2018 - Fellow of American Geophysical Union (AGU)
Mineralogy, Mantle, Olivine, Silicate and Wadsleyite are her primary areas of study. Her Mineralogy research is multidisciplinary, relying on both X-ray crystallography, Perovskite, Phase boundary and Analytical chemistry. Her biological study spans a wide range of topics, including Atmospheric temperature range, Thermodynamics, Transition zone, Geothermal gradient and Conductivity.
Her work on Ringwoodite as part of her general Olivine study is frequently connected to Asthenosphere, thereby bridging the divide between different branches of science. The Ringwoodite study combines topics in areas such as Bulk modulus and Elastic modulus. Her studies in Silicate integrate themes in fields like Terrestrial planet, Eutectic system, Peridotite and Solidus.
Her primary areas of study are Mineralogy, Analytical chemistry, Olivine, Thermodynamics and Mantle. The concepts of her Mineralogy study are interwoven with issues in Silicate, Perovskite and Conductivity. Tomoo Katsura interconnects Crystallography, Phase boundary, Bulk modulus and X-ray in the investigation of issues within Analytical chemistry.
As part of her studies on Olivine, Tomoo Katsura frequently links adjacent subjects like Dislocation. Her work on Silicate perovskite as part of general Mantle study is frequently connected to Discontinuity, therefore bridging the gap between diverse disciplines of science and establishing a new relationship between them. Her study looks at the relationship between Wadsleyite and topics such as Ringwoodite, which overlap with Elastic modulus.
Tomoo Katsura focuses on Analytical chemistry, Silicate perovskite, Thermodynamics, Olivine and Mantle. Tomoo Katsura works mostly in the field of Analytical chemistry, limiting it down to topics relating to Tin and, in certain cases, Synchrotron radiation, Germanium and Electronic band structure. Her Thermodynamics study integrates concerns from other disciplines, such as Mineral redox buffer, Aqueous solution, Transition zone and Solubility.
Her Olivine research is multidisciplinary, incorporating elements of Climb and Petrology. Her research in Mantle intersects with topics in Slab and Mineralogy. Her study in the field of Pyrolite also crosses realms of Complete Agreement.
Her primary scientific interests are in Analytical chemistry, Spinel, Bulk modulus, Ringwoodite and Mantle. Tomoo Katsura has researched Analytical chemistry in several fields, including Secondary ion mass spectrometry, Lattice diffusion coefficient, Nanoindentation and Conductivity. Tomoo Katsura has included themes like Mineralogy and Silicon in her Spinel study.
Her Mineralogy research is multidisciplinary, relying on both Adiabatic process and Pressure drop. Her Ringwoodite study introduces a deeper knowledge of Transition zone. She has included themes like Periclase and Slab in her Mantle study.
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The system Mg2SiO4‐Fe2SiO4 at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel
Tomoo Katsura;Eiji Ito.
Journal of Geophysical Research (1989)
Adiabatic temperature profile in the mantle
Tomoo Katsura;Tomoo Katsura;Akira Yoneda;Daisuke Yamazaki;Takashi Yoshino.
Physics of the Earth and Planetary Interiors (2010)
Olivine‐wadsleyite transition in the system (Mg,Fe)2SiO4
Tomoo Katsura;Hitoshi Yamada;Osamu Nishikawa;Osamu Nishikawa;Maoshuang Song.
Journal of Geophysical Research (2004)
The Postspinel Phase Boundary in Mg2SiO4 Determined by in Situ X-ray Diffraction
Tetsuo Irifune;Norimasa Nishiyama;Koji Kuroda;Toru Inoue.
Hydrous olivine unable to account for conductivity anomaly at the top of the asthenosphere
Takashi Yoshino;Takuya Matsuzaki;Shigeru Yamashita;Tomoo Katsura.
Mineralogy of subducted basaltic crust (MORB) from 25 to 37 GPa, and chemical heterogeneity of the lower mantle
Shigeaki Ono;Shigeaki Ono;Eiji Ito;Tomoo Katsura.
Earth and Planetary Science Letters (2001)
A temperature profile of the mantle transition zone
Eiji Ito;Tomoo Katsura.
Geophysical Research Letters (1989)
Core formation in planetesimals triggered by permeable flow
Takashi Yoshino;Michael J. Walter;Tomoo Katsura.
Post-spinel transition in Mg2SiO4 determined by high P–T in situ X-ray diffractometry
Tomoo Katsura;Hitoshi Yamada;Toru Shinmei;Atsushi Kubo.
Physics of the Earth and Planetary Interiors (2003)
Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
Takashi Yoshino;Geeth Manthilake;Takuya Matsuzaki;Tomoo Katsura.
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