论文部分内容阅读
The Gongzhucuo ophiolite,located near Lake Gongzhu in SW Tibet,occurs in the southern ophiolite sub-belt along the western Yarlung Zangbo suture zone.It is is mainly composed of harzburgitic and lherzolitic upper mantle peridotites,intruded by mafic dikes.The mantle
The Gongzhucuo ophiolite, located near Lake Gongzhu in SW Tibet, occurs in the southern ophiolite sub-belt along the western Yarlung Zangbo suture zone. It is mainly composed of harzburgitic and lherzolitic upper mantle peridotites, intruded by mafic dikes. Mantle