Fig. 11From: Time variations in the chemical and isotopic composition of fumarolic gases at Hakone volcano, Honshu Island, Japan, over the earthquake swarm and eruption in 2015, interpreted by magma sealing modelH2O and CO2 concentration dissolved in rhyolitic magma at 900 °C with isobaric vapor lines. G0 and G1: isobaric lines at 2256 and 2325 bar, respectivelyBack to article page