13 documents satisfont la requête. Vérifiez les termes recherchés ou relancez la recherche sur le texte intégral
DE LA MODÉLISATION DIDACTIQUE À L’ÉVALUATION EN CONTEXTE : UN PROCESSUS DYNAMIQUE
Auteur(s) : riba, patrick
Auteurs secondaires : Centre de Recherche Interdisciplinaire en Lettres, Langues, Arts et Sciences Humaines (CRILLASH) ; Université des Antilles et de la Guyane (UAG)
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La démarche qualité chez les certificateurs européens en langues étrangères. Lieu de rencontres, curricula cachées et représentations stéréotypées
Auteur(s) : riba, patrick
Auteurs secondaires : Centre de Recherche Interdisciplinaire en Lettres, Langues, Arts et Sciences Humaines (CRILLASH) ; Université des Antilles et de la Guyane (UAG)
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L'évaluation en langues étrangères à l'école et/ou à l'université. Pour une démarche qualité, entre tensions, ruptures et continuités : Ouverture
Auteur(s) : Riba, Patrick
Année de publication :

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Quelques réflexions sur l'évaluation en langues. Comment faire mieux?
Auteur(s) : riba, patrick
Auteurs secondaires : Centre de Recherche Interdisciplinaire en Lettres, Langues, Arts et Sciences Humaines (CRILLASH) ; Université des Antilles et de la Guyane (UAG)
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La validité de construit : de la modélisation didactique à l'adoption d'une démarche qualité
Auteur(s) : Riba, Patrick
Année de publication :

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Mise en place du RNO aux Antilles - Bilan de la première année de suivi hydrologique en baie de Fort-de-France
Auteur(s) : Claisse, Didier Aminot, Alain Courgeon, Laurent
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Mise en place du RNO aux Antilles - Bilan de la première année de suivi hydrologique en Guadeloupe
Auteur(s) : Claisse, Didier Aminot, Alain Courtray, Vincent
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Mission de soutien à la filière " pêche et aquaculture " en Polynésie française. Rapport et Document annexe
Auteur(s) : Knockaert, Camille
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L'évaluation en langues étrangères à l'école et/ou à l'université. Pour une démarche de qualité, entre tensions, ruptures et continuités : Clôture
Auteur(s) : Riba, Patrick
Année de publication :

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DEDUCTION : A research project for shrimp farming sustainability in New-Caledonia
Auteur(s) : Beliaeff, Benoit Chim, Liet Della Patrona, Luc Goyard, Emmanuel Herlin, Jose Labreuche, Yannick Walling, Emilie Ansquer, Dominique
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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
Microalgues marines : les enjeux de la recherche
Auteur(s) : Muller-feuga, Arnaud
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Education thérapeutique du patient asthmatique bilingue français-créole en Guadeloupe : Quels outils, quel impact ? ; Therapeutic Patient Education of the asthmatic bilingual French-Creole patients in Guadeloupe : what tools, what impact?
Auteur(s) : Gotin, Jacques
Auteurs secondaires : Antilles-Guyane Groux, Dominique Raherison-Semjen, Chantal
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