Late Cretaceous adakitic rocks from the western Tibetan Plateau: implications for the subduction of the Neo-Tethys Ocean. Issue 15 (13th October 2021)

• Record Type: Journal Article
• Authors: Wang, Wei; Zhai, Qing-Guo; Hu, Pei-Yuan; Chung, Sun-Lin; Tang, Yue; Wang, Hai-Tao; Zhu, Zhi-Cai; Wu, Hao; Huang, Zhi-Qiang
• Is Part Of: International geology review. Volume 63:Issue 15(2021)
• Page Start: 1884
• Page End: 1899
• Publication Date: 2021-10-13
• Subjects: Tibetan plateau -- adakite -- late cretaceous -- neo-tethys ocean -- subduction; Geology -- Periodicals; Electronic journals; 551.05
• DOI: 10.1080/00206814.2020.1805803
• Languages: English
• ISSNs: 0020-6814

Abstract

ABSTRACT: It is still hotly debated whether the subduction of the Indus-Yarlung Zangbo Tethyan oceanic lithosphere led to Cretaceous magmatism in the north Lhasa terrane or not. Here, we provide new data on adakitic dacite in the Rutog area, western Tibetan Plateau. Zircon U-Pb dating and Lu-Hf analyses yielded a weighted-mean 206 Pb/ 238 U age of ca . 97 Ma for a dacite sample, and corresponding positive zircon εHf ( t ) values of +5.3 to +10.1. All samples have high Sr (796–1091ppm), but low Y (10.4–11.9 ppm) and Yb (0.68–0.79 ppm) contents, with pronounced high Sr/Y (72.5–97.6) ratios. Furthermore, they have low K2 O (1.11–1.49 wt.%) and Th (4.18–4.54 ppm) contents, and low K2 O/Na2 O (0.18–0.28) and Th/La (0.22–0.24) ratios. These geochemical features are most simialr to those of adakite derived from partial melting of subducted oceanic slab. These new data, in combination with regional geology, enable us to suggest that the Late Cretaceous arc-affinity magmatic rocks were probably triggered by northward subduction of the Indus-Yarlung Zangbo oceanic lithosphere. This will give new insights into the geodynamic evolution of the Indus-Yarlung Zangbo Neo-Tethys Ocean.