Terra Nova · 2003 · 50 citations · 32 references
Natural SciencesEarth SciencesGeophysicsPhysical OceanographyTectonicsTectonophysicsPlate TectonicsThermal StructureContinental Heat FlowLithospheric EvolutionSubduction-related MagmatismSurface Heat FlowTectonic Boundary EvolutionThermal Evolution Of LithospheresTransient Thermal BehaviorTransient Thermal Evolution
Abstract The present heat flow in the southern Tyrrhenian Sea appears as a transient thermal wave that has migrated eastward in time. The higher heat flow in the south‐eastern side of the basin confirms the suggestion of an eastward‐migrating rift. Punctuation of the Tyrrhenian backarc extension in lithospheric boudins is accompanied by a concentrated increase in heat flow generated by asthenospheric intrusions and related magmatism progressively moving eastward. The migration of the asthenosphere in the same direction could explain these phenomena.
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Some remarks on the development of sedimentary basins
Dan McKenzie · Earth and Planetary Science Letters · 1978 · 3.9K citations