Q of Mode 0S0
Item
Title (Dublin Core)
en-US
Q of Mode 0S0
Description (Dublin Core)
en-US
Estimates of Q of mode oSo as measured after the Chilean (1960) and Alaskan (1964) earthquakes showed large scatter. The Indonesian quake of August 19, 1977, has provided a new opportunity to determine the attenuation factor for oSo. Time lapse spectra of a priori selected high quality data were analyzed using a maximum-likelihood method and Ricean statistics. Data from South Pole and Los Angeles gave Q values of 6324 (1 ±21 %) and 6859 (1 ± 17%) respectively. Taken together the result is 6687 (1 ± 13%).
ARK: https://n2t.net/ark:/88439/y084078
Permalink: https://geophysicsjournal.com/article/39
ARK: https://n2t.net/ark:/88439/y084078
Permalink: https://geophysicsjournal.com/article/39
Creator (Dublin Core)
Knopoff, L.
Rydelek, P.A.
Zurn, W.
Yogi, T.
Subject (Dublin Core)
en-US
Q-0S0-Time lapse spectra
en-US
Maximum Likelihood Method
en-US
Ricean statistics
en-US
Solid Earth
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1979-04-26
Type (Dublin Core)
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US
Peer-reviewed Article
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/39
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 46 No 1 (1979): Journal of Geophysics; 89-95
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/39/21