The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿岩带的岩体由地幔
榄岩
，
要岩石类型是方辉榄岩和纯榄岩，缺少典型蛇绿岩剖面中的
元。
榄岩The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿岩带的岩体由地幔榄岩，要岩石类型是方辉榄岩和纯榄岩，缺少典型蛇绿岩剖面中的元。
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