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  5. Source parameters and seismic moment-magnitude scaling for Northwestern Turkey
 
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Source parameters and seismic moment-magnitude scaling for Northwestern Turkey

Author(s)
Parolai, S.  
GFZ, Potsdam, Germany  
Bindi, D.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italia  
Durukal, E.  
KOERI, Istanbul, Turkey  
Grosser, H.  
GFZ, Potsdam - Germany  
Milkereit, C.  
GFZ, Potsdam - Germany  
Language
English
Obiettivo Specifico
3.3. Geodinamica e struttura dell'interno della Terra
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Bulletin Seismological Society of America  
Issue/vol(year)
2/97 (2007)
Publisher
Seismological Society of America
Pages (printed)
655-660
Date Issued
2007
DOI
10.1785/0120060180
URI
https://www.earth-prints.org/handle/2122/3283
Subjects
04. Solid Earth::04.06. Seismology::04.06.04. Ground motion  
Subjects

Source parameters

Abstract
Abstract The source parameters of 523 aftershocks (0.5 ML 5.9) of the 1999
Kocaeli earthquake are determined by performing a two-step spectral fitting procedure.
The source spectrum, corrected for both site and propagation effects, is described
in terms of a standard x-square model multiplied by an exponential term of
frequency. The latter term is introduced to estimate the high-frequency (f 12 Hz)
fall-off of the acceleration source spectra by computing the j parameter. The seismic
moments obtained range between 1.05 1014 and 2.41 1017 N m, whereas the
Brune stress drops are between 0.002 and 40 MPa. The j value varies between 0.00
and 0.08 sec, indicating a decay of the acceleration level at the higher frequency
part of the spectrum greater than that assumed by the x 2 model. Both the stress
drop and the j parameter show the tendency of increasing with aftershock magnitude.
No evidence of self-similarity breakdown is observed between the source radius and
M0. Finally, both the seismic moment and the moment magnitude are compared with
the local magnitude to derive new moment–magnitude relationships for the area.
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