127 documents satisfont la requête.
Les cultures marines en France et le droit Partager

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Zones franches, offshore et paradis fiscaux: l’antimonde légal
Auteur(s) : Desse, Michel Thierry, Hartog
Auteurs secondaires : Archéologie Industrielle, Histoire, Patrimoine- Géographie, Développement, Environnement de la Caraïbe [EA 929] (AIHP-GEODE) ; Université des Antilles et de la Guyane (UAG)
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La Première Guerre mondiale et l'influence française en Haïti
Auteur(s) : Gaillard-Pourchet, Gusti-Klara
Année de publication :

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Open Registers of Ships : A Gain for Small Island Economies ? : A Study from the Caribbean States ; La libre immatriculation des navires : un gain pour les petites économies insulaires ? : Étude à partir du cas d'États de la Caraïbe
Auteur(s) : Angelelli, Pierre
Auteurs secondaires : Centre de Recherche en Economie, Gestion, Modélisation et Informatique Appliquée (CEREGMIA) ; Université des Antilles et de la Guyane (UAG) Université des Antilles-Guyane Fred Célimène
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The eco-citizen youth in the digital age The legal challenges of participatory engagement ; La jeunesse éco-citoyenne à l’heure du numérique Les enjeux juridiques de l’engagement participatif
Auteur(s) : Vieira, Julien
Auteurs secondaires : Centre d’Étude et de Recherche sur le Droit Administratif et la Réforme de l’État (CERDARE) ; Université de Bordeaux (UB) - Centre National de la Recherche Scientifique (CNRS)
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Droit, tourisme et pauvreté : les difficultés et les limites de l’appréhension juridique de la pauvreté et de l’instrumentalisation normative du tourisme
Auteur(s) : Breton, Jean-Marie
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Shewanella profunda sp nov., isolated from deep marine sediment of the Nankai Trough
Auteur(s) : Toffin, Laurent Bidault, Adeline Pignet, Patricia Tindall, Brian Slobodkin, Alexander Kato, Chiaki Prieur, Daniel
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Le programme d’EXTension RAisonnée du PLAteau Continental (EXTRAPLAC). Enjeux pour les trois collectivités ultramarines du Pacifique (Nouvelle-Calédonie, Wallis & Futuna, Polynésie française).
Auteur(s) : Loubrieu, Benoit Roest, Walter Patriat, Martin Loubersac, Lionel
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Characterisation of oceanic sediments and basalts from Hole 833B, New Hebrides Island Arc (Vanuatu) from downhole measurements.
Auteur(s) : Rabaute, Alain Briqueu, Louis K. Harvey, Peter Mercadier, Henri
Auteurs secondaires : Institut des Sciences de la Terre, de l'Environnement et de l'Espace de Montpellier (ISTEEM) ; Université Montpellier 2 - Sciences et Techniques (UM2) - 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) Borehole Research Group (BRG) ; Department of Geology [Leicester] ; University of Leicester - University of Leicester Ocean Drilling Program Ocean Drilling Program
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Magmatic impregnation of oceanic lithosphere: Microstructural and geochemical study of gabbroic sequences drilled at Mid-Atlantic Ridge ; Imprégnation magmatique de la lithosphère océanique: Etude microstructurale et géochimique des séries gabbroïques forées à la dorsale Médio-Atlantique
Auteur(s) : Drouin, Marion
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 Benoit Ildefonse(Benoit.Ildefonse@gm.univ-montp2.fr)
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Effects of hydroxyurea on blood rheology in sickle cell anemia: A two-years follow-up study
Auteur(s) : Lemonne, Nathalie Möckesch, Berenike Charlot, Keyne Garnier, Yohann Waltz, Xavier Lamarre, Yann Antoine-Jonville, Sophie Etienne-Julan, Maryse
