Shear-wave velocity variations in the upper mantle beneath central Europe
A Zielhuis, G Nolet - Geophysical Journal International, 1994 - academic.oup.com
Summary A new model, EUR-S91, of shear-wave velocity variations in the upper mantle
beneath central Europe and surrounding regions, down to a depth of 670km, is presented …
beneath central Europe and surrounding regions, down to a depth of 670km, is presented …
A shear wave velocity model of the European upper mantle from automated inversion of seismic shear and surface waveforms
CP Legendre, T Meier, S Lebedev… - Geophysical Journal …, 2012 - academic.oup.com
We present a new, S-velocity model of the European upper mantle, constrained by
inversions of seismic waveforms from broad-band stations in Europe and surrounding …
inversions of seismic waveforms from broad-band stations in Europe and surrounding …
Lateral heterogeneity of Europe's upper mantle as inferred from modelling of broad-band body waves
H Paulssen - Geophysical Journal International, 1987 - academic.oup.com
The upper mantle velocity structure beneath Europe is investigated by body-wave modelling
of broad-band seismograms from earthquakes in the eastern Mediterranean recorded by …
of broad-band seismograms from earthquakes in the eastern Mediterranean recorded by …
The contrast in upper mantle shear-wave velocity between the East European Platform and tectonic Europe obtained with genetic algorithm inversion of Rayleigh …
Summary The stable, Precambrian East European Platform adjoins the younger, tectonically
active regions of central and western Europe along a distinct crustal boundary, the Tornquist …
active regions of central and western Europe along a distinct crustal boundary, the Tornquist …
The upper mantle under western Europe inferred from the dispersion of Rayleigh modes
G Nolet - Journal of Geophysics, 1977 - journal.geophysicsjournal.com
A stacking technique is applied to measure phase velocities of the fundamental and several
higher Rayleigh modes over an array of long period stations located in Western Europe. The …
higher Rayleigh modes over an array of long period stations located in Western Europe. The …
Upper-mantle structure in southern Norway from beamforming of Rayleigh wave data presenting multipathing
V Maupin - Geophysical Journal International, 2011 - academic.oup.com
A model for the upper mantle SV-wave velocity under southern Norway is obtained by depth
inversion of the average phase velocity of the Rayleigh wave fundamental mode in the area …
inversion of the average phase velocity of the Rayleigh wave fundamental mode in the area …
EurID: a regionalized 3-D seismological model of Europe
This paper presents a 3-D regionalized model of the European crust and mantle velocity
structure down to depths of approximately 300 km. The model is entirely based upon the …
structure down to depths of approximately 300 km. The model is entirely based upon the …
An upper-mantle S-wave velocity model for Northern Europe from Love and Rayleigh group velocities
A model of upper-mantle S-wave velocity and transverse anisotropy beneath northwestern
Europe is presented, based on regional surface wave observations. Group velocities for …
Europe is presented, based on regional surface wave observations. Group velocities for …
Upper mantle structure under western Europe from fundamental and higher mode surface waves using the NARS array
B Dost - Geophysical Journal International, 1990 - academic.oup.com
A generalized inversion of a new data set, consisting of surface wave phase velocities and
Sn traveltimes, has resulted in a new shear velocity and density model for the west …
Sn traveltimes, has resulted in a new shear velocity and density model for the west …
EPmantle: a 3-D transversely isotropic model of the upper mantle under the European Plate
R Schivardi, A Morelli - Geophysical Journal International, 2011 - academic.oup.com
We present a new 3-D transversely isotropic shear wave velocity model of the European and
Mediterranean upper mantle obtained by analysis of surface waves. Data used are …
Mediterranean upper mantle obtained by analysis of surface waves. Data used are …
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