Igneous garnet and amphibole fractionation in the roots of island arcs: experimental constraints on andesitic liquids

Author:

Alonso-Perez Raquel,Müntener Othmar,Ulmer Peter

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference82 articles.

1. Allen JC, Boettcher AL (1978) Amphiboles in andesite and basalt: II. Stability as a function of P–T-fH2O-fO2. Am Mineral 63:1074–1087

2. Allen JC, Boettcher AL (1983) The stability of amphibole in andesite and basalt at high pressures. Am Mineral 68:307–314

3. Allen JC, Boettcher AL, Marland G (1975) Amphiboles in andesite and basalt: I. Stability as a function of P–T-fO2. Am Min 60:1069–1085

4. Alonso-Perez R (2006) The role of garnet in the evolution of hydrous, calc-alkaline magmas: an experimental study at 0.8–1.5 GPa. PhD thesis, ETH Zurich, p 174

5. Atherton MP, Petford N (1993) Generation of sodium-rich magmas from newly underplated basaltic crust. Nature 362:144–146. doi: 10.1038/362144a0

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