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
榄
，主要石类型是方辉榄和纯榄，缺少典型蛇绿剖面中的洋
。
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榄，主要石类型是方辉榄和纯榄，缺少典型蛇绿剖面中的洋。
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