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Th. Thordarson, S. Self, D. J. Miller, G. Larsen, E. G. Vilmundardottir, in Volcanic Degassing, C. Oppenheimer, D. M. Pyle, J. Barclay, Eds., vol. 213 of Geological Society of London Special Publications (Geological Society of London, London, 2003), pp. 103-123.
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Materials and methods are available on Science Online.
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Materials and methods are available on Science Online.
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T. Sano, T. Fujii, S. S. Deshmukh, T. Fukuoka, S. Aramaki, J. Petrol. 42, 2175 2001, These authors reported 0.6 wt, water in a glass inclusion, by FTIR. We have obtained an FTIR analysis of 0.5 wt, water in an olivine-hosted glass inclusion in sample MG4
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T. Sano, T. Fujii, S. S. Deshmukh, T. Fukuoka, S. Aramaki, J. Petrol. 42, 2175 (2001). These authors reported 0.6 wt % water in a glass inclusion, by FTIR. We have obtained an FTIR analysis of 0.5 wt % water in an olivine-hosted glass inclusion in sample MG4.
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14
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16
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41149096641
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For a total mass of magma erupted, M, the mass of S released during degassing is MS,lost, M[(1, X chamber)Schamber, 1, X lava)Slava, 1) where Schamber and Slava are the S concentrations in the melt at depth, before any degassing as measured in the glass inclusions, and in the degassed matrix glass in the lava, respectively. X is the mass fraction of crystals present and is estimated by the amount of enrichment of an incompatible element with respect to the whole-rock concentration such that 1, Xchamber, Iwr/Iincl, where Iwr and Iincl are the concentrations of a highly incompatible element in the whole rock and in any nondegassed inclusion in which the sulfur value Schamber has been measured. Similarly, 1, Xlava
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2 contents are 1.55 wt % for MG4 and 1.29 wt % for MG5; see table S3.
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19
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We thank UK Natural Environment Research Council for funding this work grant NER/B/S/2003/00246, A. Jay for help with sample collection and geochemical analyses, and S. Sethna for general support of our fieldwork in India. We thank the four anonymous reviewers for their helpful comments
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We thank UK Natural Environment Research Council for funding this work (grant NER/B/S/2003/00246), A. Jay for help with sample collection and geochemical analyses, and S. Sethna for general support of our fieldwork in India. We thank the four anonymous reviewers for their helpful comments.
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