2020
DOI: 10.1093/gji/ggz579
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Deep structure of the Hellenic lithosphere from teleseismic Rayleigh-wave tomography

Abstract: SUMMARY This research provides new constraints on the intermediate depth upper-mantle structure of the Hellenic lithosphere using a three-step Rayleigh-wave tomography. Broadband waveforms of about 1000 teleseismic events, recorded by ∼200 permanent broad-band stations between 2010 and 2018 were acquired and processed. Through a multichannel cross-correlation technique, the fundamental mode Rayleigh-wave phase-velocity dispersion curves in the period range 30–90 s were derived. The phase-velocit… Show more

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Cited by 10 publications
(1 citation statement)
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“…In the area of the Aegean Sea (Greece), there have been many studies conducted on a regional scale over the past forty years. Seismic velocity models have been obtained for various areas including western Greeceand the Aegean Sea [24][25][26][27]. However, it is worth mentioning that the lack of permanent seismic stations on the islands of the southern Aegean has made imaging of the crustal structure more challenging.…”
Section: Methodsmentioning
confidence: 99%
“…In the area of the Aegean Sea (Greece), there have been many studies conducted on a regional scale over the past forty years. Seismic velocity models have been obtained for various areas including western Greeceand the Aegean Sea [24][25][26][27]. However, it is worth mentioning that the lack of permanent seismic stations on the islands of the southern Aegean has made imaging of the crustal structure more challenging.…”
Section: Methodsmentioning
confidence: 99%