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Showing 1 to 1 of 1 for “"stagnant-lid convection"”.
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The Influence of Curvature on Mantle Convection featuring a Temperature-dependent Viscosity
Convection in the silicate mantles or ice layers of terrestrial planets and moons is characterized by a strongly temperature-dependent viscosity. Mantle convection regime is first examined in 2D and 3D spherical geometry with varying mantle curvature (core-to-surface radii-ratio, f) and constant …