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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />

(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />

Interior<br />

JSS013 Poster presentation 2249<br />

Surface wave tomography in Euro-Mediterranean region<br />

Dr. Renata Schivardi<br />

Andrea Morelli<br />

We present a transversely isotropic shear wave velocity model of the upper mantle beneath Europe and<br />

the Mediterranean region, obtained by non-linear inversion of surface wave group velocity maps. Group<br />

velocity maps result from the regionalization of a dataset of measurements of fundamental mode Love<br />

and Rayleigh wave dispersion, carried out with iterated multiple filtering, and phase-matched filtering<br />

techniques. The linear inverse problem is stabilized using a priori information in the form of a global<br />

group velocity reference model, derived from the inversion of the phase velocity dataset of Ekstrom et<br />

al. (1997). The implications of different regularization constraints (mathematically equivalent to norm<br />

damping or smoothing with different criteria) are analyzed and compared. Both in group velocity maps<br />

and in shear velocity resulting model we find confirmation of the larger-scale deep geological features<br />

known for the region, namely the differentiation between fast old cratonic shields of Eastern Europe and<br />

North Western Africa and the slow seismic active Tethyan belt. At shorter scale length we image well<br />

slow anomalies associated with the magmatic provinces of the Sicily Channel, and the extensional zone<br />

of the Rhine graben. Fast anomalies are instead related to the Aegean and Hellenic Arc. Use of the<br />

dense European seismograph array results in maps with higher resolution than previously attained.<br />

Keywords: surface waves, tomography

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