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Classification diagram for peridotite and pyroxenite, based on proportions of olivine and pyroxene. The pale green area encompasses the most common compositions of peridotite in the upper part of the Earth's mantle (partly adapted from Bodinier and Godard (2004)).

かんらん岩地球のマントルを構成する超塩基性岩の特性と分類

かんらん岩超塩基性岩マントルかんらん石
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