Monica Enifome. "Sedimentary environments and provenance of the Balfour Formation (Beaufort Group) in the area between Bedford and Adelaide, Eastern Cape Province, South Africa." Thesis, University of Fort Hare, 2012. http://hdl.handle.net/10353/d1004354.

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The research examines the sedimentary environments and provenance of the Balfour Formation of the Beaufort Group (Karoo Supergroup) in the Eastern Cape Province, South Africa. This Formation occurs in the southeastern part of the Karoo Basin. It consists of sedimentary rocks, which are an alternating siltstone, shale and mudstone succession with subordinate interbedded sandstone and subsequently intruded by Karoo dolerite in the form of sills and dykes. ithostratigraphically, the Balfour Formation is subdivided into five units namely, from the base to the top, the Oudeberg, Daggaboersnek, Barb
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23

Warke, Matthew. "Stratigraphic and geochemical framework of the Palaeoproterozoic rise in atmospheric oxygen, Transvaal Supergroup (South Africa)." Thesis, University of Manchester, 2017. https://www.research.manchester.ac.uk/portal/en/theses/stratigraphic-and-geochemical-framework-of-the-palaeoproterozoic-rise-in-atmospheric-oxygen-transvaal-supergroup-south-africa(b0aa0021-946c-4f01-bf4e-297611aa2ec1).html.

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The Transvaal Supergroup (South Africa) records evidence of trace oxygen production in late Neoarchaean strata, approximately 200 million years before the 'Great Oxidation Event' (GOE) which is recorded within the Palaeoproterozoic Duitschland Formation (Transvaal Supergroup) between ~2.42 and 2.32 Ga. It is hypothesized that there was a secular rise in oxygen concentrations between the late Neoarchaean and the GOE which may be recorded within the 'mid-Transvaal' Supergroup (Tongwane Formation, Duitschland Formation, Koegas Subgroup). This project has integrated field sedimentology, petrograph
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24

Grecula, Martin. "Stratigraphy and architecture of tectonically controlled turbidite systems : Laingsburg formation, Karoo Basin, South Africa." Thesis, University of Liverpool, 2000. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.343590.

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25

Bright, Rachel. "Chinese indentured labour in South Africa and the formation of a nation 1902-10." Thesis, King's College London (University of London), 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.720570.

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26

Slabber, Nina. "The geology and geochemistry of the Bridgetown Formation of the Malmesbury Group, Western Cape Province." Thesis, Stellenbosch : Stellenbosch University, 1995. http://hdl.handle.net/10019.1/54889.

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Thesis (MSc) -- Stellenbosch University , 1995.<br>ENGLISH ABSTRACT: A number of small greenstone bodies of the Bridgetown Formation are exposed as elongated lenses and dykes within metasediments of the Malmesbury Group in the Western Cape Province, South Africa. The Malmesbury Group is part of the Neoproterozoic to Cambrian (Namibian) Saldania Subprovince which is the southern continuation of a Pan-African mobile belt system. A detailed geological and geochemical study was conducted on the largest outcrop of the Bridgetown Formation, situated 20km east of the town Moorreesburg. The Br
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Mosavel, Haajierah. "Hydrocarbon potential of the Prince Albert Formation, Ecca Group in the main Karoo Basin, South Africa." University of the Western Cape, 2020. http://hdl.handle.net/11394/8342.

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Philosophiae Doctor - PhD<br>This thesis focusses on the hydrocarbon potential of the Prince Albert Formation in terms of its shale gas potential. Unconventional gas production from hydrocarbon-rich shale formations, known as “shale gas”, is one of the most rapidly expanding trends in onshore oil and gas exploration and exploitation today. In South Africa, the southern portion of the main Karoo Basin is potentially favourable for shale gas accumulation and may become a game changer in the energy production regime of the country. The Prince Albert Formation was selected for research, since prev
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Hammond, Napoleon Quaye. "The geochemistry of ore fluids and control of gold mineralization in banded iron-formation at the Kalahari Goldridge deposit, Kraaipan greenstone belt, South Africa." Thesis, Rhodes University, 2003. http://hdl.handle.net/10962/d1008370.

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The Kalahari Goldridge mine is located within the Archaean Kraaipan Greenstone Belt about 60 km SW of Mafikeng in the Northwestern Province, South Africa. Several gold deposits are located within approximately north - south-striking banded iron-formation (BIF). Current opencast mining operations are focused on the largest of these (D Zone). The orebody is stratabound and hosted primarily in the BIF, which consists of alternating chert and magnetite-chloritestilpnomelane-sulphide-carbonate bands ranging from mm to cm scale. The ore body varies in thickness from 15 to 45 m along a strike length
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Hughes, Tim 1959. "Political liberalism in South Africa in the 1980s and the formation of the Democratic Party." Master's thesis, University of Cape Town, 1994. http://hdl.handle.net/11427/3781.

