Magister Artium - MA / This thesis explores how the hijab fashion market has emerged in Cape Town and how Capetonian Muslim women are appropriating hijab fashion as a means of redefining themselves as Muslim South Africans instead of ‘Cape Malays’, the ethnic label given to Muslims in the Western Cape during the apartheid era. I argue that through self stylisation Cape Malay women are performatively rejecting the ethnicisation of Islam during apartheid. I show that ‘Cape Malay’ women are using hijab fashion to perform their ‘Muslimness’ in order to claim a positive and legitimate spot in the ‘rainbow nation’ as Muslims as a religious-cultural category, and not as ‘Malays’, an ethnic category, while simultaneously claiming their belonging to the global umma (Muslim community)

Magister Scientiae Dentium - MSc(Dent) / Aangesien 'n nasionale register vir maligniteit nie bestaan waarin informasie ten opsigte van kanker onder die verskillende bevolkings groepe van Suid-Afrika nagegaan kan word nie, kan die verspreidings patroon alleenlik bepaal word deur spesifieke projekte. Die resultaat is dat daar nog nie 'n geheelbeeld vir kanker in Suid-Afrika bestaan nie. Wat mondkanker betref, is kennis fragmentaries. Inligting oor die ver spreiding daarvan onder die Kaapse Kleurlingbevolkingsgroep is beperk en net sekere aspekte daarvan is tot hede uitgelig. Die doel van hierdie studie is om mondkanker na te gaan in die Kaapse Kleurlingbevolkingsgroep wat woonagtig is in die Skiereiland van die Kaap die Goeie Hoop. Met hierdie oogmerk, is alle mondkankergevalle wat in die Groote Schuur- en Tygerberg-hospitale behandel is, van 1970 tot 1975, nagegaan. Bewys wyse van vergelyking en ook om die invloed van eie kultuur en akkulturasie na te gaan, is aandag gegee aan ondkankergevalle van Kleurlinge woonagtig in die Skiereiland en dié in die platteland wat in die Skiereiland behandeling ondergaan het. Verder is vergelykings ook getref tussen die,Kaapse Maleier wat die Moslem-geloof aanhang en die Kaapse Kleurling wat nie hierdie geloof aanhang nie. Die mondkankerpatroon van die Indiërs wat in die Skiereiland woonagtig is, is ook nagegaan. Bewys wyse van vergelyking en ook om die invloed van eie kultuur en akkulturasie na te gaan, is aandag gegee aan mondkankergevalle van Kleurlinge woonagtig in die Skiereiland en dié in die platteland wat in die Skiereiland behandeling ondergaan het. Verder is vergelykings ook getref tussen die,Kaapse Maleier wat die Moslem-geloof aanhang en die Kaapse Kleurling wat nie hierdie geloof aanhang nie. Die mondkankerpatroon van die Indiërs wat in die Skiereiland woonagtig is, is ook nagegaan. Ten slotte is die genoemde groepe se mondkankerpatroon vergelyk met dié gevind onder die ander groepe wat in Suid-Afrika bestudeer is, dié in die res van Afrika en ook met dié in die ander kontinente.

