Дисертації з теми "Bassus"
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Bühler, Daniel. "Macht und Treue Publius Ventidius ; eine römische Karriere zwischen Republik und Monarchie." München Allitera-Verl, 2008. http://d-nb.info/995358613/04.
Повний текст джерелаAstafan, Lauren Elizabeth. "Pagans, prefects, and emperors : a reexamination of the sarcophagus of Junius Bassus." Honors in the Major Thesis, University of Central Florida, 2010. http://digital.library.ucf.edu/cdm/ref/collection/ETH/id/1345.
Повний текст джерелаBachelors
Visual Arts and Design
Arts and Humanities
Art History
Masini, Emmanuel. "L' évolution tectono-sédimentaire syn-rift des bassins de marge passive profonde : Exemples du bassin de samedan (Alpes centrales, Suisse) et du bassin de Mauléon (Pyrénées basques françaises)." Strasbourg, 2011. https://publication-theses.unistra.fr/public/theses_doctorat/2011/MASINI_Emmanuel_2011.pdf.
Повний текст джерелаOne of the most effective geodynamical processes creating sedimentary basins is the continental rifting. Investigations performed in deep magma-poor rifted margins showed that the crust can be extremely extended and associated with low-angle detachment faulting. Therefore, the tectono-sedimentary models developed for classical hemigrabens of the most proximal domains of the margins cannot be applied to the distal margins. Unfortunately, due to access issues, this evolution remains poorly understood. This is the aim of this study focused on two fossil analogues (Alps and Pyrenees). Palinspastic restoration helped to restore the post-rift architecture of this type of basins preserving their syn-rift sedimentary record. This study shows that supra-detachment basins are controlled by the detachment faults flooring rift-basins. They are bounded by structural elements resulting from the hangingwall delamination during active exhumation (allochthons or detachment breakaway blocks). A syn-rift trilogy evolution can be observed as: 1) Onset of exhumation, with the hangingwall rupture during the basin opening over the exhumed fault plane. Deposition of hangingwall-derived basal facies tract. 2) Widening of the basin accommodated by the upstream footwall exhumation controls a source change to footwall derived deposits. 3) Tectonic cessation through the basin leads to develop the post-tectonic sequence consisting of passive infilling. Because of the cessation of active exhumation as the engine of the syn-rift gravity flows along the fault, this sequence is strongly dependent of a potential incoming sediment flux and its efficiency compare to post-tectonic space accommodation
Bassil, Bassem S. [Verfasser]. "Transition metal containing silico- and germanotungstates / Bassem S. Bassil." Bremen : IRC-Library, Information Resource Center der Jacobs University Bremen, 2008. http://d-nb.info/1034983091/34.
Повний текст джерелаCamus, Etchecopar Argitxu. "A historical comparative study of Basque institutions in the United States /." abstract and full text PDF (UNR users only), 2008. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:3329565.
Повний текст джерела"August 2008." Includes bibliographical references (leaves 393-410). Library also has microfilm. Ann Arbor, Mich. : ProQuest Information and Learning Company, [2009]. 1 microfilm reel ; 35 mm. Online version available on the World Wide Web.
Menetrier, Cédric. "Modélisation thermique appliquée aux bassins sédimentaires : Bassin de Paris (France) et Bassin de Sabinas (Mexique)." Nancy 1, 2005. http://www.theses.fr/2005NAN10205.
Повний текст джерелаAzcona, Pastor José Manuel. "Los paraísos posibles : historia de la emigración vasca a Argentina y Uruguay en el siglo XIX /." Bilbao : Universidad de Deusto, 1992. http://catalogue.bnf.fr/ark:/12148/cb36668582z.
Повний текст джерелаGUILLEMOT, HERVE. "Modelisation 3d des traumatismes lateraux du bassin : validation sur bassins humains." Rennes 1, 1993. http://www.theses.fr/1993REN1M087.
Повний текст джерелаEcheverria, Begoña. "Basque schooling : what is it good for? /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC IP addresses, 2000. http://wwwlib.umi.com/cr/ucsd/fullcit?p9984812.
Повний текст джерелаGarcía, Giráldez Teresa. "La emigración vasca a Centroamérica, 1750-1800 las redes familiares como estructuras de poder en Guatemala /." Madrid : Ed. de la Universidad autónoma de Madrid, 1994. http://catalogue.bnf.fr/ark:/12148/cb39092562w.
