Source parameters and seismic moment-magnitude scaling for Northwestern Turkey
Language
English
Obiettivo Specifico
3.3. Geodinamica e struttura dell'interno della Terra
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Issue/vol(year)
2/97 (2007)
Publisher
Seismological Society of America
Pages (printed)
655-660
Date Issued
2007
Subjects
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.
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.
Type
article
File(s)![Thumbnail Image]()
![Thumbnail Image]()
Loading...
Name
Parolai_et_al_BSSA.pdf
Size
315.79 KB
Format
Adobe PDF
Checksum (MD5)
50340b40790ac94d40b1a5e7aff65e71
Loading...
Name
Parolai_et_al_BSSA_accepted.pdf
Size
323.59 KB
Format
Adobe PDF
Checksum (MD5)
161007d34e0b1001836da9215c6d1a11
