Buoyancy of slabs and plumes enhanced by curved post-garnet phase boundary
Buoyancy of slabs and plumes enhanced by curved post-garnet phase boundary
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Publisher
London: Nature Publishing Group UK
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Language
English
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Publisher
London: Nature Publishing Group UK
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Contents
Mantle convection manifests in the subduction of cold slabs and the upwelling of hot plumes, driving both near-surface processes such as volcanism and seismicity and the chemical evolution of the Earth’s interior. Phase transitions of mantle minerals at high pressure are associated with changes in density and viscosity. Mantle convection is either...
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Full title
Buoyancy of slabs and plumes enhanced by curved post-garnet phase boundary
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TN_cdi_proquest_journals_2861509743
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2861509743
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ISSN
1752-0894
E-ISSN
1752-0908
DOI
10.1038/s41561-023-01244-w