Повний текст джерелаLa couv. porte en plus : "Facultad de filosofía y letras, historia moderna" Bibliogr. p. 539-570. Résumés en espagnol et en anglais.
Peterson, Alissa. "Traditions in transition : Basques in America /." [Boise, Idaho] : Boise State University, 2009. http://scholarworks.boisestate.edu/td/31/.
Повний текст джерелаGirou, Olivier. "Séquestration géologique du CO₂ dans les Basses-Terres du Saint-Laurent : impacts hydrogéologiques à l'échelle du bassin." Doctoral thesis, Université Laval, 2017. http://hdl.handle.net/20.500.11794/27562.
Повний текст джерелаGeological carbon sequestration is a technology aiming at transferring CO₂ from industrial facilities to geologic reservoirs, insulating the sequestered gas from the carbon cycle, allowing to reduce anthropic greenhouse gas emissions. In the province of Quebec, the most promising geological structure for carbon capture and storage is the St. Lawrence Lowlands sedimentary basin. This basin contains saline aquifers in which it is potentially possible to store several billion tons of CO₂. These aquifers are overlain by thick impervious caprocks, the Utica and Lorraine shales, preventing vertical migration of CO₂ toward the surface. However, such an injection implies that hydrogeological impacts of injection may be transmitted within the entire basin as pressure builds up, which may lead to water table rise in unconfined aquifers, and horizontal and vertical brine leakage from the reservoir to freshwater aquifers. The main objective of this thesis is to assess potential hydrogeological impacts of CO₂ sequestration at the basin scale in the St. Lawrence Lowlands basin. In order to assess these impacts, the permeabilities of the Paleozoic formations have been evaluated by reinterpreting the raw data of drillstem tests that have been conducted in the basin, during hydrocarbon exploration campaigns. These results have been integrated into a core plug analysis database to create a hydrostratigraphic model of the units and a conceptual flow model of the basin. Subsequently, a 3D geological model of the St. Lawrence Lowlands basin has been modified to incorporate faults and has been imported into the FEFLOW numerical model to simulate the injection of CO₂ in the basin. The simulations demonstrate the role played by faults, which divide the basin into multiple compartments and limit the pressure buildup across the basin. Simulations show that two wells located in two different compartments are enough to maintain an injection rate of 10 Mt/yr eq. CO₂ during a hundred years without generating hydrogeological impacts. Due to the significant uncertainty that affects parameter values, a sensitivity analysis has been undertaken to define a set of conditions that allow hydrogeological impacts to occur at the basin scale. This analysis has shown that only under very unfavorable conditions, in which faults and the top aquifer have a high hydraulic conductivity and the top boundary of the domain is a no-flow boundary condition, a watertable rise ranging from 1 to 18 meters may occur, depending on the specific yield of the uppermost formations. The sensitivity analysis has also shown that the specific storage is an important hydrodynamic parameter explaining pressure buildup within the basin, but is also the most uncertain parameter. Simulations have shown that brine leakage to the surface is unlikely. Faults, which have a low hydraulic conductivity, also tend to lower the risk of horizontal brine leakage. However, vertical brine leakage to the surface is possible through the damaged zones surrounding fault cores. Numerical analysis has shown that the storage coefficient, the specific yield of surface formations, the permeability and proximity to the surface of faults have to be better defined for better predicting the impacts of CO₂ injection in the basin. The simulations conducted during this thesis present an original approach, favoring detailed geological characterization of the basin over an exhaustive simulation of physical phenomena.
Wassara, Samson Samuel. "Le regime juridique international du bassin du nil : comparaison avec d'autres bassins fluviaux." Paris 11, 1994. http://www.theses.fr/1994PA111005.
Повний текст джерелаThe scarcity of fresh water, arising from many factors, constitues a major source of conflicts among riparian states. This problem is particularly sensitive to legal and political relations as far as countries of the nile basin are concerned. The states of this river basin have not been able to establish a comprehensive approach to cooperation in order to solve those conflicts connected with the need to share water and its ressources. The idea of an integrated approach to development of shared water resources is rather doubtful in the nile basin. In this respect, it becomes necessary to examine those problems that hamper cooperation by resorting to the study of the contemporary legal instruments regulating the management of water resources shared by two or several states. The experience of cooperation between some riparian states could help in improving the existing structure of cooperation in the nile basin as well as all those relations that emanate from it
Chaussier, Jean-Daniel. "Quel territoire pour le Pays Basque ? : les cartes de l'identité /." Paris : Éd. l'Harmattan, 1996. http://catalogue.bnf.fr/ark:/12148/cb366880077.
