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Kugimiya, Y., Umino, S., Masuda, T., & Matsuda, Y. (2004). Kanonaite from the metamorphic sole of the Oman Ophiolite: evidence for high-f (O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42(1), 143-153.

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Year2004
Original EntryKugimiya, Y., Umino, S., Masuda, T., & Matsuda, Y. (2004). Kanonaite from the metamorphic sole of the Oman Ophiolite: evidence for high-f (O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42(1), 143-153.
Mindat Ref. ID15984838Long-form Identifiermindat:1:5:15984838:0
GUID0c2a01bd-d46a-4d3d-afef-c7b395cf3645
Full ReferenceKugimiya, Y., Umino, S., Masuda, T., & Matsuda, Y. (2004). Kanonaite from the metamorphic sole of the Oman Ophiolite: evidence for high-f (O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42(1), 143-153.
Plain TextKugimiya, Y., Umino, S., Masuda, T., & Matsuda, Y. (2004). Kanonaite from the metamorphic sole of the Oman Ophiolite: evidence for high-f (O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42(1), 143-153.

Map of Localities

Locality Pages

LocalityCitation Details
Bani Hamid area, Khawr Fakkan Massif (Khor Fakkan), Semail Ophiolite, Emirate of Fujairah, United Arab Emirates

Mineral Occurrences

LocalityMineral(s)
Bani Hamid area, Khawr Fakkan Massif (Khor Fakkan), Semail Ophiolite, Emirate of Fujairah, United Arab Emirates Albite, Andalusite, Braunite, Clinochlore, Hematite, Kanonaite, Metachert, Muscovite, Plagioclase, Quartz


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