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Fig. 3 | Earth, Planets and Space

Fig. 3

From: 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 magmas

Fig. 3Fig. 3

Chemical 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 names

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