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Boland, J. N., Liebermann, Robert C. (1983) Mechanism of the olivine to spinel phase transformation in Ni2SiO4. Geophysical Research Letters, 10 (1) 87-90 doi:10.1029/gl010i001p00087

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Reference TypeJournal (article/letter/editorial)
TitleMechanism of the olivine to spinel phase transformation in Ni2SiO4
JournalGeophysical Research Letters
AuthorsBoland, J. N.Author
Liebermann, Robert C.Author
Year1983 (January)Volume10
Issue1
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/gl010i001p00087Search in ResearchGate
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Mindat Ref. ID761131Long-form Identifiermindat:1:5:761131:9
GUID0
Full ReferenceBoland, J. N., Liebermann, Robert C. (1983) Mechanism of the olivine to spinel phase transformation in Ni2SiO4. Geophysical Research Letters, 10 (1) 87-90 doi:10.1029/gl010i001p00087
Plain TextBoland, J. N., Liebermann, Robert C. (1983) Mechanism of the olivine to spinel phase transformation in Ni2SiO4. Geophysical Research Letters, 10 (1) 87-90 doi:10.1029/gl010i001p00087
In(1983, January) Geophysical Research Letters Vol. 10 (1) American Geophysical Union (AGU)

See Also

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Guyot, François, Gwanmesia, Gabriel D., Liebermann, Robert C. (1991) An olivine to beta phase transformation mechanism Mg2SiO4. Geophysical Research Letters, 18 (1) 89-92 doi:10.1029/90gl02719
Remsberg, Anne R., Boland, James N., Gasparik, Tibor, Liebermann, Robert C. (1988) Mechanism of the olivine-spinel transformation in Co2SiO4. Physics and Chemistry of Minerals, 15 (5) 498-506 doi:10.1007/bf00311131
Burnley, Pamela C., Bassett, William A., Wu, Tzy-chung (1995) Diamond anvil cell study of the transformation mechanism from the olivine to spinel phase in Co2SiO4, Ni2SiO4, and Mg2GeO4. Journal of Geophysical Research: Solid Earth, 100. 17715-17723 doi:10.1029/95jb01578
Liebermann, Robert C. (1973) Elasticity of the olivine-spinel and olivine-β phase transformations and the 400-kilometer discontinuity of the mantle. Journal of Geophysical Research, 78 (29) 7015-7017 doi:10.1029/jb078i029p07015
Boland, J. N., Liu, Lin-gun (1983) Olivine to spinel transformation in Mg2SiO4 via faulted structures. Nature, 303 (5914). 233-235 doi:10.1038/303233a0
Liebermann, Robert C. (1970) Velocity-density systematics for the olivine and spinel phases of Mg2SiO4-Fe2SiO4. Journal of Geophysical Research, 75 (20) 4029-4034 doi:10.1029/jb075i020p04029
Akimoto, Syun-iti, Fujisawa, Hideyuki, Katsura, Takashi (1965) The olivine-spinel transition in Fe2SiO4and Ni2SiO4. Journal of Geophysical Research, 70 (8) 1969-1977 doi:10.1029/jz070i008p01969
Hamaya, Nozomu, Akimoto, Syun-iti (1982) Experimental Investigation on the Mechanism of Olivine → Spinel Transformation: Growth of Single Crystal Spinel from Single Crystal Olivine in Ni2SiO4. In High-Pressure Research in Geophysics. Springer Netherlands. p.373-389. doi:10.1007/978-94-009-7867-6_29
Burnley, Pamela C., Green, Harry W., Prior, David J. (1991) Faulting associated with the olivine to spinel transformation in Mg2GeO4and its implications for deep-focus earthquakes. Journal of Geophysical Research, 96. 425 doi:10.1029/90jb01937
Li, Baosheng, Gwanmesia, Gabriel D., Liebermann, Robert C. (1996) Sound velocities of olivine and beta polymorphs of Mg2SiO4at Earth's transition zone pressures. Geophysical Research Letters, 23 (17) 2259-2262 doi:10.1029/96gl02084
Wang, Yanbin, Liebermann, Robert C., Boland, James N. (1988) Olivine as an in situ piezometer in high pressure apparatus. Physics and Chemistry of Minerals, 15 (5) 493-497 doi:10.1007/bf00311130
 
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