Publication | Open Access

Middle Triassic trachytic lava flows associated with coeval dyke swarm in the North Patagonian Massif: A postorogenic magmatism related to extensional collapse of the Gondwanide orogen

Magmatic ProcessEarth ScienceVolcanologyEngineeringMagmatismIgneous PetrogenesisGondwanide OrogenTectonic EvolutionGeologyCoeval Dyke SwarmOrogenyPetrologyNorth Patagonian MassifTectonics