Physics
Scientific paper
Oct 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002georl..29t..60p&link_type=abstract
Geophysical Research Letters, Volume 29, Issue 20, pp. 60-1, CiteID 1999, DOI 10.1029/2002GL015109
Physics
14
Seismology: Lithosphere And Upper Mantle, Seismology: Continental Crust (1242), Seismology: Body Wave Propagation, Tectonophysics: Continental Tectonics-General (0905), Tectonophysics: Dynamics Of Lithosphere And Mantle-General
Scientific paper
We used receiver functions (RFs) from broad-band seismic stations to investigate the crustal structure of the Northern Apennines, Italy. Additionally, we use data obtained in this study to provide initial constraints for a map of the Moho depth of Italy. Ten stations were deployed along a transect [N75°E] during the 1994 GeoModAp project. RF analysis shows the presence of lateral variations in the crust. We observed patterns of symmetric and anti-symmetric converted phases from radial and tangential RFs vs. back-azimuth. These patterns can be explained by the presence of dipping interfaces and/or anisotropy within the crust. We then inverted RFs following the inversion scheme proposed by Sambridge [1999]. The results show the presence of S-velocity inversions in the lower crust beneath the Apennines, the upwelling of Moho in the Tyrrhenian area and its progressive deepening from the Tyrrhenian Sea toward the Adriatic coast.
Di Bona M.
Lucente Francesco Pio
Piana Agostinetti Nicola
Selvaggi Giulio
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