Crustal Structure and Moho Geometry beneath the Northern Apennines (Italy)

Physics

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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.

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