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30

Potgieter, Katherine. "Pup provisioning and artificial pack formation in African wild dog Lycaon pictus in South Africa." Master's thesis, University of Cape Town, 2009. http://hdl.handle.net/11427/6161.

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Includes abstract.<br>Includes bibliographical references.<br>Wild dog Lacaon pictus are obligate cooperative breeders with nulliparous helpers contributing to the rearing of a dominant pair's young through pup-provisioning and defence agianst predators. Despite the importance of allo-parental care to the survival of pups and the persistance of packs, few studies have addressed the group or individual level factors that influence helping in wild dogs. In this study we use data collected as part of a long-term project in the Kruger National Park (KNP) to provide the first detailed analysis on t
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Yu, Liuji. "Measurement of the bulk flow and transport characteristics of selected fractured rock aquifer systems in South Africa: a case study of the Balfour Formation in the Eastern Cape Province." Thesis, University of Fort Hare, 2011. http://hdl.handle.net/10353/415.

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Hydrogeologists have faced serious challenges worldwide in the characterization of fractured rock aquifers due to the heterogeneous nature of the imbedded geology. The bulk flow parameters in the Karoo strata in South Africa are specifically uncertain since most models are based on homogenous block systems. As part of a WRC research project, entitled “Measurement of the bulk flow and transport characteristics of selected fractured rock aquifer systems in South Africa”, this study focuses on the characterization, borehole drilling, flow parameter measurements and groundwater quality assessment
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Katemaunzanga, David. "Lithostratigraphy sedimentology and provenance of the Balfour Formation Beaufort Group in the Fort Beaufort Alice area Eastern Cape Province South Africa." Thesis, University of Fort Hare, 2009. http://hdl.handle.net/10353/274.

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A traverse through the Balfour Formation was chosen in the area around the towns of Fort Beaufort and Alice in the Eastern Cape Province. The main objectives of the study were to map the lithological variations within the Balfour Formation and to distinguish it from the underlying Middleton Formation and the overlying Katberg Formation. A combined desktop, field and laboratory approach was used in this study. Aerial photographs, satellite images and digital topographical maps formed the basis of the desktop work. After desktop mapping, a number of field traverses were measured through the stud
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Lombard, Donovan Joseph. "Facies architecture and reservoir quality of Unit B, Permian Laingsburg Formation, southwestern Karoo Basin, South Africa." Thesis, Stellenbosch : Stellenbosch University, 2013. http://hdl.handle.net/10019/9989.

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Thesis (MSc)--Stellenbosch University, 2013.<br>This study presents a facies outcrop characterization and petrographical analysis of Unit B of the Permian Laingsburg Formation. Unit B is interpreted as a base-ofslope system, which represents a strikingly sand-rich succession. The base-of-slope system is defined by a channel-levee complex. The study provides systematically a clear understanding and description on reservoir heterogeneities, in terms of facies distribution, physical processes and architectural elements. The dataset included detailed sedimentary logs, photomosaic interpretat
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Krummeck, William Desmond. "Ichnology and sedimentology of large tetrapod burrows in the latest Early Triassic Katberg Formation, south-eastern main Karoo Basin, South Africa." Master's thesis, University of Cape Town, 2013. http://hdl.handle.net/11427/14233.

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Trace fossils in the form of large (~11 cm diameter and up to 2 m in length) burrows were studied at three localities in the Early Triassic Katberg Formation in the south-eastern and central parts of the main Karoo Basin, Eastern Cape, South Africa. The most interesting site, Hobbs Hill, northwest of Cathcart (Eastern Cape) has numerous burrows, contains an exceptionally well exposed sedimentary succession and bone beds. This site is also the type locality for the holotype of the parareptile Kitchingnathus untabeni (BP/1/1187). The aims of this dissertation are to: 1) reconstruct the local pal
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Chukwuma, Kenneth. "Spatial and temporal variations in the geometry and composition of the Permian Whitehill Formation South Africa." Doctoral thesis, University of Cape Town, 2017. http://hdl.handle.net/11427/25057.

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The Lower Permian Whitehill Formation (WHF) is an important hydrocarbon resource unit in the main Karoo Basin where it occurs in outcrops and up to 4 400 m in the subsurface and thus it is distributed over an area in excess of 260 000 km² in the southern half of South Africa. Although the formation is composed predominantly of black laminated carbonaceous shales, earlier studies detected significant spatiotemporal variability in its stratigraphy and composition, particularly the distribution of its organic carbon content across the basin. Because these stratigraphic variations and compositiona
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Mota, Lopes Jose Augusto Migueis da. "Colonialism, liberation, and structural-adjustment in the world-economy Mozambique, South Africa, Great Britain and Portugal and the formation of southern Africa (before and under European hegemony) /." Diss., Online access via UMI:, 2005.

