182 documents satisfont la requête.
Subduction and Tectonics. Discussion on the Results of the IPOD Program in Active Margins
Auteur(s) : Aubouin, J Blanchet, R
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Determining the Role of Hand Feeding Practices in Accidental Shark Bites on Scuba Divers
Auteur(s) : Clua, E. E. Torrente, F.
Auteurs secondaires : Centre de recherches insulaires et observatoire de l'environnement (CRIOBE) ; Université de Perpignan Via Domitia (UPVD) - École pratique des hautes études (EPHE) - Centre National de la Recherche Scientifique (CNRS) Laboratoire d'Excellence CORAIL (LabEX CORAIL) ; Institut de Recherche pour le Développement (IRD) - Université des Antilles et de la Guyane (UAG) - École des hautes études en sciences sociales (EHESS) - École pratique des hautes études (EPHE) - Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) - Université de la Réunion (UR) - Université de la Polynésie Française (UPF) - Université de Nouvelle Calédonie - Institut d'écologie et environnement
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Méthodologie de lutte contre la pauvreté par le développement touristique
Auteur(s) : Vellas, François
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Changes in Gene Expression and Estrogen Receptor Cistrome in Mouse Liver Upon Acute E2 Treatment
Auteur(s) : Palierne, Gaëlle Fabre, A. J. Solinhac, Romain Le Peron, Christine Avner, Stéphane Lenfant, Françoise Fontaine, Coralie Salbert, Gilles
Auteurs secondaires : Institut de Génétique et Développement de Rennes (IGDR) ; Université de Rennes 1 (UR1) - Centre National de la Recherche Scientifique (CNRS) - Structure Fédérative de Recherche en Biologie et Santé de Rennes ( Biosit : Biologie - Santé - Innovation Technologique ) Institut des Maladies Métaboliques et Cardiovasculaires (I2MC) ; Université Paul Sabatier - Toulouse 3 (UPS) - Hôpital de Rangueil - Institut National de la Santé et de la Recherche Médicale (INSERM) 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 ) Centre National de la Recherche Scientifique, University of Rennes I, Conseil Regional Midi-Pyrenees, Fondation pour la Recherche Medicale, French Government National Infrastructure, Investissements d'Avenir program [ANR-10-INBS-0009], Association pour la Recherche Contre le Cancer, Ligue Contre le Cancer (Equipe Labelisee Ligue), Region Bretagne [CREATE 4793], Agence Nationale pour la Recherche [ANR-09-BLAN-0268-01], Inserm, University of Toulouse III, Faculty of Medecine Toulouse-Rangueil, Fondation de France ANR-10-INBS-09-01/10-INBS-0009, France-Génomique, Organisation et montée en puissance d'une Infrastructure Nationale de Génomique(2010)
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Tourism and Biodiversity in Natura 2000 Sites. Case Study: Natura 2000 Valea Roșie (Red Valley) Site, Bihor County, Romania
Auteur(s) : Ilieș, Dorina Camelia Herman, Grigore Ilieș, Alexandru Baias, Ștefan Dehoorne, Olivier Buhaș, Sorin Dumbravă, Răzvan Buhaș, Raluca
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Ventilatory responses during experimental cycle-run transition in triathletes
Auteur(s) : Hue, Olivier Le Gallais, Daniel Boussana, Alain Chollet, Didier Prefaut, Christian
Auteurs secondaires : Adaptations au Climat Tropical, Exercice et Santé (ACTES) ; Université des Antilles et de la Guyane (UAG) Centre d'Optimisation de la Performance Motrice ; Université Montpellier 1 (UM1) Laboratoire de Physiologie des Interactions ; CHU Arnaud de Villeneuve Centre d'Optimisation de la Performance Motrice ; Université Montpellier 1 (UM1) Centre d’études des transformations des activités physiques et sportives (CETAPS) ; Université de Rouen Normandie (URN) ; Normandie Université (NU) - Normandie Université (NU)
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The complexity of ERK1 and ERK2 MAPKs in multiple hepatocyte fate responses.
