Abstract
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 language | English (US) |
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Pages (from-to) | 335-336 |
Number of pages | 2 |
Journal | Nature Geoscience |
Volume | 6 |
Issue number | 5 |
DOIs | |
State | Published - Jan 1 2013 |
ASJC Scopus subject areas
- General Earth and Planetary Sciences