Zugl.: Hamburg, Universiẗat, Diss., 2006.

(M. Arch.)--University of Hong Kong, 2002. / Includes bibliographical references. Also available in print.

No description available.

Shan-Mei, a Tsou aboriginal village in Taiwan, is widely known as a legend of environmental conservation, where ecotourism has been successfully combined with integrated community development. Indigenous knowledge containing "ecological wisdom" and decision-making based on consensus are perceived to be the greatest contributors to this achievement. I conducted three months of fieldwork in Shan-Mei, primarily using the methods of participant observation and semi-structured interviews. The purpose of this study was to reexamine the ecotourism and community development in Shan-Mei. I found that the ecotourism project is ecologically based, but not ecologically sound. With a combination of nature-based tourism and ethnic tourism, and later expansion into mass tourism, Shan-Mei's ecotourism project yielded negative environmental impacts. The unplanned development of mass tourism especially brought overcrowding that endangered a fragile fish species and the surrounding ecosystem. Lack of education about environmental issues created misperceptions among tourists and local people about the role of conservation in ecotourism. The community also faced problems of inappropriate government intervention, declining local participation in the project, and internal conflicts of interest. There was a need for better training and implementation of the interpretive program, professional assistance by outside experts for environmental assessment and planning, and better protection for indigenous rights in the laws of the nation state. This case illustrates that ecologically sound ecotourism not only requires indigenous knowledge but also expertise and legal protection that recognizes local autonomy. Despite the shortcomings, the Shan-Mei community was found to be proactive in creating a better future for its residents. The community used the revenue from ecotourism and government aid to establish its own social welfare program, fund various projects to revive traditional culture, assist agricultural development, and improve everyone's quality of life. The community benefited from ecotourism and community development in terms of inventing a hybrid Shan-Mei culture and forming a stronger sense of identity and autonomy. Shan-Mei provides invaluable lessons in its experience with ecotourism in its strategic adaptation to modernization. / Graduation date: 2002

Thesis (M.A.)--York University, 2008. Graduate Programme in Geography. / Typescript. Includes bibliographical references. Also available on the Internet. MODE OF ACCESS via web browser by entering the following URL: http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:MR38794

Thesis (Ph. D.)--University of Texas at Austin, 2008. / Vita. Includes bibliographical references.

Thesis (Ph. D.)-- Hua zhong shi fan da xue, 2001. / Includes bibliographical references.

