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Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantle

GeophysicsPlate TectonicsSpherical ModelEngineeringMantle DynamicMagnetohydrodynamicsKm DepthEndothermic Phase TransitionLithosphereEarth System ScienceCrust-mantle InteractionEarth ScienceMantle GeochemistryTectonics