The Sao Francisco Craton (SFC) and its marginal Aracuai and Brasilia orogens exhibit a significant diversity in their lithospheric architecture. These orogens were shaped during the Neoproterozoic-Cambrian amalgamation of West Gondwana. The rigid cratonic lithosphere of the SFC and the relatively weak lithosphere of the Aracuai Orogen were disrupted during the Cretaceous opening of the South Atlantic Ocean, whereas the Brasilia Orogen remained in the continental hinterland. In earlier research, the thermal effects of the Phanerozoic reactivations in the shallow crust of the Aracuai Orogen have been revealed by low-temperature thermochronology, mainly by apatite fission track (AFT) analysis. However, analyses from the continental interior ar...
Minor altered intrusions and drab retrogressed schists can easily be overlooked in geological studie...
The southeastern Brazilian passive margin records a complex post-rift evolution, with two parallel h...
The importance of nonrigid geological features (such as orogens) inside tectonic plates on Earth’s d...
Lithosphere of cratons and orogens generally reacts differently to tectonic events. Although these d...
The South Atlantic passive margin along the south-eastern Brazilian highlands exhibits a complex lan...
The Paleoproterozoic Transamazonian orogeny yielded a series of discrete orogens in Brazil. The pres...
Apatite fission-track (AFT) analyses, applied to Southern Brazil and Uruguay samples, was employed a...
The results of apatite fission-track analysis in 14 granitic-gneissic samples from two regional tran...
The southeastern coast of South America is an example of the complexity of passive continental margi...
The Dom Feliciano Belt in southern Brazil and Uruguay represents the western half of a Neoproterozoi...
New SHRIMP U-Pb zircon dating indicates that, contrary to previous thought, part of the Archean crus...
International audienceThere is mounting evidence that the Atlantic margin of SE Brazil has been tect...
International audienceThe difficult reconstruction of «Atlantica» Paleocontinent may remain in the g...
The Archean and Paleoproterozoic S?o Francisco craton of eastern Brazil is surrounded on all sides b...
This thesis explores the nature of the subcontinental lithosphere underlying the southwestern margin...
Minor altered intrusions and drab retrogressed schists can easily be overlooked in geological studie...
The southeastern Brazilian passive margin records a complex post-rift evolution, with two parallel h...
The importance of nonrigid geological features (such as orogens) inside tectonic plates on Earth’s d...
Lithosphere of cratons and orogens generally reacts differently to tectonic events. Although these d...
The South Atlantic passive margin along the south-eastern Brazilian highlands exhibits a complex lan...
The Paleoproterozoic Transamazonian orogeny yielded a series of discrete orogens in Brazil. The pres...
Apatite fission-track (AFT) analyses, applied to Southern Brazil and Uruguay samples, was employed a...
The results of apatite fission-track analysis in 14 granitic-gneissic samples from two regional tran...
The southeastern coast of South America is an example of the complexity of passive continental margi...
The Dom Feliciano Belt in southern Brazil and Uruguay represents the western half of a Neoproterozoi...
New SHRIMP U-Pb zircon dating indicates that, contrary to previous thought, part of the Archean crus...
International audienceThere is mounting evidence that the Atlantic margin of SE Brazil has been tect...
International audienceThe difficult reconstruction of «Atlantica» Paleocontinent may remain in the g...
The Archean and Paleoproterozoic S?o Francisco craton of eastern Brazil is surrounded on all sides b...
This thesis explores the nature of the subcontinental lithosphere underlying the southwestern margin...
Minor altered intrusions and drab retrogressed schists can easily be overlooked in geological studie...
The southeastern Brazilian passive margin records a complex post-rift evolution, with two parallel h...
The importance of nonrigid geological features (such as orogens) inside tectonic plates on Earth’s d...