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Dissertations / Theses on the topic 'Le Tibet'

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Published: 19 April 2025

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1

Ding, Yunxian. "Allegories of Tibet /." Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/6157.

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2

McDermid, Isabella Rose Cross. "Zedong Terrane, South Tibet." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2002. http://hub.hku.hk/bib/B31244610.

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3

Deshayes, Laurent. "La mission du Tibet." Nantes, 2001. http://www.theses.fr/2001NANT3025.

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Fondée en 1846, la Mission du Tibet fut confiée aux prêtres de la Société des Missions Étrangères de Paris. Ils tentèrent de pénétrer au Tibet, sans succès, et s'installèrent dans les Marches tibétaines (Sichuan, Yunnan), et dans le sud du Sikkim. Durant plus d'un siècle, sous cinq épiscopats, les religieux furent les témoins, les victimes et parfois les acteurs d'événements politiques opposant Pékin et Lhassa. Ils furent aussi l'avant-garde de la France au coeur de l'Asie. Ce fut d'abord le temps des pionniers : Mgrs ThomineDesmazures (1857-1864), Chauveau (1864-1877) et Biet (1877-1901) lancèrent de vaines expéditions vers le Toit du monde et furent confrontés, dans les Marches tibétaines, au pouvoir des monastères bouddhistes et des seigneurs locaux. Puis, grâce à Mgr Giraudeau (1901-1936), à la faveur du soulèvement des populations tibétaines (1905), et malgré les demandes d'alliance faites par le Xllle Dalai Lama, la France espéra renforcer ses liens avec la Chine impériale.
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4

Tenzin. "Marriage customs in central Tibet /." Oslo : Department of Cultural Studies and Oriental Languages, Universitetet i Oslo, 2008. http://www.duo.uio.no/publ/IKOS/2008/74471/EMENDED_6thxofxMayxTenzin.pdf.

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5

Chan, On-kee Angel. "Miocene collision related conglomerates, south Tibet." Click to view the E-thesis via HKUTO, 2004. http://sunzi.lib.hku.hk/hkuto/record/B30736870.

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6

Chan, On-kee Angel, and 陳安琪. "Miocene collision related conglomerates, south Tibet." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2004. http://hub.hku.hk/bib/B30736870.

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7

Clark, Marin Kristen 1973. "Late Cenozoic uplift of southeastern Tibet." Thesis, Massachusetts Institute of Technology, 2003. http://hdl.handle.net/1721.1/29758.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2003.
Includes bibliographical references.
Recent field work and DEM analysis show that remnant, local areas of a low-relief land scape (or "erosion surface") are geographically continuous across the southeastern Tibetan Plateau margin and can be correlated in order to define the maximum envelope of topogra phy of the margin itself. This observation contradicts earlier notions that the low-gradient plateau margin slope (i.e. the maximum elevation of the margin) is a product of landscape dissection and reduction by fluvial incision due to the presence of major rivers which drain this portion of the plateau and plateau margins. Although initial development of the erosion surface is likely diachronous, we propose that a continuous low-relief landscape existed at low elevations prior to uplift and long-wavelength tilt of the southeastern plateau margin. The modern altitude of the erosion surface provides an excellent datum for constraining the total amount of surface uplift of the southeastern plateau margin. The long-wavelength tilt of the surface across the plateau margin without major disruption mirrors the low-gradient decrease in crustal thickness across the plateau margin, which suggests that crustal thickening has occurred in a distributed manner. Because large-magnitude compressional structures of late Cenozoic age are lacking, we propose that crustal thickening beneath the southeastern plateau margin has largely been accomplished by preferential thickening the lower crust. Perched, relict landscape remnants that reflect slow erosion, low initial elevations and slow uplift rates contrast sharply with the rapidly eroding modern river gorges that incise the surface, indicating that the modern landscape is not in equilibrium. Surface remnants are preserved because incision of the fluvial system has been largely limited to major rivers and principle tributaries, and has not yet progressed throughout the entire fluvial network.
(cont.) This "transient condition" of the landscape in southeastern Tibet reflects the initiation of rapid bedrock incision into a developing plateau margin, and the altitude of the remnant erosion surface can also be used as a datum by which to measure the total amount of erosion since the beginning of plateau uplift. 2.1 Introduction The continent-continent collision between India and Eurasia is largely responsible for creating the Tibetan Plateau, the most extensive region of elevated topography on Earth [Figure 2.1]. The development of such an anomalously high landmass has been of interest to scientists in a broad range of disciplines ranging from lithospheric dynamics to the inter action between tectonics, climate and surface processes. Studies of the Tibetan Plateau have raised several first-order questions such as: 1) how is plate convergence accommodated in the continents and what are the relative contributions of continental subduction, uniform or differential shortening in the upper and lower crust, and lateral extrusion of rigid lithospheric blocks?; 2) how do spatial (or temporal) variations in crust and mantle rheology partition deformation throughout theorogen?; 3) does the convective removal of the mantle lithosphere contribute to surface uplift and high plateau elevation? ...
by Marin Kristen Clark.
Ph.D.
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8

Assandri, Sandra. ""Tenzing" : une expérience filmique au Tibet." Paris 10, 1988. http://www.theses.fr/1988PA100082.

