Host: Abstracts of Annual Meeting of the Geochemical Society of Japan
Pages 219-
Noble gas and carbon isotope ratios of volcanic and hot-spring gases collected at Kusatsu-Shirane volcano, Japan were determined. No temporal change in 3He/4He ratios was observed even after volcanic unrest since June 2014. The carbon isotope ratio and CO2/3He ratios are typical values for subduction zone volcanic fluid samples, with dominant contribution of marine carbonates.