Articles | Volume 12, issue 5
https://doi.org/10.5194/se-12-1051-2021
https://doi.org/10.5194/se-12-1051-2021
Research article
 | 
11 May 2021
Research article |  | 11 May 2021

Transversely isotropic lower crust of Variscan central Europe imaged by ambient noise tomography of the Bohemian Massif

Jiří Kvapil, Jaroslava Plomerová, Hana Kampfová Exnerová, Vladislav Babuška, György Hetényi, and AlpArray Working Group

Viewed

Total article views: 1,895 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,349 508 38 1,895 161 31 30
  • HTML: 1,349
  • PDF: 508
  • XML: 38
  • Total: 1,895
  • Supplement: 161
  • BibTeX: 31
  • EndNote: 30
Views and downloads (calculated since 27 Oct 2020)
Cumulative views and downloads (calculated since 27 Oct 2020)

Viewed (geographical distribution)

Total article views: 1,895 (including HTML, PDF, and XML) Thereof 1,764 with geography defined and 131 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 21 Feb 2024
Download
Short summary
This paper presents a high-resolution 3-D shear wave velocity (vS) model of the Bohemian Massif crust imaged from high-density data and enhanced depth sensitivity of tomographic inversion. The dominant features of the model are relatively higher vS in the upper crust than in its surrounding, a distinct intra-crustal interface, and a velocity decrease in the lower part of the crust. The low vS in the lower part of the crust is explained by the anisotropic fabric of the lower crust.