FN Archimer Export Format
PT J
TI Genetic relations between the Aves Ridge and the Grenada back‐arc Basin, East Caribbean Sea
BT 
AF Garrocq, Clément
   Lallemand, Serge
   Marcaillou, Boris
   Lebrun, Jean‐Frédéric
   Padron, Crelia
   Klingelhoefer, Frauke
   Laigle, Mireille
   Münch, Philippe
   Gay, Aurelien
   Schenini, Laure
   Beslier, Marie‐Odile
   Cornée, Jean‐Jacques
   Mercier de Lépinay, Bernard
   Quillévéré, Frédéric
   BouDagher‐Fadel, Marcelle
AS 1:1;2:1;3:2;4:3;5:4,5;6:5;7:2;8:1;9:1;10:2;11:2;12:1;13:2;14:6;15:7;
FF 1:;2:;3:;4:;5:;6:PDG-REM-GM-LAD;7:;8:;9:;10:;11:;12:;13:;14:;15:;
C1 Géosciences Montpellier CNRS Université de Montpellier Université des Antilles Place Eugène Bataillon 34095, Montpellier, France
   GéoazurUniversité Côte d'AzurCNRS IRD Observatoire de la Côte d'Azur Géoazur 250 Avenue Albert Einstein 06560 Valbonne, France
   Géosciences Montpellier Université des Antilles CNRS Université de MontpellierCampus de FouillolePointe‐à‐Pitre, Guadeloupe, France
   Departamento de Ciencias de la Tierra Universidad Simón Bolívar (USB )Caracas, Venezuela
   Géosciences Marines, Ifremer ZI de la Pointe du Diable CS 1007029280 Plouzané, France
   Université de Lyon, Université Claude Bernard Lyon 1LGLTPECNRSBd du 11 Novembre 191869622 Villeurbanne, France
   Office of the Vice‐Provost (research), University College London, 2 Taviton street, London, WC1h 0BT, UK
C2 UNIV MONTPELLIER, FRANCE
   UNIV NICE, FRANCE
   UNIV ANTILLES, FRANCE
   UNIV SIMON BOLIVAR, VENEZUELA
   IFREMER, FRANCE
   UNIV LYON, FRANCE
   UNIV COLL LONDON, UK
SI BREST
SE PDG-REM-GM-LAD
IN WOS Ifremer UPR
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 4.39
TC 26
UR https://archimer.ifremer.fr/doc/00665/77704/79792.pdf
   https://archimer.ifremer.fr/doc/00665/77704/79797.pdf
   https://archimer.ifremer.fr/doc/00665/77704/79799.zip
LA English
DT Article
CR GARANTI
BO L'Atalante
DE ;Grenada Basin;Aves Ridge;back-arc basin;seismic reflection;Caribbean
AB The Grenada Basin separates the active Lesser Antilles Arc from the Aves Ridge, described as a Cretaceous‐Paleocene remnant of the ‘Great Arc of the Caribbean'. Although various tectonic models have been proposed for the opening of the Grenada Basin, the data on which they rely are insufficient to reach definitive conclusions. This paper presents a large set of deep‐penetrating multichannel seismic reflection data and dredge samples acquired during the GARANTI cruise in 2017. By combining them with published data including seismic reflection data, wide‐angle seismic data, well data and dredges, we refine the understanding of the basement structure, depositional history, tectonic deformation and vertical motions of the Grenada Basin and its margins as follows: 1) rifting occurred during the late Paleocene‐early Eocene in a NW‐SE direction and led to seafloor spreading during the middle Eocene; 2) this newly formed oceanic crust now extends across the eastern Grenada Basin between the latitude of Grenada and Martinique; 3) asymmetrical pre‐Miocene depocenters support the hypothesis that the southern Grenada Basin originally extended beneath the present‐day southern Lesser Antilles Arc and probably partly into the present‐day forearc before the late Oligocene‐Miocene rise of the Lesser Antilles Arc; 4) the Aves Ridge has subsided along with the Grenada Basin since at least the middle Eocene, with a general subsidence slowdown or even an uplift during the late Oligocene, and a sharp acceleration on its southeastern flank during the late Miocene. Until this acceleration of subsidence, several bathymetric highs remained shallow enough to develop carbonate platforms. 
PY 2021
PD FEB
SO Journal Of Geophysical Research-solid Earth
SN 2169-9313
PU American Geophysical Union
VL 126
IS 2
UT 000631921200034
DI 10.1029/2020JB020466
ID 77704
ER

EF