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Determination of Iron Oxidation State in Omphacites Applied to Geothermometry of Sudetic Eclogites

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Abstract

A common mineral geothermometer for eclogites is based on Fe2+-Mg exchange reaction between garnets and clinopyroxenes. For the accurate determination of Fe2+ in omphacites, ten omphacite samples were isolated from eight Sudetic eclogites and studied by electron microprobe and Mössbauer spectroscopy. Garnet-clinopyroxene equilibration temperatures for two Sudetic eclogites were calculated.

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Authors and Affiliations

  1. Institute of Physics, Warsaw University of Technology, Warsaw, Poland

    J. Galazka-Friedman & N. Bakun-Czubarow

  2. Racah Institute of Physics, The Hebrew University, Jerusalem, Israel

    E.R. Bauminger

Authors
  1. J. Galazka-Friedman
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  2. E.R. Bauminger
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  3. N. Bakun-Czubarow
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Galazka-Friedman, J., Bauminger, E. & Bakun-Czubarow, N. Determination of Iron Oxidation State in Omphacites Applied to Geothermometry of Sudetic Eclogites. Hyperfine Interactions 112, 223–226 (1998). https://doi.org/10.1023/A:1010846323948

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  • DOI: https://doi.org/10.1023/A:1010846323948

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