P wave tomography of the mantle under the Alpine‐Mediterranean area
We study the upper mantle P wave velocity structure below the Euro‐Mediterranean area,
down to 1000 km depth, by seismic travel time tomography. We invert summary residuals …
down to 1000 km depth, by seismic travel time tomography. We invert summary residuals …
[BOOK][B] Evolution of the southern Tyrrhenian slab tear and active tectonics along the western edge of the Tyrrhenian subducted slab
A Argnani - 2009 - lyellcollection.org
The evolution of the southern Tyrrhenian subduction has been possibly controlled by distinct
episodes of slab break-off as indicated by a critical review of the geological literature and by …
episodes of slab break-off as indicated by a critical review of the geological literature and by …
Upper mantle seismic velocities and anisotropy in China determined through Pn and Sn tomography
S Pei, J Zhao, Y Sun, Z Xu, S Wang… - Journal of …, 2007 - Wiley Online Library
We have obtained velocity images of the uppermost mantle beneath China by performing
tomographic inversion of both Pn and Sn traveltimes. From the Annual Bulletin of Chinese …
tomographic inversion of both Pn and Sn traveltimes. From the Annual Bulletin of Chinese …
P- and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30°
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …
Evolution of the Calabrian accretionary wedge (central Mediterranean)
The Neogene tectonics of the central Mediterranean are related to the subduction and
trench rollback of the Ionian basin under Eurasia, causing the opening of the Liguro …
trench rollback of the Ionian basin under Eurasia, causing the opening of the Liguro …
Shallow subduction beneath Italy: Three‐dimensional images of the Adriatic‐European‐Tyrrhenian lithosphere system based on high‐quality P wave arrival times
This paper presents a velocity model of the Italian (central Mediterranean) lithosphere in
unprecedented detail. The model is derived by inverting a set of 166,000 Pg and Pn seismic …
unprecedented detail. The model is derived by inverting a set of 166,000 Pg and Pn seismic …
Active stress map of Italy
We present a new map of the present‐day stress field in Italy obtained from all the available
data. The map reports 200 horizontal stress directions inferred from 109 borehole breakout …
data. The map reports 200 horizontal stress directions inferred from 109 borehole breakout …
Uppermost mantle velocities and anisotropy beneath Europe
TM Hearn - Journal of Geophysical Research: Solid Earth, 1999 - Wiley Online Library
Pn data collected within southern Europe and the Mediterranean are used to
tomographically image variations in both seismic velocity and seismic anisotropy. Seismic …
tomographically image variations in both seismic velocity and seismic anisotropy. Seismic …
Crust and upper mantle of Kamchatka from teleseismic receiver functions
Teleseismic receiver functions (RFs) from a yearlong broadband seismological experiment
in Kamchatka reveal regional variations in the Moho, anisotropy in the supra-slab mantle …
in Kamchatka reveal regional variations in the Moho, anisotropy in the supra-slab mantle …
A 3D Vs model of the upper mantle beneath Italy: Insight on the geodynamics of central Mediterranean
G Giacomuzzi, M Civalleri, P De Gori… - Earth and Planetary …, 2012 - Elsevier
We compute a high resolution Vs model of the upper mantle underneath Italy by inverting
relative residuals of S-wave arrivals from teleseisms recorded at the Italian broad-band …
relative residuals of S-wave arrivals from teleseisms recorded at the Italian broad-band …