32 documents satisfont la requête.
Comment les identités sociales communes améliorent les relations entre groupes sociaux minoritaires et majoritaires chez les enfants d'âge scolaire ? ; Comment les identités sociales communes améliorent les relations entre groupes sociaux minoritaires et majoritaires chez les enfants d'âge scolaire ?
Auteur(s) : Popa Roch, Maria Popa Roch, Maria
Année de publication :

Partager

| Plus
Priorités de réduction dans le secteur de l'agriculture de quelques nations caraïbes. ; Mitigation priorities in the agricultural sector of some caribbean nations
Auteur(s) : Gob, Rosaire Gouveia, Grégory
Année de publication :

Partager

| Plus
Présentation de l'ouvrage "Saveurs de Guyane" : échanges avec le public
Auteurs secondaires : Alexandre, Rodolphe Amoida, Odette Couchili, Ti Laborieux, Gabrielle
Année de publication :

Partager

| Plus
L'atelier d'artiste : une oeuvre ouverte, en mouvement
Auteur(s) : Potoczny, Martine
Année de publication :

Partager

| Plus
Course, Piraterie et commerce illégal des esclaves au début du XIXe siècle au nord de la Caraïbe
Auteur(s) : Espersen, Ryan
Année de publication :

Partager

| Plus
The Hybridity of Caribbean Aesthetics
Auteur(s) : Lefrançois, Frédéric
Année de publication :

Partager

| Plus
Présentation de l'ouvrage "Saveurs de Guyane" : conférence
Auteur(s) : Béreau, Didier
Auteurs secondaires : Amoida, Odette Couchili, Ti Laborieux, Gabrielle Alexandre, Rodolphe
Année de publication :

Partager

| Plus
MSPE/UV for field detection of micropollutants in water
Auteur(s) : Brogat, Marine Cadiere, Axelle Thomas, Olivier Baurès, Estelle Roig, Benoit
Auteurs secondaires : 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 ) École des Hautes Études en Santé Publique [EHESP] (EHESP) Laboratoire d'étude et de recherche en environnement et santé (LERES) ; École des Hautes Études en Santé Publique [EHESP] (EHESP) This work was supported by the French Ministry of Industry in the frame of the 2010 Eco-Industries call for project.
Partager

| Plus
La Martinique en quête de mobilité
Auteur(s) : Fointiat, Valérie
Année de publication :

Partager

| Plus
TRANSMISSIONS AND LANGUAGE APPROPRIATIONS: A psycholinguistic approach to adult child interactions ; TRANSMISSIONS ET APPROPRIATIONS LANGAGIERES : Une approche psycholinguistique des interactions adultes / enfants
Auteur(s) : MIEHAKANDA, M'Badi
Auteurs secondaires : Laboratoire Interdisciplinaire de Recherche en Didactique, Éducation et Formation (LIRDEF) ; Université Paul-Valéry - Montpellier 3 (UM3) - Université de Montpellier (UM)
Partager

| Plus
Battling through the thermal boundary layer: Deep sampling in ODP Hole 1256D during IODP Expedition 335
Auteur(s) : Ildefonse, Benoit Teagle, Damon Blum, P. Iodp, Expedition 335 Scientists
Auteurs secondaires : 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) National Oceanography Centre, University of Southampton ; Université du Québec Texas A&M University [College Station]
Partager

