T Bodin, H Yuan, B Romanowicz - Geophysical Journal …, 2014 - academic.oup.com
Receiver functions are a powerful tool to isolate and interpret receiver-side structure effects in teleseismic seismic records. They are easily constructed by deconvolving one component …
We present a new data set of Moho depth estimates for peninsular Italy, obtained from receiver functions analysis and a grid search approach. Teleseismic records from 174 …
I Bianchi, G Pezzo, G Giordano… - Communications Earth & …, 2023 - nature.com
Abstract The destructive (Mw 3.9) earthquake of 21 August 2017 re-opened the question on where magma resides at the Ischia island volcano. The peculiar complexity of the seismic …
We use teleseismic receiver functions computed from an∼ 35‐day nodal dataset recorded along three profiles in the northern basins of Los Angeles, California, to map the depth and …
The present study investigates azimuthal anisotropy and its relation to the geodynamical processes beneath the back‐arc of the Hellenic subduction zone in the eastern Aegean and …
The crustal structure of central Apennines (Italy) is still poorly defined, leaving uncertainties on the tectonic style (thin or thick-skinned) responsible for the development of the thrust-and …
NP Agostinetti - Journal of Geodynamics, 2024 - Elsevier
We investigate the seismic structure of the mantle wedge of the Apennines subduction zone (Central Mediterranean) using teleseismic receiver function (RF). We inverted RF for both …
We investigate the crustal seismic structure and anisotropy around the central portion of the North Anatolian Fault Zone, a major plate boundary, using receiver function analysis. The …
The Colli Albani is a Quaternary quiescent volcano, located a few kilometers southeast of Rome (Italy). During the past decade, seismic swarms, ground deformation, and gas …