Do mantle plumes preserve the heterogeneous structure of their deep-mantle source?
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We simulate thermo-chemical plumes across a wide parameter-space, in 2-D and 3-D.

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Two conduit regimes emerge: (i) bilaterally asymmetric; and (ii) concentric.

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Bilateral: occurs over a limited parameter-space and preserves deep-mantle structure.

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Concentric: dominates parameter-space but does not preserve deep-mantle structure.

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Conclusion: deep-mantle structure may not be preserved during plume ascent.

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