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Cette thèse concerne la réalisation d'un film sur la culture tibétaine. A partir d'une préalable expérience de recherche en Inde (terrain de huit mois en 1980-81), et ayant acquis les connaissances théoriques et pratiques propres de l'Anthropologie Visuelle, (DEA en 1983), la décision est prise de vérifier les hypothèses développées à propos de l'utilisation des instruments de prise de vue pendant une recherche, par la réalisation d'un film. Le projet se développe à partir des interviews obtenues pendant le terrain précèdent et aboutit dans un film d'une heure environs tourné entre Katmandu et Lhassa. Parmi d'autres options possibles, la réalisatrice a choisi de travailler autour d'un seul personnage qui devient prétexte et fil conducteur d'une “exp1oration“ du Tibet actuel dont les aspects modernes n'arrivent pas à cacher l'attachement encore très profond aux les valeurs traditionnels. Options méthodologiques et stratégies adoptées à la prise de vue et au montage sont objet de réflexion en relation avec différents aspects de la culture étudiée
This thesis describes the process of making a film on the Tibetan Culture. The film-maker conducted field-work in 1980-81 for a period of eight months in a Tibetan village in Northern India. The film is based on a number of long interviews with villagers and monks, concerning social life and customs (past and present) of Tibetan refugees in India. The interviews where carried on during this period of research. The thesis deals with hall the problems involved in the making of an ethnographic film taking into account of the theoretical, methodological and practical implications. The focus of the film is a single person (a young businessman going back to Tibet for the first time) whose portrait (and journey from Katmandu to Lhasa) is a pretext and an artifice to explore and bring to light some aspects of Tibetan Culture. Methods and strategies in filming and editing are discussed at different levels and in relation to certain aspects of Tibetan Culture
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9

Assandri, Sandra. ""Tenzig" une expérience filmique au Tibet /." Lille 3 : ANRT, 1990. http://catalogue.bnf.fr/ark:/12148/cb376114107.

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10

Martínez, Diana. "The journey of an image the Western perception of Tibet from 1900-1950 /." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2009. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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11

劉建兵 and Jianbing Liu. "Yamdrok melange, Gyantze district, Xizang (Tibet), China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2001. http://hub.hku.hk/bib/B31224830.

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12

Liu, Jianbing. "Yamdrok melange, gyantze district, Xizang (Tibet), China /." Hong Kong : University of Hong Kong, 2001. http://sunzi.lib.hku.hk:8888/cgi-bin/hkuto%5Ftoc%5Fpdf?B23316822.

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13

Barton, Philip J. "Tibet and China : history, insurgency, and beyond /." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2003. http://library.nps.navy.mil/uhtbin/hyperion-image/03Jun%5FBarton.pdf.

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14

Liu, Qing. "Paléoclimat et contraintes chronologiques sur les mouvements récents dans l'ouest du Tibet : failles du Karakorum et de Longmu Co-Gozha Co, Lacs en Pull-Apart de Longmu Co et de Sumxi Co." Paris 7, 1993. http://www.theses.fr/1993PA077076.

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Cette these comprend deux parties principales : une etude paleohydrologique et paleoclimatique et une etude neotectonique. A partir des sediments lacustres des lacs de sumxi et longmu, nous avons obtenu le premier enregistrement continu des changements climatiques et hydrologiques depuis 13 ka dans le tibet occidental. Trois principaux stades evolutifs sont definis : (1) 13-10 ka, remplissage des lacs et transition climatique wurm-holocene ; (2) 10-5. 5 ka, optimum climatique et hydrologique et hauts niveaux lacustres et (3) 5. 5-0 ka, regression des lacs, et l'assechement et refroidissement climatique. L'etude neotectonique concerne deux zones de failles. Nous utilisons les informations paleoclimatiques pour estimer l'age des nombreuses structures morphologiques que ces failles decalent et deduire l'ordre de grandeur de leurs vitesses de mouvement post-glaciaire. (1) au coeur du tibet ouest, la zone de failles de longmu-gozha co, formee de trois segments principaux en echelon de direction n80e, se caracterise par un mouvement senestre avec une vitesse holocene moyenne de 8. 51. 5 mm/a. (2) a la limite sud-ouest du plateau tibetain, la faille du karakorum est sans conteste la faille majeure de la region par la rapidite de son jeu en decrochement dextre. La faille se presente comme un decrochement pur de direction n142e entre chushul et chaxi-kang avec une vitesse dextre holocene de 3510 mm/a. Au sud de chaxi-kang, la faille se divise en plusieurs branches dans le bassin en pull-apart de gar. Ces failles combinent rejet lateral dextre et rejet normal. La vitesse de decrochement est de 188 mm/a dans la direction n120-130e, accompagnee par une extension de 4. 52. 5 mm/a dans la direction n35e. Plus au sud, un systeme de failles decrochantes sub-paralleles de direction n120e borde au nord du bassin de menshi avec une vitesse holocene dextre de 3010 mm/a. L'extremite nord de la faille du karakorum est formee par l'ensemble des failles du graben de muji-tashgorgan, qui sont des decrochements dextres a composantes normales. Une vitesse dextre moyenne de 17. 57. 5 mm/a et une vitesse de mouvement vertical de 4-5 mm/a ont ete obtenues pour l'ensemble du graben. Ces resultats permettent d'affiner un modele cinematique des deformations recentes de l'ouest tibetain. Meme a une echelle inferieure de 1000 km, le comportement de cette region continentale est bien decrit par la tectonique des plaques, sur le plan quantitatif
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15

Meyer, Bertrand. "Mécanismes des grands tremblements de terre et du raccourcissement crustal oblique au bord Nord-Est du Tibet." Paris 6, 1991. http://www.theses.fr/1991PA066581.

