Determination of Iron Oxidation State in Omphacites Applied to Geothermometry of Sudetic Eclogites
Jolanta Gałązka-Friedman , E.r. Bauminger , N. Bakun-Czubarow
AbstractA 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.
|Journal series||Hyperfine Interactions, ISSN 0304-3843, 1572-9540|
|Keywords in English||Atoms, Molecules, Clusters and Plasmas, Condensed Matter, Nuclear Physics, Heavy Ions, Hadrons, Surfaces and Interfaces, Thin Films|
|Citation count*||7 (2015-08-13)|
* presented citation count is obtained through Internet information analysis and it is close to the number calculated by the Publish or Perish system.