Hydrous peridotites with Ti-rich chromian spinel as a low-temperature forearc mantle facies: evidence from the Happo-O’ne metaperidotites (Japan)
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-009-0420-7.pdf
Reference105 articles.
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3. Arai S (1975) Contact metamorphosed dunite–harzburgite complex in the Chugoku district, western Japan. Contrib Mineral Petrol 52:1–16
4. Arai S (1980) Dunite–harzburgite–chromitite complexes as refractory residue in the Sangun–Yamaguchi zone, western Japan. J Petrol 21:141–165
5. Arai S (1992) Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry. Mineral Mag 56:173–184
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