Tectono-sedimentary evolution of the Suriname margin in the cretaceous: A sequence-stratigraphic framework

V Delhaye-Prat, J Bourget, G Gaillot, J Gaillot… - Earth-Science …, 2024 - Elsevier
The offshore margins of Guyana, Suriname, and French Guyana (the “Guyanas Equatorial
Margin”) have become the focus of active hydrocarbon exploration over the last decade, with …

The protracted evolution of a plate boundary: Eastern Cuba block and Old Bahamas Channel

A Oliviera de Sá, S Leroy, E d'Acremont… - Geochemistry …, 2024 - Wiley Online Library
Abstract The Eastern Cuban block has experienced a complex tectonic history characterized
by plate interactions, resulting in a diverse array of geological features observable in the …

[HTML][HTML] Along-strike variation in volcanic addition controlling post-breakup sedimentary infill: Pelotas margin, austral South Atlantic

MC Cassel, N Kusznir, G Manatschal, D Sauter - Solid Earth, 2024 - se.copernicus.org
We investigate, using observations from seismic reflection data, the lateral variability in
breakup extrusive magmatic addition along the strike of the Pelotas segment of the austral …

Mantle Deformation Processes During the Rift‐To‐Drift Transition at Magma‐Poor Margins

NJ Montiel, E Masini, L Lavier… - Geochemistry …, 2023 - Wiley Online Library
The rift‐to‐drift transition at rifted margins is an area of active investigation due to an
incomplete understanding of the spatial and temporal evolution of physical and chemical …

[PDF][PDF] Inverted Magma-rich Versus Magma-poor Rifted Margins: Implications for Early Orogenic Systems

J Gómez-Romeu, S Jammes, M Ducoux, R Lescoutre… - Tektonika, 2023 - researchgate.net
Mountain belts are often the result of former inverted rifts or rifted margins. Up to date, relics
of magma-poor rifted margins have been found in orogens allowing the investigation of how …