Li isotopic analysis with MC-ICP-MS and its application to mantle xenoliths from Avacha volcano, the Kamchatka arc

KIM Taehoon; NAKAI Shun'ichi; ARAI Shoji

doi:10.14862/geochemproc.52.0.186.0

2005年度日本地球化学会第52回年会講演要旨集

セッションID: 2P40

DOI https://doi.org/10.14862/geochemproc.52.0.186.0

会議情報

主催: 日本地球化学会

共催: 日本化学会

課題講演4 地殻-マントル-核の物質循環と固体地球の化学進化

Li isotopic analysis with MC-ICP-MS and its application to mantle xenoliths from Avacha volcano, the Kamchatka arc

*KIM Taehoon, NAKAI Shun'ichi, ARAI Shoji

著者情報

キーワード: Li isotopes, MC-ICP-MS, mantle xenolith, Kamchatka arc, mantle metasomatism

会議録・要旨集フリー

詳細

抄録

Li isotopic ratio and its contents were determined using MC-ICP-MS. Li was separated through cation-exchange resin, based on the procedure by Nishio and Nakai (2002). In its application, we report the Li isotopic ratio and its contents of mantle xenoliths from Avacha volcano as fragments of mantle wedge of the Kamchatka arc, and discuss the relationship between Li isotopes and mantle metasomatism.

責任著者(Corresponding author)

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