Publication | Closed Access

Tectonically-driven mud volcanism since the late Pliocene on the Calabrian accretionary prism, central Mediterranean Sea

Marine GeologyEngineeringCentral Mediterranean SeaQuaternary Tectonic DeformationTectonic EvolutionGeologyCalabrian Accretionary PrismOrogenyTectonically-driven Mud VolcanismSedimentologyCentral MediterraneanTectonics