Fig. 2From: Middle Miocene forearc alkaline magmatism in Amami-Oshima Island, central Ryukyu Arc: implications for paleoreconstruction of Shikoku BasinOccurrence of basaltic dikes at Naon in Amami-Oshima Island. a Two basaltic dikes intrude massive basalt and grey chert in the mélange. b Basaltic dike cuts massive basalt, reddish chert, varicolored shale, and grey chert. c Contact between dike and chert. d Chilled margin preserved along the boundary between dike and massive basalt. Locations of panels b–d are shown in aBack to article page