登录注册
Quick Links : Mindat手册The Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
主页关于 MindatMindat手册Mindat的历史版权Who We Are联系我们于 Mindat.org刊登广告
捐赠给 MindatCorporate Sponsorship赞助板页已赞助的板页在 Mindat刊登 广告的广告商于 Mindat.org刊登广告
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
搜索矿物的性质搜索矿物的化学Mineral Visual ExplorerAdvanced Locality Search随意显示任何一 种矿物Random Locality使用minID搜索邻近产地Search Articles搜索词汇表更多搜索选项
搜索:
矿物名称:
地区产地名称:
关键字:
 
Mindat手册添加新照片Rate Photos产区编辑报告Coordinate Completion Report添加词汇表项目
Mining Companies统计会员列表Mineral MuseumsClubs & Organizations矿物展及活动The Mindat目录表设备设置The Mineral QuizTime Machine
照片搜索Photo GalleriesSearch by ColorPhoto Colour Explorer今天最新的照片昨天最新的照片用户照片相集过去每日精选照片相集Photography

O'Neill, Hugh St. C., Canil, Dante, Rubie, David C. (1998) Oxide-metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core. Journal of Geophysical Research: Solid Earth, 103. 12239-12260 doi:10.1029/97jb02601

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleOxide-metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core
JournalJournal of Geophysical Research: Solid Earth
AuthorsO'Neill, Hugh St. C.Author
Canil, DanteAuthor
Rubie, David C.Author
Year1998 (June 10)Volume103
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/97jb02601Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID916623Long-form Identifiermindat:1:5:916623:7
GUID0
Full ReferenceO'Neill, Hugh St. C., Canil, Dante, Rubie, David C. (1998) Oxide-metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core. Journal of Geophysical Research: Solid Earth, 103. 12239-12260 doi:10.1029/97jb02601
Plain TextO'Neill, Hugh St. C., Canil, Dante, Rubie, David C. (1998) Oxide-metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core. Journal of Geophysical Research: Solid Earth, 103. 12239-12260 doi:10.1029/97jb02601
In(1998) Journal of Geophysical Research: Solid Earth Vol. 103. American Geophysical Union (AGU)

See Also

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

Canil, Dante, Scarfe, Christopher M. (1990) Phase relations in peridotite+CO2Systems to 12 GPa: Implications for the origin of kimberlite and carbonate stability in the Earth's upper mantle. Journal of Geophysical Research, 95. 15805 doi:10.1029/jb095ib10p15805
Tsuno, Kyusei, Frost, Daniel J., Rubie, David C. (2013) Simultaneous partitioning of silicon and oxygen into the Earth's core during early Earth differentiation. Geophysical Research Letters, 40 (1) 66-71 doi:10.1029/2012gl054116
Bolfan-Casanova, N., Mackwell, S., Keppler, H., McCammon, C., Rubie, D. C. (2002) Pressure dependence of H solubility in magnesiowüstite up to 25 GPa: Implications for the storage of water in the Earth's lower mantle. Geophysical Research Letters, 29 (10) 89 doi:10.1029/2001gl014457
CANIL, DANTE, O'NEILL, HUGH ST. C. (1996) Distribution of Ferric Iron in some Upper-Mantle Assemblages. Journal of Petrology, 37 (3) 609-635 doi:10.1093/petrology/37.3.609
Liu, Ming, Kerschhofer, Ljuba, Mosenfelder, Jed L., Rubie, David C. (1998) The effect of strain energy on growth rates during the olivine-spinel transformation and implications for olivine metastability in subducting slabs. Journal of Geophysical Research: Solid Earth, 103. 23897-23909 doi:10.1029/98jb00794
Jamieson, John C., Demarest, Harold H., Schiferl, David (1978) A reevaluation of the Grüneisen parameter for the Earth's core. Journal of Geophysical Research: Solid Earth, 83. 5929-5935 doi:10.1029/jb083ib12p05929
Farver, John R., Yund, Richard A., Rubie, David C. (1994) Magnesium grain boundary diffusion in forsterite aggregates at 1000°-1300°C and 0.1 MPa to 10 GPa. Journal of Geophysical Research: Solid Earth, 99. 19809-19819 doi:10.1029/94jb01250
Young, G., Fan, Lili, Zhao, Bin, Chen, Xing, Liu, Xun, Huang, Haijun (2021) Equation of State for Fe‐9.0 wt% O up to 246 GPa: Implications for Oxygen in the Earth's Outer Core. Journal of Geophysical Research: Solid Earth, 126 (2) doi:10.1029/2020jb021056
Nakajima, Yoichi, Frost, Daniel J., Rubie, David C. (2012) Ferrous iron partitioning between magnesium silicate perovskite and ferropericlase and the composition of perovskite in the Earth's lower mantle. Journal of Geophysical Research: Solid Earth, 117. doi:10.1029/2012jb009151
Frost, Daniel J., Asahara, Yuki, Rubie, David C., Miyajima, Nobuyoshi, Dubrovinsky, Leonid S., Holzapfel, Christian, Ohtani, Eiji, Miyahara, Masaaki, Sakai, Takeshi (2010) Partitioning of oxygen between the Earth's mantle and core. Journal of Geophysical Research, 115. doi:10.1029/2009jb006302
Mao, H. K., Wu, Y., Chen, L. C., Shu, J. F., Jephcoat, Andrew P. (1990) Static compression of iron to 300 GPa and Fe0.8Ni0.2alloy to 260 GPa: Implications for composition of the core. Journal of Geophysical Research, 95. 21737 doi:10.1029/jb095ib13p21737
 
and/or  
版权所有© mindat.org1993年至2026年，除了规定的地方。 Mindat.org全赖于全球数千个以上成员和支持者们的参与。
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
隐私政策 - 条款和条款细则 - 联络我们 - Report a bug/vulnerability Current server date and time: 2026.6.6 17:58:36
Go to top of page