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A curved post-garnet boundary enhances slab and plume dynamics in the Earth's mantle - Nature Geoscience

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A curved post-garnet boundary enhances slab and plume dynamics in the Earth's mantle - Nature Geoscience

The post-garnet transition has been found to have a curved phase boundary, with negative slopes in cold regions and positive slopes in hot regions of the Earth's mantle. This varying slope could be a reason for the puzzling dynamics of subducting slabs and upwelling plumes observed seismically in the upper part of the lower mantle.

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A curved post-garnet boundary enhances slab and plume dynamics in the Earth's mantle - Nature Geoscience

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A curved post-garnet boundary enhances slab and plume dynamics in the Earth's mantle - Nature Geoscience

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