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Sr isotopic variation of the CM1A core samples of Oman ophiolite

We analyzed Sr isotopic ratios of gabbros and peridotites (dunite and harzburgite) collected from the drilling CM1A site that penetrates the crustal-mantle boundary of the Wadi Tayin massif in the southern Oman ophiolite. The Sr isotope ratios show good correlation with degree of alteration and estimated Sr isotope ratio of the solution circulated in peridotites is around 87Sr/86Sr = 0.7040.

[Chairperson] Noriyoshi Tsuchiya: S2-01 - S2-14

日本鉱物科学会年会

2021 Annual Meeting of Japan Association of Mineralogical Sciences (JAMS)

2021 Annual Meeting of Japan Association of Mineralogical Sciences (JAMS)

[S2-03]Sr isotopic variation of the CM1A core samples of Oman ophiolite

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