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

在近交界带上有重的一连串的含镍榄岩（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.

摘该蛇绿岩带的岩体由地幔榄岩组成，主岩石类型是榄岩和纯榄岩，缺少典型蛇绿岩剖面中的洋壳单元。