J2：地球内部・高圧化学（共催：日本地球化学会）
Experimental studies on carbon isotope fractionation in the deep Earth
詳細
Carbon is the fourth most abundant element in the solar system. It has an important role in the melting phase relations of mantle rocks and metallic core. However, our understanding of carbon isotopic composition of deep Earth is very limited. Here we review the recent results of experimental determination of partitioning of carbon isotopes at high-pressure high-temperature conditions.
