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

在靠近交界带上有重的一连串的含镍橄榄岩（体）的。

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

岩带的岩体由地幔橄榄岩组成，主岩石类型是方辉橄榄岩和纯橄榄岩，缺少典型岩剖面中的洋壳单元。