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Le ne du plateau du tibet est une zone montagneuse de 1000 km de long, 600 km de large, limitee au sud par la faille du kunlun et au nord par la depression du desert de gobi. Cette region d'altitude moyenne 3500 m est bordee par deux decrochements senestres actifs, l'altyn tagh a l'ouest dont la vitesse de mouvement senestre est de 42 mm/an a sa terminaison orientale, et la faille de haiyuan a l'est dont la vitesse de mouvement senestre atteint 20 mm/an. Les reliefs actuels et la sismicite importante de cette region, structuree au paleozoique inferieur lors du cycle caledonien, sont dus a sa reactivation apres la collision inde-asie. Les principaux chainons montagneux nw-se, paralleles et separes par des bassins intramontagneux sont associes a des rampes crustales qui rejoignent un niveau de decollement qui s'approfondit vers le sud. Le raccourcissement fini total de cette zone est de 15688 km et suggere que le materiel non deforme sous-jacent soit resorbe par subduction continentale au niveau de la faille et de la chaine du kunlun. Les failles inverses qui construisent les reliefs ont des taux de rejet vertical de 21 mm/an et sont responsables d'une surrection regionale de 0. 20. 1 mm/an. Ces valeurs impliquent que cette region a atteint son altitude moyenne de 3500 m par rapport a la depression du desert de gobi d'altitude 1500 m en moins de 20 ma. Le bord ne du plateau du tibet peut s'interpreter comme un relais en compression d'echelle crustale qui se construit en deux decrochements actifs. En annexe, sont regroupes deux articles qui documentent les mecanismes de croissance de l'anticlinal de rampe d'el asnam
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16

Jolivet, Marc. "Cinématique des déformations au nord Tibet. Thermochronologie, traces de fission, modélisation analogique et étude de terrain." Montpellier 2, 2000. http://www.theses.fr/2000MON20202.

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Contraindre la cinematique des deformations sur la marge nord du plateau du tibet est essentiel pour comprendre l'evolution de l'ensemble du plateau. De nombreuses questions se posent sur le mode de propagation de la deformation dans la lithosphere asiatique, sur la vitesse d'exhumation des roches, sur la vitesse de formation des reliefs et sur l'age de ces derniers. Une etude thermochronologique par traces de fission, des modelisations analogiques a base de materiaux granulaires et une etude de terrain, apportent des elements nouveaux pour repondre a ces interrogations. Nous faisons la preuve que les structures heritees des episodes tectoniques paleozoiques et mesozoiques jouent un role essentiel dans la localisation de la deformation. Les traces de fission sur zircon attestent que, depuis le jurassique, l'exhumation des roches n'a pas depasse 10 km, expliquant le peu d'ages cenozoiques obtenus par les autres methodes geochronologiques. Les traces de fission sur apatite confirment l'enregistrement au nord tibet de mouvements tectoniques importants lies aux episodes d'accretion mesozoiques. Enfin, nous mettons pour la premiere fois en evidence la localisation tres precoce (vers 40 ma) de la deformation, liee a la collision inde - asie, sur les structures lithospheriques que sont les failles de l'altyn tagh et du kunlun. La deformation se generalise ensuite a toute la zone nord tibetaine des l'oligocene superieur, enregistrant une nette acceleration au miocene superieur. Ce travail demontre l'interet des traces de fission pour l'etude des phenomenes tectoniques recents et nous permet de proposer un nouveau modele tectonique du nord tibet.
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17

Anhal, Aarti. "Internationalising Tibet at the United Nations, 1950-2005." Thesis, University of Cambridge, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.613208.

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18

Wang, Weiliang, and 王維亮. "Amphibolites of the Bangong-Nujiang suture zone, Tibet." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B41897237.

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19

Bell, Marcus Antony. "The earthquake cycle of the Manyi Fault, Tibet." Thesis, University of Oxford, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.669902.

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20

Julien, Agnès. "Le statut international du Tibet : évolution ou permanence ?" Montpellier 1, 2002. http://www.theses.fr/2002MON10036.

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Actuellement, le Tibet est une " région autonome " de la Chine, et ce en vertu de la Constitution de la République populaire. Depuis des années, les Tibétains accusent la Chine d'avoir pénétré au Tibet alors que celui-ci était un état indépendant. Le problème se pose réellement depuis 1950, date de l'arrivée au pouvoir de Mao et de l'entrée de l'armée de libération populaire au Tibet. La question qui se pose alors, est de savoir si le Tibet était indépendant à l'époque des faits, or, lorsqu'on étudie son histoire, on s'aperçoit que la relation sino-tibétaine est largement basée sur un concept proprement oriental qu'est le chö-yön. Cette relation a souvent mal été interprétée et est à la base de la revendication de souveraineté de la Chine. Son droit à l'autodétermination devient un droit à l'autonomie par la force des choses et notamment en raison de la politique démographique chinoise et du transfert de population. A l'heure actuelle, sans pour autant éluder la question de son droit à l'indépendance, une réelle autonomie paraît plus appropriée.
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21

Wang, Weiliang. "Amphibolites of the Bangong-Nujiang suture zone, Tibet." Click to view the E-thesis via HKUTO, 2008. http://sunzi.lib.hku.hk/hkuto/record/B41897237.

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22

Verhagen, Pieter Cornelis. "A history of Sanskrit grammatical literature in Tibet." Leiden : E. J. Brill, 1994. http://catalogue.bnf.fr/ark:/12148/cb356106379.

