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Development of a Modern-Style Trench-Arc-Backarc System in the Proto-Tethys Ocean (Qilian Orogenic Belt, NW China)

Qiao, Jinran; Dong, Jie; Song, Shuguang; Allen, Mark B.; Wang, Chao; Xia, Xiaohong; Su, Li

Authors

Jinran Qiao

Jie Dong

Shuguang Song

Chao Wang

Xiaohong Xia

Li Su



Abstract

The development of trench-arc-backarc (TABA) systems is uniquely associated with modern-style plate tectonics on Earth. The Qilian orogenic belt in NW China records the evolution history of the Proto-Tethys Ocean at the transition time from the Proterozoic to Phanerozoic. This paper presents systematic studies of petrography, U-Pb chronology and geochemistry on various rocks from a middle-ocean ridge (MOR)-type ophiolite belt, active continental margin and back-arc basin in the Qilian orogenic belt to address the development of a modern-style TABA system. Arc magmas include felsic intrusions with ages of 531 to 477 Ma and felsic-mafic arc volcanic rocks with ages of 506 to 439 Ma, showing distinctive features of typical magmatic rocks formed at an Andean-type continental margin. The back-arc basin is recorded by a 490- to 448-Ma suprasubduction zone (SSZ)-type ophiolite with boninite, and Silurian turbidite flysch formation. We establish a three-stage tectonic history from the initiation of subduction to the formation of a mature Japan-Sea-type back-arc basin at the active continental margin in the Early Paleozoic era. (1) Northward subduction of Proto-Tethys Ocean initiated and the Andean-type continental arc developed at ∼530 to 500 Ma with continual crustal thickening; (2) a tectonic transition occurred from an Andean-type active continental margin to a West Pacific-type active continental margin at ∼500 to 490 Ma with rapid thinning of crust to ∼35 km; and (3) mature ocean basins and back-arc-basin (BAB) ophiolites were formed in the back-arc extensional environment at ∼490 to 450 Ma.

Citation

Qiao, J., Dong, J., Song, S., Allen, M. B., Wang, C., Xia, X., & Su, L. (2023). Development of a Modern-Style Trench-Arc-Backarc System in the Proto-Tethys Ocean (Qilian Orogenic Belt, NW China). Journal of Petrology, 64(5), Article egad029. https://doi.org/10.1093/petrology/egad029

Journal Article Type Article
Acceptance Date Apr 25, 2023
Online Publication Date Apr 29, 2023
Publication Date May 1, 2023
Deposit Date Feb 27, 2025
Journal Journal of Petrology
Print ISSN 0022-3530
Electronic ISSN 1460-2415
Publisher Oxford University Press
Peer Reviewed Peer Reviewed
Volume 64
Issue 5
Article Number egad029
DOI https://doi.org/10.1093/petrology/egad029
Public URL https://durham-repository.worktribe.com/output/3550552