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. 2024 Nov 25;14:29164. doi: 10.1038/s41598-024-80729-z

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© The Author(s) 2024

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 1 — Topographic map of the greater Alpine region. Black lines delimit the main geotectonic provinces of the area based on the recent compilation by Hasterok et al. (2022)⁴³: (A) Apennine orogen, (B) Campanian arc, (C) Adriatic-Apulian Foreland, (D) Dinarides, (E) Alps, (F) Pannonian basin, (G) Molasse basin, (H) Moldanubian belt, (I) Saxo-Thuringian belt, (J) Rheno-Hercynian belt, (K) Avalonia, (L) Carpathian mountains, (M) Tyrrhenian basin, (N) Balearic basin, (O) Sardinia-Corsica block, (P) Jura mountains, (Q) Cantabrian-Pyrenean belt. Red triangles denote the locations of seismic stations. MC: Massif Central, URG: Upper Rhine Graben, BM: Bohemian Massif, VB: Vienna Basin. This map was created using PyGMT⁴⁴.