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Texte remanié de: Proefschrift--Rijksuniversiteit te Leiden, 1991. Titre de soutenance : Sanskrit grammatical literature in Tibet : a study of the Indo-Tibetan canonical literature on Sanskrit grammar and the development of Sanskrit studies in Tibet.
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23

Fromentin, Libouthet Marion. "Le Tibet dans les relations internationales (1950-1971)." Nantes, 2013. http://www.theses.fr/2013NANT3027.

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Lorsqu'en 1950 la République populaire de Chine envahit le Tibet, pays indépendant de facto depuis 1911, la communauté internationale n'émet que de timides protestations. Quel est son rôle et son action, bien souvnt caractérisés par l'ambiguité, dans un conflit qui plonge ses raciens au cœur du XIXe siècle? Peut-on affirmer que le Tibet, au nom d'intérêts politiques et stratégiques qui le dépassent est un pays sacrifié pour la communauté internationale ? Victime du jeu des puissances, le pays des neiges se retrouve isolé en 1950 face à la république populaire de Chine. L'Inde, la Grande-Bretagne et les Etats-Unis assistent en toute connaissance de cause à la disparition d'un Eatta souverain. La cohabitation entre la Chine communsite et le Tibet prend brutalement fin en 1959 avec la fuite du dalaï-lama en Inde. Bien que celle-ci soit devenue le refuge de milliers de Tibétains fuyant leur pays, Nehru fait le choix de sacrifier le Tibet au nom de l'amitié sino-indienne. Le toit du monde se retrouve alors au cœur de al grande croisade menée par Washington et ses alliés contre le communisme. Cette période, caractérisée par le double langage et l'ambiguité, prend fin en 1971, lorsque l'administration de Nixon décide de se rapprocher de Pékin. La fermeture du pays pendant la révolution culturelle aidant, l'opinion, d'abord émue par le sort du Pays des neiges, finit par se désintéresser de son sort et le laisse sombrer dans l'oubli.
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24

Yang, Chao. "Geology, geochronology, stable isotope, and sulfides of the Tiegelongnan porphyry-epithermal Cu (Au) deposit, Tibet, China." Doctoral thesis, Université Laval, 2020. http://hdl.handle.net/20.500.11794/67954.

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25

Assis, Vinicius de [UNESP]. "Thangka: a pintura sagrada tibetana: tradição, história e método." Universidade Estadual Paulista (UNESP), 2016. http://hdl.handle.net/11449/141973.

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Submitted by Vinicius de Assis null (deassis.vinicius@gmail.com) on 2016-07-29T14:46:59Z No. of bitstreams: 2 THANGKA A PINTURA SAGRADA TIBETANA.docx: 18848509 bytes, checksum: 0f3bea4566b0c4667ffea6f21ff1af6f (MD5) THANGKA A PINTURA SAGRADA TIBETANA.pdf: 8432818 bytes, checksum: f357a28d3e4d03a1d5eb7cb6ce23a613 (MD5)
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O presente estudo intenta apresentar os princípios básicos, históricos e processuais, da pintura tradicional tibetana, thangka. Tal objetivo se justifica pela escassez de estudos em língua portuguesa sobre o assunto. Ainda que seja perceptível nos tempos atuais uma expansão dos estudos asiáticos no Brasil, em confluência com uma crescente aproximação e interesse pela cultura oriental na contemporaneidade; esta pesquisa, por meio de estudo de campo, levantamento bibliográfico e histórico, busca a investigação e exposição do profundo e específico âmbito do simbólico, sagrado e tradicional na pintura tibetana. Acreditando que o reconhecimento das artes e teorias estéticas não eurocêntricas corroboram a cognição e produção da inestimável diversidade cultural humana.
The following study intends to present the basic, historical and procedural principles of the traditional Tibetan painting, thangka. This objective is justified by the lack of studies in Portuguese on the subject. Although it is noticeable nowadays an expansion of Asian studies in Brazil, in confluence with a growing approach and interest in Eastern culture in contemporary society; this dissertation, by field research, literature and history, wishes to investigate, explain and expose the deep and specific scope of the symbolic, sacred and traditional in Tibetan painting. Believing that the recognition of the arts and non eurocentric aesthetic theories corroborate the cognition and production of the invaluable human cultural diversity.
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Wan, Deke. "Zang zu mu qu zheng zhi jie gou de bian qian : chong tu yu tiao shi = Change of the political structures in the Tibetan nomads areas : conflicts and adaptations /." click here to view the abstract and table of contents, 2001. http://net3.hkbu.edu.hk/~libres/cgi-bin/thesisab.pl?pdf=b16745991a.pdf.

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27

Askew, Joseph. "The status of Tibet in the diplomacy of China, Britain, the United States and India, 1911-1959." Online version, 2002. http://bibpurl.oclc.org/web/25604.

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28

Wernsdörfer, Martina. "Experiment Tibet Felder und Akteure auf dem Schachbrett der Bildung 1951 - 2003." Bern Berlin Bruxelles Frankfurt, M. New York, NY Oxford Wien Lang, 2006. http://d-nb.info/991380304/04.

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Ardley, Jane. "The Tibetan independence movement : political, religious and Gandhian perspectives /." London [u.a.] : RoutledgeCurzon, 2003. http://swbplus.bsz-bw.de/bsz261069918inh.pdf.

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30

Travers, Alice. "La noblesse thibétaine du Ganden phodrang (1895-1959) : permanences et transitions." Paris 10, 2009. http://www.theses.fr/2009PA100091.