Auteurs secondaires : Unité Transversale de la Drépanocytose ; CHU Pointe-à-Pitre/Abymes Université des Antilles (Pôle Guadeloupe) ; Université des Antilles (UA) Biologie intégrée du globule rouge ; Université des Antilles et de la Guyane (UAG) - Institut National de la Transfusion Sanguine [Paris] (INTS) - Université Paris Diderot - Paris 7 (UPD7) - Institut National de la Santé et de la Recherche Médicale (INSERM) Biologie Intégrée du Globule Rouge ; Institut National de la Transfusion Sanguine [Paris] (INTS) - Université Paris Diderot - Paris 7 (UPD7) - Université de la Réunion (UR) - Institut National de la Santé et de la Recherche Médicale (INSERM) - CHU de Pointe-à-Pitre Dynamique des Structures et Interactions des Macromolécules Biologiques- Pôle de La Réunion (DSIMB Réunion) ; Dynamique des Structures et Interactions des Macromolécules Biologiques (DSIMB) ; Institut National de la Transfusion Sanguine [Paris] (INTS) - Université Paris Diderot - Paris 7 (UPD7) - Institut National de la Santé et de la Recherche Médicale (INSERM) - Institut National de la Transfusion Sanguine [Paris] (INTS) - Université Paris Diderot - Paris 7 (UPD7) - Institut National de la Santé et de la Recherche Médicale (INSERM) - Université de la Réunion (UR) Adaptations au Climat Tropical, Exercice et Santé (ACTES) ; Université des Antilles et de la Guyane (UAG) Protéines de la membrane érythrocytaire et homologues non-érythroides ; Université des Antilles et de la Guyane (UAG) - Institut National de la Transfusion Sanguine [Paris] (INTS) - Université Paris Diderot - Paris 7 (UPD7) - Université de la Réunion (UR) - Institut National de la Santé et de la Recherche Médicale (INSERM)
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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
Les courants de la Manche
Auteur(s) : Houette, M.
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Non-specific activation of antiviral immunity and induction of RNA interference may engage the same pathway in the Pacific white leg shrimp Litopenaeus vannamei
Auteur(s) : Labreuche, Yannick Veloso, Artur De La Vega, Enrique Gross, Paul S. Chapman, Robert W. Browdy, Craig L. Warr, Gregory W.
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Grenada ; Country environmental profile
Auteur(s) : United States -- Agency for International Development Grenada -- Ministry of External Affairs, Agriculture, Lands, Forestry, Tourism, and Legal Affairs Caribbean Conservation Association Island Resources Foundation (Virgin Islands of the United States) Grenada National Trust
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Island Worlds: Spaces, Temporalities, Resources ; Mondes insulaires : espaces, temporalités, ressources
Auteur(s) : Baldacchino, Godfrey Dehoorne, Olivier
Auteurs secondaires : University of Prince Edward Island Lieux, Identités, eSpaces, Activités (LISA) ; Université Pascal Paoli (UPP) - Centre National de la Recherche Scientifique (CNRS)
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Le tournant environnemental en Amazonie : ampleur et limites du découplage entre production et déforestation
Auteur(s) : Laurent, François Arvor, Damien Daugeard, Marion Osis, Reinis Tritsch, Isabelle Coudel, Emilie Piketty, Marie-Gabrielle Piraux, Marc
Auteurs secondaires : Espaces et Sociétés (ESO) ; Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) - Le Mans Université (UM) - Université d'Angers (UA) - Université de Nantes (UN) - AGROCAMPUS OUEST - Université de Rennes 2 (UR2) - Centre National de la Recherche Scientifique (CNRS) Littoral, Environnement, Télédétection, Géomatique (LETG) ; Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) - Université d'Angers (UA) - Université de Nantes (UN) - École pratique des hautes études (EPHE) - Université de Brest (UBO) - Université de Rennes 2 (UR2) - Centre National de la Recherche Scientifique (CNRS) CREDA - Centre de Recherche Et de Documentation sur les Amériques - UMR 7227 (CREDA) ; Université Sorbonne Nouvelle - Paris 3 - Centre National de la Recherche Scientifique (CNRS) 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 - Université de Guyane (UG) - Centre National de la Recherche Scientifique (CNRS) Territoires, Environnement, Télédétection et Information Spatiale (UMR TETIS) ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) - AgroParisTech - Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) UR GREEN ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) Universidade de Brasilia [Brasília] (UnB) Littoral, Environnement, Télédétection, Géomatique (LETG - Rennes) ; Littoral, Environnement, Télédétection, Géomatique (LETG) ; Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) - Université d'Angers (UA) - Université de Nantes (UN) - École pratique des hautes études (EPHE) - Université de Brest (UBO) - Université de Rennes 2 (UR2) - Centre National de la Recherche Scientifique (CNRS) - Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) - Université d'Angers (UA) - Université de Nantes (UN) - École pratique des hautes études (EPHE) - Université de Brest (UBO) - Université de Rennes 2 (UR2) - Centre National de la Recherche Scientifique (CNRS)
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