Le Tian Shan est une chaîne intracontinentale d’Asie Centrale, dont la structure lithosphérique résulte de l’accrétion de divers blocs au cours du Paléozoïque. Son histoire tectonique récente est marquée par sa réactivation au Tertiaire, liée à la collision entre l’Inde et l’Asie. L’histoire topographique et tectonique de la chaine entre les deux orogenèses majeures (paléozoïque terminal et cénozoïque) reste peu contrainte. Cette thèse associe deux approches, la sédimentologie et la thermochronologie basse température, dans le but de déterminer de façon qualitative l’évolution de la topographie au cours du Mésozoïque.Le démantèlement des reliefs associés à la chaine tardi-paléozoïque s’achève au Trias supérieur. Il est suivi d’une activité tectonique très faible au Jurassique, majoritairement transtensive et caractérisée par des taux d’exhumation très faibles dans le Tian Shan. Une surface majeure de pénéplanation se développe alors en Asie Centrale. A la limite Jurassique – Crétacé, la mise en place de cônes alluviaux indique une réactivation de la chaîne, qui n’est néanmoins pas suffisante pour être enregistrée par la thermochronologie. Cette période est caractérisée par un régime généralement extensif en Asie Centrale (jusqu’au Bassin Caspien qui s’ouvre à l’est), et précède la phase d’exhumation lente, qui suit au Crétacé inférieur. La chaîne est progressivement réactivée à partir de 100 Ma et pendant le Crétacé supérieur, ce qui pourrait correspondre à un effet retardé de la collision du Bloc de Lhassa (140 - 120 Ma). Vers 65 - 60 Ma, une phase d’exhumation rapide atteste d’une réactivation plus intense et localisée le long des principales failles. Elle est sans doute liée aux collisions de blocs le long de la marge sud-ouest de l’Asie (e.g. Bloc du Kohistan, arc du Dras, Bloc Afghan). Dans la région du Tian Shan, l’activité tectonique semble totalement s’arrêter au Paléocène permettant le développement d’un niveau majeur de calcrêtes, avant la nouvelle réactivation au Néogène. Par conséquent, l’association des données de thermochronologie sur le socle avec la reconstruction des milieux de dépôt dans les différents bassins, montre que la paléo-chaîne du Tian Shan s’aplanit durant le Mésozoïque. Des évènements tectoniques de faible envergure ont lieu en Asie Centrale, induits par les principaux mouvements géodynamiques le long des bordures entourant l’Asie. Pourtant leur enregistrement est incomplet et seule la combinaison des deux approches étudiées permet de reconstituer l’évolution topographique et paléogéographique du Tian Shan. / The Tian Shan is an intracontinental range located in Central Asia. The structure of the range formed during the Paleozoic through the accretion of several blocks. Recently the range has been reactivated due to far-field effects of the collision between India and Asia. The topographic and tectonic evolution of the range in-between these two major relief-building phases (Late Paleozoic and Cenozoic) is still poorly understood. Two different approaches are combined in this work, in order to determine the Mesozoic topographic evolution of the area, in a qualitative way.The Late-Paleozoic range has been progressively eroded until the Upper Triassic/Lower Jurassic. Tectonic activity was relatively quiet during the Jurassic characterised by low exhumation rates. We suggest that the tectonic regime was dominated by transtension in the Tian Shan area. This period is linked to a regional peneplanation in Central Asia. At the Jurassic-Cretaceous boundary, the occurrence of alluvial fan deposits shows a reactivation of the range, though not strong enough to be recorded by low-temperature thermochronology. This period is characterised by an overall extensional tectonic regime all over Central Asia, with the opening of the Caspian Basin further west. It precedes the phase of very slow exhumation that occurs during the Lower Cretaceous. From 100 Ma and during the Upper Cretaceous, the range is progressively reactivated. We suggest that this correspond to a delayed answer of the Lhassa bloc collision (140 - 120 Ma). Around 65 - 60 Ma, a new phase of rapid exhumation attests of a stronger reactivation, localised along the major faults. This is contemporary of bloc collisions along the south-west margin of Asia, such as the Kohistan Block, the Dras arc or the Afghan Block. In the Tian Shan area, the development of calcrete features in the Paleocene suggests the end of tectonic activity, before the new reactivation in the Neogene.The combination of low temperature thermochronology on the basement rocks and facies sedimentology in the various basins indicate that while during the Mesozoic, the Palaeo-Tian Shan topography generally flattens, some small-scale tectonic events driven by far-field effects of major geodynamic processes around the edges of Asia did occur. However, those tectonic movements did not induce enough exhumation to be recorded by low temperature thermochronometers. Only the sediment record allows their detection and detailed description.

published_or_final_version / Housing Management / Master / Master of Housing Management

內容大要如下： 第一章、說明三民主義對吾人之時代需要，及其與時代環境的關係，並論當前民族主 義研究的重要，以及本文的研究方法。 第二章、主要說明 中山先生的民族主義思想浦源、歷史發展，並歸納出其內涵具有 文化、統一、理性、圓融等特性。再由此特性為基礎開展出三、四、五、六章的討論 主題。 第三章、先說明 中山先生民族主義的文化內涵，再論當前中國文化的危機，最後提 出當前文化民族主義的實踐方向。 第四章、先說明 中山先生民族主義的統一內涵，再論當前中國統一的障礙，最後提 出當前統一民族主義的實踐方向。 第五章、先說明 中山先生民族主義的理性內涵，再論當前國際上民族主義的危機， 最後提出當前理性民族主義的實踐方向。 第六章、先說明 中山先生民族主義圓融的內涵，再論民族文化與當前民權主義、民 生主義實踐的關係。 第七章、結論。