The Malaysian granitoids form the backbone of the Malay Peninsula and have long been recognized as composed of two distinct granitic provinces separated by the Bentong-Raub suture zone: <table><ol><li>Early Permian to Late Triassic Eastern Province (Indochina – East Malaya) with mainly “I-type” hornblende-bearing granitoids, associated with Cu-Au deposits, and subordinate hornblende-free pluton roof-zones hosting limited Sn-W deposits; and</li> <li>Late Triassic Main Range Province, western Malaysia (Sibumasu) with mainly “S-type” hornblende-free granitoids, associated with Sn-W deposits, and subordinate hornblende-bearing granitoids.</li></ol></table> Field observations and new geochemical data suggested that the division of the Eastern Province and Main Range granitoids using Chappell and White’s (1974) I-S classification could be problematic, as there is a large degree of overlap between the two granitic provinces in terms of lithology, mineralogy and metallogenic affinity. The Main Range granitoids are more fractionated than the hornblende-bearing Eastern Province. Although the two granitic provinces were emplaced into different continental terranes, both granitic provinces exhibit common trace element geochemistry in the enrichment of high field strength elements (HFSE) and rare earth elements (REE) compared to typical Cordilleran I-S granites. Such enrichment is interpreted as an inheritance signature from the protoliths. The Kontum massif (an analogue of Indochina lower continental crust) comprises intraplate ortho-amphibolites and para-gneisses, which could serve as two hypothetical source end-members for the Malaysian granitoids. The model suggests that the geneses of the parental magmas of the Eastern Province and the Main Range Province were related to hybridization of melts derived from protoliths, geochemically and isotopically similar to these two source end-members, but in differing proportions. The fact that the granites from the two granitic provinces are so similar compositionally and metallogenically, suggests that similar protoliths were involved in their source. The incorporation of sedimentary-sourced melt makes the Main Range granitoids transitional I/S-type in nature, but this is unlikely to be true for the less evolved Eastern Province fractionated I-type granitoids. The hybridization of igneous- and sedimentary-sourced melts, and granite fractionation promotes Sn metallogenesis in the Main Range granitic province. Previous ages were obtained using whole rock Rb-Sr and biotite K-Ar geochronology in the 1970s and 1980s, dating methods that almost certainly do not accurately represent the crystallization age of granites. New ion microprobe U-Pb zircon ages are presented that provide new temporal constraints for the Malaysian granitic magmatism. Eastern Province granitoids have U-Pb zircon ages that range from 289 to 220 Ma, while Main Range Province magmatism is constrained between 227 and 201 Ma. A progressive westward younging trend is apparent across the Eastern Province, but becomes less obvious in the Main Range Province. In addition, the U-Pb zircon analysis of the Malaysian granitoids suggests that both granitic provinces have Cambro-Ordovician and Mesoproterozoic inheritance signatures, which match the ages of the Kontum intraplate ortho-amphibolites and para-gneisses, the two source end-members of the suspected Indochina basement. Two different tectonic models have been suggested to explain the formation and the emplacement of the Malaysian granitoids. Both models involve an east-dipping subduction zone during the Early and Mid-Triassic with Palaeo-Tethys lithosphere rolling back along the Bentong-Raub suture zone to produce westward younging ages in the Eastern Province granitoids. The first model (modified after Searle et al. 2012) suggests the younger Main Range granitoids were produced by another Late Triassic – Cretaceous east-dipping (Neo-Tethyan) subduction to the west of Sibumasu, after the Sibumasu – East Malaya collision. The transitional I/S-type geochemistry of the Main Range granitoids was caused by the partial melting of the more heterogeneous Sibumasu basement. The second model (Oliver et al. 2014) suggests the younger Main Range granitoids were produced by the westward underthrusting of Indochina crust of East Malaya beneath Sibumasu along the Bentong-Raub suture zone after the continental collision. In this model, the source of the Main Range granitoids was the pre-collision I-type Eastern Province granitoids. The second model is less likely, as no geological evidence for such underthrust is found in the Malay Peninsula.

Approved for public release, distribution is unlimited / This thesis explores the ongoing Malay-Muslim separatist insurgency in southern Thailand. In particular, it argues that historically-rooted structural factors, to include relative economic deprivation, limited political integration, and struggle for the maintenance of ethnic-religious identity, are at the root of this insurgency. The year 2001 produced two catalysts for the renewal of this insurgency, one internal and one external. The internal catalyst was a newly elected suppressive government regime under the leadership of Prime Minister Thaksin and the Thai Rak Thai Party. The external catalyst was the growing, increasingly radicalized Islamist movement, largely defined through terrorist violence, that expressed itself in the 9/11 attacks. The combination of these has produced rekindled secessionist violence of a previously unknown level in the Thai provinces of Pattani, Narathiwat, and Yala. Given the deeply ingrained structural cause of this insurgency, as well as a government administration whose policies and conflict mismanagement continually fuels the violence, the prospect for conflict resolution is not promising. Nonetheless, it remains in the best interests of the United States that this conflict is soon resolved. Should the insurgency continue growing, the situation may reach a point of drastic consequences for Thailand as well as the United States. / Captain, United States Air Force

