Publication | Closed Access

Two generations of mafic dyke swarms in the Southeastern Brazilian coast: reactivation of structural lineaments during the gravitational collapse of the Araçuaí-Ribeira Orogen (500 Ma) and West Gondwana breakup (140 Ma)

GeophysicsMarine GeologyEngineeringStructural GeologyMafic Dyke SwarmsGeographySoutheastern Brazilian CoastGeologyRegional TectonicsGravitational CollapseOrogenyEarth ScienceTectonics