Articles | Volume 16, issue 6
https://doi.org/10.5194/se-16-503-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-16-503-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Relict landscape evolution and fault reactivation in the eastern Tian Shan: insights from the Harlik Mountains
Zihao Zhao
Institute of Geological Survey, China University of Geosciences, Wuhan, 430074, China
Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China
Guocan Wang
CORRESPONDING AUTHOR
Institute of Geological Survey, China University of Geosciences, Wuhan, 430074, China
Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China
Peter van der Beek
Institute of Geosciences, University of Potsdam, 14476 Potsdam, Germany
Yabo Zhou
PowerChina Huadong Engineering Corporation Limited, Hangzhou, 310012, China
Cheng Ma
Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China
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Maxime Bernard, Pieter van der Beek, Cody Colleps, Xavier Robert, Kerry Gallagher, William Guenthner, Julien Amalberti, and Georgina E. King
EGUsphere, https://doi.org/10.5194/egusphere-2026-2286, https://doi.org/10.5194/egusphere-2026-2286, 2026
This preprint is open for discussion and under review for Geochronology (GChron).
Short summary
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Pecube, a 3D thermal-kinematic software that predicts thermochronometer data, has been widely used to constrain the past evolution of mountain belts, but its accessibility and application is still limited. This work overcomes this limitation by offering a graphical user interface to Pecube, PecubeGUI, and by broadening its application to a wider range of tectonic settings through the implementation thermochronometer prediction models in line with the most recent research developments.
Maxime Bernard, Georgina E. King, Pieter van der Beek, Isabel Wapenhans, Lingxiao Gong, and Xavier Robert
EGUsphere, https://doi.org/10.5194/egusphere-2026-2508, https://doi.org/10.5194/egusphere-2026-2508, 2026
This preprint is open for discussion and under review for Geochronology (GChron).
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Thermochronometry data inversions using the Pecube software are useful to constrain the past evolution of mountain belts. However, configuring the neighbourhood algorithm for Pecube inversions remains challenging for new Pecube users. This contribution aims to provide intuition and guidelines for setting up NA-Pecube inversions to support informed decision-making. It forms part of a broader effort to improve the accessibility of Pecube to new users.
Lingxiao Gong, Peter van der Beek, Taylor F. Schildgen, Edward R. Sobel, Simone Racano, Apolline Mariotti, and Fergus McNab
Earth Surf. Dynam., 12, 973–994, https://doi.org/10.5194/esurf-12-973-2024, https://doi.org/10.5194/esurf-12-973-2024, 2024
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We choose the large Saryjaz river from South Tian Shan to analyse topographic and fluvial metrics. By quantifying the spatial distribution of major metrics and comparing with modelling patterns, we suggest that the observed transience was triggered by a big capture event during the Plio-Pleistocene and potentially affected by both tectonic and climate factors. This conclusion underlines the importance of local contingent factors in driving drainage development.
Marion Roger, Arjan de Leeuw, Peter van der Beek, Laurent Husson, Edward R. Sobel, Johannes Glodny, and Matthias Bernet
Solid Earth, 14, 153–179, https://doi.org/10.5194/se-14-153-2023, https://doi.org/10.5194/se-14-153-2023, 2023
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We study the construction of the Ukrainian Carpathians with LT thermochronology (AFT, AHe, and ZHe) and stratigraphic analysis. QTQt thermal models are combined with burial diagrams to retrieve the timing and magnitude of sedimentary burial, tectonic burial, and subsequent exhumation of the wedge's nappes from 34 to ∼12 Ma. Out-of-sequence thrusting and sediment recycling during wedge building are also identified. This elucidates the evolution of a typical wedge in a roll-back subduction zone.
Peter van der Beek and Taylor F. Schildgen
Geochronology, 5, 35–49, https://doi.org/10.5194/gchron-5-35-2023, https://doi.org/10.5194/gchron-5-35-2023, 2023
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Thermochronometric data can provide unique insights into the patterns of rock exhumation and the driving mechanisms of landscape evolution. Several well-established thermal models allow for a detailed exploration of how cooling rates evolved in a limited area or along a transect, but more regional analyses have been challenging. We present age2exhume, a thermal model that can be used to rapidly provide a synoptic overview of exhumation rates from large regional thermochronologic datasets.
Coline Ariagno, Caroline Le Bouteiller, Peter van der Beek, and Sébastien Klotz
Earth Surf. Dynam., 10, 81–96, https://doi.org/10.5194/esurf-10-81-2022, https://doi.org/10.5194/esurf-10-81-2022, 2022
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The
critical zonenear the surface of the Earth is where geologic substrate, erosion, climate, and life meet and interact. This study focuses on mechanisms of physical weathering that produce loose sediment and make it available for transport. We show that the sediment export from a monitored catchment in the French Alps is modulated by frost-weathering processes and is therefore sensitive to complex modifications in a warming climate.
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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.
This study examines the evolution of the Harlik Mountains in the eastern Tian Shan. Low-relief...