TY - JOUR
T1 - Determination of iron oxidation state in omphacites applied to geothermometry of sudetic eclogites
AU - Gala̧zka-Friedman, J.
AU - Bauminger, E. R.
AU - Bakun-Czubarow, N.
PY - 1998
Y1 - 1998
N2 - 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.
AB - 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.
UR - http://www.scopus.com/inward/record.url?scp=0141690320&partnerID=8YFLogxK
U2 - 10.1023/a:1010846323948
DO - 10.1023/a:1010846323948
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AN - SCOPUS:0141690320
SN - 0304-3843
VL - 112
SP - 223
EP - 226
JO - Hyperfine Interactions
JF - Hyperfine Interactions
IS - 1-4
ER -