CaO + MgO + Al 2 O 3 + SiO 2 + H 2 O to 35 kb; amphibole, talc, and zoisite dehydration and melting reactions in the silica-excess part of the system and their possible significance in subduction zones, amphibolite melting, and magma fractionation
- 1 December 1994
- journal article
- Published by American Journal of Science (AJS) in American Journal of Science
- Vol. 294 (10) , 1229-1289
- https://doi.org/10.2475/ajs.294.10.1229
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