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
榄组
，主要石类型是方辉榄和纯榄，缺少典型蛇绿剖面中的洋壳单元。
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组，主要石类型是方辉榄和纯榄，缺少典型蛇绿剖面中的洋壳单元。
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