The southeast Brazilian rifted continental margin is not a single, continuous upwarp: Variations in morphology and denudation patterns along the continental drainage divide
Tobias Fonte-Boa, Daniel Peifer, Ana Fonseca, Tiago Amâncio Novo
Topics & Concepts
EscarpmentDenudationContinental marginGeologyRiftContinental shelfPaleontologyPassive marginTectonicsOceanographyGeological and Geochemical AnalysisGeological formations and processesearthquake and tectonic studies