The stability and equation of state of majoritic garnet synthesized from natural basalt at mantle conditions
- 15 November 1996
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 23 (23) , 3377-3380
- https://doi.org/10.1029/96gl03027
Abstract
No abstract availableThis publication has 25 references indexed in Scilit:
- MgSiO3‐FeSiO3‐Al2O3 in the Earth's lower mantle: Perovskite and garnet at 1200 km depthJournal of Geophysical Research, 1994
- Static compression of chondrodite: Implications for water in the upper mantleGeophysical Research Letters, 1994
- Melting phase relations of an anhydrous mid‐ocean ridge basalt from 3 to 20 GPa: Implications for the behavior of subducted oceanic crust in the mantleJournal of Geophysical Research, 1994
- THE FATE OF DESCENDING SLABSAnnual Review of Earth and Planetary Sciences, 1994
- Mantle control of a dynamically evolving spreading center: Mid-Atlantic Ridge 31–34°SEarth and Planetary Science Letters, 1994
- Compositional vs. thermal buoyancy and the evolution of subducted lithosphereGeophysical Research Letters, 1994
- Tomographic imaging of subducted lithosphere below northwest Pacific island arcsNature, 1991
- Is subducted lithosphere trapped at the 670-km discontinuity?Nature, 1988
- Transition region of the Earth's upper mantleNature, 1986
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981