Jinran Qiao
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
Jie Dong
Shuguang Song
Professor Mark Allen m.b.allen@durham.ac.uk
Professor
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 |
You might also like
Garnet zoning patterns record multiple processes of chemical transfer during subduction
(2024)
Journal Article
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2025
Advanced Search