Повний текст джерелаMA, ZHONG CAI. "Modelisation du transfert des nitrates : du bassin de recherche au grand bassin (exemples des bassins de melarchez et de la charente)." Université Louis Pasteur (Strasbourg) (1971-2008), 1991. http://www.theses.fr/1991STR13020.
Повний текст джерелаNeurdin-Trescartes, Jacqueline. "Le remplissage sédimentaire du bassin néogène du Chélif, modèle de référence de bassins intramontagneux." Pau, 1992. http://www.theses.fr/1992PAUU3021.
Повний текст джерелаMartinez-Angeles, Raymundo. "Cartographie des bassins pétroliers par traitement numérique d'image : exemple du bassin de Chihuahua (Mexique)." Nice, 1989. http://www.theses.fr/1989NICE4323.
Повний текст джерелаLEBRETON, MARIE-LUCE. "Les bassins stephano-permiens du sud du bassin de paris : controle structural et sedimentologique." Paris 11, 1990. http://www.theses.fr/1990PA112227.
Повний текст джерелаLe, Gouche Chloé. "Sédimentation de la matière organique dans les bassins profonds : cas du Bassin Arctique à l'Eocène." Thesis, Rennes 1, 2017. http://www.theses.fr/2017REN1S025/document.
Повний текст джерелаThe continental organic matter deposited in the deep basins is little described and represents a definite interest for the petroleum industry. Understanding the sedimentary processes that allow the deposit and preservation of this organic material of terrestrial origin in the deep basins is fundamental. During the Palaeogene, a period of glacial transition to icehouse, the Mackenzie Delta, located in the Arctic Basin, receives and maintains continental organic matter from the continent. What is the stratigraphic and climatic context that made possible the export of continental organic matter? Initially, the sedimentary study of the basin showed a mixed mixture dominated by the fluviatile process, with less influence of the process of storms and tides. This model of facies associated with the study of the logs of wells available in the zone made it possible to propose a model of electrical appliances of the wells of the basin and to characterize the sedimentary sequences of the delta to evolve over time and to demonstrate its migration to Beginning of the Paleogene in response to the establishment of the Brooks and Rocky Ranges. Despite the contradictory biostratigraphic constraints that had to be re-evaluated and poor quality seismic data and strongly impacted by the contemporary deformation of the Brooks chain, it is possible to propose a stratigraphic and sedimentological division along two land-sea transects. Paleogeographic series of the Mackenzie Delta. The sedimentary study of the basin showed the presence of influence of the tidal process in the internal zone of the Arctic Basin. The common presence of pollen from Avicenna and Nypa showed the existence of a mangrove well established in the Arctic domain during the Palaeogene with associated temperatures of at least 18-20 ° C. The deposits of organic matter are in the Almost all of continental origin of the Mackenzie Delta. This organic matter is of two types: (1) deposits of coal deposited during the period when the mangrove develops and (2) deposits formed by association of plant debris and amorphous organic matter and deposited under reducing conditions under the water interface -sediment. These deposits of organic matter are the most important at the end of the prograding sequences in the facies of the deltaic plain. A positive correlation was found between the increase in OCD and the increase in detrital inputs in the delta, as well as between deposits of coal and illite. On the other hand, no correlation between the second type (organic debris + MO amoprhe) of organic matter and the clayey cortege could not be demonstrated. From the comparison of organic matter deposits in the Mackenzie Delta and Lomonosov Ridge, the sedimentation rate and anteriority appear to be key parameters in sedimentation conditions and especially in the preservation of organic matter according to l Oxygenation of the medium. Moreover, Lomonosov's Ride presents itself as a guest in a home where it is permitted to remain in semi-emerged position during the Paleogene
Blanc-Valleron, Marie-Madeleine. "Les formations paléogènes évaporitiques du bassin potassique de Mulhouse et des bassins plus septentrionaux d'Alsace /." Orléans : Ed. du BRGM, 1991. http://catalogue.bnf.fr/ark:/12148/cb35518158n.
Повний текст джерелаKong, A. Siou Line. "Modélisation des crues de bassins karstiques par réseaux de neurones. Cas du bassin du Lez (France)." Phd thesis, Université Montpellier II - Sciences et Techniques du Languedoc, 2011. http://tel.archives-ouvertes.fr/tel-00649103.
