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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

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Reference TypeJournal (article/letter/editorial)
TitleThermal expansion of MgSiO3perovskite at 20.5 GPa
JournalGeophysical Research Letters
AuthorsMorishima, HideakiAuthor
Ohtani, EijiAuthor
Kato, TakumiAuthor
Shimomura, OsamuAuthor
Kikegawa, TakumiAuthor
Year1994 (May 15)Volume21
Issue10
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/94gl00844Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID777282Long-form Identifiermindat:1:5:777282:9
GUID0
Full ReferenceMorishima, 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
Plain TextMorishima, 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
In(1994, May) Geophysical Research Letters Vol. 21 (10) American Geophysical Union (AGU)

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Kato, Takumi, Ohtani, Eiji, Morishima, Hideaki, Yamazaki, Daisuke, Suzuki, Akio, Suto, Minoru, Kubo, Tomoaki, Kikegawa, Takumi, Shimomura, Osamu (1995) In situ X ray observation of high-pressure phase transitions of MgSiO3and thermal expansion of MgSiO3perovskite at 25 GPa by double-stage multianvil system. Journal of Geophysical Research: Solid Earth, 100. 20475-20481 doi:10.1029/95jb01688
Kubo, Tomoaki, Ohtani, Eiji, Kato, Takumi, Morishima, Hideaki, Yamazaki, Daisuke, Suzuki, Akio, Mibe, Kenji, Kikegawa, Takumi, Shimomura, Osamu (1998) An in situ X ray diffraction study of the α-β transformation kinetics of Mg2SiO4. Geophysical Research Letters, 25 (5) 695-698 doi:10.1029/98gl00224
Utsumi, Wataru, Funamori, Nobumasa, Yagi, Takehiko, Ito, Eiji, Kikegawa, Takumi, Shimomura, Osamu (1995) Thermal expansivity of MgSiO3perovskite under high pressures up to 20 GPa. Geophysical Research Letters, 22 (9) 1005-1008 doi:10.1029/95gl00584
Suzuki, Akio, Ohtani, Eiji, Morishima, Hideaki, Kubo, Tomoaki, Kanbe, Yuichi, Kondo, Tadashi, Okada, Taku, Terasaki, Hidenori, Kato, Takumi, Kikegawa, Takumi (2000) In situ determination of the phase boundary between Wadsleyite and Ringwoodite in Mg2SiO4. Geophysical Research Letters, 27 (6) 803-806 doi:10.1029/1999gl008425
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
Ohtani, Eiji, Kato, Takumi, Ito, Eiji (1991) Correction to “Transition metal partitioning between lower mantle and core materials at 27 GPA”. Geophysical Research Letters, 18 (4) 796 doi:10.1029/91gl00904
Hirao, Naohisa, Kondo, Tadashi, Ohtani, Eiji, Takemura, Kenichi, Kikegawa, Takumi (2004) Compression of iron hydride to 80 GPa and hydrogen in the Earth's inner core. Geophysical Research Letters, 31 (6) doi:10.1029/2003gl019380
Suito, Kaichi, Miyoshi, Makoto, Onodera, Akifumi, Shimomura, Osamu, Kikegawa, Takumi (1996) Thermal expansion studies of stishovite at 10.5 GPa using synchrotron radiation. Physics of the Earth and Planetary Interiors, 93 (3). 215-222 doi:10.1016/0031-9201(95)03074-3
Ohtani, Eiji, Toma, Motomasa, Kubo, Tomoaki, Kondo, Tadashi, Kikegawa, Takumi (2003) In situ X-ray observation of decomposition of superhydrous phase B at high pressure and temperature. Geophysical Research Letters, 30 (2) doi:10.1029/2002gl015549
Hirao, Naohisa, Ohtani, Eiji, Kondo, Tadashi, Endo, Noriaki, Kuba, Toshiko, Suzuki, Toshiaki, Kikegawa, Takumi (2006) Partitioning of potassium between iron and silicate at the core-mantle boundary. Geophysical Research Letters, 33 (8) doi:10.1029/2005gl025324
Tsuno, Kyusei, Terasaki, Hidenori, Ohtani, Eiji, Suzuki, Akio, Asahara, Yuki, Nishida, Keisuke, Sakamaki, Tatsuya, Funakoshi, Ken-ichi, Kikegawa, Takumi (2007) In situ observation and determination of liquid immiscibility in the Fe-O-S melt at 3 GPa using a synchrotron X-ray radiographic technique. Geophysical Research Letters, 34 (17) doi:10.1029/2007gl030750
 
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