44 documents satisfont la requête.
Atlas de sensibilité du littoral aux pollutions marines. Dispositif opérationnel ORSEC départemental de La Réunion. Annexe technique du dispositif spécifique Polmar-Terre
Auteur(s) : Le Berre, Iwan Louze, Julien David, Laurence
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Ecological and economic viability for the sustainable management of mixed fisheries
Auteur(s) : Gourguet, Sophie
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Small scale fisheries in Europe: A comparative analysis based on a selection of case studies
Auteur(s) : Guyader, Olivier Berthou, Patrick Koutsikopoulos, Constantin Alban, Frederique Demaneche, Sebastien Gaspar, M. B. Eschbaum, R. Fahy, E.
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Platinum-group element systematics and petrogenetic processing of the continental upper mantle: A review
Auteur(s) : Lorand, Jean-Pierre Luguet, Ambre Alard, Olivier
Auteurs secondaires : Laboratoire de Planétologie et Géodynamique de Nantes (LPGN) ; Université de Nantes (UN) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) Rheinische Friedrich-Wilhelms-Universität Bonn ; Université du Québec 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)
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Identifying fishing trip behaviour and estimating fishing effort from VMS data using Bayesian Hidden Markov Models
Auteur(s) : Vermard, Youen Rivot, Etienne Mahevas, Stephanie Marchal, Paul Gascuel, Didier
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La mobilité professionnelle des Martiniquais dans la Caraïbe : analyse de la situation, enjeux, propositions ; Martinican’s Vocational Mobility in Caribbean : situation Analysis, Issues and Proposals
Auteur(s) : Boniface, Philippe
Auteurs secondaires : Antilles-Guyane Groux, Dominique
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Superfast Spreading Rate Crust 4 Integrated Ocean Drilling Program Expedition 335 Scientific Prospectus
Auteur(s) : Teagle, D. Ildefonse, Benoit Blum, P.
Auteurs secondaires : National Oceanography Centre, Southampton ; Université du Québec 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) Texas A&M University [College Station]
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200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks."> 200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks."> 200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks."> 200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks."> | 200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks.">Plus
Kernel Theorems in Spaces of Tempered Generalized Functions
Auteur(s) : Delcroix, Antoine
Auteurs secondaires : Analyse Optimisation Controle (AOC) ; Université des Antilles et de la Guyane (UAG)
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Des politiques nationales à une politique communautaire de coopération au développement : Jeux de pouvoir et conflits d’intérêts entre l’Union européenne et ses Etats membres ; From national policies to a european policies of development cooperation : power struggle and conflics of interests between the eu and ist member states
Auteur(s) : Sabourin, Amandine
Auteurs secondaires : Antilles-Guyane Réno, Fred
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Data Report: Microprobe analyses of primary mineral phases (plagioclase, pyroxene, olivine, and spinel) from Site U1309, Atlantis Massif, Integrated Ocean Drilling Program Expedition 304/305. In : Blackman, D.K., Ildefonse, B., John, B.E., Ohara, Y., Miller, D.J., MacLeod, C.J., and the Expedition 304/305 Scientists, 2006
Auteur(s) : Miller, Dj. Abratis, M. Christie, D. Drouin, Marion Godard, Marguerite Ildefonse, Benoit Et, Al
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)
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Decoupled leaf and stem economics in rain forest trees
Auteur(s) : Baraloto, Christopher Paine, Cet. Poorter, L. Beauchêne, J. Bonal, D. Domenach, A.-M. Hérault, Bruno Patiño, S.
