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

在靠近交界带上有重要的一连串的含镍（体）的侵入。

Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.

虽然发生了强化（现在），但中保留了斜方辉石和石的假象。

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

摘要该绿带的体由地幔组成，主要石类型是方辉和纯，缺少典型绿剖面中的洋壳单元。