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Takashi Yoshino

Institute for Study of the Earth's Interior

Okayama University

Misasa

Tottori 682-0193

Japan

[email]@*.okayama-u.ac.jp

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Affiliation

Institute for Study of the Earth's Interior, Okayama University, Misasa, Tottori 682-0193, Japan. 2003 - 2008

References

Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite. Yoshino, T., Manthilake, G., Matsuzaki, T., Katsura, T. Nature (2008) [Pubmed]
Hydrous olivine unable to account for conductivity anomaly at the top of the asthenosphere. Yoshino, T., Matsuzaki, T., Yamashita, S., Katsura, T. Nature (2006) [Pubmed]
Core formation in planetesimals triggered by permeable flow. Yoshino, T., Walter, M.J., Katsura, T. Nature (2003) [Pubmed]