Based on the concept of rhetorical situation, the purpose of this study is to compare and describe the three Socialist leader's May Day speech from the years 1954, 1978 and 2011. The results of the analysis showed that there is a big difference in how the leaders chooses to appeal to the rhetorical audience. Erlander, 1954, never appealed directly to his audience which Palme, 1978, did both initially as repeatedly throughout his speech. Juholt, 2011, has a personal and frequent appeal which is repeated throughout his speech, which is interpreted as a sign of the intimization of the public language. It proved difficult to discuss the Socialist rhetoric as one unified form. The rhetoric realm is influenced by too many external factors, such as the media, which makes it impossible to speak of it as one. The analysis revealed that the language of the 1th may-speeches is characterized by the people who use it. It is inevitable that the speaker puts his utmost emphasis, in both language and speeches. It would require a larger and more comprehensive analysis to allow any conclusions about a social-democratic language.Keywords: Rhetorical situation, genre, ethos-logos-pathos, 1th May, the Swedish Social Democratic Party, Tage Erlander, Olof Palme, Håkan Juholt

The thesis puts forward the problematic situation in the very urban center of Ankara with an analytical method to investigate the roots of several problems. Building its argument on historical facts, in depth observations, and political, social, and urban analysis, it proposes a rational basis for the rehabilitation of 19 Mayis Sports District, mainly focusing on the means of elevating the physical quality through the capacity of social inclusion concerning the sports activity settings and places in the region. All in all, the basic argument stands on the belief that the spatial basis of the 19 Mayis Sports District and the neighboring urban tissue around it might be re-defined and rehabilitated, if only its historical, political, ideological, and socio-cultural bases are redefined. Therefore, the study searches for rehabilitation of the 19 Mayis Sports District in Ulus, Ankara, by adapting and integrating sports with other cultural collective practices, and defining it as an alternative life-style for citizens. Because the district lays on the second division of Atat&uuml / rk Culture Center Region, a sports culture and its policy should be defined and designed for to amend that division of the region by preparing a principal master plan for the region and for the division.

A number of critics have observed that there is no tradition of women's writing in Russian. The writings of Lydia Chukovskaya, I. Grekova and Tatiana Tolstaya--the principle subjects of the present work--partially contradict this perception, and defy the restrictions imposed by ideological authoritarianism and of gender. / All three writers describe aspects of the Soviet, and human, condition, in unique ways. Lydia Chukovskaya's fiction portrays women, paralyzed by the scope of the Stalinist terror, who attempt to survive with dignity and accept their individual responsibility. I. Grekova writes about single women who maintain their autonomy through a balance between their professional and domestic lives. Tatiana Tolstaya's characters inhabit an atmosphere of lyrical alienation from which there is no exit. / This study examines in detail the work of these writers in the context of other Soviet men and women writers, as well as in the light of Western, feminist thought.

This thesis traces the self-creation and autonomy of the woman artist figure in Virginia Woolf's To the Lighthouse, Doris Lessing's The Golden Notebook, and Margaret Atwood's Cat's Eye. The first chapter conveys the progression of autonomy and self-creation in Western-European philosophy through contemporary thinkers such as Charles Taylor, Robert Pippin, Alexander Nehamas, and Richard Rorty. This narrative culminates in a rift between public and private, resulting from the push--especially by Nietzsche--toward a radical, unmediated independence. Taylor and Rorty envision different ways to resolve the public/private rift, yet neither philosopher distinguishes how this rift has affected women by enclosing them in the private, barring them from the public, and delimiting their autonomy. The second chapter focusses on each woman artist's resistance to socially scripted roles, accompanied by theories about resistance: Woolf with Rachel Blau DuPlessis on narrative resistance, Lessing with Julia Kristeva on dissidence, and Atwood with Stephen Hawking and Kristeva on space-time. The third chapter contrasts the narratives of chapters 1 and 2 and reveals how the woman artist avoids the problematic public/private rift by incorporating the ethics developed within the private into her art; she balances her creative goals with responsibility to others. Drawing on the work of women moral theorists, this thesis suggests that women's self-creation and autonomy result in an undervalued but nevertheless workable solution to the public/private rift.

This thesis has examined some women writers of the 1950s in an attempt to discover if there could be a "women" school of writers as definable as the Black, Jewish or Southern schools which gained recognition during that ten-year period. During the 1950s American literature became fragmented as various minorities began to search into personal histories in order to discover human identities within the framework of race, religion or geography. It was the contention of this paper that women were involved in much the same type of identity search, that through their own literature they were searching out a human identity' within, but not confined to, their sexual role in society.The cliche of the decade is that this was a placid time in feminist history, a time when women docilely sacrificed education and personal talents to return to the in a search for their homes as wives and mothers. However, a study of the works of Sylvia Plath, Carson McCullers, May Sarton and Elizabeth Janeway shows a group of women in active rebellion against the sexual stereotyping so prevalent in the 1950s. Through art these women were rejecting traditional concepts of a "woman's place," and instead were exploring their own talents, strengths and potentials human identity.This thesis has sought to combine a study of the cultural influences operating on society of the 1950s with the literature being written by women during this period in order to more fully understand the female attitude toward herself and her role. This study indicates that the active rebellion of the women's liberation movement a decade later arose from the search for identity found in much literature by women of the 1950s.

