Early Pleistocene age of fluvial sediment in the Stará Garda Cave revealed by 26Al/10Be burial dating: implications for geomorphic evolution of the Malé Karpaty Mts. (Western Carpathians)

Physically based morphostructural land surface segmentation: Case of the Alps and Western Carpathians

“…Systematic investigation of relationships between tectonic uplift, denudation rate, and topography is missing here. The high spatio‐temporal variability of the published denudation, accommodation, and uplift rates across the Western Carpathians and the adjacent Pannonian Basin (e.g., Bella et al., 2019; Jacko et al., 2021; Šujan et al., 2017, 2018, 2021; Zuchiewicz, 2009) argues against a neotectonic (Pliocene–Quaternary) tendency to steady state. Due to a dominant extensional regime, the highest differential vertical neotectonic movements are supposed on the boundary with the Pannonian basin (Šujan et al., 2021) and on the boundaries of small intramountain basins (e.g., Kováč et al., 2011).…”