The first attempts to quantify the width and height of hotspot swells were made more than 30
years ago. Since that time, topography, ocean-floor age, and sediment thickness datasets …

The concept of interplay between mantle convection and tectonics goes back to about a
century ago, with the proposal that convection currents in the Earth's mantle drive …

The number of heat flow measurements at the Earth surface has significantly increased
since the last global analysis (Pollack et al., 1993, https://doi. org/10.1029/93RG01249), and …

We propose a continental lithosphere heat production model based on the petrology of crust
and mantle, heat production measurements of surface and xenolith samples, and tectono …

Even a cursory historical look at the development of geology reveals that the cooling of the
Earth has always been a central issue (Birch, 1965; Fourier, 1824; Holmes, 1915; Joly …

The large scale structure of the earth is caused by geodynamic processes which are
explained using energetic, kinematic and dynamic descriptions. While" geodynamic …

Convective circulation of the mantle causes deflections of the Earth's surface that vary as a
function of space and time. Accurate measurements of this dynamic topography are …

Because it lies at the intersection of Earth's solid, liquid, and gaseous components, sea level
links the dynamics of the fluid part of the planet with those of the solid part of the planet …

Half‐space cooling and plate models of varying complexity have been proposed to account
for changes in basement depth and heat flow as a function of lithospheric age in the oceanic …

We reassess the applicability of the thermal plate cooling model to the subsidence of the
North Pacific, Atlantic and North Indian Ocean Basins. We use a new numerical plate model …