Previous compilation of crustal structure in South America had large unsampled areas
including the thin crust in the Sub‐Andean lowlands, largely estimated by gravity data, and …

Cratonic basins comprise a significant component of the Earth's continental crust and
surface geology. Their subcircular form and large areas of flat-lying, largely undeformed …

A regional Pre-Silurian unconformity marks the erosive planar base of the Phanerozoic
Parnaíba Basin (PB), and indistinctly truncates key tectonic units for the understanding of the …

The crustal structure of the Recôncavo–Tucano basin, an aborted rift system that developed
in NE Brazil during extension related to the opening of the South Atlantic Ocean, has been …

Syneclises are long-lived sedimentary basins characterized by complex subsidence and
erosion histories. The premise that these geotectonic units evolve from initial rifting …

Several sag-type basins apparently developed from rift systems, but there is no consensus
about how and if these grabens influenced the sedimentation of the post-rift thermal …

The Parnaíba intracratonic basin exhibits sedimentation that reflects the different
evolutionary stages of climate and paleogeography in the West Gondwana supercontinent …

The origin and evolution of the Pantanal basin have been investigated through velocity‐
depth profiles developed from the joint inversion of receiver functions and surface‐wave …

We assess the performance of the joint inversion of receiver functions (RF) and surface‐
wave dispersion in the characterization of the sedimentary package comprising the …

We model the contribution of the stresses generated by the topography and density
heterogeneities in the stress field of NE Brazil and the interplay between these and regional …