Fig. 5From: Magma ascent and degassing processes of the 2011 and 2017–18 eruptions of Shinmoedake in Kirishima volcano group, Japan, based on petrological characteristics and volatile content of magmasBSE images of melt inclusions (arrows) in a olivine phenocryst in 2011-2SGP (11-2SG-p6-i1 and 11-2SG-p6-i2); b orthopyroxene phenocryst in 2011-2SGP (11-2SG-p13-i1 and 11-2SG-p13-i2); c clinopyroxene phenocryst in 2018-1VGP (18-1 V-p3-i1 and 18-1 V-p3-i2); and d orthopyroxene phenocryst in 2018-1VGP (18-1 V-p6-i1 and 18-1 V-p6-i2). Chemical compositions of cores and rims in the host phenocrysts are also shownBack to article page