Articles | Volume 13, issue 5
https://doi.org/10.5194/esurf-13-907-2025
© 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/esurf-13-907-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Sep 2025
Research article |
| 15 Sep 2025
| 15 Sep 2025
Grain size dynamics using a new planform model – Part 3: Stratigraphy and flexural foreland evolution
GFZ Helmholtz Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
The Institute of Geosciences, Universität Potsdam, Potsdam, Germany
Jean Braun
GFZ Helmholtz Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
The Institute of Geosciences, Universität Potsdam, Potsdam, Germany
Alexander C. Whittaker
Department of Earth Science and Engineering, Royal School of Mines, Imperial College London,London, UK
Sebastien Castelltort
Department of Earth Sciences, University of Geneva, Rue des Maraîchers 13, 1205 Geneva, Switzerland
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Sediments deposited within river channels form the stratigraphic record, which has been used to interpret tectonic events, basin subsidence, and changes in precipitation long after ancient mountain chains have eroded away. Our work combines methods for estimating gravel fining with a landscape evolution model in order to analyze the grain size preserved within the stratigraphic record with greater complexity (e.g. considering topography and channel dynamics) than past approaches.
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Sediments deposited within river channels form the stratigraphic record, which has been used to interpret tectonic events, basin subsidence, and changes in precipitation long after ancient mountain chains have eroded away. Our work combines methods for estimating gravel fining with a Landscape Evolution Model in order to analyze the grain size preserved within the stratigraphic record with greater complexity (e.g. considering topography and channel dynamics) than past approaches.
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Sediments deposited within river channels form the stratigraphic record, which has been used to interpret tectonic events, basin subsidence, and changes in precipitation long after ancient mountain chains have eroded away. Our work combines methods for estimating gravel fining with a landscape evolution model in order to analyze the grain size preserved within the stratigraphic record with greater complexity (e.g. considering topography and channel dynamics) than past approaches.
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Short summary
Sediments deposited within river channels form the stratigraphic record, which has been used to interpret tectonic events, basin subsidence, and changes in precipitation long after ancient mountain chains have eroded away. Our work combines methods for estimating gravel fining with a landscape evolution model in order to analyze the grain size preserved within the stratigraphic record with greater complexity (e.g. considering topography and channel dynamics) than past approaches.
Sediments deposited within river channels form the stratigraphic record, which has been used to...
