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Kato, Takumi, Kumazawa, Mineo (1986) Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet. Geophysical Research Letters, 13 (3) 181-184 doi:10.1029/gl013i003p00181

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Reference TypeJournal (article/letter/editorial)
TitleMelting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet
JournalGeophysical Research Letters
AuthorsKato, TakumiAuthor
Kumazawa, MineoAuthor
Year1986 (March)Volume13
Issue3
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/gl013i003p00181Search in ResearchGate
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Mindat Ref. ID764546Long-form Identifiermindat:1:5:764546:8
GUID0
Full ReferenceKato, Takumi, Kumazawa, Mineo (1986) Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet. Geophysical Research Letters, 13 (3) 181-184 doi:10.1029/gl013i003p00181
Plain TextKato, Takumi, Kumazawa, Mineo (1986) Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet. Geophysical Research Letters, 13 (3) 181-184 doi:10.1029/gl013i003p00181
In(1986, March) Geophysical Research Letters Vol. 13 (3) American Geophysical Union (AGU)

See Also

These are possibly similar items as determined by title/reference text matching only.

Kato, Takumi, Kumazawa, Mineo (1986) Melting and phase relations in the system Mg2SiO4-MgSiO3at 20 GPa under hydrous conditions. Journal of Geophysical Research, 91. 9351 doi:10.1029/jb091ib09p09351
Kato, Takumi, Kumazaw, Mineo (1985) Stability of phase B, A hydrous magnesium silicate, to 2300°C at 20 GPA. Geophysical Research Letters, 12 (8) 534-535 doi:10.1029/gl012i008p00534
Kato, Takumi, Kumazawa, Mineo (1985) Incongruent melting of Mg2SiO4 at 20 GPa. Physics of the Earth and Planetary Interiors, 41 (1). 1-5 doi:10.1016/0031-9201(85)90097-4
Kato, Takumi, Kumazawa, Mineo (1985) Garnet phase of MgSiO3 filling the pyroxene–ilmenite gap at very high temperature. Nature, 316 (6031). 803-805 doi:10.1038/316803a0
KATO, Takumi, KUMAZAWA, Mineo (1985) Effect of high pressure on the melting relation in the system Mg2SiO4-MgSiO3 part I. Eutectic relation up to 7 GPa. Journal of Physics of the Earth, 33 (6) 513-524 doi:10.4294/jpe1952.33.513
Morishima, Hideaki, Ohtani, Eiji, Kato, Takumi, Shimomura, Osamu, Kikegawa, Takumi (1994) Thermal expansion of MgSiO3perovskite at 20.5 GPa. Geophysical Research Letters, 21 (10) 899-902 doi:10.1029/94gl00844
Ohtani, Eiji, Kumazawa, Mineo, Kato, Takumi, Irifune, Testuo (1982) Melting of Various Silicates at Elevated Pressures. In High-Pressure Research in Geophysics. Springer Netherlands. p.259-270. doi:10.1007/978-94-009-7867-6_21
Ohtani, Eiji, Sawamoto, Hiroshi (1987) Melting experiment on a model chondritic mantle composition at 25 GPa. Geophysical Research Letters, 14 (7) 733-736 doi:10.1029/gl014i007p00733
Luth, Robert W. (1993) Melting in the Mg2SiO4-H2O system at 3 to 12 GPa. Geophysical Research Letters, 20 (3) 233-235 doi:10.1029/92gl03008
Ohtani, Eiji, Kato, Takumi, Sawamoto, Hiroshi (1986) Melting of a model chondritic mantle to 20 GPa. Nature, 322 (6077). 352-353 doi:10.1038/322352a0
Ohtani, Eiji, Kato, Takumi, Ito, Eiji (1991) Transition metal partitioning between lower mantle and core materials at 27 GPa. Geophysical Research Letters, 18 (1) 85-88 doi:10.1029/90gl02717
 
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