A Raman calibration for the quantification of SO42− groups dissolved in silicate glasses: Application to natural melt inclusions

Yann Morizet; Mimma Emanuela Gennaro; Sébastien Jégo; Zajack Zoltan; Giada Iacono-Marziano; Michel Pichavant; Ida Di Carlo; Clément Ferraina; Priscille Lesne

doi:10.2138/am-2017-6100

A Raman calibration for the quantification of SO42− groups dissolved in silicate glasses: Application to natural melt inclusions

Yann Morizet ¹ Mimma Emanuela Gennaro ^{2, 3, 4} Sébastien Jégo ^{2, 4} Zajack Zoltan ⁵ Giada Iacono-Marziano ^{2, 4} Michel Pichavant ^{2, 4} Ida Di Carlo ^{2, 4} Clément Ferraina ^{2, 4} Priscille Lesne ^{2, 4}

1 LPG - Laboratoire de Planétologie et Géodynamique de Nantes

2 ISTO - Institut des Sciences de la Terre d'Orléans - UMR7327

3 Dipartimento DiSTeM

4 Magma - UMR7327

ISTO - Institut des Sciences de la Terre d'Orléans - UMR7327

5 Department of Earth Sciences

Abstract : Sulfur is an important volatile element involved in magmatic systems. Its quantification in silicate glasses relies on state-of-the-art techniques such as electronprobe microanalyses (EPMA) or X-ray absorption spectroscopy but is often complicated by the fact that S dissolved in silicate glasses can adopt several oxidation states (S6+ for sulfates or S2− for sulfides). In the present work, we use micro-Raman spectroscopy on a series of silicate glasses to quantify the S content. The database is constituted by 47 silicate glasses of various compositions (natural and synthetic) with S content ranging from 1179 to 13 180 ppm. Most of the investigated glasses have been synthesized at high pressure and high temperature and under fully oxidizing conditions. The obtained Raman spectra are consistent with these fO2 conditions and only S6+ is present and shows a characteristic peak located at ~1000 cm−1 corresponding to the symmetric stretch of the sulfate molecular group (ν1 SO42−). The intensity of the ν1 SO42− peak is linearly correlated to the parts per million of S6+ determined by EPMA.

Keywords : S speciation melt inclusions silicate glass redox conditions Micro-Raman spectroscopy S content

Type de document :

Article dans une revue

American Mineralogist, Mineralogical Society of America, 2017, 102, pp.2065-2076. 〈10.2138/am-2017-6100〉

Domaine :

Planète et Univers [physics]

Liste complète des métadonnées

https://hal-insu.archives-ouvertes.fr/insu-01622574
Contributeur : Nathalie Pothier <>
Soumis le : mardi 24 octobre 2017 - 14:50:54
Dernière modification le : mercredi 19 septembre 2018 - 01:22:41

A Raman calibration for the quantification of SO42− groups dissolved in silicate glasses: Application to natural melt inclusions

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A Raman calibration for the quantification of SO42− groups dissolved in silicate glasses: Application to natural melt inclusions

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