Fig. 3From: 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 magmasChemical compositions of a plagioclase-phenocryst cores, b plagioclase-phenocryst rims, c groundmass-plagioclase cores, d olivine-phenocryst cores, e olivine-phenocryst rims, f groundmass-olivine cores, g clinopyroxene-phenocryst cores, h clinopyroxene-phenocryst rims, i groundmass-clinopyroxene cores, j orthopyroxene-phenocryst cores, k orthopyroxene-phenocryst rims, and l groundmass-orthopyroxene cores. An = Ca/(Ca + Na) × 100% in mol. Mg# = Mg/(Mg + Fe) × 100% in mol. Refer to Table 1 for sample namesBack to article page