Kinetics of high-pressure phase transformations: Implications to the evolution of the olivine → spinel transition in the downgoing lithosphere and its consequences on the dynamics of the mantle-Reference-Cited by-同舟云学术

Kinetics of high-pressure phase transformations: Implications to the evolution of the olivine → spinel transition in the downgoing lithosphere and its consequences on the dynamics of the mantle

Published:1976-03 Issue:1-2 Volume:31 Page:1-32
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Chien-Min Sung,Burns Roger G.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference63 articles.

1. The mineralogic distribution of iron in the upper mantle;Ahrens;Phys. Earth Planet. Inter.,1972

2. Calculated mineral reactions in the earth's mantle;Ahrens;J. Geophys. Res.,1967

3. The system MgO—FeO—SiO2 at high pressures and temperatures —phase equilibria and elastic properties;Akimoto;Tectonophysics,1972

4. Olivine—spinel transition in the system Mg2SiO4—Fe2SiO4 at 800° C;Akimoto;Earth Planet. Sci. Let.,1966

5. Olivine—spinel solid solution equilibria in the system Mg2SiO4—Fe2SiO4;Akimoto;J. Geophys. Res.,1968

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