Au début des années 1880, un grand nombre de traductions malaises de romans chinois émanant de descendants de Chinois (appelés en malais peranakan) parurent aux Indes néerlandaises sous la forme d’ouvrages imprimés. Nous avons choisi d’en étudier deux, parues simultanément pendant les années 1910-1913, à un moment où la communauté chinoise d’Insulinde essayait de repenser son identité culturelle et politique, sous les angles littéraire, philologique, historique et sociologique. Il s’agit de deux traductions complètes du Sanguo yanyi 三国演义, le plus remarquable des romans historiques chinois traitant de la période des Trois Royaumes. Une analyse textuelle, nous a permis de constater que les traducteurs des deux Sam Kok (titre abrégé couramment utilisé en Indonésie pour désigner le « Roman des Trois Royaumes »), qui n’avaient pourtant qu’une éducation chinoise du premier degré et une connaissance du malais en usage dans les milieux urbains de Java, mais une grande volonté, ont réussi à exprimer toutes les valeurs littéraires et culturelles du Sanguo yanyi. Afin d’examiner l’impact des Sam Kok sur communauté chinoise, nous les avons replacés dans leur contexte historique et dans l’ensemble des traductions parues pendant les années 1880-1910. Nous sommes parvenue ainsi à montrer que grâce à ces traductions, et particulièrement celles du « Roman des Trois Royaumes », les peranakan ont pu obtenir une certaine compréhension de l’histoire et de la culture du pays de leurs ancêtres, lesquelles constituaient aussi une partie de leur passé. / In the early 1880s, the descendants of Chinese immigrants (called Peranakan in Malay) achieved and printed a large number of Malay translations of Chinese novel in the Dutch Indies. We chose to study two translations published simultaneously during the years 1910-1913 when the Chinese community of Insular Southeast Asia was trying to rethink its cultural and political identity from the literary, philological, historical and sociological angles. The research is about two complete translations of the Sanguo yanyi 三国演义, the most remarkable Chinese historical novels that depict the period of Three Kingdoms. Through textual analysis, we found that although the translators of two Sam Kok (abbreviated title commonly used in Indonesia to refer to the “Romance of the Three Kingdoms”) had some rudimentary Chinese education and knowledge of the language Malay used in the urban areas of Java, they exhibited a great willingness to express all the literary and cultural values of the novel Sanguo yanyi. In order to examine the impact of Sam Kok on the Chinese community, we have put them in their historical context and compare them with other Malay translations published during 1880-1910. Consequently, we are able to assert that, through those translations, especially those of Romance of the Three Kingdoms, the peranakan have acquired some understanding of the history and culture of their ancestral country, which also constituted their past.

