Thermally stable regional inversion lenses below the Pacific and Africa survive strong chemical buoyancy in thermochemical core simulations, and light elements accumulate near the poles to form chemically stable layers.
Bouffard , author G
3 Pith papers cite this work, alongside 222 external citations. Polarity classification is still indexing.
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representative citing papers
Top-heavy thermochemical geodynamo simulations show heterogeneous outer boundary heat flux reproduces observed longitudinal inclination anomaly variations, while elevated chemical driving reduces longitudinal structures and promotes polar radial field minima.
citing papers explorer
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Thermochemical models of outer core convection with heterogeneous core-mantle boundary heat flux
Thermally stable regional inversion lenses below the Pacific and Africa survive strong chemical buoyancy in thermochemical core simulations, and light elements accumulate near the poles to form chemically stable layers.
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Paleomagnetic signatures of core-mantle interactions inferred from top-heavy thermochemical geodynamo simulations
Top-heavy thermochemical geodynamo simulations show heterogeneous outer boundary heat flux reproduces observed longitudinal inclination anomaly variations, while elevated chemical driving reduces longitudinal structures and promotes polar radial field minima.
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