Physics
Scientist
Bayerisches Geoinstitut, Universität Bayreuth, Bayreuth, Germany
Institute for Solid State Physics, University of Tokyo, 277-8581, Kashiwa, Japan
Division of Earth and Planetary Sciences, Hokkaido University, Sapporo, Japan
Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany
Institute for Solid State Physics, University of Tokyo, Kashiwa, Japan
Institute for Solid State Physics, University of Tokyo, Kashiwa 277-8581, Japan; Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany
Bayerisches Geoinstut, Universität Bayreuth, D95440 Bayreuth, Germany
Institute for Solid State Physics, University of Tokyo, Kashiwanoha, Kashiwa, Japan
A new high-pressure form of KAlSi3O8 under lower mantle conditions
Amorphization of Serpentine at High Pressure and High Temperature
Approach to the mineralogy of the lower mantle by a combined method of a laser-heated diamond anvil cell experiment and analytical electron microscopy
Chemical and magnetic properties of rapidly cooled metastable ferri-ilmenite solid solutions: implications for magnetic self-reversal and exchange bias - II. Chemical changes during quench and annealing
Chemical and magnetic properties of rapidly cooled metastable ferri-ilmenite solid solutions: implications for magnetic self-reversal and exchange bias—I. Fe-Ti order transition in quenched synthetic ilmenite 61
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