Повний текст джерелаBlanc-Valleron, Marie-Madeleine. "Les Formations paléogènes évaporitiques du bassin potassique de Mulhouse et des bassins plus septentrionaux d' Alsace." Université Louis Pasteur (Strasbourg) (1971-2008), 1990. http://www.theses.fr/1990STR13113.
Повний текст джерелаKong, A. SIou Line. "Modélisation des crues de bassins karstiques par réseaux de neurones. Cas du bassin du Lez (Hérault)." Thesis, Montpellier 2, 2011. http://www.theses.fr/2011MON20070/document.
Повний текст джерелаKarst is one of the most widespread aquifer formations in the worlds. Their exploitation provides fresh water to practically 25% of the global population. The high level of structure heterogeneity in these aquifers however makes them complex and their behavior is difficult to study, simulate and forecast.Artificial neural networks are machine learning models widely used in surface hydrology since the 90's thanks to their properties of parsimony and universal approximation.In this thesis, artificial neural networks are used to study karst aquifer behavior. Application is done in the Lez. This aquifer situated near Montpellier conurbation (400 000 inhabitants) provides fresh water for a large part of this population.First, a “classical” black box neural network is applied to simulate and forecast Lez spring discharge. A rainfall input selection method is proposed, using cross correlation analysis and cross validation method at the same time. Results show neural model efficiency in order to simulate and forecast the spring discharge of a complex karstic aquifer. The model was tested using two hydrologic cycles including the two most intense floods of the database. Hydrographs shows that neural model was able to extrapolate the maximum flood discharge of the learning database. Forecasting is satisfactory until a one-day horizon.In a second time, extraction of the knowledge data included in the black box is proposed. In order to constrain the model to give physically plausible solution, a priori knowledge about aquifer geology is included into the network architecture. KnoX (Knowledge eXtraction) method proposed in this study aims at extract geological zone contributions to the Lez spring and corresponding response times. The KnoX methodology was applied to a fictitious hydrosystem built using a model with controlled parameters, in particular contributions of subbasin to the outlet and lag time of each subbasin. This application permitted to validate the KnoX methodology. Results obtained on the Lez basin are satisfactory and agree with current knowledge about this hydrosystem. In addition, the KnoX methodology allows to refine this knowledge, in particular concerning delayed infiltration because of infiltration in perched aquifer and concerning Lez spring alimentation basin boundaries. Lastly the KnoX methodology is a generic methodology that can be applied on any basin with available discharge and rainfall data
Podkhlebnik, Yvette. "Subsidence et régime thermique des bassins intracratoniques et des marges continentales passives = Subsidence and thermal regime of intracratonic basins and continental passive margins /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1992. http://theses.uqac.ca.
Повний текст джерелаPhilipp-Muller, Aviva. "Differentiating Subjective and Structural Moral Bases of Attitudes: Two Separable Constructs." The Ohio State University, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=osu152482636205763.
Повний текст джерелаPettex, Emeline. "Ecologie alimentaire du Fou de Bassan Morus bassanus en Atlantique Nord à des échelles spatio-temporelles multiples." Phd thesis, Université Montpellier II - Sciences et Techniques du Languedoc, 2011. http://tel.archives-ouvertes.fr/tel-00825001.
Повний текст джерелаHutcheon, Nicholas R. ""Basques are born wherever they want" : a qualitative study of intra-state immigrants in Basque nationalist movements." Thesis, University of Leeds, 2015. http://etheses.whiterose.ac.uk/9965/.
Повний текст джерелаNguyen, Cong Nghia. "Restauration des propriétés mécaniques originelles des sédiments repris en glissements synsédimentaires (slumping)." Paris, ENMP, 2006. http://www.theses.fr/2006ENMP1459.
Повний текст джерелаThe sedimentary modification in form of synsedimentary slumping is a witness of long-term geodynamic evolution of a sedimentary basin. This study of the Vocontian Basin (South-East of France), in paleogeographic context of submarine valley, tried to highlight the role of the initial properties of sediment in the phenomenon of submarine sliding. Main part of accomplished works concerns limestone-marl alternations and their modifications (slumps) during Hauterivian, particularly in the region of Serres. The biostratigraphy of slumps was accomplished due to the abundance of ammonites. To characterize the original lithology of the slice affected by sliding, a representative composite section was constructed from different sections exempt from slumps. The correlation between this composite and the section of Serres-Montclus, followed by an interpretation at time, allowed to differentiate on one hand two types of the slided material (very marly alternation and alternation rich in limestone), and on the other hand to suggest that climatic changes cause a indirect condition favourable to the generation of slidings (cycles of Milankovitch). The heterogeneity of the slided mass and internal structures in slumps underlined a mechanism of disintegration by shearing in marly layers. However, the presence of intact blocks testifies an incomplete disintegration. An initial configuration of the affected slice was restored by a decompaction. Basic elements for a geomechanic modelling of the behaviour of a heterogeneous massif with limestone-marl alternation, were set up. .