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Cette thèse propose une étude d’histoire sociale de la noblesse tibétaine (tib. Sku drag) du Ganden phodrang (tib. Dga’ ldan pho brang), le gouvernement central du Tibet, de 1895 à 1959, par la méthode prosopographique. L’objectif est de comprendre comment cette élite administrative héréditaire a réussi à perpétuer sa domination dans cette période de mutations. Grâce à des sources orales (entretiens avec des nobles) et écrites (archives britanniques et autobiographies de nobles), des outils ont été constitués (liste des familles nobles, des bureaux de l’administration, des districts, et des titres et postes des fonctionnaires) ainsi qu’une base de données informatisée. Celle-ci permet l’analyse des deux piliers de l’identité noble, l’appartenance à un lignage et le service du gouvernement, ainsi que des différents « moyens » (éducation, forte sociabilité, commerce et investissement de la modernité occidentale) qui ont rendu possible le maintien de son capital social pendant cette période. L’étude d’un large échantillon a conduit à confirmer certaines idées déjà connues (pertinence du principe d’homogamie et division petite noblesse / haute noblesse), et au contraire à en réfuter d’autres (prépondérance de la polyandrie ou de la patrilinéarité et endogamie stricte puisqu’un renouvellement non négligeable par le mariage en dehors du groupe noble a été mis en évidence). Concernant les carrières, la thèse confirme l’absence de spécialisation des fonctionnaires, mais relativise la domination de la haute noblesse sur les hautes charges. Elle fait enfin apparaître une administration en pleine expansion, en partie patrimoniale, où les sphères privées et publiques se recoupent
This dissertation is a socio-historical investigation into the aristocracy (tib. Sku drag) of the Ganden phodrang (tib. Dga’ ldan pho brang), the central government of Tibet, from 1895 to 1959, through a prosopographical study. The aim is to understand how this hereditary administrative elite could perpetuate its domination in a period of massive changes. Oral and written sources (interviews with noble men and women, British archives and autobiographies by noble men and women) made it possible to draw up several lists (noble families, offices of the administration, and officials’ posts and titles) and to build up a database. This database provides a basis from which one can analyze the two pillars of noble identity  being of a noble lineage and in the government’s service , and the means (education, sociability, trade and privileged access to the western modernity) by which the aristocracy maintained its social capital. The study of a large sample confirms a number of known facts (relevance of the homogamy principle and strong division between high and small families), and refutes others (supremacy of polyandry and patrilineality, and strict endogamy, as a certain amount of renewal of the nobility through marriage outside of the group was brought to the fore). Regarding careers, this study confirms the absence of specialization of Tibetan noble officials but puts the domination of the high aristocrats over the higher offices into perspective, by the evidencing of a certain degree of social mobility within the aristocracy. Finally, it brings to light a fast expanding administration which is partly patrimonial, with a certain intermingling of private and public spheres
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31

Vergne, Jérôme. "Imagerie des structures et dynamique de la lithosphère de la marge nord-est du Tibet." Université Louis Pasteur (Strasbourg) (1971-2008), 2002. http://www.theses.fr/2002STR13070.

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Le plateau tibétain est un remarquable exemple de collision continentale mais les processus géodynamiques qui ont conduit à sa formation et qui gouvernent son évolution, demeurent incertains. Plusieurs concepts, faisant intervenir des modes de déformation très variés, s'opposent. En 1998, un réseau de stations sismologiques, essentiellement destiné à l'enregistrement de séismes lointains, a été déployé sur la marge Nord-Est du plateau. Cette région est considérée comme la zone où le plateau s'agrandit encore actuellement et constitue donc une cible privilégiée pour comprendre les mécanismes qui ont conduit à la construction de cet ensemble. Nous avons appliqué aux données enregistrées lors de cette expérience deux méthodes sismologiques complémentaires, la tomographie télésismique et les fonctions récepteur. Leur utilisation conjointe nous a permis de mieux caractériser la croûte et le manteau de cette région. Alors que le manteau asthénosphérique apparaît comme relativement homogène, la lithosphère, et plus particulièrement la croûte, présente des variations importantes de structure et de composition. La croûte s'épaissit en direction du centre du plateau par des "sauts'' successifs de l'interface croûte-manteau, localisés aux niveaux d'anciennes sutures mésozoi͏̈ques réactivées. Les valeurs du rapport VP/VS des vitesses sismiques révèlent des variations de la composition crustale suivant l'unité géologique considérée. Elles ne sont cependant pas en accord avec la présence d'une fusion partielle généralisée souvent invoquée. Enfin, plusieurs observations indiquent que la faille du Kunlun affecte l'ensemble de la croûte et concentre une part importante des déformations. Ce grand décrochement semble également être associé à une subduction du bloc Nord Kunlun vers le sud qui induit une fusion partielle dans le manteau et des remontées magmatiques dans la croûte. Nos résultats seraient-ils le reflet d'une tectonique des plaques cachée à l'intérieur du plateau tibétain ?
The Tibetan Plateau is a classical example of a continental collision, but the geodynamical processes that led to its formation and that govern its present day evolution remain unclear. Several conflicting concepts, involving various deformation mechanisms, have been proposed. In 1998, a network of seismic stations, essentially designed to record long distance earthquakes, was deployed across the Northeastern margin of the plateau. This region is assumed to be the part where present-day growth of the plateau takes place; it is thus the right place to understand the mechanisms that led to the formation of the plateau as a whole. We applied two complementary seismic methods, teleseismic tomography and receiver functions analysis, to the data recorded during this experiment. This joined approach helps us to better image the crust and the mantle of this area. The lithosphere, and especially the crustal part, exhibits important lateral variations in both structure and composition, whereas the asthenospheric mantle is relatively homogeneous. The crust thickens towards the centre of the plateau by successive "steps" of the crust-mantle interface, located near reactivated Mesozoic sutures. The seismic velocity ratio VP/VS indicates variations in the crustal composition depending on the considered geological unit. But these values are not in favour of widespread partial melted zones in the crust. Finally, several observations indicate that the Kunlun fault extends through the whole crust and concentrates most of the deformation. This large strike-slip fault seems also to be associated with ongoing subduction of the North Kunlun block toward the south. This inducing probably partial melt in the mantle and intrusion of magma into the crust. Our results can be seen as an indication of buried plate tectonics inside the Tibetan Plateau
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32

