橄榄岩

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

在靠近交界带上有重要一连串含镍橄岩（体）侵入。

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

橄岩虽然发生了强烈岩化（现在岩），但岩中保了斜方辉和橄假象。

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

摘要该绿岩带岩体由地幔橄岩组成，主要岩类型是方辉橄岩和纯橄岩，缺少典型绿岩剖面中洋壳单元。