Element Partitioning Between Magnesiowustite and Silicate Melt as a Function of Melt Composition and Temperature at High Pressure
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概要
著者
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Rubie D.
Bayerisches Geoinstitut University Of Bayreuth
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Rubie D.
Bayerisches Geoinstitut Universitaet Bayreuth
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GEβMANN C.
Bayerisches Geoinstitut, University of Bayreuth
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OHTANI E.
Institute of Mineralogy, Petrology and Economic Geology, Tohoku University
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Geβmann C.
Bayerisches Geoinstitut University Of Bayreuth
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Gessmann C.K.
Bayerisches Geoinstitut, University of Bayreuth
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Rubie D.C.
Bayerisches Geoinstitut, University of Bayreuth
関連論文
- Intracrystalline Olivine-Ringwoodite Transformation and Time-Dependent Growth Rates
- Element Partitioning Between Magnesiowustite and Silicate Melt as a Function of Melt Composition and Temperature at High Pressure
- Possible Sites for Hydrogen in a New Hydrous Magnesium Silicate Phase G Synthesized at 22 GPa and 1050°C