Systematic study of sulfur isotopic composition in iron meteorites and the occurrence of excess S-33 and S-36

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Iron Alloys, Iron Meteorites, Meteoritic Composition, Schreibersite, Sulfur Isotopes, Troilite, Chondrites, Evaporation, Fractionation, Metal Compounds

Scientific paper

The paper concentrates on isotopic measurements of sulfur in different sulfur-carrier phases: troilite inclusions, Fe-Ni alloy, and schreibersite (possibly including daubreelite). Variations in S-34 isotope ratio are observed in some troilite inclusions, and no evidence of nucleosynthetic sulfur isotopic anomalies are found in the troilite inclusions. Excesses of S-33 and S-36 are observed in both FeNi alloy and schreibersite of Grant, Santa Clara, Tlacotepec, and Gibeon, with schreibersite possessing the greater magnitude of presumably spallogenic S-33 and S-36. It is concluded that the magnitude of the observed fractionation is consistent with troilite dissociation and/or vaporization following a collisional impact.

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