4.3 Article

Manganese incorporation in synthetic hercynite

Journal

MINERALOGICAL MAGAZINE
Volume 79, Issue 3, Pages 635-647

Publisher

MINERALOGICAL SOC
DOI: 10.1180/minmag.2015.079.3.09

Keywords

hercynite; spinel; manganese; oxygen fugacity; disorder; crystal chemistry

Categories

Funding

  1. Italian Ministry of Education, MIUR [2010EARRRZ_003]

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Manganese incorporation in synthetic hercynite, and partitioning between hercynite and silicate melt synthesized at 1.0 GPa, 1250 degrees C, and at an f(O2) buffered by Fe-FeO, has been studied by X-ray absorption spectroscopy and single-crystal X-ray structure refinement. Spectra indicate the presence of both Mn2+ and Mn3+ (and possibly also Mn4+) in synthetic hercynite and partitioning of Mn2+ into the melt phase, and Mn3+ into hercynite, respectively, under run conditions. X-ray refinement is consistent with partial disorder of Fe and Al across tetrahedral and octahedral sites. A higher than expected degree of Fe-Al disorder in the Mn-bearing hercynite can be explained by preferential incorporation of Mn2+ onto the tetrahedral site, and indicates that Fe-Al disorder in pure, stoichiometric hercynite cannot necessarily be used to determine closure temperatures in natural spinel. However, partitioning of Mn2+ and Mn3+ between melt and hercynite suggests that Mn incorporation in hercynite could be used as a measure of f(O2) conditions in magmas during spinel crystallization.

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