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
该蛇绿岩带
岩体由地幔
榄岩组
，
岩石类型是方辉榄岩和纯榄岩，缺少典型蛇绿岩剖面中
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.
摘该蛇绿岩带岩体由地幔榄岩组，岩石类型是方辉榄岩和纯榄岩，缺少典型蛇绿岩剖面中单元。
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