The intellectual and political roots of present-day China lie in the late imperial era and the transition to modern statehood. As the last chain of the thousands years of dynastic rule in China, the Qing Dynasty ended in 1911 with a revolution. Even though the Republican regime was immediately established after their revolution, it took three decades until thenew government (People&rsquo / s Republic of China) achieved full sovereignty on the territory. The thesis argues that the 1911 Revolution is a major turning point in Chinese transformation not only because of the regime change but also the ideological shift towards modern statehood. In this study, first, the social forces and actors on the eve of the Revolution are analyzed. The gentry-domination of society and the power relations within the forces involved in the Revolution - especially the intellectuals and the military - appear to be the two major reasons why the transition was not completed with the Revolution. The second focus of the study: the process of breaking with the past. In other words, how was the shift in people&rsquo / s mind achieved? In China, this turning point did not coincide with the 1911 Revolution and/or regime change. It came later in 1910s, reaching its peak in 1919, with the New Culture Movement of the May Fourth intellectuals. There had been some influential intellectuals building a nationalist discourse even before the May Fourth Movement (e.g. Liang Qichao, reformist and ideologue in late Qing dynasty) but the radical and outspoken tone of the New Culture Movement achieved the grounds for a shift in minds. I will briefly analyze the intellectual work of the period and its politicization. A special emphasis is given on Sun Yat-sen&rsquo / s political and intellectual contribution to the transition since he was not only a major political activist but also a theoretician whose works (Three Principles of People) have been influential on China&rsquo / s nation-building process.

Thesis (Ph. D.)--University of Hawaii at Manoa, 1995. / Includes bibliographical references (leaves 304-315). / Microfiche. / x, 315 leaves, bound 29 cm

The Mount Isa and May Downs Faults are part of a network of significant faults that define, control, or partition deformation in the Early to mid-Proterozoic Mount Isa Inlier. The middle Proterozoic deformation history includes at least two extensional basin-forming events (Leichhardt Superbasin: ~1800 Ma to ~1700 Ma and Isa Superbasin: ~1700 Ma to ~ 1600 Ma) and a major protracted contractional orogenic event (Isan Orogeny: ~1585 Ma to ~ 1500 Ma). Uplift between the Mount Isa and May Downs Faults during the Isan Orogeny has exposed mid to upper amphibolite facies rocks of the structurally deeper levels of the early rift systems. Also exposed is the Sybella Granite, a composite batholith of variably deformed gneissic granite, which, at ~1660 Ma, is broadly coeval with inception of the Isan Superbasin basin. Two prevailing kinematic models had been proposed for the fault systems during Isan Superbasin formation. The traditionally accepted model involves episodic E-W or NW-SE extension with the N-S Mount Isa Fault, but Southgate et al (2000b) presented an alternative sinistral strike-slip model in which the May Downs Fault acted as a releasing bend fault associated with motion on the Mt Isa Fault. In the Southgate model, the Sybella Granite was interpreted as syn-tectonically filling the dilational releasing bend. This study provides a detailed structural analysis of the 100 km by 40 km area west of Mount Isa City lying between the Mount Isa and May Downs Faults. The aim was to resolve a number of outstanding issues, including those outlined above. The resultant 1:250 000 structural map of the area is based on: reconnaissance-scale mapping; aerial photography, satellite, magnetic and radiometric image interpretation; field observations at locations throughout the area; and local detailed mapping (1:12000 scale or less). The mapping and associated geometrical analysis of the area has shown that the Sybella Batholith consists of two granite sills and a more globular body of microgranite. The deepest, gneissic, sill is up to 5 km thick and was emplaced at about 15 km below the basal Mount Isa Group unconformity (palaeosurface). The other, less deformed, sill formed higher in the crust, and the microgranite intruded to within 1-2 km of the palaeosurface. The two sills are located between two major fault systems (Mount Isa and May Downs Faults) that developed from inherited basin margin faults. The fault systems dip toward each other and the rocks between them have been folded into a single large antiform and uplifted as a wedge. Previous interpretations of the area have suggested that the batholith consists of a single sill folded by tighter, shorter wavelength folds. A cross-sectional reconstruction of the study area suggests that thin-skinned processes dominated much of the Isan Orogeny, contrary to previous interpretations. A three-dimensional reconstruction of the area, evaluated by comparing the predicted strain and amount of shortening with measured strain and shortening estimates, suggests deformation was driven by a rigid block to the west of the May Downs Fault moving toward the northeast. In the restored pre-Isan geometry, both the margins of the lowermost gneissic granite sill and its immediate country rocks have a strong, horizontal, layer-parallel, shear foliation with top-to-the-east asymmetry. The fabrics are strongly constrictional and 2 Abstract the stretching lineation trends east-west. Field observations and thin sectional analysis of these fabrics provide positive evidence that the Sybella Batholith was syn-tectonically emplaced in a basin-forming environment. A kinematic model is presented to show that these features are consistent with granite emplacement into a dilational jog in a sub-horizontal shear zone with a top-to-the-east shear sense. A component of east-west directed horizontal simple shear across the dilating zone explains the strongly constrictional fabrics in the granite. Under these conditions significant north-south shortening in the deforming zone leads to the initiation of folds parallel to the stretching direction (as observed). The shear zone into which the granite was emplaced developed at about fifteen kilometres depth and was probably at or near the brittle-ductile transition. The consistent shear sense, very high strains and implied 30 km of translation required to accommodate the sill indicates that this was a major crustal structure, rather than a simple detachment at the brittle-ductile transition in a crustal pure shear extension. The results are consistent with the east-west extensional model for basin development and totally inconsistent with the sinistral strike-slip model.

