Shear-wave velocity structure beneath the Dinarides from the inversion of Rayleigh-wave dispersion

Medientyp: E-Artikel

Titel: Shear-wave velocity structure beneath the Dinarides from the inversion of Rayleigh-wave dispersion

Beteiligte: Belinic, Tena [VerfasserIn]; Kolínský, Petr [VerfasserIn]; Stipčević, Josip [VerfasserIn]; Abreu, Rafael [VerfasserIn]; Allegretti, Ivo [VerfasserIn]; Apoloner, Maria-Theresia [VerfasserIn]; Aubert, Coralie [VerfasserIn]; Besançon, Simon [VerfasserIn]; Bés de Berc, Maxime [VerfasserIn]; Bianchi, Irene [VerfasserIn]; Bokelmann, Götz [VerfasserIn]; Brunel, Didier [VerfasserIn]; Capello, Marco [VerfasserIn]; Čarman, Martina [VerfasserIn]; Cavaliere, Adriano [VerfasserIn]; Chéze, Jérôme [VerfasserIn]; Chiarabba, Claudio [VerfasserIn]; Clinton, John [VerfasserIn]; Cougoulat, Glenn [VerfasserIn]; C. Crawford, Wayne [VerfasserIn]; Cristiano, Luigia [VerfasserIn]; Czifra, Tibor [VerfasserIn]; D’Alema, Ezio [VerfasserIn]; Danesi, Stefania [VerfasserIn]; [...]

Erschienen: Elsevier, 2021-02-01

Sprache: Englisch

DOI: https://doi.org/10.1016/j.epsl.2020.116686

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Beschreibung: Highlights • Rayleigh-wave phase velocity in the wider Dinarides region using the two-station method. • Uppermost mantle shear-wave velocity model of the Dinarides-Adriatic Sea region. • Velocity model reveals a robust high-velocity anomaly present under the whole Dinarides. • High-velocity anomaly reaches depth of 160 km in the northern Dinarides to more than 200 km under southern Dinarides. • New structural model incorporating delamination as one of the processes controlling the continental collision in the Dinarides. The interaction between the Adriatic microplate (Adria) and Eurasia is the main driving factor in the central Mediterranean tectonics. Their interplay has shaped the geodynamics of the whole region and formed several mountain belts including Alps, Dinarides and Apennines. Among these, Dinarides are the least investigated and little is known about the underlying geodynamic processes. There are numerous open questions about the current state of interaction between Adria and Eurasia under the Dinaric domain. One of the most interesting is the nature of lithospheric underthrusting of Adriatic plate, e.g. length of the slab or varying slab disposition along the orogen. Previous investigations have found a low-velocity zone in the uppermost mantle under the northern-central Dinarides which was interpreted as a slab gap. Conversely, several newer studies have indicated the presence of the continuous slab under the Dinarides with no trace of the low velocity zone. Thus, to investigate the Dinaric mantle structure further, we use regional-to-teleseismic surface-wave records from 98 seismic stations in the wider Dinarides region to create a 3D shear-wave velocity model. More precisely, a two-station method is used to extract Rayleigh-wave phase velocity while tomography and 1D inversion of the phase velocity are employed to map the depth dependent shear-wave velocity. Resulting velocity model reveals a robust high-velocity anomaly present under the whole Dinarides, reaching the depths of 160 km in the ...

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