GRUNER, LAURENT. "Les hemorragies digestives basses." Lyon 1, 1990. http://www.theses.fr/1990LYO1M373.
Повний текст джерелаLekumberri, Terexa. "Femmes basques et société contemporaine : rupture et continuité : étude menée en Pays Basque intérieur : Baigorri et ses environs." Bordeaux 2, 1990. http://www.theses.fr/1990BOR21011.
Повний текст джерелаAlthough she has kept, by tradition, a comparative equality of rights within the structure of the "etexe" (home), the rural basque woman, in her masked plurality and dialectic, has hardly ever been treated by researchers as a principal theme. Paradoxically irreplaceable and belittled, ignored in her motherhood, divided between her traditional values and those of the surrounding domineering world, she is now searching for her new identity. History, access to a career and to knowledge, the rupture of the family unit, come to gradually define a new space for the woman as a wife, as a sexual being, as a mother. Old fashioned mentalities but also assimilation, isolation and loss of her cultural identity are still obstacles. But they are being overcome thanks to an astonishing reconciliation with the past, sometimes through nationalistic claims and often through day-to-day involvement in favour of an inherited but modernised culture
POLAND, ROWAN ELISABETH. "Histoire thermique et hydrogeologique des bassins sedimentaires. Cas du bassin de l'illinois, usa, et du district de l'albigeois." Paris 6, 1998. http://www.theses.fr/1998PA066596.
Повний текст джерелаBourlon, Nicolas. "Développement durable et gestion des bassins hydrographiques : Conception et mise en place d'Agences de bassin en Amérique latine." Rouen, 1997. http://www.theses.fr/1997ROUES089.
Повний текст джерелаBenammi, Mouloud. "Etude biochronologique et magnétostratigraphique des bassins continentaux néogènes du Maroc (bassin d'Ai͏̈t Kandoula et formation du Jebel Rhassoul)." Montpellier 2, 1997. http://www.theses.fr/1997MON20087.
Повний текст джерелаGajurel, Ananta Prasad. "Etude sédimentologique et géochimique (isotopes stables) des bassins synorogéniques de l'Hymalaya du Népal (Siwaliks et bassin de Kathmandu)." Université Joseph Fourier (Grenoble), 2006. http://www.theses.fr/2006GRE10102.
Повний текст джерелаThe work deals with paleo-environmental study of the Siwalik foreland basin (upper Miocene) and the intermountain Kathmandu basin (Plio-Pleistocene). O and C composition of modern mollusks and waters of Ganga Plain and intermountain basins were realized as a reference for paleo-environmental study. The δ18O of rivers varies from -18‰ in north of Himalaya to -4‰ in the plain. The δ18Ocar of modern shell show an equilibrium fractionation with the river waters (20 to 25°C). Both carbonate and river water values are different according to catchment basin extension. The δ13CDIC of rivers are higher than δ13Ccar due to organic carbon incorporation in shell. In the Siwaliks, 18Ocar varies from -16. 4 to 0. 6‰. For the Late Miocene, the δ18Ocar values are lower than Pliocene and modern values. Therefore, rivers running through the Siwalik plain should show different geometry. The δ13C show a sharp increase up to 0‰ around 5 Ma, which seems to be linked to the contemporaneous evolution of C4 plant. The Kathmandu Basin (3-0 Ma) is a transported basin and characterized by fluvio-lacustrine sediments. The evolution of lake is controlled by tectonic, landslide and debris-flow. The δ18Ocar older than 1 Ma vary from -11 to -4‰ and are compatible with river water (-10. 1 to -7‰) as well as monsoon water (-18 to 2‰) in Kathmandu. In contrast δ18Ocar of Gokarna Formation (< 50 Ka) is extremely high (-2. 4 to 8‰) and is compatible to dry period meteoric water (-6. 5 to 7. 5‰). Such values are generally associated with diatomite. Two processes could be interacted for diatomite time: reduction in summer precipitation and strong evaporation; both phenomena tend to make a strong concentration in 18O
Droux, Jean-Philippe. "Hydrologie et flux de matieres solides particulaires et dissoutes sur petits bassins versants du bassin du fleuve niger au mali. (bassins du dounfing, de djitiko et de belekoniʿ". Université Louis Pasteur (Strasbourg) (1971-2008), 1999. http://www.theses.fr/1999STR1GE01.