Les bassins sédimentaires se développent souvent le long des zones internes d'anciennes chaînes orogéniques. Nous considérons dans ce projet la Péninsule Malaise (Marge Ouest de la Sonde) comme un haut crustal séparant deux régions de croûte continentale étirée ; les bassins d'Andaman/Malacca du côté occidental et les bassins thaïlandais/malais à l'est. Plusieurs stades de rifting ont été documentés grâce à une intense exploration géophysique régionale. Cependant, la corrélation entre les bassins riftés en mer et le noyau continental terrestre est mal connue. Dans ce mémoire, nous explorons par la cartographie, de missions de terrain et les données sismiques, comment ces structures réactivent des hétérogénéités mésozoïques crustales préexistantes. Le noyau continental semble être relativement peu déformé après l'orogénèse triasique Indosinienne. L’épais méga-horst crustal est bordé par des zones de cisaillement complexes (zones de failles de Ranong, Klong Marui et du Batholithe du Main Range) initiées au Crétacé Supérieur/Paléogène inférieur lors d’une déformation transpressive d’échelle crustale et plus tard réactivées à la fin du Paléogène. L'extension est localisée sur les bords de cette épine dorsale crustale le long d'une bande où la précédente déformation crétacée supérieure est bien exprimée. À l'ouest, le plateau continental est aminci en trois étapes principales qui correspondent à des blocs basculés d’échelle crustale bordés par de larges failles contre-régionales profondément enracinées (Bassin de Mergui). À l'est, des systèmes de rifts prononcés sont également présents, avec de grands blocs basculés (les bassins western Thai, de Songkhla et de Chumphon) qui pourraient représenter de grands boudins de croûte. Dans le domaine central, l'extension est limitée à de demi-grabens étroits isolés de direction N-S développés sur une croûte continentale épaisse, et contrôlés par failles normales pelliculaires, qui se développent souvent au contact entre les granitoïdes et l’encaissant. Les bords extérieurs des régions affectées par le boudinage crustal délimitent le bassin d'Andaman plus grand et profond à l'ouest et les bassins Malais et de Pattani à l'est. À une échelle régionale, les bassins riftés ressemblent à des structures en-échelon N-S le long de grandes bandes de cisaillement de NW-SE. Le rifting est accommodé par de larges failles normales à faible pendage (LANF : Low Angle Normal Faults) réactivant les morpho-structures de la croûte telles que de larges plis et batholithes mésozoïques. Les bassins profonds d'Andaman, Malais et de Pattani semblent situés sur une croûte à rhéologie plus faible qui pourrait être héritée des blocs continentaux dérivés du Gondwana (Birmanie, Sibumasu, et Indochine). L'ensemble des long bassins étroits au coeur de la région (bassins de Khien SA, de Krabi, et du Malacca) apparaissent avoir souffert de relativement peu d'extension. Ce travail montre que le cœur de l’orogène Crétacé supérieure est faiblement réactivé avec seulement quelques traces d’un étirement précoce par rapport aux bords qui sont sujets à un amincissement crustal en larges blocs basculés. A mesure que la déformation augmente, le rifting migre et se localise vers les zones externes et sa géométrie apparait plus « molle » suggérant un mécanisme influencé par la thermique. La coexistence de ces deux géométries au sein d’un même cycle de rifting fait de la marge Ouest de la sonde un cas d’étude édifiant. / Sedimentary basins often develop above internal zones of former orogenic belts. We hereafter consider the Malay Peninsula (Western Sunda) as a crustal high separating two regions of stretched continental crust; the Andaman/Malacca basins in the western side and the Thai/Malay basins in the east. Several stages of rifting have been documented thanks to extensive geophysical exploration. However, little is known on the correlation between offshore rifted basins and the onshore continental core. In this paper, we explore through mapping and seismic data, how these structures reactivate pre-existing Mesozoic basement heterogeneities. The continental core appears to be relatively undeformed after the Triassic Indosinian orogeny. The thick crustal mega-horst is bounded by complex shear zones (Ranong, Klong Marui and Main Range Batholith Fault Zones) inititiated during the Late Cretaceous/Early Paleogene during a thick-skin transpressional deformation and later reactivated in the Late Paleogene. The extension is localized on the sides of this crustal backbone along a strip where earlier Late Cretaceous deformation is well expressed. To the west, the continental shelf is underlain by three major crustal steps which correspond to wide crustal-scale tilted blocks bounded by deep rooted counter regional normal faults (Mergui Basin). To the east, some pronounced rift systems are also present, with large tilted blocks (Western Thai, Songkhla and Chumphon basins) which may reflect large crustal boudins. In the central domain, the extension is limited to isolated narrow N-S half grabens developed on a thick continental crust, controlled by shallow rooted normal faults, which develop often at the contact between granitoids and the host-rocks. The outer limits of the areas affected by the crustal boudinage mark the boundary toward the large and deeper Andaman basin in the west and the Malay and Pattani basins in the east. At a regional scale, the rifted basins resemble N-S en-echelon structures along large NW-SE shear bands. The rifting is accommodated by large low angle normal faults (LANF) running along crustal morphostructures such as broad folds and Mesozoic batholiths. The deep Andaman, Malay and Pattani basins seem to sit on weaker crust inherited from Gondwana-derived continental blocks (Burma, Sibumasu, and Indochina). The set of narrow elongated basins in the core of the Region (Khien Sa, Krabi, and Malacca basins) suffered from a relatively lesser extension. This work shows that the core of the late Cretaceous Orogeny is weakly reactivated during the subsequent rifting with only few evidences of stretching whereas its sides are thinned with large tilted blocks. The rifting migrates and localizes on the external regions and its geometry appears more ductile suggesting the influence of a thermal activity in the process. The coexistence of both geometries in a single rifting cycle makes the western margin of Sundaland an enlightening example.

This case study explored the revision strategies of four Malaysian native speakers of English when they composed aloud while writing an argumentative essay. Think aloud verbal protocols were analysed using the grounded theory approach in conjunction with written texts. The findings suggest that contextual factors influenced classroom practices. The contextual factors included a teacher who was not provided with adequate training, administrative policies which did not provide support for the development of writers based on their abilities, writing instruction which viewed revision as a process of error correction and public assessment practices which were non-transparent. These classroom practices influenced the participants� beliefs about revision. These beliefs affected the quality of their essays as judged by Malaysian public examiners. Additionally, the findings suggest a mismatch between classroom instruction and public examination. Suggestions are made to address these concerns by considering the theoretical underpinnings of the cognitive process, socio-cultural and community of practice models of writing and learning. These include instruction on revision strategies, considering alternative assessment practices, providing formative feedback, ability streaming, focussing on critical reading skills and providing adequate support to the teacher.