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Moodley, Adam. "The sedimentary petrology of carbonate nodules in the Elliot Formation, Karoo Supergroup, main Karoo Basin (South Africa)." Master's thesis, University of Cape Town, 2016. http://hdl.handle.net/11427/20345.

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In South Africa, fossils found in the upper part of the Elliot Formation (Stormberg Group, Karoo Supergroup) are often associated with genetically poorly-constrained carbonate nodules. The origin of carbonate nodules i.e., pedogenic versus diagenetic, is important as pedogenic carbonate nodules can be used as palaeoclimate indicators, while diagenetic nodules carry limited palaeoclimatic information on the depositional setting. This research aims to characterize the carbonate nodules of the Elliot Formation macroscopically, petrographically and geochemically and to establish a diagnostic set o
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Mulaudzi, Lufuno J. P. "Historicising the politics of vhuhosivhuhulu : the Venda polity and state formation in South Africa, c.1800s-2020." Thesis, University of Pretoria, 2020. http://hdl.handle.net/2263/76929.

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This thesis offers a critical narrative of the history of the conflicts around the vhuhosivhuhulu (“kingship”) of the Venda polity over the last three centuries, with a stronger emphasis on events as from the second half of the twentieth century, and specifically the way history had been employed in the political arena. The point of departure was to critique and revise the views of scholars who had previously focused solely on the Venda history in their attempt to ascertain what the motives of the disputing parties were. My argument had been that academic research on a discourse as complex as
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Lundall, Paul Arnold. "Co-ordination of enterprise skill formation: a sociological and historical narrative of professional, market and state initiatives in South Africa." Doctoral thesis, University of Cape Town, 2018. http://hdl.handle.net/11427/29794.

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This thesis analyses the sociological and historical genesis of enterprise skill formation in South Africa and its effective coordination. South Africa’s late nineteenth century development as an emerging economy contributed to the state often taking the lead and being at the forefront of efforts to ensure coordination in enterprise skill formation. But gradually, concerns shaped by issues related to labour supply motivated leaders in firms and enterprises to forge their own imprint on the coordination of enterprise skill formation. The thesis also shows how these concerns with the coordinatio
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Van, der Merwe Justin Daniel Sean. "The 2003 Cricket World Cup : implications for identity formation and democratization prospects for Zimbabwe." Thesis, Stellenbosch : Stellenbosch University, 2004. http://hdl.handle.net/10019.1/16507.

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Thesis (MPhil)--Stellenbosch University, 2004.<br>ENGLISH ABSTRACT: There can be little doubt about the ability of major international sporting events to capture the aspirations and hopes of nations. These events have an uncanny ability of seemingly effortlessly doing what a hundred speeches and mass rallies by politicians could only hope to achieve. Therefore, it is no surprise that they are commonly understood to be able to bring nations and people together and provide a focus for national identity and unity. The 1995 Rugby World Cup in South Africa is an obvious proponent of such a cla
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Hicks, Judith Anne. "Gahnite and its formation in the context of regional metamorphism and mineralization in the Namaqualand metamorphic complex." Master's thesis, University of Cape Town, 1988. http://hdl.handle.net/11427/22024.

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Bibliography: pages 150-158.<br>Gahnite (ZnAl₂O₄) is commonly associated with sulphide mineralization in metamorphosed massive sulphide deposits, and also occurs in marbles, pegmatites and quartz veins. Its formation has been attributed to the breakdown of Zn-staurolite or desulphidation of sphalerite during metamorphism. The stability of zinc-rich spinels under a wide range of metamorphic conditions in a variety of lithologies results in its persistence in rocks where many other prograde, high temperature minerals and sulphides have been altered. Thfs has resulted in various investigations in
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McIntosh, Robert. "State policies in rural South Africa c. 1948 to c. 1960 : Bantu authorities, policy formation and local responses." Thesis, SOAS, University of London, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.313791.

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Abstract The thesis explores the formation, implementation and execution of 'Bantu administration' policies in the African 'reserves' of South Africa. The study begins with an examination of the institutions of segregation, the strains during the 1940s, and the responses of the government of JC Smuts and of the Nationalist opposition. The thesis covers the administrations of OF Malan, JG Strijdom and HF Verwoerd, from 1948 until the beginning of the period of 'grand apartheid', c1960. It examines a major dispute within the cabinet over African representation in state legislatures during Malan'
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Sixsmith, Peter John. "Stratigraphic development of a Permian turbidite system on a deforming basin floor : Lainsburg Formation, Karoo Basin, South Africa." Thesis, University of Liverpool, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.367065.

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Smith, Roger M. H. "Fluvial facies, vertebrate taphonomy and palaeosols of the Teekloof formation (Permian) near Beaufort West, Cape Province, South Africa." Doctoral thesis, University of Cape Town, 1989. http://hdl.handle.net/11427/23646.

