Conduction mechanisms of fayalite and γ-Fe2SiO4: Implication to electrical conductivity jump through olivine-spinel transition in the Earth’s interior

Abstracts for Annual Meeting of the Mineralogical Society of Japan

Abstracts for the 50th Anniversary Meeting (2002) of the Mineralogical Society of Japan

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Host: The Mineralogical Society of Japan

Conduction mechanisms of fayalite and γ-Fe₂SiO₄:

Implication to electrical conductivity jump through olivine-spinel transition in the Earth’s interior

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