57 documents satisfont la requête.
Les contrariétés de la "préférence locale" ; Les contrariétés de la "préférence locale"
Auteur(s) : Giraud, Michel Giraud, Michel
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La négresse, figure de la modernité
Auteur(s) : Hamot, Odile
Auteurs secondaires : Viard, Bruno
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Le tourisme de croisière dans la Caraïbe : spatialisation et concentration des flux : analyse en impact financier
Auteur(s) : Petit-Charles, Nathalie Marques, Bruno
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Le tourisme de croisière dans la Caraïbe : spatialisation et concentration des flux : analyse en impact financier
Auteur(s) : Petit-Charles, Nathalie Marques, Bruno
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Slip rates and coseismic slips analyses along strike-slip faults in Mongolia and Iran - Morphotectonic and paleoseismic approach ; Analyses des vitesses et des déplacements co-sismiques sur des failles décrochantes en Mongolie et en Iran - Approche morphotectonique et paléosismologique
Auteur(s) : Rizza, Magali
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Université Montpellier II - Sciences et Techniques du Languedoc Jean-François Ritz(ritz@gm.univ-montp2.fr)
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Des conséquences psychologiques de l'esclavage
Auteur(s) : Charles-Nicolas, Aimé Pago, Gilbert
Auteurs secondaires : Odent-Allet, Patrick
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Along strike variations of crustal deformation in the Himalayas ; Variations latérales de la déformation crustale en Himalaya
Auteur(s) : Berthet, Théo
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Université Montpellier II - Sciences et Techniques du Languedoc Rodolphe Cattin György Hetényi
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Le traitement de l'orthographe en UPE2A : étude de cas aux collèges "Dillon2" et "Aimé Césaire" de Fort-de-France
Auteur(s) : Marin, Gabriela
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Analyse technico-économique de projets d'élevage d'ombrine (Sciaenops ocellata) en cages flottantes à la Martinique
Auteur(s) : Houel, S Falguiere, Jean-claude Paquotte, Philippe
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Contribution et Dépendance des flottilles de pêche aux espèces commerciales majeures du Golfe de Gascogne
Auteur(s) : Daures, Fabienne Planchot, Marie Demaneche, Sebastien Van Isenghem, Sylvie Berthou, Patrick Leblond, Emilie Jezequel, Michele
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Dynamiques d’exploitation et conditions d’évolution de la rente dans les pêches maritimes françaises
Auteur(s) : Guyader, Olivier
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Retour sur deux projets de développement en aquaculture outre-mer : leçons pour l’avenir
Auteur(s) : Lacroix, Denis
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Fluctuations à long terme du thon rouge: validité, origines et conséquences
Auteur(s) : Ravier, Christelle
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Le tourisme mondial, les inégalités internationales et le problème de la pauvreté
Auteur(s) : Célimène, Fred Vellas, François
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Détection d’Aspergillus dans le liquide bronchiolo-alvéolaire pour le diagnostic de l’aspergillose invasive : comparaison des performances de 2 méthodes PCR
Auteur(s) : Comacle, P. Belaz, S. Robert-Gangneux, F. Chevrier, S. Gangneux, J
Auteurs secondaires : CHU Pontchaillou [Rennes] Laboratoire de Parasitologie-Mycologie ; Centre Hospitalier Universitaire de Rennes Institut de recherche, santé, environnement et travail [Rennes] (Irset) ; Université d'Angers (UA) - Université des Antilles et de la Guyane (UAG) - Université de Rennes 1 (UR1) - École des Hautes Études en Santé Publique [EHESP] (EHESP) - Institut National de la Santé et de la Recherche Médicale (INSERM) - Structure Fédérative de Recherche en Biologie et Santé de Rennes ( Biosit : Biologie - Santé - Innovation Technologique ) Service de Parasitologie-Mycologie [Rennes] ; Université de Rennes 1 (UR1) - Hôpital Pontchaillou - CHU Pontchaillou [Rennes]
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A petrological and geochemical cross section oflower crust at the Wadi Gideah (Samail ophiolite):Implications for the crustal accretion at fast-spreading mid-ocean ridges ; Une coupe pétrologique et géochimique dans la croûte inférieure à Wadi Gideah (ophiolite de Samail): implications pour l’accrétion crustale aux dorsales océaniques rapides
Auteur(s) : MUELLER, Tim
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Manteau et Interfaces ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Université de Montpellier Benoit Ildefonse Juergen Koepke
