Melting of Biotite + Plagioclase + Quartz Gneisses: the Role of H2O in the Stability of Amphibole

Biotite + plagioclase + quartz (BPQ) is a common assemblage in gneisses, metasediments and metamorphosed granitic to granodioritic intrusions. Melting experiments on an assemblage consisting of 24 vol. % quartz, 25 vol. % biotite (XMg = 0[middot]38-0[middot]40), 42 vol. % plagioclase (An

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Veröffentlicht in:Journal of petrology 2000-05, Vol.41 (5), p.651-666
Hauptverfasser: GARDIEN, VÉRONIQUE, THOMPSON, ALAN BRUCE, ULMER, PETER
Format: Artikel
Sprache:eng
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Zusammenfassung:Biotite + plagioclase + quartz (BPQ) is a common assemblage in gneisses, metasediments and metamorphosed granitic to granodioritic intrusions. Melting experiments on an assemblage consisting of 24 vol. % quartz, 25 vol. % biotite (XMg = 0[middot]38-0[middot]40), 42 vol. % plagioclase (An
ISSN:0022-3530
1460-2415
DOI:10.1093/petrology/41.5.651