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<span style="color:#FF7F27">[Presentation award entry]</span>

Antigorite vein formation and fluid flow in the crust-mantle transition zone in the Oman ophiolite

Antigorite is an important mineral for the estimation of the pressure/temperature condition during serpentinization. In this study, we investigated completely serpentinized dunite with antigorite veins from the crust-mantle transition zone of the Oman ophiolite. We investigated vein structures, mass transport, and fluid flux during the antigorite vein formation. The results suggest that alkaline fluid moved through the crust-mantle transition zone during the antigorite vein formation.

[Chairperson]<br />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)

[S2-04]Antigorite vein formation and fluid flow in the crust-mantle transition zone in the Oman ophiolite[Presentation award entry]

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