Magma Redox Geochemistry. Группа авторов

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      49 Cottrell, E., & Kelley, K. A. (2011). The oxidation state of Fe in MORB glasses and the oxygen fugacity of the upper mantle. Earth and Planetary Science Letters, 305(3–4), 270–282. doi: 10.1016/j.epsl.2011.03.014

      50 Cottrell, E., Kelley, K. A., Lanzirotti, A., & Fischer, R. A. (2009). High‐precision determination of iron oxidation state in silicate glasses using XANES. Chemical Geology, 268(3–4), 167–179. doi: 10.1016/j.chemgeo.2009.08.008

      51 Cottrell, E., Birner, S. K., Brounce, M., Davis, F. A., Waters, L. E., & Kelley, K. A. (2021). Oxygen Fugacity Across Tectonic Settings, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). http://doi.org/10.26022/IEDA/111899

      52 Cottrell, E., Lanzirotti, A., Mysen, B., Birner, S., Kelley, K. A., Botcharnikov, R., et al. (2018). A Mössbauer‐based XANES calibration for hydrous basalt glasses reveals radiation‐induced oxidation of Fe. American Mineralogist: Journal of Earth and Planetary Materials, 103(4), 489–501.

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      54 Crabtree, S. M., & Lange, R. A. (2011). Complex phenocryst textures and zoning patterns in andesites and dacites: Evidence of degassing‐induced rapid crystallization? Journal of Petrology, 52(1), 3–38. doi: 10.1093/petrology/egq067

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      60 Davis, F. A., & Cottrell, E. (2018). Experimental investigation of basalt and peridotite oxybarometers: implications for spinel thermodynamic models and Fe3+ compatibility during generation of upper mantle melts. American Mineralogist, 103(7), 1056–1067. doi: http://doi.org/10.2138/am‐2018‐6280

      61 Davis, F. A., Humayun, M., Hirschmann, M. M., & Cooper, R. S. (2013). Experimentally determined mineral/melt partitioning of first‐row transition elements (FRTE) during partial melting of peridotite at 3GPa, Geochimica et Cosmochimica Acta, 104, 232–260. doi: 10.1016/j.gca.2012.11.009

      62 Davis, F. A., Cottrell, E., Birner, S. K., Warren, J. M., & Lopez, O. G. (2017). Revisiting the electron microprobe method of spinel‐olivine‐orthopyroxene oxybarometry applied to spinel peridotites. American Mineralogist, 102(2), 421–435.

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      64 Devine, J. D., Rutherford, M. J., Norton, G. E., & Young, S. R. (2003). Magma storage region processes inferred from geochemistry of Fe‐Ti oxides in andesitic magma, Soufriere Hills Volcano, Montserrat, WI. Journal of Petrology, 44(8), 1375–1400. doi: 10.1093/petrology/44.8.1375

      65 El‐Rus, M. A. A., Neumann, E. R., & Peters, V. (2006). Serpentinization and dehydration in the upper mantle beneath Fuerteventura (eastern Canary Islands): Evidence from mantle xenoliths. Lithos, 89(1), 24–46.

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      69 Evans, K. A. (2021), Redox decoupling, redox budgets and magma recycling. In: D. R. Neuville and R. Moretti, (eds.) AGU Geophysical Monograph Redox variables and mechanisms in magmatism and volcanism. Wiley.

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      73 Farner,