200 mm/yr full rate). Three earlier cruises to Hole 1256D have drilled through the sediments, lavas and dikes and 100 m into a complex dike-gabbro transition zone. The specific objectives of IODP Expedition 335 were to: (1) test models of magmatic accretion at fast spreading ocean ridges; (2) quantify the vigor of hydrothermal cooling of the lower crust; (3) establish the geological meaning of the seismic Layer 2-3 boundary at Site 1256; and (4) estimate the contribution of lower crustal gabbros to marine magnetic anomalies. It was anticipated that even a shortened IODP Expedition could deepen Hole 1256D a significant distance (300 m) into cumulate gabbros. Operations on IODP Expedition 335 proved challenging from the outset with almost three weeks spent re-opening and securing unstable sections of the Hole. When coring commenced, the destruction of a hard-formation C9 rotary coring bit at the bottom of the hole required further remedial operations to remove junk and huge volumes of accumulated drill cuttings. Hole-cleaning operations using junk baskets returned large samples of a contact-metamorphic aureole between the sheeted dikes and a major heat source below. These large (up to 3.5 kg) irregular samples preserve magmatic, hydrothermal and structural relationships hitherto unseen because of the narrow diameter of drill core and previous poor core recovery. Including the ~60 m-thick zone of granoblastic dikes overlying the uppermost gabbro, the dike-gabbro transition zone at Site 1256 is over 170 m thick, of which more than 100 m are recrystallized granoblastic basalts. This zone records a dynamically evolving thermal boundary layer between the principally hydrothermal domain of the upper crust and a deeper zone of intrusive magmatism. The recovered samples document a sequence of evolving geological conditions and the intimate coupling between temporally and spatially intercalated intrusive, hydrothermal, contact-metamorphic, partial melting and retrogressive processes. Despite the operational challenges, we achieved a minor depth advance to 1522 m, but this was insufficient penetration to complete any of the primary objectives. However, Hole 1256D has been thoroughly cleared of junk and drill cuttings that have hampered operations during this and previous Expeditions. At the end of Expedition 335, we briefly resumed coring and stabilized problematic intervals with cement. Hole 1256D is open to its full depth and ready for further deepening in the near future."> 200 mm/yr full rate). Three earlier cruises to Hole 1256D have drilled through the sediments, lavas and dikes and 100 m into a complex dike-gabbro transition zone. The specific objectives of IODP Expedition 335 were to: (1) test models of magmatic accretion at fast spreading ocean ridges; (2) quantify the vigor of hydrothermal cooling of the lower crust; (3) establish the geological meaning of the seismic Layer 2-3 boundary at Site 1256; and (4) estimate the contribution of lower crustal gabbros to marine magnetic anomalies. It was anticipated that even a shortened IODP Expedition could deepen Hole 1256D a significant distance (300 m) into cumulate gabbros. Operations on IODP Expedition 335 proved challenging from the outset with almost three weeks spent re-opening and securing unstable sections of the Hole. When coring commenced, the destruction of a hard-formation C9 rotary coring bit at the bottom of the hole required further remedial operations to remove junk and huge volumes of accumulated drill cuttings. Hole-cleaning operations using junk baskets returned large samples of a contact-metamorphic aureole between the sheeted dikes and a major heat source below. These large (up to 3.5 kg) irregular samples preserve magmatic, hydrothermal and structural relationships hitherto unseen because of the narrow diameter of drill core and previous poor core recovery. Including the ~60 m-thick zone of granoblastic dikes overlying the uppermost gabbro, the dike-gabbro transition zone at Site 1256 is over 170 m thick, of which more than 100 m are recrystallized granoblastic basalts. This zone records a dynamically evolving thermal boundary layer between the principally hydrothermal domain of the upper crust and a deeper zone of intrusive magmatism. The recovered samples document a sequence of evolving geological conditions and the intimate coupling between temporally and spatially intercalated intrusive, hydrothermal, contact-metamorphic, partial melting and retrogressive processes. Despite the operational challenges, we achieved a minor depth advance to 1522 m, but this was insufficient penetration to complete any of the primary objectives. However, Hole 1256D has been thoroughly cleared of junk and drill cuttings that have hampered operations during this and previous Expeditions. At the end of Expedition 335, we briefly resumed coring and stabilized problematic intervals with cement. Hole 1256D is open to its full depth and ready for further deepening in the near future."> 200 mm/yr full rate). Three earlier cruises to Hole 1256D have drilled through the sediments, lavas and dikes and 100 m into a complex dike-gabbro transition zone. The specific objectives of IODP Expedition 335 were to: (1) test models of magmatic accretion at fast spreading ocean ridges; (2) quantify the vigor of hydrothermal cooling of the lower crust; (3) establish the geological meaning of the seismic Layer 2-3 boundary at Site 1256; and (4) estimate the contribution of lower crustal gabbros to marine magnetic anomalies. It was anticipated that even a shortened IODP Expedition could deepen Hole 1256D a significant distance (300 m) into cumulate gabbros. Operations on IODP Expedition 335 proved challenging from the outset with almost three weeks spent re-opening and securing unstable sections of the Hole. When coring commenced, the destruction of a hard-formation C9 rotary coring bit at the bottom of the hole required further remedial operations to remove junk and huge volumes of accumulated drill cuttings. Hole-cleaning operations using junk baskets returned large samples of a contact-metamorphic aureole between the sheeted dikes and a major heat source below. These large (up to 3.5 kg) irregular samples preserve magmatic, hydrothermal and structural relationships hitherto unseen because of the narrow diameter of drill core and previous poor core recovery. Including the ~60 m-thick zone of granoblastic dikes overlying the uppermost gabbro, the dike-gabbro transition zone at Site 1256 is over 170 m thick, of which more than 100 m are recrystallized granoblastic basalts. This zone records a dynamically evolving thermal boundary layer between the principally hydrothermal domain of the upper crust and a deeper zone of intrusive magmatism. The recovered samples document a sequence of evolving geological conditions and the intimate coupling between temporally and spatially intercalated intrusive, hydrothermal, contact-metamorphic, partial melting and retrogressive processes. Despite the operational challenges, we achieved a minor depth advance to 1522 m, but this was insufficient penetration to complete any of the primary objectives. However, Hole 1256D has been thoroughly cleared of junk and drill cuttings that have hampered operations during this and previous Expeditions. At the end of Expedition 335, we briefly resumed coring and stabilized problematic intervals with cement. Hole 1256D is open to its full depth and ready for further deepening in the near future."> 200 mm/yr full rate). Three earlier cruises to Hole 1256D have drilled through the sediments, lavas and dikes and 100 m into a complex dike-gabbro transition zone. The specific objectives of IODP Expedition 335 were to: (1) test models of magmatic accretion at fast spreading ocean ridges; (2) quantify the vigor of hydrothermal cooling of the lower crust; (3) establish the geological meaning of the seismic Layer 2-3 boundary at Site 1256; and (4) estimate the contribution of lower crustal gabbros to marine magnetic anomalies. It was anticipated that even a shortened IODP Expedition could deepen Hole 1256D a significant distance (300 m) into cumulate gabbros. Operations on IODP Expedition 335 proved challenging from the outset with almost three weeks spent re-opening and securing unstable sections of the Hole. When coring commenced, the destruction of a hard-formation C9 rotary coring bit at the bottom of the hole required further remedial operations to remove junk and huge volumes of accumulated drill cuttings. Hole-cleaning operations using junk baskets returned large samples of a contact-metamorphic aureole between the sheeted dikes and a major heat source below. These large (up to 3.5 kg) irregular samples preserve magmatic, hydrothermal and structural relationships hitherto unseen because of the narrow diameter of drill core and previous poor core recovery. Including the ~60 m-thick zone of granoblastic dikes overlying the uppermost gabbro, the dike-gabbro transition zone at Site 1256 is over 170 m thick, of which more than 100 m are recrystallized granoblastic basalts. This zone records a dynamically evolving thermal boundary layer between the principally hydrothermal domain of the upper crust and a deeper zone of intrusive magmatism. The recovered samples document a sequence of evolving geological conditions and the intimate coupling between temporally and spatially intercalated intrusive, hydrothermal, contact-metamorphic, partial melting and retrogressive processes. Despite the operational challenges, we achieved a minor depth advance to 1522 m, but this was insufficient penetration to complete any of the primary objectives. However, Hole 1256D has been thoroughly cleared of junk and drill cuttings that have hampered operations during this and previous Expeditions. At the end of Expedition 335, we briefly resumed coring and stabilized problematic intervals with cement. Hole 1256D is open to its full depth and ready for further deepening in the near future."> | 200 mm/yr full rate). Three earlier cruises to Hole 1256D have drilled through the sediments, lavas and dikes and 100 m into a complex dike-gabbro transition zone. The specific objectives of IODP Expedition 335 were to: (1) test models of magmatic accretion at fast spreading ocean ridges; (2) quantify the vigor of hydrothermal cooling of the lower crust; (3) establish the geological meaning of the seismic Layer 2-3 boundary at Site 1256; and (4) estimate the contribution of lower crustal gabbros to marine magnetic anomalies. It was anticipated that even a shortened IODP Expedition could deepen Hole 1256D a significant distance (300 m) into cumulate gabbros. Operations on IODP Expedition 335 proved challenging from the outset with almost three weeks spent re-opening and securing unstable sections of the Hole. When coring commenced, the destruction of a hard-formation C9 rotary coring bit at the bottom of the hole required further remedial operations to remove junk and huge volumes of accumulated drill cuttings. Hole-cleaning operations using junk baskets returned large samples of a contact-metamorphic aureole between the sheeted dikes and a major heat source below. These large (up to 3.5 kg) irregular samples preserve magmatic, hydrothermal and structural relationships hitherto unseen because of the narrow diameter of drill core and previous poor core recovery. Including the ~60 m-thick zone of granoblastic dikes overlying the uppermost gabbro, the dike-gabbro transition zone at Site 1256 is over 170 m thick, of which more than 100 m are recrystallized granoblastic basalts. This zone records a dynamically evolving thermal boundary layer between the principally hydrothermal domain of the upper crust and a deeper zone of intrusive magmatism. The recovered samples document a sequence of evolving geological conditions and the intimate coupling between temporally and spatially intercalated intrusive, hydrothermal, contact-metamorphic, partial melting and retrogressive processes. Despite the operational challenges, we achieved a minor depth advance to 1522 m, but this was insufficient penetration to complete any of the primary objectives. However, Hole 1256D has been thoroughly cleared of junk and drill cuttings that have hampered operations during this and previous Expeditions. At the end of Expedition 335, we briefly resumed coring and stabilized problematic intervals with cement. Hole 1256D is open to its full depth and ready for further deepening in the near future.">Plus
Tourists’ Weather Perceptions and Weather Related Behavior. A Qualitative Pilot Study with Holiday Tourists to Martinique
Auteur(s) : Lohmann, Martin C. Hübner, Anna
Partager

