Solid Earth
Solid Earth
SE
Articles | Volume 17, issue 6
Articles | Volume 17, issue 6
https://doi.org/10.5194/se-17-867-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-17-867-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 17, issue 6
Research article
 | 
25 Jun 2026
Research article |  | 25 Jun 2026

A vast Caledonian fan and an Ediacaran arc: the contrasting provenance of Devonian clastics of Brunia (Bohemian Massif)

Stephen Collett, Igor Soejono, Tomáš Kumpan, Pavel Hanžl, Jitka Míková, Nikol Novotná, and Jiří Sláma

Viewed

Total article views: 1,953 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,085 739 129 1,953 151 82 114
  • HTML: 1,085
  • PDF: 739
  • XML: 129
  • Total: 1,953
  • Supplement: 151
  • BibTeX: 82
  • EndNote: 114
Views and downloads (calculated since 16 Jan 2026)
Cumulative views and downloads (calculated since 16 Jan 2026)

Viewed (geographical distribution)

Total article views: 1,953 (including HTML, PDF, and XML) Thereof 1,953 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 25 Jun 2026
Download
Short summary
Brunia is a Neoproterozoic crustal block whose pre-Variscan history is unclear. New U–Pb and Lu–Hf detrital zircon data from Devonian strata reveal two provenance types. Type-1 spectra reflect recycling of local Brunia arc sources and show isotopic similarity to West Avalonia, indicating a shared Neoproterozoic history. Type-2 spectra match Fennoscandian datasets, implying sediment input from the Caledonides and an Early Devonian connection between Brunia and Baltica.
Read more
Share