Abstract
The basins of the Eastern and Southeastern Brazilian margin have their origin and evolution related to the Gondwana breakup and the opening of the South Atlantic Ocean. Although the sedimentary record of the pre-rift (Juro-Cretaceous), rift (Eocretaceous), post-rift (Eocretaceous/Aptian) and drift (Eocretaceous/Albian to recent) phases, related to their tectonostratigraphic evolution, hav…