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Pratiques éducatives dans un contexte multiculturel L'exemple plurilingue de la Guyane. Le primaire ; : Volume I
Auteur(s) : Ailincai, Rodica Crouzier, Marie-Françoise
Auteurs secondaires : Modèles, Dynamiques, Corpus (MoDyCo) ; Université Paris Nanterre (UPN) - Centre National de la Recherche Scientifique (CNRS) Centre de Recherche Interdisciplinaire en Lettres, Langues, Arts et Sciences Humaines (CRILLASH) ; Université des Antilles et de la Guyane (UAG)
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Seismic hazard assessment for Tehran, Tabriz and Zandjan cities (NW Iran) based on morphotectonical and paleoseismological approaches. ; Evaluation de l'aléa sismique pour les villes de Téhéran, Tabriz et Zandjan dans le NW de l'Iran. Approche morphotectonique et paléosismologique.
Auteur(s) : Solaymani, Shahryar
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Université Montpellier 2 Sciences et Techniques du Languedoc Hervé Philip
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Comportement mécanique des amphibolites àl’interface de subduction
Auteur(s) : Soret, Mathieu Agard, Philippe Dubacq, Benoît Ildefonse, Benoit Yamato, Philippe Prigent, Cécile
Auteurs secondaires : Institut des Sciences de la Terre de Paris (iSTeP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS) Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Géosciences Rennes (GR) ; Université de Rennes 1 (UR1) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire des Sciences de l'Univers de Rennes (OSUR) - Centre National de la Recherche Scientifique (CNRS) Institut des Sciences de la Terre (ISTerre) ; Université Joseph Fourier - Grenoble 1 (UJF) - Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR) - Institut national des sciences de l'Univers (INSU - CNRS) - Institut de recherche pour le développement [IRD] : UR219 - PRES Université de Grenoble - Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]) - Centre National de la Recherche Scientifique (CNRS) Société Géologique de France
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Deformation at the transition between subduction and collision east of Taiwan: seismological approach ; Déformation à la transition entre subduction et collision à l'est de Taïwan: approche sismologique
Auteur(s) : Theunissen, Thomas
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Université Montpellier II - Sciences et Techniques du Languedoc Serge Lallemand(serge.lallemand@gm.univ-montp2.fr) ANR ACTS
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180degre). Synthetic tests show the effectiveness of MAXI (using P-wave only) to determine the parameters x, y and z even when the azimuthal gap is important. In the latter case, the quality of the results is dependent on the velocity model to represent the 3D structure of the Earth. We propose an approach involving the use of a 3D a priori P-wave velocity model to locate earthquakes which are lateral and remote to the seismic network. An application to the case of Taiwan and Ecuador validates this approach. Finally, at the level of a few months, the marine geophysical campaign RATS (Ryukyu Arc: Tectonics and Seismology) was conducted in two stages. A passive seismology experiment from July to October, 2008 (RATS1) has been conducted over the forearc of the Ryukyus and then active seismic experiment (refraction and reflection) was conducted in May 2009 in a NNE - SSW line through the Ryukyu margin. These two combined experiments allow improving our knowledge about the crustal structure of the margin. At the level of the forearc, the basement of the forearc is characterized by vertical backstop and a very deformed basis certainly associated with a significant out of sequence deformation. In depth, the downgoing plate is certainly affected by a tear that controls the seismicity in the region of transition between the subduction and collision."> 180degre). Synthetic tests show the effectiveness of MAXI (using P-wave only) to determine the parameters x, y and z even when the azimuthal gap is important. In the latter case, the quality of the results is dependent on the velocity model to represent the 3D structure of the Earth. We propose an approach involving the use of a 3D a priori P-wave velocity model to locate earthquakes which are lateral and remote to the seismic network. An application to the case of Taiwan and Ecuador validates this approach. Finally, at the level of a few months, the marine geophysical campaign RATS (Ryukyu Arc: Tectonics and Seismology) was conducted in two stages. A passive seismology experiment from July to October, 2008 (RATS1) has been conducted over the forearc of the Ryukyus and then active seismic experiment (refraction and reflection) was conducted in May 2009 in a NNE - SSW line through the Ryukyu margin. These two combined experiments allow improving our knowledge about the crustal structure of the margin. At the level of the forearc, the basement of the forearc is characterized by vertical backstop and a very deformed basis certainly associated with a significant out of sequence deformation. In depth, the downgoing plate is certainly affected by a tear that controls the seismicity in the region of transition between the subduction and collision."