Based on a vast set of in situ data, a first comprehensive overview of the oceanographic
characteristics of Baía de Todos os Santos (BTS) is provided. BTS is the second largest …

The eastern continental margin of South America comprises a series of rift basins developed
during the breakup of Pangea in the Jurassic–Cretaceous. We integrated high resolution …

From the Parnaiba Basin to the Borborema Plateau (northeastern Brazil), the crystalline and
sedimentary highlands and plains of the huge Jaguaribe–Piranhas amphitheatre are …

Using the average directions of the main wave-fronts which approach the coast of Bahia
State-coinciding with that of the main wind occurring in the area-and of their periods, we …

The Brazilian Northeast affords good opportunities for obtaining reliable timings and rates of
landscape evolution based on stratigraphic correlations across a vast region. The landscape …

The Barreiras Group is a Miocene to Lower Pleistocene continental terrigenous sedimentary
deposit exhibiting a large occurrence along the Brazilian coast. In the Conde region, located …

Todos os Santos Bay is a large ($\approx $1000 km²), structurally controlled tidal bay in
northeast Brazil. Three main drainage basins debouch into the bay, providing a mean …

Quaternary post-Barreiras sediments are widespread along Brazil's passive margin. These
deposits are well exposed in the onshore Paraíba Basin, which is one of the rift basins …

The continental margin of Northeast Brazil (NE Brazil) is the most seismogenic of the
passive margin of South America and has several evidence of neotectonics. However, the …

The majority of numerical models of landscape evolution in divergent margins are focused
on the simulation of margins with simplified lithological control on landscape erosion …