Add to ORKGThe structure of the lithosphere is key to reconciling the dynamic topography predicted by mantle convection models with residual topography derived from observations, suggest analyses of both models and data
Earth\u27s large-scale topography and lower-mantle structure are linked to past tectonic motions and...
It has long been known that solid-state convection within Earth\u27s mantle should result in deforma...
Elevations on Earth are dominantly controlled by crustal buoyancy, primarily through variations in c...
Earth's surface topography is a direct physical expression of our planet's dynamics. Most is isostat...
While the bulk of topography on Earth is generated and maintained by variations in the thickness and...
The changing pattern of convective circulation in the Earth’s mantle induces slowly developing, vert...
Dynamic topography, the surface deflection induced by sublithosheric mantle flow, is an important pr...
Convective circulation of the Earth’s mantle maintains some fraction of surface topography that vari...
Dynamic topography, the surface deflection induced by sublithosheric mantle flow, is an important pr...
Dynamic topography, the surface deflection induced by sublithosheric mantle flow, is an important pr...
Oceanic residual depth varies on urn:x-wiley:jgrb:media:jgrb54314:jgrb54314-math-0001 5,000 km wavel...
The long-wavelength geoid and topography are dynamic effects of a convecting mantle. The long-wavele...
Contrasting results on the magnitude of the dynamic component of topography motivate us to analyse t...
Contrasting results on the magnitude of the dynamic component of topography motivate us to analyse t...
In the oceans, our understanding of plate subsidence as a function of age permits residual depth ano...
Earth\u27s large-scale topography and lower-mantle structure are linked to past tectonic motions and...
It has long been known that solid-state convection within Earth\u27s mantle should result in deforma...
Elevations on Earth are dominantly controlled by crustal buoyancy, primarily through variations in c...
Earth's surface topography is a direct physical expression of our planet's dynamics. Most is isostat...
While the bulk of topography on Earth is generated and maintained by variations in the thickness and...
The changing pattern of convective circulation in the Earth’s mantle induces slowly developing, vert...
Dynamic topography, the surface deflection induced by sublithosheric mantle flow, is an important pr...
Convective circulation of the Earth’s mantle maintains some fraction of surface topography that vari...
Dynamic topography, the surface deflection induced by sublithosheric mantle flow, is an important pr...
Dynamic topography, the surface deflection induced by sublithosheric mantle flow, is an important pr...
Oceanic residual depth varies on urn:x-wiley:jgrb:media:jgrb54314:jgrb54314-math-0001 5,000 km wavel...
The long-wavelength geoid and topography are dynamic effects of a convecting mantle. The long-wavele...
Contrasting results on the magnitude of the dynamic component of topography motivate us to analyse t...
Contrasting results on the magnitude of the dynamic component of topography motivate us to analyse t...
In the oceans, our understanding of plate subsidence as a function of age permits residual depth ano...
Earth\u27s large-scale topography and lower-mantle structure are linked to past tectonic motions and...
It has long been known that solid-state convection within Earth\u27s mantle should result in deforma...
Elevations on Earth are dominantly controlled by crustal buoyancy, primarily through variations in c...