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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