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

在靠近交界带上有要的一连串的含镍岩（体）的侵入。

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

摘要该蛇绿岩带的岩体由地幔岩组成，主要岩石类型是方岩和纯岩，缺少典型蛇绿岩剖面中的洋壳单元。