Guo, Jing. "2008 Tibet Riots Through a Western Lens: a Frame Analysis of News Coverage of 2008 Tibet Riots on BBC and CNN networks." Miami University / OhioLINK, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=miami1250138062.

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33

Guo, Jing. "2008 Tibet riots through a western lens a frame analysis of news coverage of 2008 Tibet riots on BBC and CNN networks /." Oxford, Ohio : Miami University, 2008. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=miami1250138062.

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34

Troughton, Thomas 1964. "Tibetan mind training : tradition and genre." Thesis, McGill University, 2008. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=116035.

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In response to Tibetan social pressures in the 11th century, Atisa initiated a renewal of Buddhist monasticism that resulted in all Buddhist praxis outside of meditation being strictly framed by attitudes and behaviors informed by love and compassion. Atisa's teachings are exemplified in pithy sayings that point to the heart of bodhisattva practice, and this mind training practice developed into a tradition in the period immediately following his passing. The success of the method, and of the emulation of Atisa as exemplar of a perfect bodhisattva, led to the adoption of mind training throughout Tibetan Buddhism. "Tibetan Mind Training: Tradition and Genre" explains the relation between a native Tibetan literary genre and monastic Buddhist practice found in the 14th century compilation Mind Training: The Great Collection (theg pa chen po blo sbyong rgya tsa). The introduction provides context and presents methodology. Chapter one argues that 'blo sbyong' should be translated as 'mind training.' Chapter two has two broad arguments: a rebuttal of a conception of mind training as an essentially psychological preparation for other practices; and an explanation of its praxis as the interaction of mind and real objects. Chapter three explains the relation of mind training praxis and tradition, with reference to Atisa's reforms. Chapter four explains some characteristics of the literary genre of mind training.
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35

Spence, Heather. "British policy and the 'developemt' of Tibet 1912-1933." Online version, 1993. http://bibpurl.oclc.org/web/26707.

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36

Leier, Andrew. "The Cretaceous Evolution of the Lhasa Terrane, Southern Tibet." Diss., Tucson, Ariz. : University of Arizona, 2005. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu%5Fetd%5F1340%5F1%5Fm.pdf&type=application/pdf.

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37

Nodari, Maria Luisa. "Climbing for the nation : epics of mountaineering in Tibet." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648226.

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38

白館, 戒雲, ཨཱ་ཙརྱ་ཁང་དཀར་ཚུལ་ཁྲིམས་སྐལ་བཟང་།།, and Tshul khrim skal bzaṅ. "A History of Logical Studies in Tibet (in Tibetan)." 名古屋大学印度学仏教学研究会, 1986. http://hdl.handle.net/2237/21033.

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39

Anand, Dibyesh. "World politics, representation, identity : Tibet in Western popular imagination." Thesis, University of Bristol, 2002. http://hdl.handle.net/1983/5858a3bf-ee85-4d17-ba68-74444581a5d5.

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40

Magnatta, Sarah J. "Portraits of the Dalai Lama in Tibet and Beyond." The Ohio State University, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=osu1396265966.

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41

Garthwaite, Matthew Campbell. "Deformation of Tibet : InSAR analysis and viscous flow models." Thesis, University of Leeds, 2011. http://etheses.whiterose.ac.uk/2611/.

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The Tibetan plateau in central Asia is a prime example of the distributed deformation that occurs in the lithosphere as a result of continental collision. Large scale lithospheric deformation can be estimated using viscous continuum models that balance the vertical stress induced by lateral variations of potential energy, and horizontal stress induced by tectonic boundary forces. I find that the 2-dimensional Thin Viscous Sheet (TVS) model gives a good approximation to deformation during continental collision, providing that the indenter half-width is greater than the lithospheric thickness. However even when this ratio approaches one, reasonable correspondence exists when the strain-rate exponent (n) of the rheological constitutive law is ≤ 3. By applying the TVS to model the contemporary deformation of Asia, I find that the first order features of the geodetically-determined velocity field can be explained. Models which can best predict the observed velocity field have n between 2 and 5 Argand numbers of between 1 and 4, and the strength of the Tibetan plateau and Tien Shan is between 3 and 8 times weaker than the foreland regions. Models with these parameters give a value of FL = 7-15x1012 N m-1 for the vertically integrated horizontal driving force on the Himalayan arc. I describe the π-rate method for determining slow linear deformation rates from Interferometric Synthetic Aperture Radar (InSAR) observations and validate it using synthetic data. When using real data, the π-rate method out-performs the conventional stacking method. The RMS difference between the two methods and observed GPS measurements are 3.7 and 7.1 mm/yr for π-rate and stacking respectively. I used the ~rate method to determine the interseismic velocity field across the Tibetan plateau in an approximately north-south orientated, ~1000 km-long swath using ESA Envisat data spanning a period of 6.23 years. The resulting InSAR rate map indicates a factor of 2 variation in the magnitude of line-of-sight (LOS) velocity between the latitudes of 29-40oN. Significant localisation of deformation around mapped fault zones is not observed. A deviation of up to 8 mm/yr in LOS between the InSAR rate map and GPS-derived horizontal velocity field suggests either ~8 mm/yr of vertical uplift, an additional ~20 mm/yr of eastward motion, or a combination of horizontal and vertical motion that has not been measured using horizontal-component campaign GPS data. Comparison of InSAR and GPS observations with predictions of kinematic block and viscous continuum models suggests that the latter provides a more useful description for large-scale continental deformation.
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42

