Articles | Volume 9, issue 3
https://doi.org/10.5194/gmd-9-997-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-9-997-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Model description paper
| 
08 Mar 2016
Model description paper |
| 08 Mar 2016
Open-source modular solutions for flexural isostasy: gFlex v1.0
Institut für Erd- und Umweltwissenschaften, Universität Potsdam, Potsdam-Golm, Germany
Department of Earth Sciences, University of Minnesota, Minneapolis, MN, USA
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- Development of Foreland Intracratonic Plateaus (Ozark Plateau and Appalachian Plateaus): A Consequence of Topographic Inversion Due To Erosion of Adjacent Fold‐Thrust Belts A. Anders et al. 10.1029/2021TC006957
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- Mechanisms of Subsidence and Uplift of Southern Patagonia and Offshore Basins During Slab Window Formation X. Ding et al. 10.1029/2022GC010844
- PALEOSTRIPv1.0 – a user-friendly 3D backtracking software to reconstruct paleo-bathymetries F. Colleoni et al. 10.5194/gmd-14-5285-2021
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- Glacial isostatic uplift of the European Alps J. Mey et al. 10.1038/ncomms13382
- Toolbox for Analysis of Flexural Isostasy (TAFI)—A MATLAB toolbox for modeling flexural deformation of the lithosphere S. Jha et al. 10.1130/GES01421.1
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Saved (preprint)
Latest update: 26 Dec 2024
Short summary
Earth's lithosphere bends beneath surface loads, such as ice, sediments, and mountain belts. The pattern of this bending, or flexural isostatic response, is a function of both the loads and the spatially variable strength of the lithosphere. gFlex is an easy-to-use program to calculate flexural isostastic response, and may be used to better understand how ice sheets, glaciers, large lakes, sedimentary basins, volcanoes, and other surface loads interact with the solid Earth.
Earth's lithosphere bends beneath surface loads, such as ice, sediments, and mountain belts. The...
