Anisotropic Reversible‐Jump McMC Shear‐Velocity Tomography of the Eastern Alpine Crust

Abstract The eastern Alpine crust has been shaped by the continental collision of the European and Adriatic plates beginning at 35 Ma and was affected by a major reorganization after 20 Ma. To better understand how the eastern Alpine surface structures link with deep seated processes, we analyze the...

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Détails bibliographiques
Auteurs principaux: E. D. Kästle, F. Tilmann, AlpArray and Swath‐D Working Groups
Format: Article
Langue:English
Publié: Wiley 2024-03-01
Collection:Geochemistry, Geophysics, Geosystems
Sujets:
Accès en ligne:https://doi.org/10.1029/2023GC011238