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The provenance of Late Ediacaran and Early Ordovician siliciclastic rocks in the Southwest Central Iberian Zone: Constraints from detrital zircon data on northern Gondwana margin evolution during the late Neoproterozoic

Marine GeologyEngineeringPrecambrian GeologyLate NeoproterozoicTectonic EvolutionGeologyDetrital Zircon DataGeochronologyPetrologyOrogenyEarth ScienceLate EdiacaranTectonics