Mineralogy: Garnet goes hungry

Craig R Bina*

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

14 Scopus citations


Sinking slabs of oceanic lithosphere often stagnate in Earth's mantle. Experiments show that common slab minerals transform to their high-pressure, high-density counterparts at very slow rates, thus keeping the slabs buoyant and impeding subduction.

Original languageEnglish (US)
Pages (from-to)335-336
Number of pages2
JournalNature Geoscience
Issue number5
StatePublished - Jan 1 2013

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)


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