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The andesite phenocrysts have a range of textures and zonation patterns which suggest that non‐uniform reheating of the magma occurred shortly before the current eruption. Reheating resulted in remobilisation of the resident magma and may have induced eruption.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380013168798309376","@type":"Researcher","foaf:name":[{"@value":"M. D. Murphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213853824","@type":"Researcher","foaf:name":[{"@value":"R. S. J. Sparks"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213853827","@type":"Researcher","foaf:name":[{"@value":"J. Barclay"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213853828","@type":"Researcher","foaf:name":[{"@value":"M. R. Carroll"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579929792834560","@type":"Researcher","foaf:name":[{"@value":"A.‐M. Lejeune"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846213853696","@type":"Researcher","foaf:name":[{"@value":"T. S. 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