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- W1994688617 abstract "Abstract An analysis of P n -wave time residuals for the seismic stations aligned along a profile crossing Northern Apennines Ligurian Belt, Western Alps and Provence has been carried out. The waves generated by the Friuli seismic sequence have been used as input data. The data, statistically treated have shown strong variations along the profile with negative residuals (high velocity in the crust) for some Alpine stations and positive residuals in the Northern Apennines. On the basis of these data a velocity model, tested with the ray-tracing technique, is proposed. From some delayed arrivals of P n phase, very clearly observed in the Ligurian region the presence of a layer characterized by a velocity of 7.6 km/s at a depth of 25 km overlying a Moho discontinuity at 40 km has been proposed." @default.
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- W1994688617 date "1985-09-01" @default.
- W1994688617 modified "2023-09-25" @default.
- W1994688617 title "Crustalinhomogeneities in northwestern Italy as inferred by Pn-wave time residuals" @default.
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- W1994688617 doi "https://doi.org/10.1016/0040-1951(85)90164-7" @default.
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