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The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.

该蛇绿带的体由地幔橄石类型是方辉橄和纯橄,缺少典型蛇绿剖面中的洋壳单元。

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3G, 401(K), a,

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