The crustal structure from teleseismic P-wave coda. II. Application to data of the NARS array in western Europe and comparison with deep seismic sounding data.

Details The crustal structure from teleseismic P-wave coda. II. Application to data of the NARS array in western Europe and comparison with deep seismic sounding data. The crustal structure from teleseismic P-wave coda. II. Application to data of the NARS array in western Europe and comparison with deep seismic sounding data.

Jan 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993geoji.112...26v&link_type=abstract

Geophysical Journal International, Vol. 112, No. 1, p. 26 - 38

Physics

6

Scientific paper

The crustal structure beneath a seismic station has a large influence on
the P-wave coda recorded by that station. In this study the authors
employ the vertical and radial component of the crustal receiver
response to determine the most important features of the crustal
velocity structure beneath stations of the NARS array.

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