74 documents satisfont la requête.
Joint inversion of teleseismic and GOCE gravity data: application to the Himalayas
Auteur(s) : Basuyau, Clemence Diament, M. Tiberi, Christel Hetenyi, G. Vergne, J. Peyrefitte, A.
Auteurs secondaires : 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) 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) Eidgenössische Technische Hochschule [Zürich] (ETH Zürich) Sismologie ; Ecole et Observatoire des sciences de la terre de Strasbourg (EOSTS) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université Louis Pasteur - Strasbourg I - Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Université Louis Pasteur - Strasbourg I - Centre National de la Recherche Scientifique (CNRS) - Institut de physique du globe de Strasbourg (IPGS) ; Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)
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Perspectives de developpement des DCP ancres dans les Petites Antilles. L'exemple de trois iles: Guadeloupe, Martinique et Curacao
Auteur(s) : Reynal, Lionel Van Buurt, G Taquet, Marc
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Spatial patterns of rainfall regimes related to levels of double cropping agriculture systems in Mato Grosso (Brazil)
Auteur(s) : Arvor, Damien Dubreuil, Vincent Ronchail, Josyane Meirelles, Margareth Simões Penello Funatsu, B. M.
Auteurs secondaires : Espace pour le Développement (ESPACE-DEV) ; Université Montpellier 2 - Sciences et Techniques (UM2) - Université des Antilles et de la Guyane (UAG) - Institut de recherche pour le développement [IRD] - Université de la Réunion Littoral, Environnement, Télédétection, Géomatique (LETG - Costel) ; Université de Nantes (UN) - Université de Caen Basse-Normandie - Université de Bretagne Occidentale (UBO) - Université de Rennes II - Haute Bretagne - CNRS Université Rennes 2 - UFR Sciences sociales (UR2 UFRSS) ; Université européenne de Bretagne (UEB) - Université de Rennes II - Haute Bretagne Centre Armoricain de Recherche en Environnement (CARE) ; CNRS - Institut national de la recherche agronomique (INRA) - Ecole Nationale Supérieure Agronomique de Rennes - Université de Rennes 1 (UR1) - Université de Rennes II - Haute Bretagne Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) ; CNRS - Université Pierre et Marie Curie - Paris 6 (UPMC) - Muséum national d'histoire naturelle (MNHN) - Institut de recherche pour le développement [IRD] - INSU Departamento de Engenharia de Sistemas e Computação – Pos Graduação em Geomatica (Departamento de Engenharia de Sistemas e Computação) ; Universidade do Estado do Rio de Janeiro Laboratoire de Météorologie Dynamique (LMD) ; CNRS - INSU - Polytechnique - X - École normale supérieure - Paris (ENS Paris) - Université Pierre et Marie Curie - Paris 6 (UPMC) ANR-06-BLAN-0176, DURAMAZ, Les déterminants géographiques, démographiques et socio-économiques de la durabilité en Amazonie brésilienne.(2006)
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CAREST—Multilingual Regional Integration for Health Promotion and Research on Sickle Cell Disease and Thalassemia
Auteur(s) : Knight-Madden, Jennifer Romana, Marc Villaescusa, Rinaldo Reid, Marvin Etienne-Julan, Maryse Boutin, Laurence Elana, Gisèle Elenga, Narcisse
Auteurs secondaires : Sickle Cell Unit, Tropical Medicine Research Institute ; Sickle Cell Unit, Tropical Medicine Research Institute 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) Institut d'hématologie et d'immunologie, La Havane Unité Transversale de la Drépanocytose ; CHU Pointe-à-Pitre/Abymes EA 3593 Université des Antilles et de la Guyane ; Service de Pédiatrie ; Centre Hospitalier de Cayenne Andrée Rosemon - Centre Hospitalier de Cayenne Andrée Rosemon Centre d'investigation clinique Antilles-Guyane ; Institut National de la Santé et de la Recherche Médicale (INSERM) - CH Cayenne Epidémiologie Clinique et Médecine EA 4097 (ECM) ; UFR des sciences médicales de l'UAG 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)
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Système d’acteurs et gestion littorale aux Antilles
Auteur(s) : Desse, Michel
Auteurs secondaires : Migrations internationales, espaces et sociétés (MIGRINTER UMR 7301) ; Centre National de la Recherche Scientifique (CNRS) - Université de Poitiers 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 production aquacole de coquille Saint-Jacques (Pecten maximus) et le soutien scientifique à l'operation pilote
Auteur(s) : Dao, Jean-claude Barret, Jean Carval, Jean-pierre Connan, Jean-paul Corre, Christian Devauchelle, Nicole Fleury, Pierre-gildas Laurent, Pascale
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Method for identifying spatial reservoirs of malaria infection and control strategies
Auteur(s) : Zongo, Pascal Dorville, René Gouba, Elisée
Auteurs secondaires : L3MA-Laboratoire des matériaux et molécules en milieu Agressif
