New geochronological constraints on the geological evolution of Espinhaço basin within the São Francisco Craton—Brazil

A Danderfer, B De Waele, AJ Pedreira, HA Nalini - Precambrian Research, 2009 - Elsevier
The São Francisco Craton, in the central-eastern region of Brazil, is a cratonic fragment
stabilized after the Rhyacian tectono-metamorphic event (2.25–2.05 Ga). Volcanic and …

First precise U–Pb baddeleyite ages of 1500 Ma mafic dykes from the São Francisco Craton, Brazil, and tectonic implications

EM Silveira, U Söderlund, EP Oliveira, RE Ernst… - Lithos, 2013 - Elsevier
The São Francisco Craton (SFC) is an Archaean–Proterozoic craton that hosts a significant
number of mafic intrusions. Previous attempts to date the igneous emplacement of these …

Denudation history and landscape evolution of the northern East-Brazilian continental margin from apatite fission-track thermochronology

AR Jelinek, F Chemale Jr, PA Van der Beek… - Journal of South …, 2014 - Elsevier
We reconstruct the history of denudation and landscape evolution of the northern East-
Brazilian continental margin using apatite fission-track thermochronology and thermal …

The lomagundi-jatuli carbon isotopic event recorded in the marbles from the northeast São Francisco Craton, Brazil: a review, new data, palaeogeography and …

TS Ribeiro, A Misi… - International Geology …, 2024 - Taylor & Francis
ABSTRACT The Lomagundi-Jatuli Event (LJE) is a significant positive δ13Ccarb anomaly in
Paleoproterozoic carbonates globally. In the northeast São Francisco Craton (SFC), this …

U–Pb ages and geochemistry of mafic dyke swarms from the Uauá Block, São Francisco Craton, Brazil: LIPs remnants relevant for Late Archaean break-up of a …

EP Oliveira, EM Silveira, U Söderlund, RE Ernst - Lithos, 2013 - Elsevier
The São Francisco Craton (SFC) is an Archaean craton that hosts a significant number of
mafic intrusions. Previous attempts to date the igneous emplacement of these rocks are …

Paleogeography of the Congo/São Francisco craton at 1.5 Ga: expanding the core of Nuna supercontinent

JM Salminen, DAD Evans, RIF Trindade… - Precambrian …, 2016 - Elsevier
The Congo/São Francisco (C/SF) craton, one of the largest cratons in Proterozoic
paleogeography, has been lacking reliable paleomagnetic data for the supercontinent Nuna …

The Recôncavo-Tucano-Jatobá rift and associated Atlantic continental margin basins

A Gordon, N Destro, M Heilbron - … , Eastern Brazil: Tectonic Genealogy of a …, 2017 - Springer
During the opening of the South Atlantic, in the Lower Cretaceous, the Recôncavo-Tucano-
Jatobá aborted rift, together with the Camamu-Almada and Jacuípe continental margin …

Thick chromitite of the Jacurici Complex (NE Craton São Francisco, Brazil): Cumulate chromite slurry in a conduit

JC Marques, JRVP Dias, BM Friedrich, JC Frantz… - Ore Geology …, 2017 - Elsevier
Abstract The Jacurici Complex, located in the NE part of the São Francisco Craton, hosts the
largest chromite deposit in Brazil. The mineralized intrusion is considered to be a single NS …

Revisiting the paleomagnetism of the Neoarchean Uauá mafic dyke swarm, Brazil: Implications for Archean supercratons

J Salminen, EP Oliveira, EJ Piispa, AV Smirnov… - Precambrian …, 2019 - Elsevier
The original connections of Archean cratons are becoming traceable due to an increasing
amount of paleomagnetic data and refined magmatic barcodes. The Uauá block of the …

Petrogenesis of the massive chromitite layer from the Jacurici Complex, Brazil: evidence from inclusions in chromite

BM Friedrich, JC Marques, GR Olivo, JC Frantz… - Mineralium …, 2020 - Springer
Abstract The Jacurici Complex hosts the largest chromite deposit in Brazil in an up to 8-m-
thick chromitite layer within a tectonically segmented 300-m-thick intrusion. The ore has …