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 high-f (O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42(1), 143-153. |
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Mindat Ref. ID | 15984838 | Long-form Identifier | mindat:1:5:15984838:0 |
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GUID | 0c2a01bd-d46a-4d3d-afef-c7b395cf3645 |
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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 high-f (O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42(1), 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 high-f (O2) conditions during retrograde metamorphism. The Canadian Mineralogist, 42(1), 143-153. |
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