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The main Karoo Basin of South Africa contains a relatively continuous sequence of continental deposits that accumulated over a 100 million year period from Permo-Carboniferous (280 Ma) to early Jurassic (180 Ma). In the southwestern region of the basin the Karoo succession is approximately 4 000 m thick, the upper half of which consists of vertebrate fossil-bearing fluvial rocks of the Beaufort Group. This study deals with Lower Beaufort (Adelaide Subgroup) strata belonging to the Teekloof Formation which are exposed in the cast-west trending erosional escarpment between the towns of Beaufort
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Mauger, Carla. "The formation and origin of carbonate minerals in the Darling and Yzerfontein hypersaline pans, Western Cape, South Africa." Master's thesis, University of Cape Town, 2009. http://hdl.handle.net/11427/9240.

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Includes bibliographical references.<br>The Darling and Yzerfontein hypersaline pans are located on the western coastal plain of South Africa. The area has an arid, Mediterranean type climate. The carbonate minerals calcite and dolomite have precipitated in the pans through the evaporation and concentration of ions derived from weathering of bedrock, marine aerosols and coastal rainfall. Five pans were studied, the brine-type pans Rooipan South, Zwartwater North and Zwartwater South, the brackish saline pan Rooipan North, and the coastal Yzerfontein pan. Directly below the surficial halite cru
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Black, Dawn Ebony. "Stratigraphic characterisation of the Collingham formation in the context of shale gas from a borehole (SFT 2) near Jansenville, Eastern Cape, South Africa." Thesis, Nelson Mandela Metropolitan University, 2015. http://hdl.handle.net/10948/d1021148.

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This study is an extensive lithological, petrographical, mineralogical and geochemical description of fresh Collingham Formation core samples collected from borehole SFT 2, located on the farm Slangfontein, south of Jansenville in the Eastern Cape, South Africa. The borehole, drilled to 295 m on the northerly limb of a shallow westerly plunging syncline, intersected the lower Ecca Group rocks of the Ripon, Collingham, Whitehill and Prince Albert Formations and terminated in the upper Dwyka Group. A comprehensive log and stratigraphic column were compiled for the Collingham Formation and fresh
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Klausen, Susanne Maria. "The formation of a national birth-control movement and the establishment of contraceptive services in South Africa, 1930-1939." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape9/PQDD_0002/NQ42950.pdf.

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Sonibare, Wasiu Adedayo. "Sedimentary modelling and petrophysical characterisation of a Permian Deltaic Sequence (Kookfontein Formation), Tanqua Depocentre, SW Karoo Basin, South Africa." Thesis, Stellenbosch : University of Stellenbosch, 2011. http://hdl.handle.net/10019.1/17884.

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Thesis (MSc)--Stellenbosch University, 2011.<br>ENGLISH ABSTRACT: This study presents an outcrop characterisation and modelling of the excellently exposed Permian Kookfontein Formation of the Ecca Group in the Tanqua-Karoo sub-Basin. The sedimentary modelling (i.e. facies architecture and geometry) and petrophysical characterisation followed a hierarchical and deterministic approach. Quantitative outcrop data were based on the thirteen sedimentary cycles that characterise this stratigraphic succession at the Pienaarsfontein se Berg locality; and these data were analysed using a combinatio
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Poignant-Molina, Léo. "Primary controls on iron and manganese distribution in sphalerite of the Gams Formation, Gamsberg zinc deposit, Namaqualand, South Africa." Thesis, Rhodes University, 2018. http://hdl.handle.net/10962/63775.

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The Gamsberg deposit is a 200 Mt zinc reserve belonging to the world class base metalrich Aggeneys-Gamsberg mining district. A rifting environment permitted the development of four proximal SEDEX-type deposits whereby Gamsberg is localized in the eastern side of the district and characterised by a peculiar enrichment in manganese. This study investigates the geochemistry of sphalerite in the Gams Formation holding the economic units of the deposit. Microscopic petrography revealed that most of primary textures have been overprinted by recrystallization, alteration, replacement and deformationa
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Cousins, David Patrick. "A stratigraphic, petrographic and geochemical study of the gamagara formation at the maremane dome, Northern Cape province, South Africa." Thesis, Rhodes University, 2017. http://hdl.handle.net/10962/4679.

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Between 80 and 90 percent of the potential iron ore reserves in the Griqualand West basin in the Northern Cape province of South Africa is situated in the Asbesheuwels Iron-formation immediately below an unconformity that separates it from the Gamagara Formation of the Olifantshoek Supergroup. This extensive regional unconformity marks a lengthy period of non-deposition and erosion which preceded the deposition of the Gamagara Formation. Due to the nature of the intimate relationship between the shales and iron ore body, specifically on the Maremane dome, new insights into the Gamagara Formati
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