Articles | Volume 16, issue 7
https://doi.org/10.5194/se-16-619-2025
https://doi.org/10.5194/se-16-619-2025
Research article
 | Highlight paper
 | 
10 Jul 2025
Research article | Highlight paper |  | 10 Jul 2025

Evidence for multi-rifting in the Variscan–Alpine cycle transition: insights from the European western Southern Alps

Emanuele Scaramuzzo, Franz A. Livio, Maria Giuditta Fellin, and Colin Maden

Viewed

Total article views: 2,583 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,889 292 402 2,583 95 120 161
  • HTML: 1,889
  • PDF: 292
  • XML: 402
  • Total: 2,583
  • Supplement: 95
  • BibTeX: 120
  • EndNote: 161
Views and downloads (calculated since 29 Apr 2024)
Cumulative views and downloads (calculated since 29 Apr 2024)

Viewed (geographical distribution)

Total article views: 2,583 (including HTML, PDF, and XML) Thereof 2,571 with geography defined and 12 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 22 Oct 2025
Download
Executive editor
I concur with the AE's assessment that this paper presents valuable new models on the Permo-Triassic evolution of the Alps.
Short summary

We address the transition between the Paleozoic Variscan and Alpine Mesozoic–Cenozoic cycles using tectono-stratigraphy and thermochronology. This transition unfolds through a multi-phase rifting history. An initial rifting stage occurred in the early Permian, followed in the early–middle Permian by a phase of transcurrent tectonics. This was succeeded by a period of erosion/non-deposition in the middle Permian. Crustal stretching in the Middle Triassic marked the onset of the Alpine cycle.

Share