Study notes on water and magmas in the depths of the Earth
Author:
Affiliation:
1. Institute for Geothermal Sciences Graduate School of Sciences, Kyoto University
Publisher
Japan Association of Mineralogical Sciences
Subject
Economic Geology,Geochemistry and Petrology
Link
https://www.jstage.jst.go.jp/article/gkk/47/1/47_180108/_pdf
Reference76 articles.
1. Abe, Y. and Matsui, T. (1986): Early evolution of the Earth: Accretion, atmosphere formation and thermal history. J. Geophys. Res., 91, E291-E302.
2. Adam, J., Locmelis, M., Afonso, J.C., Rushmer, T. and Fiorentini, M.L. (2014): The capacity of hydrous fluids to transport and fractionate incompatible elements and metals within the Earth's mantle. Geochem. Geophys. Geosystems, 15, 2241-2253.
3. Baker, D.R. and Eggler, D.H. (1983): Fractionation paths of Atka (Aleutians) high-alumina basalts: constraints from phase relations. J. Volcanol. Geotherm. Res., 18, 387-404.
4. Bowen, N.L. (1928): The evolution of the igneous rocks. Princeton Univ. Press.
5. Bureau, H. and Keppler, H. (1999): Complete miscibility between silicate melts and hydrous fluids in the upper mantle: experimental evidence and geochemical implications. Earth Planet. Sci. Lett., 165, 187-196.
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