The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该带的体地幔榄组成,主要石型是方辉榄和纯榄,缺少典型剖面中的洋壳单元。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该带的体地幔榄组成,主要石型是方辉榄和纯榄,缺少典型剖面中的洋壳单元。
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