Повний текст джерелаPaquet, Fabien. "Evolution morphostructurale des bassins de marge active en subduction : l'exemple du bassin avant arc de Hawke Bay en Nouvelle-Zélande = Morphostructural evolution of active subduction margin basins : the example of the Hawke Bay forearc basin, New Zealand /." Rennes : CNRS, Université de Rennes, 2008. http://library.canterbury.ac.nz/etd/adt-NZCU20080225.224857.
Повний текст джерела"Thése de Doctorat de l'Université de Rennes 1 réalisée en co-tutelle avec l'Université de Canterbury (Christchurch, Nouvelle-Zélande)." "Soutenue le 9 novembre 2007." Includes bibliographical references. Also available via WWW.
Angrand, Paul. "Évolution 3D d'un rétro-bassin d'avant-pays : le Bassin aquitain, France." Thesis, Université de Lorraine, 2017. http://www.theses.fr/2017LORR0227/document.
Повний текст джерелаForeland basins develop in front of orogens by flexure of the lithosphere. When they initiate over a crust that has been affected by a previous tectonic event, structural and thermal inheritance have a fundamental role in their evolution and different sources may contribute to basin subsidence. The present work analyzes the impact of inheritance from a rifting event on a foreland basin, which develops while thermal reequilibration has not been achieved at the time of loading. The Aquitaine Basin is the Pyrenean retro-foreland basin that developed from Campanian to Miocene. The Pyrenean orogenesis follows an Aptian-Cenomanian rifting during which the continental crust is thinned and sub-continental mantle exhumed. The orogenesis starts only 10 Myr after the end of rifting. The effects of crustal inheritance due to rifting on the evolution of the basin are studied by analyzing crustal structures, flexural behavior of the European plate, and foreland succession distribution. The subsidence evolution of the basin is studied by the 1D backstripping technique using borehole data. Finally, inversion mechanisms of the European margin are studied by cross-section construction and restoration at crustal scale. This study helps to define the role of rift inheritance on the initiation and the evolution of a retro-foreland basin, as well as the relative role of subsidence sources and their variations in space and time. The present work also shows the strong relationship between the retro-foreland basin's history and both mechanism and the history and mechanisms of inversion of a hyper-extended margin
Lacroix, Isabelle. "Actions militantes et identités basques : trajectoires d'engagement, socialisations militantes et constructions identitaires dans les organisations nationalistes (et non-nationalistes) au Pays basque français." Versailles-St Quentin en Yvelines, 2009. http://www.theses.fr/2009VERS007S.
Повний текст джерелаWhat kind of process brings an individual, in the French Basque Country, to become involved in a group of activists and to claim a position on “Basque identity”, different from that of other groups? To study the influence of socio-cultural trajectories and institutional memberships on individuals’ worldviews, the dissertation focuses on Nationalist actors and their “field of commitment” which is structured by various militant organisations (cultural, political, economical, unionist). Combining biographical interviews, documentary analysis and participant observation, the dissertation wishes to depart from approaches of nationalism that are confined to the sole analysis of ideology. It draws upon theories of collective action that take into consideration the processual dimension of activist engagement and its “organisational shapings”. After examining the struggles between nationalists and non-nationalists and between nationalists themselves for the appropriation and the definition of a “Basque” space, the universes of socialisation that have brought individuals to an involvement in the “Basque cause” are described. Then, the dissertation proceeds to explicate the norms that help maintain the commitment of nationalist activists by means of organisational systems and rituals. Their study unsettles notions of the criteria generally associated with belonging to the “Basque” group
Leamer, Micah J. "Groebner Finite Path Algebras." Thesis, Virginia Tech, 2004. http://hdl.handle.net/10919/9998.
Повний текст джерелаMaster of Science
Prijac, Christophe. "De la subsidence tectonique à la subsidence thermique d'un bassin intracratonique : application à l'histoire méso-cénozoi͏̈que du bassin de Paris." Rennes 1, 1999. http://www.theses.fr/1999REN10071.
