On the mechanism of the olivine-spinel phase transformation

Author:

Hamaya Nozomu,Akimoto Syun-iti

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference19 articles.

1. High pressure chemistry of orthosilicates and the formation of the mantle transition zone;Akimoto,1976

2. Crystal Defects and Crystalline Interfaces;Bollmann,1970

3. Seismic anisotropy, flow, and constitution of the upper mantle;Carter,1972

4. The continuum theory of lattice defects;Eshelby,1956

5. Experimental investigation on the mechanism of olivine-spinel transformation: growth of single crystal spinel from single crystal olivine in Ni2SiO4;Hamaya,1982

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1. TEM Studies on the Olivine to Modified Spinel Transformation in Mg2SiO4;High-Pressure Research: Application to Earth and Planetary Sciences;2013-03-18

2. The Effect of Nonhydrostatic Stress on the α→β and α→γ Olivine Phase Transformations;High-Pressure Research: Application to Earth and Planetary Sciences;2013-03-18

3. Study of high-pressure and high-temperature behaviors and α-to-β phase transition of forsterite by first-principles and quasi-harmonic Debye model;Computer Physics Communications;2008-09

4. Formation of spinel from olivine;Applied Physics Letters;2004-03-15

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