The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要
带的体由地幔橄榄组成，主要石类型是方辉橄榄和纯橄榄，缺少典型剖面中的洋壳单元。
浆The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要带的体由地幔橄榄组成，主要石类型是方辉橄榄和纯橄榄，缺少典型剖面中的洋壳单元。
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