Post-garnet transitions in the system Mg4Si4O12–Mg3Al2Si3O12 up to 28 GPa: phase relations of garnet, ilmenite and perovskite
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Reference39 articles.
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3. Olivine-modified spinel–spinel transitions in the system Mg2SiO4–Fe2SiO4: calorimetric measurements, thermochemical calculation, and geophysical application;Akaogi;J. Geophys. Res.,1989
4. Calorimetric study on majorite–perovskite transition in the system Mg4Si4O12–Mg3Al2Si3O12: transition boundaries with positive pressure–temperature slope;Akaogi;Phys. Earth Planet. Inter.,1999
5. High pressure transitions in the system MgAl2O4–CaAl2O4: a new hexagonal aluminous phase with implication for the lower mantle;Akaogi;Phys. Earth Planet. Inter.,1999
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