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Maureen Feineman, Takuya Moriguti, Tetsuya Yokoyama, Sakiko Terui and Eizo Nakamura Sediment-enriched adakitic magmas from the Daisen volcanic field, Southwest Japan Geochemistry, Geophysics, Geosystems 14

Version of Record online: 28 AUG 2013 | DOI: 10.1002/ggge.20176

Key Points

  • Daisen intermediate lavas equilibrated with garnet, likely during slab melting
  • All Daisen lavas contain significant subducted sediment
  • The basalts erupted at Daisen are not parental to the intermediate lavas

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