Origins and tectonic implications of Late Cretaceous adakite and primitive high-Mg andesite in the Songdo area, southern Lhasa subterrane, Tibet

• Published in: Gondwana research Vol. 76; pp. 185 - 203
• Main Authors: Liu, Jinheng, Xie, Chaoming, Li, Cai, Fan, Jianjun, Wang, Ming, Wang, Wei, Yu, Yunpeng, Dong, Yuchao, Hao, Yujie
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.12.2019
• Subjects: Adakite; Mid-ocean ridge subduction; Neo-Tethys; Primitive high-Mg andesite; Slab rollback; Primitive high-Mg andesite; Neo-Tethys; Mid-ocean ridge subduction; Slab rollback; Adakite
• ISSN: 1342-937X; 1878-0571
• DOI: 10.1016/j.gr.2019.06.014

Late Cretaceous igneous rocks in the southern Lhasa subterrane, Tibet, include primitive high-Mg andesites and adakites, which provide important constraints on the tectonic evolution of the Neo-Tethys Ocean. Here, we present detailed zircon UPb and Hf isotopic and whole-rock geochemical data for granodioritic and dioritic porphyry samples from the Songdo area in the southern Lhasa subterrane. Zircon UPb dating indicates that the granodiorite crystallized at 88 Ma, whereas the diorite yields ages of 68 and 66 Ma. The granodiorite has adakite-like geochemical characteristics, including high Sr (801–1005 ppm) and low Y (6.8–15.2 ppm) and Yb (0.6–1.3 ppm) concentrations, and high Sr/Y (62–145) and La/Yb (39–93) ratios. We infer that the adakitic granodiorites formed through partial melting of subducted oceanic crust. The dioritic porphyry has intermediate moderate SiO2 (53–58 wt%) and high MgO (5.6–8.2 wt%) contents, and high Mg# (66.4–69.5) values, and is therefore classified as a primitive high-Mg andesite that was derived from interaction between subducted sediment and mantle. The presence of coeval adakite and charnockite, as well as high-temperature granulite-facies metamorphism, indicates that mid-ocean ridge subduction occurred at 100–80 Ma, followed by a 10 Myr hiatus in magmatism and subsequent rollback of the Neo-Tethys slab at 68 Ma. These processes resulted in significant crustal growth within the Lhasa terrane. [Display omitted] •The ocean ridge subduction of the Neo-Tethys occurred at 100–80 Ma.•The slab rollback of the Neo-Tethys was at 68 Ma and formed sanukitoid.•There was significant crustal growth in Lhasa terrane during the Late Cretaceous.