Late Cretaceous high Sr/Y rocks and local crustal thickening in the eastern Gangdese batholith, southern Tibet

The voluminous Late Cretaceous calc-alkaline magmatic rocks in the Gangdese batholith provide an important record on the mechanisms of the thickening and growth of the continental crust in a continental arc environment. Here, we report data from zircon UPb geochronology and geochemical (whole-rock element and SrNd isotopes and zircon Hf isotope) analyses for the granodiorite and granite from Langxian to Lilong in the eastern Gangdese batholith. These data show that 1) the intermediate-felsic rocks formed at 82–70 Ma and are Na-rich peraluminous rocks. 2) The granodiorite commonly developed magmatic epidote with allanite-rich cores. 3) They are characterized by high Sr/Y and (La/Yb)N ratios, exhibiting an adakitic affinity. 4) Most of the samples have positive εHf(t) (+5.2 − +12.4) and bulk εNd(t) (+1.9 − +2.8) values, indicating that they were derived from partial melting of juvenile crust. 5) The crustal thickness in the eastern part of the Gangdese batholith locally thickened to ∼67 km. The data presented in this paper demonstrates that the Late cretaceous granodiorite and granite were generated by partial melting of the juvenile thickened lower crust (∼67 km) with deep seated emplacement, and then they experienced rapid exhumation. The magmatic flare-up (90–75 Ma) and ocean ridge subduction in the eastern Gangdese batholith are responsible for the magma inflation and local crustal thickening.