摘要
The Cretaceous Xigaze ophiolite is best exposed at the central Yarlung Zangbo Suture Zone （YZSZ, Tibet） which also includes the Gangdese arc and the Xigaze forearc basin. This study reports new geochronological and geochemical data for this ophiolite to revisit its geodynamic and petrogenetic evolution.
The Cretaceous Xigaze ophiolite is best exposed at the central Yarlung Zangbo Suture Zone （YZSZ, Tibet） which also includes the Gangdese arc and the Xigaze forearc basin. This study reports new geochronological and geochemical data for this ophiolite to revisit its geodynamic and petrogenetic evolution.