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Signatures de transitions démographiques des arbres de la Forêt Tropicale Humide du plateau des Guyanes
Auteur(s) : Barthe, Stéphanie
Auteurs secondaires : Antilles-Guyane Scotti, Ivan Hérault, Bruno
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Different behavioural strategies among seven highly invasive ant species
Auteur(s) : Bertelsmeier, Cleo Avril, Amaury Blight, Olivier Confais, Amandine Diez, Lise Jourdan, Hervé Orivel, Jérôme St Germes, Noemie
Auteurs secondaires : Ecologie Systématique et Evolution (ESE) ; Université Paris-Sud - Paris 11 (UP11) - AgroParisTech - Centre National de la Recherche Scientifique (CNRS) Université d'Avignon et des Pays de Vaucluse (UAPV) Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE) ; Université d'Avignon et des Pays de Vaucluse (UAPV) - Aix Marseille Université (AMU) - Institut national des sciences de l'Univers (INSU - CNRS) - INEE - INSB - Institut de recherche pour le développement [IRD] : UMR237 - 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 - Centre National de la Recherche Scientifique (CNRS)
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Analyse du comportement des flottilles de pêche de Boulogne sur Mer
Auteur(s) : Allard, M. O.
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Determinantes de la satisfacción de los navegantes europeos con los puertos de escala de Canarias (España)
Auteur(s) : E. Lam-González, Yen J. León, Carmelo M. González Hernández, Matías
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Online Sketch Recognition with Incremental Fuzzy Models
Auteur(s) : Tencer, Lukas Režnáková, Marta Cheriet, Mohamed
Auteurs secondaires : Département de génie de la production automatisée ; Ecole de Technologie Supérieure [Montréal] (ETS) International Graphonomics Society (IGS) Université des Antilles (UA) Céline Rémi Lionel Prévost Eric Anquetil
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Les relations entre l'Union européenne et les organisations d'intégration économique régionale d'Amérique latine et des Caraïbes - Quelles mutations ? ; The relationship between the European Union and the organisations of economic regional integration from Latin America and the caribbean basin - which mutations ?
Auteur(s) : Nelzin de Pizzol, Audrey
Auteurs secondaires : Antilles-Guyane Perrot, Danielle Ténier, Jacques
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Potential of Bagassa guianensis and Cordia alliodora for planting under the tropics : Description of an optimal growth strategy mixing high growth rate and good wood quality ; Potentiel de Bagassa guianensis et Cordia alliodora pour la plantation en zone tropicale : Description d'une stratégie de croissance optimale alliant vitesse de croissance et qualité du bois
Auteur(s) : Bossu, Julie
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) Université de Guyane Bruno Clair Jacques Beauchêne
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Les apprentissages sur l'aménagement côtier dans deux territoires côtiers du littoral acadien du Nouveau-Brunswick vulnérables à l'érosion et aux inondations
Auteur(s) : Chouinard, Omer Rabeniaina, Tiavina Weissenberger, Sebastian
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Pervasive Local-Scale Tree-Soil Habitat Association in a Tropical Forest Community
Auteur(s) : Allie, Elodie Pélissier, Raphaël Engel, Julien Petronelli, Pascal Freycon, Vincent Deblauwe, Vincent Soucémarianadin, Laure Weigel, Jean
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) 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]) Centre National de la Recherche Scientifique (CNRS) Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) UPR BSEF ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) Diversité, adaptation, développement des plantes (DIADE) ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Institut de Recherche pour le Développement (IRD [France-Sud]) International Center for Tropical Botany, Department of Biological Sciences ; University of Florida Fonds Social Européen ; La Région Guyane ; Centre National d'Etudes Spatiales (CNES) ; Université des Antilles et de la Guyane (UAG) ; "Investissement d'Avenir" grant Agence Nationale de la Recherche (CEBA) ANR-10-LABX-25-01
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Rutas Alimentarias: una estrategia de negocios inclusivos que vincula las políticas agrarias y turísticas
Auteur(s) : Barrera, Ernesto Bringas Alvarado, Olivia
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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
Caribbean Island Tourism: Pathway to Continued Colonial Servitude
Auteur(s) : Wong, Alfred
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Large-scale population genetic structure in Bonelli's Eagle Aquila fasciata
Auteur(s) : Mira, Sara Arnaud-haond, Sophie Palma, Luis Cancela, Maria Leonor Beja, Pedro
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