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...

Повний опис

Бібліографічні деталі
Автори: Buckley, V, Sparks, R, Wood, B
Формат: Journal article
Мова:English
Опубліковано: 2006

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