Повний текст джерелаCastro, Maria Clara. "Transfert des gaz rares dans les eaux des bassins sédimentaires." Paris 6, 1995. http://www.theses.fr/1995PA066040.
Повний текст джерелаDemongodin, Lionel. "Reconnaissance de l'état thermique des bassins sédimentaires : transferts de chaleur par conduction et convection : application au Bassin de Paris." Montpellier 2, 1992. http://www.theses.fr/1992MON20142.
Повний текст джерелаBesson, David. "Architecture du bassin rhodano-provençal miocène (Alpes, SE France). Relations entre déformation, physiographie et sédimentation dans un bassin molassique d’avant-pays." Paris, ENMP, 2005. https://pastel.archives-ouvertes.fr/pastel-00003284.
Повний текст джерелаInventory and analysis of incised valleys through the “rhodano-provencal” molassic basin (BMRP) results in re-examining the miocene sea submergence and the tectonic deformations of the alpine chain foreland basin. Three great fluviatile erosion stages have been characterized : between late Aquitanian and early Burdigalian, between late Burdigalian and early Langhian and early Tortonian. These Miocene networks who supply the platform and the slope of Lions Gulf provide some elements for a better geodynamic understanding of this area: in particular how the deceleration and the stop of the opening of the Lion Gulf interact with the alpine shortening. The marine Miocene invasions of the peri-alpine furrow are controlled by these successive fluviatile networks existence. The first fluviatile network filling is composed of bioclastic carbonates of “foramol” facies. A high frequency sequential model of an incised valleys complex is proposed. The identification of the three Miocene incised valleys networks allow a completely new BMRP geomorphological evolution analysis. The Aquitano-Burdigalian valleys are generally superimposed and encased in the Oligo-Aquitanian deposits in direct relation with the tectonic foreland basin morphostructural heritage and sign a regional large wavelength deformation reported to a compression stage of this field at the lower Miocene. The next networks are in quasi-conformity with the septentrional pyreneo-provencal structures. They are in relation with the activation of the folds and thrust. They sign a shorter wavelength folded deformation associated, for the late Burdigalian network, to a regional rising. Their superposition underlines the tectonic control perenniality. Their dismantling is the consequence of the folds and thrust activation causing not only depotcenters migration but also of the successive valleys networks whose deformation amplifies the digging
Dugué, Olivier. "Géodynamique d'une bordure de massifs anciens : la bordure occidentale du bassin anglo-parisien au Callovo-Oxfordien : pulsations épirogéniques et cycles eustatisques." Caen, 1989. http://www.theses.fr/1989CAEN2034.
Повний текст джерелаJiménez, de Aberasturi Corta Juan Carlos. "De la derrota a la esperanza : políticas vascas durante la Segunda guerra mundial (1937-1947) /." [Oñati] : Herri arduralaritzaren euskal erakundea, 1999. http://catalogue.bnf.fr/ark:/12148/cb37717085n.
Повний текст джерелаHabets, Florence. "Modélisation du cycle continental de l'eau à l'échelle régionale : application aux bassins versants de l'Adour et du Rhône." Toulouse 3, 1998. http://www.theses.fr/1998TOU30139.
Повний текст джерелаPaquet, Fabien. "Evolution morphostructurale des bassins de marge active en subduction : L'exemple du bassin avant-arc de Hawke Bay en nouvelle Zélande." Phd thesis, Université Rennes 1, 2007. http://tel.archives-ouvertes.fr/tel-00342682.
Повний текст джерелаLedier, Jacques. "Etude du bassin versant du Sauzay (Nièvre) : géologie, hydrogéologie, géophysique, comparaison avec les bassins versants de l’Armance et de l’Auxois." Dijon, 1986. http://www.theses.fr/1986DIJOS072.
Повний текст джерелаAndriamahefa, Heriniaina. "Les hydro-écorégions du bassin de la Loire : morphologie, hydrologie, pressions anthropiques sur les cours d'eau et les bassins-versants." Saint-Etienne, 1999. http://www.theses.fr/1999STET2058.
Повний текст джерелаChristophoul, Frédéric. "Discrimination des influences tectoniques et eustatiques dans les bassins liés à des zones de convergence : exemples du Bassin subandin d'Equateur." Toulouse 3, 1999. http://www.theses.fr/1999TOU30262.
Повний текст джерела