An experimental study of Fe-Mg partitioning between olivine and orthopyroxene at 1173, 1273 and 1423 K and 1.6 GPa

The partitioning of magnesium and iron between coexisting olivines and orthopyroxenes in the system MgO-FeO-SiO2 is investigated experimentally at 1173, 1273, 1423 K and 1.6 GPa over the whole range of magnesium/iron ratios.

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Published inContributions to mineralogy and petrology Vol. 113; no. 2; pp. 196 - 207
Main Authors SECKENDORFF, Volker von, O'NEILL, Hugh St. C
Format Conference Proceeding Journal Article
LanguageEnglish
Published Berlin Springer 01.02.1993
Springer Nature B.V
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Abstract The partitioning of magnesium and iron between coexisting olivines and orthopyroxenes in the system MgO-FeO-SiO2 is investigated experimentally at 1173, 1273, 1423 K and 1.6 GPa over the whole range of magnesium/iron ratios.
AbstractList The partitioning of magnesium and iron between coexisting olivines and orthopyroxenes in the system MgO-FeO-SiO2 is investigated experimentally at 1173, 1273, 1423 K and 1.6 GPa over the whole range of magnesium/iron ratios.
Author O'NEILL, Hugh St. C
SECKENDORFF, Volker von
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  givenname: Hugh St. C
  surname: O'NEILL
  fullname: O'NEILL, Hugh St. C
  organization: Univ. Bayreuth, Bayer. Geoinst., D-8580 Bayreuth, Germany
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Issue 2
Keywords experimental studies
orthopyroxene
magnesium
partitioning
thermodynamic properties
olivine
high pressure
high temperature
coexisting minerals
Language English
License CC BY 4.0
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Springer Nature B.V
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Snippet The partitioning of magnesium and iron between coexisting olivines and orthopyroxenes in the system MgO-FeO-SiO2 is investigated experimentally at 1173, 1273,...
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SubjectTerms Chemical elements
Crystalline rocks
Earth sciences
Earth, ocean, space
Exact sciences and technology
Experimental petrology
Iron
Magnesium
Mineralogy
Mineralogy: general, methodology, regional studies
Minerals
Petrology
Title An experimental study of Fe-Mg partitioning between olivine and orthopyroxene at 1173, 1273 and 1423 K and 1.6 GPa
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