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Formation–exhumation history of the Carboniferous Axi epithermal gold deposit in the Chinese Western Tianshan based on zircon U–Pb and pyrite Re–Os geochronology and (U–Th)/He zircon–apatite thermochronometry

Li, Nuo; Zhang, Bo; Danišík, Martin; Chen, Yan-Jing; Selby, David; Xiao, Wenjiao

Formation–exhumation history of the Carboniferous Axi epithermal gold deposit in the Chinese Western Tianshan based on zircon U–Pb and pyrite Re–Os geochronology and (U–Th)/He zircon–apatite thermochronometry Thumbnail


Authors

Nuo Li

Martin Danišík

Yan-Jing Chen

Wenjiao Xiao



Abstract

The Central Asian Orogenic Belt represents a Late Paleozoic archipelago, but crustal growth and the reworking and exhumation of the individual microcontinental massifs remain poorly constrained. Here, we use the Axi epithermal deposit to examine continental preservation and exhumation in the Central Asian Orogenic Belt of the Chinese Western Tianshan region. Zircon U–Pb dating and geochemistry demonstrate that the andesitic host rock formed via the incremental addition of magma in an Andean-type magmatic arc setting at 362, 354 and 342 Ma. Pyrite Re–Os data and textural evidence reveal two mineralization events at 355 and 332 Ma. Zircon (U–Th)/He data reveal temperatures of c. 180°C until 317.8 ± 9.8 Ma, which is interpreted to record the timing of exhumation of the andesite and gold ore bodies prior to their burial by Carboniferous-age sediments. Further sedimentary concealment continued until the Late Mesozoic when the system was re-exhumed between 148.6 ± 8.6 and 120.0 ± 13 Ma at a rate of c. 9.8 m Ma−1, as shown by apatite (U–Th)/He data. Collectively, the geochronology/thermochronology data show that the Chinese Western Tianshan region records a transition from compressional to extensional tectonism during the Late Paleozoic and Late Mesozoic. The shallow epithermal mineralization was protected from erosion by post-mineralization deposition.

Citation

Li, N., Zhang, B., Danišík, M., Chen, Y.-J., Selby, D., & Xiao, W. (2023). Formation–exhumation history of the Carboniferous Axi epithermal gold deposit in the Chinese Western Tianshan based on zircon U–Pb and pyrite Re–Os geochronology and (U–Th)/He zircon–apatite thermochronometry. Journal of the Geological Society, 180(4), Article jgs2021–150. https://doi.org/10.1144/jgs2021-150

Journal Article Type Article
Acceptance Date May 10, 2023
Online Publication Date Jun 27, 2023
Publication Date Jul 7, 2023
Deposit Date Nov 24, 2023
Publicly Available Date Jun 28, 2024
Journal Journal of the Geological Society
Print ISSN 0016-7649
Electronic ISSN 2041-479X
Publisher The Geological Society
Peer Reviewed Peer Reviewed
Volume 180
Issue 4
Article Number jgs2021–150
DOI https://doi.org/10.1144/jgs2021-150
Public URL https://durham-repository.worktribe.com/output/1948405