Auteur(s) : Frémin, Christophe Ezan, Frédéric Guegan, Jean-Philippe Gailhouste, Luc Trotard, Maud Le Seyec, Jacques Rageul, Julie Théret, Nathalie
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 ) Université européenne de Bretagne (UEB) Institut National de la Santé et de la Recherche Médicale (INSERM U522 and U620); Région Bretagne; Association pour la Recherche contre le Cancer (ARC)
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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]
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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
Fishing strategies, economic performance and management of moored fishing aggregating devices in Guadeloupe
Auteur(s) : Guyader, Olivier Bellanger, Manuel Reynal, Lionel Demaneche, Sebastien Berthou, Patrick
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Illegal gold miners in French Guiana: a neglected population with poor health
Auteur(s) : Douine, Maylis Mosnier, Emilie Le Hingrat, Quentin Charpentier, Charlotte Corlin, Florine Hureau, Louise Adenis, Antoine Lazrek, Yassamine
Auteurs secondaires : Centre d'Investigation Clinique Antilles-Guyane (CIC - Antilles Guyane) ; Université des Antilles et de la Guyane (UAG) - Institut National de la Santé et de la Recherche Médicale (INSERM) - CHU de Pointe-à-Pitre - Centre Hospitalier de Cayenne Andrée Rosemon - CHU de Fort de France Ecosystemes Amazoniens et Pathologie Tropicale (EPat) ; Institut Pasteur de la Guyane - Institut National de la Santé et de la Recherche Médicale (INSERM) - Université de Guyane (UG) Département des Centres Délocalisés de Prévention et de Soins ; Centre Hospitalier de Cayenne Andrée Rosemon Infection, Antimicrobiens, Modélisation, Evolution (IAME) ; Université Paris Diderot - Paris 7 (UPD7) - Université Paris 13 (UP13) - Université Sorbonne Paris Cité (USPC) - Institut National de la Santé et de la Recherche Médicale (INSERM) Laboratoire de Parasitologie, Centre National de Référence du Paludisme - Région Antilles-Guyane ; Institut Pasteur de la Guyane - Réseau International des Instituts Pasteur (RIIP) - WHO Collaborating Center for Surveillance of Antimalarial Drug Resistance Laboratoire Hospitalo-Universitaire de Parasitologie-Mycologie [Cayenne, Guyane Française] ; Centre Hospitalier de Cayenne Andrée Rosemon - Coordination Régionale de la lutte contre le Virus de L'Immunodéficience Humaine (COREVIH) This study was funded by European Funds for Regional Development (Feder), N° Presage 32,078. The Funding body had no role in the study and in the publication process.
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Urban growth and natural hazards, in particular in mountainous areas of developing countries ; Croissance urbaine et risques naturels dans les montagnes des pays en développement
Auteur(s) : Thouret, Jean-Claude D'Ercole, Robert
Auteurs secondaires : Université Blaise Pascal - Clermont-Ferrand 2 (UBP) Université des Antilles et de la Guyane (UAG) Association des Géographes Français Association de la Revue de Géographie Alpine (ARGA, Grenoble I) Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Université Blaise Pascal (Clermont II) Université des Antilles et de la Guyane CERAMAC (Centre d'Etudes et de Recherches Appliquées au Massif Central, à la moyenne montagne et aux espaces fragiles)
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Ta’ta’, Huayani: Perception of leishmaniasis and evaluation of medicinal plants used by the Chayahuita in Peru. Part II
Auteur(s) : Odonne, G. Bourdy, G. Castillo, D. Estevez, Y. Lancha-Tangoa, A. Alban-Castillo, J. Deharo, E. Rojas, R.
Auteurs secondaires : Institut de recherche pour le développement [IRD] : UMR152 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) Laboratoire de Pharmacochimie des Substances Naturelles et Pharmacophores Redox (UMR152) ; Université Paul Sabatier - Toulouse 3 (UPS) Laboratorio de Enfermedades Infecciosas, Laboratorios de Investigacion y Desarrollo ; Universidad Peruana Cayetano Heredia - FACULTAD DE CIENCIAS Y FILOSOFIA Universidad Nacional Mayor de San Marcos
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Biological traits, rather than environment, shape detection curves of large vertebrates in neotropical rainforests
Auteur(s) : Denis, Thomas Richard-Hansen, Cécile Brunaux, Olivier Etienne, Marie Pierre Guitet, Stéphane Herault, Bruno
Auteurs secondaires : 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) Recherche et Développement, Réserve de Montabo ; Office National des Forêts (ONF) Mathématiques et Informatique Appliquées (MIA-Paris) ; Institut National de la Recherche Agronomique (INRA) - AgroParisTech Botanique et Modélisation de l'Architecture des Plantes et des Végétations (UMR AMAP) ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) - Institut national de la recherche agronomique [Montpellier] (INRA Montpellier) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Institut de Recherche pour le Développement (IRD [France-Sud]) Recherche et Développement - Réserve de Montabo ; Office National des Forêts (ONF)
