Water contents and pressures of melts in unerupted felsic magma constrained by SEM-EDS analysis of homogenized melt inclusions in zircon
Author:
Affiliation:
1. Department of Earth Sciences, Graduate School of Science and Engineering, Ehime University
2. Department of Applied Chemistry for Environment, School of Biological and Environmental Sciences, Kwansei Gakuin University
Publisher
Japan Association of Mineralogical Sciences
Link
https://www.jstage.jst.go.jp/article/jmps/119/1/119_230904/_pdf
Reference37 articles.
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2. Barker, F. (1979) Trondhjemite: Definition, environment and hypotheses of origin. In Trondhjemites, dacites and related rocks (Barker, F. Ed.). pp. 659, Developments in Petrology, 6, Elsevier, Amsterdam, 1-12.
3. Bégué, F., Deering, C.D., Gravley, D.M., Kennedy, B.M., et al (2014a) Extraction, storage and eruption of multiple isolated magma batches in the paired Mamaku and Ohakuri eruption, Taupo Volcanic Zone, New Zealand. Journal of Petrology, 55, 1653-1684.
4. Bégué, F., Gualda, G.A.R., Ghiorso, M.S., Pamukcu, A.S., et al (2014b) Phase-equilibrium geobarometers for silicic rocks based on rhyolite-MELTS. Part 2: application to Taupo Volcanic Zone rhyolites. Contributions to Mineralogy and Petrology, 168, 1082.
5. Chabiron, A., Pironon, J. and Massare, D. (2004) Characterization of water in synthetic rhyolitic glasses and natural melt inclusions by Raman spectroscopy. Contributions to Mineralogy and Petrology, 146, 485-492.
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