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Hornblende phenocrysts in recent andesites of the Soufriere Hills Volcano display reaction rims of microcrystalline plagioclase, pyroxene, Fe-oxides and interstitial glass, formed by decompression during magma ascent. Mass balance calculations give t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8bafdbaa7363b73563f7dff22ff9b379
https://doi.org/10.1007/s00410-005-0060-5
https://doi.org/10.1007/s00410-005-0060-5
