Abstract: Variations in Fe<sup>3+</sup>/Fe<sup>T </sup>ratios in volcanic amphibole as a function of magmatic oxygen fugacity and mineral composition (AGU Fall Meeting 2018)

Variations in Fe³⁺/Fe^Tratios in volcanic amphibole as a function of magmatic oxygen fugacity and mineral composition

Barbara Cäcilia Ratschbacher¹, Claire E Bucholz², Jennifer M Jackson³ and Natalia V Solomatova^3,4, (1)California Institute of Technology, Seismological Laboratory, Pasadena, United States, (2)California Institute of Technology, Geological and Planetary Sciences, Pasadena, United States, (3)California Institute of Technology, Pasadena, CA, United States, (4)CNRS, École Normale Supérieure de Lyon, Lyon, France

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Variations in Fe3+/FeT ratios in volcanic amphibole as a function of magmatic oxygen fugacity and mineral composition

Variations in Fe³⁺/Fe^Tratios in volcanic amphibole as a function of magmatic oxygen fugacity and mineral composition