On the global geodynamic consequences of different phase boundary morphologies
<p>Phase transitions can influence mantle convection patterns, inhibiting or promoting vertical flow. One such transition is the ringwoodite-to-bridgmanite plus periclase transition, which has a negative Clapeyron slope and therefore reduces mantle flow between the upper and lower mantle. Inte...
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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-05-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/16/297/2025/se-16-297-2025.pdf |
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