Early Cretaceous MORB-type basalt and A-type rhyolite in northern Tibet: Evidence for ridge subduction in the Bangong–Nujiang Tethyan Ocean. (1st April 2018)

• Record Type: Journal Article
• Authors: Fan, Jian-Jun; Li, Cai; Sun, Zhen-Ming; Xu, Wei; Wang, Ming; Xie, Chao-Ming
• Is Part Of: Journal of Asian earth sciences. Volume 154(2018)
• Page Start: 187
• Page End: 201
• Publication Date: 2018-04-01
• Subjects: Tibetan plateau -- Bangong–Nujiang suture zone -- MORB-type basalt -- A-type rhyolite -- Ridge subduction; Earth sciences -- Asia -- Periodicals; Sciences de la terre -- Asie -- Périodiques; Earth sciences; Asia; Periodicals; 555.05
• DOI: 10.1016/j.jseaes.2017.12.020
• Languages: English
• ISSNs: 1367-9120

Abstract

Graphical abstract: Highlights: There are Early Cretaceous MORB-type basalt and A-type rhyolite in the Bangong–Nujiang suture zone. Ridge subduction of the Bangong–Nujiang Tethyan oceanic lithosphere occurred during the Early Cretaceous. The BNTO underwent conversion from ocean opening to ocean closure during the Late Jurassic–Early Cretaceous. Abstract: New zircon U–Pb ages, major- and trace-element data, and Hf isotopic compositions are presented for bimodal volcanic rocks of the Zhaga Formation (ZF) in the western–middle segment of the Bangong–Nujiang suture zone (BNSZ), northern Tibet. The genesis of these rocks is described, and implications for late-stage evolution of the Bangong–Nujiang Tethyan Ocean (BNTO) are considered. Detailed studies show that the ZF bimodal rocks, which occur as layers within a typical bathyal to abyssal flysch deposit, comprise MORB-type basalt that formed at a mid-ocean ridge, and low-K calc-alkaline A-type rhyolite derived from juvenile crust. The combination of MORB-type basalt, calc-alkaline A-type rhyolite, and bathyal to abyssal flysch deposits in the ZF leads us to propose that they formed as a result of ridge subduction. The A-type ZF rhyolites yield LA–ICP–MS zircon U–Pb ages of 118–112 Ma, indicating formation during the Early Cretaceous. Data from the present study, combined with regional geological data, indicate that the BNTO underwent conversion from ocean opening to ocean closure during the Late Jurassic–Early Cretaceous. The eastern segment of the BNTO closed during this period, while the western and western–middle segments were still at least partially open and active during the Early Cretaceous, accompanied by ridge subduction within the Bangong–Nujiang Tethyan Ocean.