| Plus
Antepartum dalteparin versus no antepartum dalteparin for the prevention of pregnancy complications in pregnant women with thrombophilia (TIPPS): a multinational open-label randomised trial
Auteur(s) : Rodger, Marc A Hague, William M Kingdom, John Kahn, Susan R Karovitch, Alan Sermer, Mathew Clement, Anne Marie Coat, Suzette
Auteurs secondaires : Haematology ; University of Ottawa [Ottawa] Clinical Epidemiology Program (PSW) ; The Ottawa Health Research Institute Thrombosis Program ; University of Ottawa Centre de Physique des Particules de Marseille (CPPM) ; Centre National de la Recherche Scientifique (CNRS) - Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3) - Aix Marseille Université (AMU) Laboratoire d'Hydrologie et de Géochimie de Strasbourg (LHyGeS) ; École Nationale du Génie de l'Eau et de l'Environnement de Strasbourg (ENGEES) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) Dynamique des écosystèmes Caraïbe et biologie des espèces associées (DYNECAR EA 926) ; Université des Antilles et de la Guyane (UAG) Université Grenoble Alpes - UFR de Langues étrangères (LLCE et LEA) (UGA UFR LLCE LEA) ; Université Grenoble Alpes (UGA) Institut de génétique humaine (IGH) ; Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)
Partager

