Hydrous peridotites with Ti-rich chromian spinel as a...

Contributions to Mineralogy and Petrology 2010 / 02 Vol. 159; Iss. 2

Hydrous peridotites with Ti-rich chromian spinel as a low-temperature forearc mantle facies: evidence from the Happo-O’ne metaperidotites (Japan)

Mohamed Zaki Khedr, Shoji Arai
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Volume:
159
Language:
english
Pages:
21
DOI:
10.1007/s00410-009-0420-7
Date:
February, 2010
File:
PDF, 1.34 MB
english, 2010
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