Hornblende dehydration reactions during magma ascent at Soufriere Hills Volcano, Montserrat

Hornblende phenocrysts in recent andesites of the Soufrière Hills Volcano display reaction rims of microcrystalline plagioclase, pyroxene, Fe-oxides and interstitial glass, formed by decompression during magma ascent. Mass balance calculations give the following reactions with mineral proportions in...

תיאור מלא

מידע ביבליוגרפי
Main Authors: Buckley, V, Sparks, R, Wood, B
פורמט: Journal article
שפה:English
יצא לאור: 2006