| Plus
L'intercompréhension des langues : un chemin parcouru et des voies à ouvrir
Auteur(s) : Gonzales Delgado, Rita Fernandez Hernandez, Eric
Année de publication :

Partager

| Plus
Tourisme et lutte contre la pauvreté : opportunités et défis ; Tourisme et lutte contre la pauvreté : opportunités et défis : Tourism and Poverty Alleviation: Opportunities and Challenge
Auteur(s) : Dehoorne, Olivier
Auteurs secondaires : Lieux, Identités, eSpaces, Activités (LISA) ; Université Pascal Paoli (UPP) - Centre National de la Recherche Scientifique (CNRS) Centre de Recherche en Economie, Gestion, Modélisation et Informatique Appliquée (CEREGMIA) ; Université des Antilles et de la Guyane (UAG)
Partager

| Plus
L'agir enseignant à l'interface du sociologique et du didactique
Auteur(s) : Poggi, Marie-Paule Brière, Fabienne
Auteurs secondaires : Centre de recherches et de ressources en éducation et formation (CRREF) ; Université des Antilles et de la Guyane (UAG) Laboratoire Interdisciplinaire de Recherche sur les Transformations des pratiques Éducatives et des pratiques Sociales (LIRTES) ; Université Paris-Est (UPE)
Partager

| Plus
Mission de soutien à la filière " pêche et aquaculture " en Polynésie française. Rapport et Document annexe
Auteur(s) : Knockaert, Camille
Partager

| Plus
Regional Development Through Religious Tourism. San Juan de los Lagos and Jalostotitlán in Los Altos de Jalisco Region, Mexico
Auteur(s) : Martínez Cárdenas, Rogelio
Partager

| Plus
Teaching of french as a language for integration for haïtians migrants in Guadalupe. From linguistic insecurity to contextual pedagogic tools. ; L’enseignement du Français Langue d’Intégration aux adultes migrants haïtiens en Guadeloupe : de l’insécurité linguistique héritée du scolaire à des modalités de remédiations pédagogiques.
Auteur(s) : Beaubrun, Frédéric
Auteurs secondaires : Centre de recherches et de ressources en éducation et formation (CRREF) ; Université des Antilles et de la Guyane (UAG)
Partager

| Plus
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
Partager

| Plus