Articles | Volume 74, issue 1
https://doi.org/10.5194/egqsj-74-59-2025
https://doi.org/10.5194/egqsj-74-59-2025
Research article
 | 
18 Feb 2025
Research article |  | 18 Feb 2025

Iterative outlier identification for robust cosmogenic 26Al∕10Be burial dating of fluvial terraces: a case study from the Danube River (Vienna Basin, Austria)

Zsófia Ruszkiczay-Rüdiger, Stephanie Neuhuber, Esther Hintersberger, and Jesper Nørgaard

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Cited articles

Balco, G. and Rovey, C. W.: An isochron method for cosmogenic-nuclide dating of buried soils and sediments, Am. J. Sci., 308, 1083–1114, https://doi.org/10.2475/10.2008.02, 2008. 
Balco, G.: Production rate calculations for cosmic-ray-muon-produced 10Be and 26Al benchmarked against geological calibration data, Quat. Geochronol. 39, 150–173, https://doi.org/10.1016/j.quageo.2017.02.001, 2017. 
Bender, A. M., Amos, C. B., Bierman, P., Rood, D. H., Staisch, L., Kelsey, H., and Sherrod, B.: Differential uplift and incision of the Yakima River terraces, central Washington State, J. Geophys. Res.-Sol. Earth, 121, 365–384, https://doi.org/10.1002/2015JB012303, 2016. 
Blard, P. H., Bourlés, D., Lave, J., and Pik, R.: Applications of ancient cosmic-ray exposures: theory, techniques and limitations, Quat. Geochronol., 1, 59–73, https://doi.org/10.1016/j.quageo.2006.06.003, 2006. 
Borchers, B., Marrero, S., Balco, G., Caffee, M., Goehring, B., Lifton, N., Nishiizumi, K., Phillips, F., Schaefer, J., and Stone, J.: Geological calibration of spallation production rates in the CRONUS-Earth project, Quat. Geochronol., 31, 188–198, https://doi.org/10.1016/j.quageo.2015.01.009, 2016. 
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Short summary
Accurateness of dates and rates of landscape evolution depends on the precision of the geochronological data. This study offers a robust methodology of outlier identification for modelling the cosmogenic nuclide isochron burial age of fluvial sediments. The method is tested on a fluvial terrace of the Danube River in the Vienna Basin and provides novel information for the quantification of the uplift rate of the area. The presented methodology is applicable in other fluvial settings as well.
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