Late Paleozoic granitoids from central Qiangtang, northern Tibetan plateau: A record of Paleo-Tethys Ocean subduction. (November 2018)

• Record Type: Journal Article
• Authors: Zhai, Qing-guo; Wang, Jun; Hu, Pei-yuan; Lee, Hao-yang; Tang, Yue; Wang, Hai-tao; Tang, Suo-han; Chung, Sun-lin
• Is Part Of: Journal of Asian earth sciences. Volume 167(2018)
• Page Start: 139
• Page End: 151
• Publication Date: 2018-11
• Subjects: Tibet -- Qiangtang -- Late Paleozoic -- Granitoid -- Zircon U-Pb age -- Subduction -- Paleo-Tethys Ocean; Earth sciences -- Asia -- Periodicals; Sciences de la terre -- Asie -- Périodiques; Earth sciences; Asia; Periodicals; 555.05
• DOI: 10.1016/j.jseaes.2017.07.030
• Languages: English
• ISSNs: 1367-9120

Abstract

Graphical abstract: Highlights: There are Late Paleozoic granitic plutons along the Longmu Co-Shuanghu suture. These plutons emplaced between 346 Ma and 364 Ma and formed in a subduction related tectonic setting. Subduction of the Paleo-Tethys Ocean began in the Late Devonian and lasted till the Triassic. Abstract: The Longmu Co-Shuanghu suture zone in central Qiangtang, northern Tibetan plateau, is a segment of the main suture zone of the Paleo-Tethys Ocean. Numerous studies have focused on ophiolite and high-pressure metamorphic rocks from this suture zone, whereas the associated subduction-related magmatic rocks have received little attention. In this study, we present new data for the Late Paleozoic granitoids from the Gangma Co, Guoganjianian and Chasum areas along the Longmu Co-Shuanghu suture zone. Zircon U-Pb dating indicates that these granitic rocks were emplaced between 364 Ma and 346 Ma (Late Devonian-Early Carboniferous). Three granitic plutons exhibit different geochemical compositions, but show uniform Sr-Nd and zircon Hf isotopic features with positive ƐNd (T) and zircon ƐHf (T) values. Furthermore, these rocks were all formed in a volcanic arc setting associated with an oceanic subduction zone. Together with data from coeval volcanic rocks, we suggest that the Late Paleozoic magmatic rocks were formed as a result of northward subduction of the Paleo-Tethys Ocean. Subduction of the Paleo-Tethys Ocean probably commenced in the Late Devonian, continued throughout the Late Paleozoic, and ended in the Triassic.