Reference Type | - plain text - |
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Year | 2004 |
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Original Entry | Kugimiya, Y., Umino, S., Masuda, T., Matsuda, Y. (2004) Kanonaite from the metamorphic sole of the Oman Ophiolite: evidence for the high-f(O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42, 143-153. |
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Mindat Ref. ID | 16113601 | Long-form Identifier | mindat:1:5:16113601:7 |
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GUID | 8eae80bf-80fa-4475-a043-665ae85c142d |
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Full Reference | Kugimiya, Y., Umino, S., Masuda, T., Matsuda, Y. (2004) Kanonaite from the metamorphic sole of the Oman Ophiolite: evidence for the high-f(O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42, 143-153. |
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Plain Text | Kugimiya, Y., Umino, S., Masuda, T., Matsuda, Y. (2004) Kanonaite from the metamorphic sole of the Oman Ophiolite: evidence for the high-f(O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42, 143-153. |
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