Articles | Volume 16, issue 6
https://doi.org/10.5194/se-16-503-2025
https://doi.org/10.5194/se-16-503-2025
Research article
 | 
23 Jun 2025
Research article |  | 23 Jun 2025

Relict landscape evolution and fault reactivation in the eastern Tian Shan: insights from the Harlik Mountains

Zihao Zhao, Tianyi Shen, Guocan Wang, Peter van der Beek, Yabo Zhou, and Cheng Ma

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Cited articles

Allen, M. B. and Vincent, S. J.: Fault reactivation in the Junggar region, northwest China: The role of basement structures during Mesozoic–Cenozoic compression, J. Geol. Soc., 154, 151–155, https://doi.org/10.1144/gsjgs.154.1.0151, 1997. 
Allen, M. B., Alsop, G. I., and Zhemchuzhnikov, V. G.: Dome and basin refolding and transpressive inversion along the Karatau Fault System, southern Kazakstan, J. Geol. Soc., 158, 83–95, https://doi.org/10.1144/jgs.158.1.83, 2001. 
Andjic, G., Zhou, R. J., Jonell, T. N., and Aitchison, J. C.: A single Dras–Kohistan–Ladakh Arc revealed by volcaniclastic records, Geochem. Geophy. Geosy., 23, 22, https://doi.org/10.1029/2021gc010042, 2022. 
Bande, A., Sobel, E. R., Mikolaichuk, A., and Torres Acosta, V.: Talas–Fergana Fault Cenozoic timing of deformation and its relation to Pamir indentation, Geol. Soc. London Spec. Publ., 427, 295, https://doi.org/10.1144/SP427.1, 2015. 
Bande, A., Sobel, E. R., Mikolaichuk, A., Schmidt, A., and Stockli, D. F.: Exhumation history of the western Kyrgyz Tien Shan: Implications for intramontane basin formation, Tectonics, 36, 163–180, https://doi.org/10.1002/2016tc004284, 2017. 
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Short summary
This study examines the evolution of the Harlik Mountains in the eastern Tian Shan. Low-relief surfaces were formed by the Early Cretaceous erosion and subsequent tectonic stability. Later fault activity segmented these surfaces, with uplift and tilting in the Cenozoic driven by tectonic reactivation. These findings provide insights into how landscapes evolve in response to geological and environmental changes over millions of years.
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