Global finite-frequency S-wave delay-times: how much crust matters
نویسندگان
چکیده
منابع مشابه
Crust and upper mantle P- and S-wave delay times at Eurasian seismic stations
Median crust and upper mantle Pand S-wave delay times, based on residuals for teleseismic Pand S-wave arrival times included in the groomed ISC/NEIC database of Engdahl et al. [Bull. Seism. Soc. Am. 88 (1998) 722] are estimated as functions of time and azimuth for Eurasian seismic stations. The effects of source and lower mantle 3-D structure on the station residuals are corrected by ray tracin...
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ژورنال
عنوان ژورنال: Geophysical Journal International
سال: 2019
ISSN: 0956-540X,1365-246X
DOI: 10.1093/gji/ggz222