Garnet-perovskite transformation under conditions of the Earth's lower mantle: an analytical transmission electron microscopy study
- 1 December 1999
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 116 (1-4) , 117-131
- https://doi.org/10.1016/s0031-9201(99)00127-2
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- High‐pressure transformation of pyrope (Mg3Al2Si3O12) in a sintered diamond cubic anvil assemblyGeophysical Research Letters, 1998
- Electrical conductivity of magnesiowüstite/perovskite produced by laser heating of synthetic olivine in the diamond anvil cellJournal of Geophysical Research, 1997
- High-pressure and high-temperature phase relations in diopside CaMgSi2O6Physics of the Earth and Planetary Interiors, 1997
- Ferric Iron Content of Mineral Inclusions in Diamonds from São Luiz: A View into the Lower MantleScience, 1997
- Transformation in Garnet from Orthorhombic Perovskite to LiNbO 3 Phase on Release of PressureScience, 1997
- The Effect of Alumina on Phase Transformations at the 660-Kilometer Discontinuity from Fe-Mg Partitioning ExperimentsScience, 1996
- An experimental study of the garnet-perovskite transformation in the system MgSiO3Mg3Al2Si3O12Physics of the Earth and Planetary Interiors, 1996
- MgSiO3‐FeSiO3‐Al2O3 in the Earth's lower mantle: Perovskite and garnet at 1200 km depthJournal of Geophysical Research, 1994
- A new high-pressure form of MgAl2O4Nature, 1991
- High-pressure and high-temperature phase relations in CaSiO3 and CaMgSi2O6 and elasticity of perovskite-type CaSiO3Physics of the Earth and Planetary Interiors, 1989