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
榄岩组成，主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洋壳单元。
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组成，主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洋壳单元。
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