Background: Diabetes mellitus and vascular diseases have a significant impact on the eye. / Aim: To determine the prevalence, risk factors, and racial/ethnic differences of major eye conditions, particularly retinal conditions, associated with diabetes and vascular diseases. / Scope: To date, the majority of studies have examined the association of retinal vascular calibre and diabetes in predominantly white Caucasian populations. Further elucidation of ethnic differences in effects of hyperglycaemia on early microvascular disease is relevant, particularly amongst Asians where diabetes is likely to see the largest increase in prevalence over the next decade. We therefore examined these findings from three Asian population-based studies, the Singapore Malay Eye Study (n=3280), Singapore Prospective Cohort Study and Singapore Cardiovascular Cohort Study 2 (n=3748). / Results: The prevalence of diabetic retinopathy in the Singapore Malay Eye Study was 35%, and associated with longer duration of diabetes, poorer glycemic and blood pressure control. More importantly, 9.0% had vision-threatening retinopathy, and retinopathy was found in 6.0% of people without diabetes. Retinal vascular calibre changes were incriminated in diseases such as diabetes and hypertension, independent of traditional cardiovascular risk factors. Wider venular calibre was independently associated with early age-related macular degeneration. We also found a novel association between peripheral artery disease and glaucoma, stronger in persons with diabetes, independent of vascular risk factors, supporting the vascular theory of glaucoma. / Implications: Subtle changes in retina, including retinal vascular calibre may be early markers of widespread microvascular changes in diabetes, resulting from chronic hyperglycaemia and other pathogenic processes. These results will have broad implications for understanding the impact of both microvascular and macrovascular complications of diabetes in the Asia Pacific region and targeting relevant therapeutic interventions.

This case study explored the revision strategies of four Malaysian native speakers of English when they composed aloud while writing an argumentative essay. Think aloud verbal protocols were analysed using the grounded theory approach in conjunction with written texts. The findings suggest that contextual factors influenced classroom practices. The contextual factors included a teacher who was not provided with adequate training, administrative policies which did not provide support for the development of writers based on their abilities, writing instruction which viewed revision as a process of error correction and public assessment practices which were non-transparent. These classroom practices influenced the participants� beliefs about revision. These beliefs affected the quality of their essays as judged by Malaysian public examiners. Additionally, the findings suggest a mismatch between classroom instruction and public examination. Suggestions are made to address these concerns by considering the theoretical underpinnings of the cognitive process, socio-cultural and community of practice models of writing and learning. These include instruction on revision strategies, considering alternative assessment practices, providing formative feedback, ability streaming, focussing on critical reading skills and providing adequate support to the teacher.

The Spanish colonisation of the Philippines in 1565 opened up trade between China, Latin America and Europe via the Pacific crossing, changing the history of global trade forever. The traditional understanding of the early colonial period in the Philippines suggests that colonial control spread rapidly and peacefully across the islands, ushering in dramatic changes to the social, political and economic environment of the archipelago. This dissertation argues by contrast that the extent of Spanish control has been overstated - partially as a by-product of an over-reliance on religious and secular chronicles that sought to magnify the role and interests of the colonial state. Through extensive archival work examining different sites of colonial authority and power, I demonstrate that Philippine communities contested and limited the nature of colonisation in their archipelago. In making this argument, I challenge prevalent assumptions of indigenous passivity in the face of imperial expansion. By demonstrating the agency of Southeast Asians, particular actors come to the fore in each of the chapters: Chinese labourers, indigenous elites, fugitives and apostates, unpacified mountain communities, native priestesses and Moro slave raiders. The culture and social organisation of these Southeast Asian communities impacted on the nature of Spanish imperialism and the capacity for the Spanish to retain and extend their control. Throughout the seventeenth century, the Spanish presence within the archipelago was always tenuous. A number of communities remained outside of Spanish control for the duration of the century, while still others oscillated between integration and rebellion, by turns participating in and resisting the consolidation of empire. These communities continued to maintain their local and regional economies and customs. Thus, by the end of the seventeenth century, imperial control remained fragmented, partial and incomplete. The dissertation contributes not only to the historiography of the Philippines - which remains under-explored - but also to the historiographies of Colonial Latin America, Southeast Asia and early modern empires. Conceptualising the Philippines as a frontier space helps to overturn the foundations of the myth of a completed conquest. This dissertation thus raises questions about the inevitability of empire by arguing that indigenous communities were active respondents to Spanish colonisation attempts and that indigenous traditions and culture in this region were both resilient and enduring in the face of colonial oppression.