Articles | Volume 16, issue 2
https://doi.org/10.5194/se-16-135-2025
https://doi.org/10.5194/se-16-135-2025
Research article
 | 
19 Feb 2025
Research article |  | 19 Feb 2025

On the crustal composition of the Sardinia–Corsica continental block inferred from receiver functions

Fabio Cammarano, Henrique Berger Roisenberg, Alessio Conclave, Islam Fadel, and Mark van der Meijde

Viewed

Total article views: 1,089 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
709 129 251 1,089 81 23 16
  • HTML: 709
  • PDF: 129
  • XML: 251
  • Total: 1,089
  • Supplement: 81
  • BibTeX: 23
  • EndNote: 16
Views and downloads (calculated since 24 Jul 2024)
Cumulative views and downloads (calculated since 24 Jul 2024)

Viewed (geographical distribution)

Total article views: 1,089 (including HTML, PDF, and XML) Thereof 1,065 with geography defined and 24 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Mar 2025
Download
Short summary
Sardinia and Corsica separated and have been drifting in the Mediterranean Sea for 35 Myr due to the retreat of the Ionian plate beneath the Tyrrhenian Sea. Using in-house and public data, we measured and interpreted receiver functions based on prior geophysical and petrological studies. Our findings indicate that the islands' ancient continental structure remains mostly unchanged. Alpine orogenesis about 50 million years ago influenced Corsica's crust, enriching it with water-bearing minerals.
Share