Details for: Tetsuo Irifune
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Tetsuo Irifune (Ehime University, Japan)
Theme chair: 04
Goldschmidt2016
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Note: abstracts are only listed if one of the following email addresses was provided when the abstract was submitted: irifune@dpc.ehime-u.ac.jp. Otherwise, try an advanced search.
(2016) Creep Strength of Ringwoodite Measured up to 1700 K at 17-18 GPa Using a deformation-Dia Apparatus
Kawazoe T, Nishihara Y, Ohuchi T, Miyajima N, Maruyama G, Higo Y, Funakoshi K-I & Irifune T04a/11:15/Mo
(2016) Melting of Tagish Lake Meteorite at High Pressure: Implications for the Fate of the Carbonaceous Matter during Planetary Accretion
Stagno V, Du W, Kebukawa Y & Irifune T18e/10:15/Fr
(2016) Na-Bearing Phases in the Deep Transition Zone and Lower Mantle: Composition, Structural Features and Na Transport to the Deep Earth
Tamarova A, Bindi L, Bobrov A, Sirotkina E, Tschauner O, Walter M & Irifune T07d/09:30/Fr
(2016) Phase Relations in the System MgSiO3-Al2O3 to 52 GPa and 2000 K
Liu Z, Irifune T, Nishi M, Tange Y, Arimoto T & Shinmei T18c/10:45/Th
(2018) Interphase Partitioning of Minor Elements in the Transition Zone and Uppermost Lower Mantle
Bobrov A, Tamarova A, Sirotkina E, Zhang G & Irifune T(2017) Phase Diagram and Melting of NiSi up to 115 GPa
Briggs R, Boccato S, Giampaoli R, Irifune T, Ishimatsu N, Lord O, Rosa A, Torchio R & Pascarelli S(2017) Do Fe-Bearing Minerals Control the Deep Carbon Cycle in the Interior of the Earth?
Stagno V, McCammon CA, Cerantola V, Andreozzi GB, Caruso M, Arimoto T & Irifune T(2017) From Carbon in Meteorites to Carbonatite Rocks on Earth
Stagno V, Kono Y, Greaux S, Kebukawa Y, Stopponi V, Scarlato P, Lustrino M & Irifune T(2017) Element Absorption and Release during Serpentine Involved Reactions: Element Cycles in Subduction Zones
Luginbuehl SM, Rosa AD, Louvel M, Merkulova M, Krstulovic M, Munoz M, Wilke M & Irifune T(2017) Noble Gas Partitioning between Earth’s Mantle and Core: Implications for Earth's Global Geodynamics
Rosa AD, Bouhifd MA, Briggs R, Morard G, Garbarino G & Irifune T(2017) Melting Temperature of Tagish Lake (CI2) Meteorite from 5 to 30 GPa
Greaux S, Stagno V & Irifune T(2017) Ti-Rich Phases in the MgO–SiO2–TiO2 System at 10–24 GPa:composition, Solid Solutions, and Structural Features
Sirotkina E, Bobrov A, Bindi L & Irifune T(2015) Structural Properties of Carbonate-Silicate Melts: An EXAFS Study on Y and Sr
Pohlenz J, Pascarelli S, Mathon O, Belin S, Shiryaev A, Safonov O, Veligzhanin A, Murzin V, Irifune T & Wilke M(2015) Toward the Unified Image of the Spin Transition of Iron in the Lower Mantle Minerals
Fujino K & Irifune T(2013) Experimental Study of the System Mg<sub>4</sub>Si<sub>4</sub>O12 – Mg<sub>3</sub>Cr<sub>2</sub>Si<sub>3</sub>O12 at 12-25 GPa and 1600℃
Sirotkina E, Bobrov A, Luca B & Tetsuo ITheme chair
Goldschmidt2016 - Theme 04: Deep Earth
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