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
带的体由地幔
组
，主要石类型是方辉和纯，缺少典型蛇绿剖面中的洋壳单元。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿带的体由地幔组，主要石类型是方辉和纯，缺少典型蛇绿剖面中的洋壳单元。
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