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榄（）入。

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

橄榄虽然发生了强烈蛇纹化（现在为蛇纹），但蛇纹中保了斜方辉石和橄榄石假象。

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

摘要该蛇绿带由地幔橄榄，主要石类型是方辉橄榄和纯橄榄，缺少典型蛇绿剖面中洋壳单元。