The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该绿岩带的岩体由地幔
榄岩组成,主要岩石类
是
榄岩和纯
榄岩,缺少典
绿岩剖面中的洋壳单元。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该绿岩带的岩体由地幔
榄岩组成,主要岩石类
是
榄岩和纯
榄岩,缺少典
绿岩剖面中的洋壳单元。
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