U-Pb ages and geochemistry of mafic dyke swarms from the Uaua Block, Sao Francisco Craton, Brazil: LIPs remnants relevant for Late Archaean break-up of a supercraton
The Sao 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 limited to a few dates of poor precision. Here, two dyke swarms from the Uaua Block in the northeastern portion of the craton were dated using U-Pb on baddeleyite (ID-TIMS) and zircon (SIMS). The older dyke swarm trends mainl