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Fluid Dynamics Research, 2008
The solid-state convection in the Earth mantle is characterized by plate tectonics, which shapes the tectonic activities of the Earth, and superplumes as broad hot regions chemically distinct from the surrounding regions in deep lower mantle. Recent numerical studies of mantle convection suggest that the rigidly moving plates occur on the Earth because
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The solid-state convection in the Earth mantle is characterized by plate tectonics, which shapes the tectonic activities of the Earth, and superplumes as broad hot regions chemically distinct from the surrounding regions in deep lower mantle. Recent numerical studies of mantle convection suggest that the rigidly moving plates occur on the Earth because
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Mountain building, mantle convection, and supercontinents: revisited
Earth and Planetary Science Letters, 2021Thorsten Becker +2 more
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Benchmarking multiphysics software for mantle convection
Computers and Geosciences, 2021Sean Trim +2 more
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A benchmark comparison for mantle convection codes
Geophysical Journal International, 1989Hartwig Harder +2 more
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