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

在靠近交界带上有重一连镍榄岩（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.

摘该蛇绿岩带岩体由榄岩组成，主岩石类型是方辉榄岩和纯榄岩，缺少典型蛇绿岩剖面中洋壳单元。