Near the border zone an important string of nickeliferous peridotites is emplaced.

在靠近交界上有要一连串含镍橄榄（体）侵入。

The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.

摘要该蛇绿体由地幔橄榄组成，主要石类型是方辉橄榄和纯橄榄，缺少典型蛇绿剖面中洋壳单元。