Miocene adakitic intrusions in the Zhongba terrane: Implications for the origin and geochemical variations of post-collisional adakitic rocks in southern Tibet
Newly discovered adakitic rocks (ca. 16 Ma) in the Zhongba Terrane Adakitic rocks were derived from partial melting of thickened lower crust. Heterogeneity of lower crust led to geochemical variety of adakitic rocks.