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Neogene evolution and demise of the Amapá carbonate platform, Amazon continental margin, Brazil ArchiMer
Cruz, A.m.; Reis, A.t.; Suc, J.p.; Silva, C.g.; Praeg, D.; Granjeon, D.; Rabineau, Marina; Popescu, S.m.; Gorini, C..
The Amazon continental shelf hosted one of the world's largest mixed carbonate-siliciclastic platforms from the late Paleocene onwards - the Amapá carbonates. The platform architecture, however, remains poorly understood and causes and timing of the cessation of carbonate deposition are still controversial. Here we present a stratigraphic analysis of the Neogene succession of the Amapá carbonates, based on a grid of 2D/3D seismic data correlated to revised micropaleontological data from exploration wells. The results provide improved constraints on the age of the transition from predominantly carbonate to siliciclastic sedimentation, which is shown to have varied through time across three different sectors of the shelf (NW, Central and SE). Four Neogene...
Tipo: Text Palavras-chave: Mixed carbonate-siliciclastic platform; Carbonate architecture; Chonostratigraphic model; Non-eustatic accommodation; Shelf paleogeography.
Ano: 2019 URL: https://archimer.ifremer.fr/doc/00489/60066/63351.pdf
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Tectonics and sedimentation interactions in the east Caribbean subduction zone: An overview from the Orinoco delta and the Barbados accretionary prism ArchiMer
Deville, Eric; Mascle, A.; Callec, Y.; Huyghe, P.; Lallemant, S.; Lerat, O.; Mathieu, X.; De Carillo, C. Padron; Patriat, Martin; Pichot, Thibaud; Loubrieux, B.; Granjeon, D..
Several marine geophysical data and piston-coring surveys acquired during the last decade allow one to better understand the close dynamic interactions between the sand-rich Orinoco turbidite system and the compressional structures of the Barbados prism. These interactions have been active since Eocene time as illustrated by the study of outcrops onshore Barbados Island. Because of strong morphologic and tectonic control in the east-Caribbean active margin, the present-day Orinoco turbiditic pattern system does not exhibit a classic fan geometry. The sea-floor geometry between the slope of the front of the Barbados prism and the slope of the South-American margin induces the convergence of the turbidite channels toward the abyssal plain, at the front of...
Tipo: Text Palavras-chave: Turbidite system; Active margin; Orinoco; Barbados.
Ano: 2015 URL: https://archimer.ifremer.fr/doc/00252/36373/34913.pdf
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