Clair, Erin Joy. "Spatial Dynamics of the Earliest Human Occupants of Tibet." Thesis, The University of Arizona, 2012. http://hdl.handle.net/10150/243883.

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My research, conducted summer 2011, was undertaken to obtain a better understanding of how, when, and why prehistoric peoples initially extended their range up from the lower elevation valleys of northern India and Tibet to the 4,000 – plus - meter elevations of the Tibet Plateau. Recent archaeological research headed by Professor John W. Olsen in western Tibet suggests multiple routes onto the Plateau at different times in prehistory. My research focused on: 1) conducting reconnaissance for ancient sources of raw stone material and 2) examining ancient river terrace and lake shoreline formations to determine the timing and directionality of human movement onto the plateau. We identified new sites to help reconstruct prehistoric land - use patterns in one segment of the Yarlung Zangbo as a hypothetical model for understanding population dynamics on a larger geographical scale. Global positioning systems (GPS) data allowed me to generate hypotheses of prehistoric land - use in south - central Tibet that can be tested in future field seasons against archaeological and spatial data collected over a larger region. This thesis aims to examine data collected during summer field seasons with well - documented geographic locations of sites, archaeological evidence, and research to understand migration onto the Tibet Plateau.
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43

Lu, Xuan. "La question tibétaine et ses deux principales solutions depuis les années 1980." Thesis, Paris 4, 2010. http://www.theses.fr/2010PA040214.

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Cette thèse est consacrée à l’étude de la question tibétaine et des différents aspects sous lesquels elle est traitée : géographique, économiques, stratégiques et politiques. Nous étudions l’évolution des attitudes et les divergences d’opinion selon une polarisation allant du conservatisme au progressisme. Nous en mesurons les influences dans l’histoire récente et nous projetons les développements probables à court et moyen termes.- Cette thèse s’attache à démontrer que le Tibet reste un enjeu important pour la Chine et qu’à ce titre, la ligne de chemin de fer reliant le Qinghai au Tibet symbolise la politique et la solution chinoise vis-à-vis du Tibet. - Cette thèse s’attache à démontrer que le dalaï-lama est toujours considéré par les tibétains comme la seule instance à même de pouvoir résoudre les problèmes tibétains, et ceci en dépit des nombreuses crises auxquelles le chef spirituel a pu être confronté.- Enfin, cette thèse s’attache à démontrer que la société chinoise est en train d’évoluer vers une attitude plus progressiste. Sur cette question notamment, les intellectuels chinois ont acquis davantage d’influence que par le passé, influence qui pourrait, à l’avenir, se développer davantage. Ce travail, relevant d’un champ d’analyse pluridisciplinaire, couvre l’essentiel du XXème siècle et de l’époque actuelle. Il se focalise particulièrement sur la période postérieure aux années 1980, qui a été le témoin d’une internalisation plus poussée de la question tibétaine
This thesis focuses on the Tibetan issue in its various aspects: geographic, economic, strategic and political. We examine the evolution of attitudes and differences of opinion according to their polarization ranging from conservatism to progressivism. We assess their influences in recent history and we project the likely developments in the near future.- This thesis aims at showing that Tibet remains an important matter at stake for China. Hence the Qinghai-Tibet rail link embodies the Chinese national policy as well as the Chinese solution vis-à-vis Tibet.- This thesis aims at demonstrating that the Dalai Lama is still regarded by Tibetans as the key to the resolution of Tibetan problems despite the many crises the spiritual leader has had to face.- Finally this thesis aims at pointing out that the Chinese society is evolving towards a more progressive attitude. On this issue Chinese intellectuals have acquired more influence than before and this influence could develop even further in the future. This work belongs to an inter-disciplinary field of study and covers most of the 20th century and present times. It focuses especially on the post 1980’s period when the Tibetan issue became more international
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44

Ho, Hoi-to Lucas, and 何海濤. "The Nielaxiongbo metamorphic core complex and its associated granites,in Southern Tibet." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2002. http://hub.hku.hk/bib/B30252052.

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45

Rui, Yichao. "Soil Carbon, Nitrogen and Phoshorus Dynamics in Response to Warming and Grazing in Alpine Meadow Ecosystem of the Tibet plateau." Thesis, Griffith University, 2013. http://hdl.handle.net/10072/366008.

