published_or_final_version / abstract / History / Master / Master of Philosophy

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No description available.

This study develops a model explaining support for contemporary extreme-right parties. The history and political setting of relevant countries are examined. The research explores necessary state-level conditions, which are postindustrialism, convergence to the center by major parties, and proportional representation. Individual support is probed using survey data with bivariate and probit analyses. Being male and younger proved to be significant variables, while socio-economic status did not. Concerning issues, personal disaffection for immigrants, favoring nationalistic hiring practices, and free-market tendencies were significant variables. Opposition to feminism and pride to be from one's nation were insignificant explanations for extreme-right support. Implications of the analysis are discussed as are issues concerning future research.

University of Macau / Faculty of Social Sciences and Humanities / Department of Government and Public Administration

Thesis (doctoral) - Vrije Universiteit, Amsterdam, 2001. / This book is a slightly revised version of the doctoral dissertation the author completed in June 2001 and defended at the Faculty of Arts of the Vrije Universiteit Amsterdam in October 2001. Includes bibliographical references (p. 255-285) and index.

Thesis (doctoral)--Vrije Universiteit, Amsterdam, 2001. / This book is a slightly revised version of the doctoral dissertation the author completed in June 2001 and defended at the Faculty of Arts of the Vrije Universiteit Amsterdam in October 2001. Description based on print version record. Includes bibliographical references (p. 255-285) and index.

The Lower Jurassic stratigraphy of seven contrasting areas in western Europe is compared in order to seek evidence for a pan-Western European stratigraphic forcing mechanism. Sequencestratigraphic models are discussed and emphasis is placed upon the differing response of sedimentary systems in "accommodation space-dominated" and "supply-dominated" settings. Spectral gamma-ray data from clastic successions in the Wessex and Cleveland basins (England) are used to elucidate vertical trends. A proximal-distal model for control of Th/K ratios is advanced. Stage-frequency regressive-transgressive cycles in the two areas are shown to be closely correlative. Sedimentolgical logs and spectral gamma-ray data are presented for the carbonate ramp into turbidite sequence of Peniche (Portugal) and for a new exposure of the Pliensbachian-Toarcian in southern Germany. Systematic variation in clay mineralogy across Europe is suggested. Cycles in the Lower Jurassic of the North Viking Graben (Norwegian North Sea) are examined using wireline log correlation and the stratigraphic evolution of the Tethyan Rift in the Western and Southern Alps is reviewed. X-ray diffraction studies of the Pliensbachian-Toarcian interval in the Southern Alps are presented in order to elucidate sediment supply to the pelagic realm. The cycles observed in the English sections appear to be manifest widely across western Europe in a variety of tectonic and sedimentary settings. Sharp basinward facies shifts (candidate sequence boundaries) do not appear to be synchronous between basins. ⁸⁷SR/⁸⁶SR analysis of belemnites from the Portuguese and German sections confirms the regional applicability of the results of Jones (1992) and the utility of this technique in long range correlation. Carbon and oxygen analysis of the same material supplements the data of other workers and a direct relationship is suggested between relative sea level and organic carbon burial in the Early Jurassic.

Thesis (Ph. D.)--State University of New York at Binghamton, Department of Sociology, 2007. / Includes bibliographical references.