The Mount Isa and May Downs Faults are part of a network of significant faults that define, control, or partition deformation in the Early to mid-Proterozoic Mount Isa Inlier. The middle Proterozoic deformation history includes at least two extensional basin-forming events (Leichhardt Superbasin: ~1800 Ma to ~1700 Ma and Isa Superbasin: ~1700 Ma to ~ 1600 Ma) and a major protracted contractional orogenic event (Isan Orogeny: ~1585 Ma to ~ 1500 Ma). Uplift between the Mount Isa and May Downs Faults during the Isan Orogeny has exposed mid to upper amphibolite facies rocks of the structurally deeper levels of the early rift systems. Also exposed is the Sybella Granite, a composite batholith of variably deformed gneissic granite, which, at ~1660 Ma, is broadly coeval with inception of the Isan Superbasin basin. Two prevailing kinematic models had been proposed for the fault systems during Isan Superbasin formation. The traditionally accepted model involves episodic E-W or NW-SE extension with the N-S Mount Isa Fault, but Southgate et al (2000b) presented an alternative sinistral strike-slip model in which the May Downs Fault acted as a releasing bend fault associated with motion on the Mt Isa Fault. In the Southgate model, the Sybella Granite was interpreted as syn-tectonically filling the dilational releasing bend. This study provides a detailed structural analysis of the 100 km by 40 km area west of Mount Isa City lying between the Mount Isa and May Downs Faults. The aim was to resolve a number of outstanding issues, including those outlined above. The resultant 1:250 000 structural map of the area is based on: reconnaissance-scale mapping; aerial photography, satellite, magnetic and radiometric image interpretation; field observations at locations throughout the area; and local detailed mapping (1:12000 scale or less). The mapping and associated geometrical analysis of the area has shown that the Sybella Batholith consists of two granite sills and a more globular body of microgranite. The deepest, gneissic, sill is up to 5 km thick and was emplaced at about 15 km below the basal Mount Isa Group unconformity (palaeosurface). The other, less deformed, sill formed higher in the crust, and the microgranite intruded to within 1-2 km of the palaeosurface. The two sills are located between two major fault systems (Mount Isa and May Downs Faults) that developed from inherited basin margin faults. The fault systems dip toward each other and the rocks between them have been folded into a single large antiform and uplifted as a wedge. Previous interpretations of the area have suggested that the batholith consists of a single sill folded by tighter, shorter wavelength folds. A cross-sectional reconstruction of the study area suggests that thin-skinned processes dominated much of the Isan Orogeny, contrary to previous interpretations. A three-dimensional reconstruction of the area, evaluated by comparing the predicted strain and amount of shortening with measured strain and shortening estimates, suggests deformation was driven by a rigid block to the west of the May Downs Fault moving toward the northeast. In the restored pre-Isan geometry, both the margins of the lowermost gneissic granite sill and its immediate country rocks have a strong, horizontal, layer-parallel, shear foliation with top-to-the-east asymmetry. The fabrics are strongly constrictional and 2 Abstract the stretching lineation trends east-west. Field observations and thin sectional analysis of these fabrics provide positive evidence that the Sybella Batholith was syn-tectonically emplaced in a basin-forming environment. A kinematic model is presented to show that these features are consistent with granite emplacement into a dilational jog in a sub-horizontal shear zone with a top-to-the-east shear sense. A component of east-west directed horizontal simple shear across the dilating zone explains the strongly constrictional fabrics in the granite. Under these conditions significant north-south shortening in the deforming zone leads to the initiation of folds parallel to the stretching direction (as observed). The shear zone into which the granite was emplaced developed at about fifteen kilometres depth and was probably at or near the brittle-ductile transition. The consistent shear sense, very high strains and implied 30 km of translation required to accommodate the sill indicates that this was a major crustal structure, rather than a simple detachment at the brittle-ductile transition in a crustal pure shear extension. The results are consistent with the east-west extensional model for basin development and totally inconsistent with the sinistral strike-slip model.

Thesis (Ph. D.)--Flinders University of South Australia, 2000. / Title from PDF title page (viewed on July 9, 2005). Includes bibliographical references (p. 307-379).