Auteurs secondaires : Department of Biology ; University of Michigan [Ann Arbor] Ecologie des forêts de Guyane (ECOFOG) ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) - Institut National de la Recherche Agronomique (INRA) - Université des Antilles et de la Guyane (UAG) - AgroParisTech - Centre National de la Recherche Scientifique (CNRS) Commissariat général du Plan (CGP) ; Premier ministre Instituto de Investigación de Recursos Biológicos Alexander von Humboldt. Diagonal 27 No. 15-09 ; Instituto de Investigación de Recursos Biológicos Alexander von Humboldt. Diagonal 27 No. 15-09 Earth and Biosphere Institute ; School of Geography Evolution et diversité biologique (EDB) ; Université Paul Sabatier - Toulouse 3 (UPS) - Ecole Nationale Supérieure Agronomique de Toulouse - Centre National de la Recherche Scientifique (CNRS)
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Ocean remote sensing data integration - examples and outlook
Auteur(s) : Chapron, Bertrand Bingham, A Collard, Fabrice Donlon, Craig Johannessen, Johnny A. Piolle, Jean-francois Reul, Nicolas
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Calculation of elongated carbon structures with Density Functional Theory and fast Poisson solver
Auteur(s) : Zuvovski, Michael Boag, Amir Slepyan, Gregory Poullet, Pascal Natan, Amir
Auteurs secondaires : Department of Electrical Engineering ; Tel Aviv University [Tel Aviv] Laboratoire de Mathématiques Informatique et Applications (LAMIA) ; Université des Antilles et de la Guyane (UAG)
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Water storage variations monitored by gravity and tilt in a karst system ; APPORT DE LA GRAVIMETRIE ET DE L'INCLINOMETRIE A L'HYDROLOGIE KARSTIQUE
Auteur(s) : Jacob, 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 Roger Bayer, Jean Chery
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Development of an optical fibers displacement sensor for applications in tiltmetry and seismology ; DÉVELOPPEMENT D'UN CAPTEUR DE DÉPLACEMENT À FIBRE OPTIQUE APPLIQUÉ À L'INCLINOMÉTRIE ET À LA SISMOLOGIE
Auteur(s) : Chawah, Patrick
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 Chéry(Jean.Chery@gm.univ-montp2.fr) ANR-Risknat LINES
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La mobilité professionnelle des Martiniquais dans la Caraïbe : Analyse de la situation, enjeux, propositions ; Martinican's Vocationale Mobility in Caribbean : Situation Analysis, Issues and Proposals
Auteur(s) : Boniface, Philippe
Auteurs secondaires : Antilles-Guyane Groux, Dominique
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An integrated fish-plankton aquaculture system in brackish water
Auteur(s) : Gilles, S. Fargier, L. Lazzaro, X. Baras, E. De Wilde, Nicolas Drakides, C. Amiel, C. Rispal, B.
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Decoupled leaf and stem economics in rain forest trees
Auteur(s) : Baraloto, Christopher PAINE, Timothy Charles Eliot Poorter, Lourens Beauchene, Jacques Bonal, Damien Domenach, Anne-Marie Herault, Bruno Patino, Sandra
Auteurs secondaires : Ecologie des forêts de Guyane (ECOFOG) ; Université des Antilles et de la Guyane (UAG) - AgroParisTech - Institut national de la recherche agronomique (INRA) - Centre de coopération internationale en recherche agronomique pour le développement [CIRAD] - CNRS Ecologie et Ecophysiologie Forestières (EEF) ; Institut national de la recherche agronomique (INRA) - Université Henri Poincaré - Nancy I
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Comparison of IASI water vapour products over complex terrain with COPS campaign data
Auteur(s) : Masiello, Guido Serio, Carmine Deleporte, Thomas Herbin, Hervé Di Girolamo, Paolo Champollion, Cédric Behrendt, Andreas Bosser, Pierre
Auteurs secondaires : Dipartimento di Ingegneria e Fisica dell'Ambiente (Difa) ; Universita degli Studi della Basilicta TACT - LATMOS ; Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) ; Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) - Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) Université de Lille, Sciences et Technologies Institut Pasteur de Lille ; Institut Pasteur de Lille 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) Institut für Physik und Meteorologie [Stuttgart] (IPM) ; Universität Hohenheim École nationale des sciences géographiques (ENSG) ; Institut National de l'Information Géographique et Forestière [IGN] (IGN) LAboratoire de REcherche en Géodésie [Paris] (LAREG/IGN) ; Institut National de l'Information Géographique et Forestière [IGN] (IGN)
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