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Bali (Indonésie) : le patrimoine culturel contre ou avec le développement touristique ? Un paradis en sursis et le risque d’un tourisme de luxe non maîtrisé
Auteur(s) : Michel, Franck
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Tools for modeling radioactive contaminants in chip materials
Auteur(s) : Wrobel, F. Kaouache, A. Saigné, F. Touboul, A. d. Schrimpf, R. d. Warot, G. BRUGUIER, Olivier
Auteurs secondaires : Institut d’Electronique et des Systèmes (IES) ; Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Vanderbilt University, Nashville, Laboratoire Souterrain de Modane (LSM - UMR 6417) ; Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3) - Commissariat à l'énergie atomique et aux énergies alternatives (CEA) - 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) Dynamique de la Lithosphere ; 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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Earthquake synchrony and clustering on Fucino faults (Central Italy) as revealed from in situ Cl-36 exposure dating
Auteur(s) : Benedetti, Lucilla Manighetti, Isabelle Gaudemer, Yves Finkel, Robert Malavieille, Jacques Pou, Khemrak Arnold, Maurice Aumaitre, Georges
Auteurs secondaires : Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) Géoazur (GEOAZUR) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire de la Côte d'Azur - Centre National de la Recherche Scientifique (CNRS) Institut de Physique du Globe de Paris (IPGP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - IPG PARIS - Université Paris Diderot - Paris 7 (UPD7) - Université de la Réunion (UR) - Centre National de la Recherche Scientifique (CNRS) Dynamique de la Lithosphere ; 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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The influence of prior cycling on biomechanical and cardiorespiratory response profiles during running in triathletes
Auteur(s) : Hue, Olivier Le Gallais, Daniel Chollet, Didier Boussana, Alain Prefaut, Christian
Auteurs secondaires : Adaptations au Climat Tropical, Exercice et Santé (ACTES) ; Université des Antilles et de la Guyane (UAG) Centre d'Optimisation de la Performance Motrice ; Université Montpellier 1 (UM1) Laboratoire de Physiologie des Interactions ; CHU Arnaud de Villeneuve Interface Biopsychosociale des A.P.A. ; Université Montpellier 1 (UM1) Centre d’études des transformations des activités physiques et sportives (CETAPS) ; Université de Rouen Normandie (URN) ; Normandie Université (NU) - Normandie Université (NU) Centre d'Optimisation de la Performance Motrice ; Université Montpellier 1 (UM1) Euromov (EuroMov) ; Université de Montpellier (UM) - Institut National de la Santé et de la Recherche Médicale (INSERM) - Centre Hospitalier Régional Universitaire [Montpellier] (CHRU Montpellier)
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Transmission per os du white spot syndrome virus : facteur limitant l'extension de la maladie chez les crustacés marins
Auteur(s) : Hernandez Herrera, Rosa Idalia
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MAPK signaling in cisplatin-induced death: predominant role of ERK1 over ERK2 in human hepatocellular carcinoma cells.
Auteur(s) : Guégan, Jean-Philippe Ezan, Frédéric Théret, Nathalie Langouët, Sophie Baffet, Georges
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 ) Institut National de la Santé et de la Recherche Médicale (Inserm); Université de Rennes 1; Rennes Métropole and Ligue contre le cancer du Grand Ouest. Ministère de l'Enseignement Supérieur et de la Recherche; the Fondation ARC (20120604652) (to JP.G.)
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Les apports de la gouvernance adaptative pour analyser les enjeux d’une mise en œuvre effective de la Trame Verte et Bleue. L’exemple du PNR des Volcans d’Auvergne
Auteur(s) : Angeon, Valérie Caron, Armelle Birard, Cécile Cayre, Patrick Chambon, Philippe LARADE, Arnaud Méasson, Ludovic Planchat, Claire
Auteurs secondaires : Centre de Recherche en Economie, Gestion, Modélisation et Informatique Appliquée (CEREGMIA) ; Université des Antilles et de la Guyane (UAG) Mutations des activités des espaces et des formes d'organisation dans les territoires ruraux (METAFORT) ; AgroParisTech - AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement - Institut National de la Recherche Agronomique (INRA) - VetAgro Sup - Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) Syndicat Mixte du Parc naturel régional des Volcans d’Auvergne DGER/BIPI ; Ministère de l'Agriculture de la Pêche et de l'Alimentation Agrosystèmes tropicaux (ASTRO) ; Institut National de la Recherche Agronomique (INRA) Société Française de l'Evaluation (SFE) Vous Etes D'ici (VEDI)
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