Oriented growth due to topotactic replacement of antigorite by olivine as a mechanism for the formation of B-type olivine CPO in convergent margins
- ADS bibcode
- 2012AGUFMMR11A2473N
- year
- 2012
- Listed Authors
- Nagaya, T.
- Wallis, S.
- Kobayashi, H.
- Michibayashi, K.
- Mizukami, T.
- Listed Institutions
- Department of Earth and Planetary Sciences, Nagoya University, Nagoya, Japan;
- Department of Earth and Planetary Sciences, Nagoya University, Nagoya, Japan;
- Department of Earth and Planetary Sciences, Nagoya University, Nagoya, Japan;
- Institute of Geosciences, Shizuoka University, Shizuoka, Japan;
- Earth Science Course, Kanazawa University, Kanazawa, Japan;
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