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Titel Strong spurious phase in teleseismic correlations
VerfasserIn Lei Li, Michel Campillo, Pierre Boué, Christine Thomas, Philippe Roux, Nikolai Shapiro
Konferenz EGU General Assembly 2016
Medientyp Artikel
Sprache en
Digitales Dokument PDF
Erschienen In: GRA - Volume 18 (2016)
Datensatznummer 250136893
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2016-18036.pdf
 
Zusammenfassung
In the teleseismic correlations of continuous ambient noise data from Fnet array in Japan and Lapnet array in Finland, we observed a clear spurious phase with an apparent slowness of about 4.6 s/deg and an arrival time of about 430 s, far ahead of the P arrival at around 628 s. The spurious signal is rather strong from Fnet to Lapnet, arising from the correlating between the P wave from New Zealand arriving at Fnet and the PKP wave at Lapnet. The spurious phase in the opposite direction is weaker, with the source region locating in the low-latitude Atlantic Ocean near South America. Spurious phases near P and PcP waves are also present.