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
岩带的岩体由地幔
榄岩组
，主要岩石类型是方辉榄岩
榄岩，缺少典型岩剖面中的洋壳单元。
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