Tetragonal almandine pyrope phase (TAPP): retrograde Mg-perovskite from subducted oceanic crust? Tetragonal almandine pyrope phase (TAPP): retrograde Mg-perovskite from subducted oceanic crust? (2012)
Attributed to:
How did Earth's Mantle Become Oxidized? The Role of Perovskite Crystal Chemistry in Earth's Evolution
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1127/0935-1221/2012/0024-2211
Publication URI: http://dx.doi.org/10.1127/0935-1221/2012/0024-2211
Type: Journal Article/Review
Parent Publication: European Journal of Mineralogy
Issue: 4