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Ongoing global climate change is predicted to substantially impact on terrestrial ecosystems. The Qinghai-Tibet plateau is very sensitive to climate change. Alpine meadows, one of the major ecosystems on the Qinghai-Tibet Plateau, is very vulnerable and can be sensitive to both climate change and human disturbance. Grazing is the main land use mode of the alpine meadow ecosystem. Soil carbon (C), nitrogen (N), and phosphorus (P) availability are key to ecosystem productivity, while the alterations in soil C, N and P dynamics can affect ecosystem substantially. Investigation on the response of soil C, N and P cycling and the associated functional microorganisms in the alpine meadow can provide insights into soil function under warming and grazing conditions and sustainable management of the ecosystem. In this thesis, the study was conducted based on a controlled warming-grazing experiment in the Haibei Alpine Meadow Ecosystem Station, Chinese Academy of Sciences (CAS). A free-air temperature enhancement (FATE) system and a moderate grazing intensity were applied to simulate the effects of warming and grazing. Four treatments including no warming with no grazing (NWNG), no warming with grazing (NWG), warming with no grazing (WNG) and warming with grazing (WG) were applied.
Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Biomolecular and Physical Sciences
Science, Environment, Engineering and Technology
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46

Pritzker, David Thomas. "Canopy of everlasting joy : an early source in Tibetan historiography and the history of West Tibet." Thesis, University of Oxford, 2017. http://ora.ox.ac.uk/objects/uuid:f231f283-1711-4428-820d-0c2ccfa11f5f.

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A more descriptive title for the dissertation might be "Early historiography in Purang-Guge and its relationship between orality, kingship, and Tibetan identity: a close study of a recently uncovered 12th century historical manuscript from Tholing monastery in West Tibet." The present study is therefore a close textual analysis of all the outer and inner features of the Tholing Manuscript. When reading the text, there is the gradual realization that the archaic peculiarities in script, binding, spelling, vocabulary, prose, and narrative twists, all highlight the work as a wholly rare and different version from those early histories typically found in Central Tibet. The key difference lies primarily in the focal point of the narrative. Whereas most similar narratives from the time of the phyi dar (11th-13th centuries) onwards place at the core of their structure the history of Buddhism in Tibet, the Tholing text puts as its central focus kingship and the history of kings in Tibet. For this reason, while Buddhism plays an essential and integral part of the story as a whole, the text can be viewed as a more secular work then any comparable monastic history of the period. The narrative structure of the manuscript, with its heavy use of rhythmical prose, similes, archaic topoi and motifs, is hauntingly familiar to those parallel passages found among Old Tibetan Documents and is emblematic of the liminal period in which the text was written. At this time, histories were transitioning from disperse and possibly oral transmissions to predominantly formal organized written traditions. The poetic nature of the text, together with its unusual physical features, raises questions relating to its purpose and function, with the possibility of its use as a ritual manuscript for royal legitimization. Through a close study of the text, I offer some insights on the formative nature of early Tibetan historiography in establishing the sacred and political power of the kings of West Tibet.
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47

Kaufmann, Wolfgang. "Das Dritte Reich und Tibet die Heimat des "östlichen Hakenkreuzes" im Blickfeld der Nationalsozialisten." Ludwigsfelde Ludwigsfelder Verl.-Haus, 2008. http://d-nb.info/1000655393/04.

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48

Spengen, Willem van. "Tibetan border worlds : a geo-historical analysis of trade and traders /." [Netherlands] : W. van Spengen, 1992. http://catalogue.bnf.fr/ark:/12148/cb35766825h.

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49

Verhagen, Pieter Cornelis. "Sanskrit grammatical literature in Tibet : a study of the Indo-Tibetan canonical literature on Sanskrit grammar and the development of Sanskrit studies in Tibet /." [Leiden?] : P. C. Verhagen, 1991. http://catalogue.bnf.fr/ark:/12148/cb35502127q.

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50

Guidoni, Rachel. "Les reliques dans le monde tibétain." Paris 10, 2006. http://www.theses.fr/2006PA100165.

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En s'appuyant sur des sources textuelles et des matériaux de terrain, cette étude vise à décrire les représentations et les usages des reliques dans l'aire de langue et de culture tibétaines. La première partie situe la catégorie des reliques dans des cadres de référence plus larges. Elle rappelle la place des reliques dans les trois monothéismes, les concepts relatifs à la mort dans les mondes indien, centralasiatique et chinois, ainsi que les traditions bouddhiques relatives aux reliques telles qu'elles figurent dans les sources canoniques. La deuxième partie présente la catégorie des reliques dans le monde tibétain. Elle décrit les concepts relatifs à la mort des saints, les types d'obsèques qui leur sont appliqués, les modalités de recueil des reliques, leur terminologie, leurs spécificités et leurs typologies. La troisième partie décrit les modalités de circulation des reliques, leurs bienfaits et leurs usages. Les textes décrivent les bienfaits, tandis que les usages sont surtout documentés par les données de terrain. La tradition tibétaine des reliques se caractérise par sa diversité, que ce soit dans sa terminologie, ses typologies ou ses usages
Based on literary sources and fieldwork materials, this Ph. D. Thesis aims at describing the traditions concerning the relies all over the Tibetan cultural area. The first part aims at placing the category of relies in a broader context. It reminds of the place of relies in the three monotheisms, the concepts on death in the Indian, Central Asian and Chinese civilizations, and of the Buddhist traditions on relics as they are mentioned in canonicate sources. The second part presents the category of relies in the Tibetan culture. It describes conceptions on saints' death, funerals which are applied to them, the different circumstances in which relies may be collected, their terminology, properties and classifications. The third part describes the ways relies may be put into circulation, their benefits and uses. Textual sources are mainly concerned with benefits, whereas uses are mostly documented by fieldwork materials. The Tibetan tradition of relies is remarkable through its diversity, be it the terminology, the classifications or the uses of these sacred objects
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