> 180degre). Synthetic tests show the effectiveness of MAXI (using P-wave only) to determine the parameters x, y and z even when the azimuthal gap is important. In the latter case, the quality of the results is dependent on the velocity model to represent the 3D structure of the Earth. We propose an approach involving the use of a 3D a priori P-wave velocity model to locate earthquakes which are lateral and remote to the seismic network. An application to the case of Taiwan and Ecuador validates this approach. Finally, at the level of a few months, the marine geophysical campaign RATS (Ryukyu Arc: Tectonics and Seismology) was conducted in two stages. A passive seismology experiment from July to October, 2008 (RATS1) has been conducted over the forearc of the Ryukyus and then active seismic experiment (refraction and reflection) was conducted in May 2009 in a NNE - SSW line through the Ryukyu margin. These two combined experiments allow improving our knowledge about the crustal structure of the margin. At the level of the forearc, the basement of the forearc is characterized by vertical backstop and a very deformed basis certainly associated with a significant out of sequence deformation. In depth, the downgoing plate is certainly affected by a tear that controls the seismicity in the region of transition between the subduction and collision."> 180degre). Synthetic tests show the effectiveness of MAXI (using P-wave only) to determine the parameters x, y and z even when the azimuthal gap is important. In the latter case, the quality of the results is dependent on the velocity model to represent the 3D structure of the Earth. We propose an approach involving the use of a 3D a priori P-wave velocity model to locate earthquakes which are lateral and remote to the seismic network. An application to the case of Taiwan and Ecuador validates this approach. Finally, at the level of a few months, the marine geophysical campaign RATS (Ryukyu Arc: Tectonics and Seismology) was conducted in two stages. A passive seismology experiment from July to October, 2008 (RATS1) has been conducted over the forearc of the Ryukyus and then active seismic experiment (refraction and reflection) was conducted in May 2009 in a NNE - SSW line through the Ryukyu margin. These two combined experiments allow improving our knowledge about the crustal structure of the margin. At the level of the forearc, the basement of the forearc is characterized by vertical backstop and a very deformed basis certainly associated with a significant out of sequence deformation. In depth, the downgoing plate is certainly affected by a tear that controls the seismicity in the region of transition between the subduction and collision."> | 180degre). Synthetic tests show the effectiveness of MAXI (using P-wave only) to determine the parameters x, y and z even when the azimuthal gap is important. In the latter case, the quality of the results is dependent on the velocity model to represent the 3D structure of the Earth. We propose an approach involving the use of a 3D a priori P-wave velocity model to locate earthquakes which are lateral and remote to the seismic network. An application to the case of Taiwan and Ecuador validates this approach. Finally, at the level of a few months, the marine geophysical campaign RATS (Ryukyu Arc: Tectonics and Seismology) was conducted in two stages. A passive seismology experiment from July to October, 2008 (RATS1) has been conducted over the forearc of the Ryukyus and then active seismic experiment (refraction and reflection) was conducted in May 2009 in a NNE - SSW line through the Ryukyu margin. These two combined experiments allow improving our knowledge about the crustal structure of the margin. At the level of the forearc, the basement of the forearc is characterized by vertical backstop and a very deformed basis certainly associated with a significant out of sequence deformation. In depth, the downgoing plate is certainly affected by a tear that controls the seismicity in the region of transition between the subduction and collision.">Plus