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