The continental margin of southeast Brazil is elevated. Onshore Tertiary basins and Late
Cretaceous/Paleogene intrusions are good evidence for post breakup tectono‐magmatic …

On the continental margin of southeast Brazil there is good geological evidence for post-rift
tectonic reactivation, in the form of onshore Tertiary basins up to 800m deep and Cretaceous …

Studies on the geomorphological evolution of the South American passive margin have
been based on the pediplanation model, which predicts that its morphology is a response to …

The Mesozoic sediments of the Araripe Basin peak at ca. 1000 m, more than 500 m above
the host Precambrian basement. This means that an intracontinental graben has been …

We investigate the evolution of uplifted areas in NE Brazil, which have been considered as
residual landforms. The study focuses on the 130km-long, 41km-wide Pereiro Massif (PM) …

The area between São Paulo and Porto Alegre in southeastern Brazil plays a key area to
understand and quantify the evolution of the South Atlantic passive continental margin …

Abstract The South Atlantic passive margin along the south-eastern Brazilian highlands
exhibits a complex landscape, including a northern inselberg area and a southern elevated …

Low-temperature thermochronology focuses on the comprehension of the upper crust's
thermal history, where morphotectonic processes take place. We present a robust …

We present a novel age-equation calibration for fission-track age determinations by laser
ablation inductively coupled plasma mass spectrometry. This new calibration incorporates …

We investigate the role of reactivation of Precambrian basement fabric in the tectono-
sedimentary and geomorphological evolution of the Paraíba Basin, continental margin of …