Open AccessBody‐wave spectral structure of 14 earthquakes with m b ≥ 6.0 determined from long‐period records of WWSSN stations for 1964–74
Author(s) -
Zamani A.,
Murrell S. A. F.
Publication year - 1978
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1978.tb04231.x
Subject(s) - seismology , geology , amplitude , period (music) , displacement (psychology) , spectral line , noise (video) , geodesy , physics , acoustics , psychology , optics , astronomy , artificial intelligence , computer science , image (mathematics) , psychotherapist
Summary. The far‐field displacement amplitude spectra of 14 earthquakes from Iran, Fiji Islands, Tonga—Kermadec Islands, and South America were obtained using the long‐period P and 5‐wave records of the WWSSN stations. Despite recent improvements in theories of the seismic‐source mechanism there is continuing doubt concerning the interpretation of the observed seismic spectrum. Although the dislocation model has been adopted by many investigators, and in particular Brune's model is widely used, there has often not been satisfactory evidence in the observed spectral data to justify this. Generally speaking, however, the spectral structures obtained in the present work have a form closely similar to those calculated by Brune and Savage, and it is shown that anomalies in the observed amplitude spectral structure are most likely due to noise and propagation effects.