Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Bulletin of the Seismological Society of America Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Bulletin of the Seismological Society of America; June 2006; v. 96; no. 3; p. 968-983; DOI: 10.1785/0120050071
© 2006 Seismological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Tusa, G.
Right arrow Articles by Gresta, S.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Source Parameters of Microearthquakes in Southeastern Sicily, Italy

Giuseppina Tusa1, Alfonso Brancato2 and Stefano Gresta1

1 Dipartimento di Scienze Geologiche
Università di Catania
Corso Italia 57
95129 Catania, Italy
gtusa{at}unict.it
gresta{at}unict.it
 (G.T., S.G.)
2 Dipartimento di Scienze della Terra
Università di Napoli
Largo San Marcellino 10
80138 Napoli, Italy
abranca{at}unict.it
 (A.B.)

We computed the source parameters of 135 local earthquakes that occurred in southeastern Sicily (Italy) between 1994 and 2001. Magnitudes ranged from 0.6 to 2.5. The source parameters were determined from the spectral analysis of P waves, after corrections for attenuation and site effects. P-wave quality (Qp) and site (S) factors are known in the two frequency ranges 3–9 Hz and 16–27 Hz (Giampiccolo et al., 2003). Because the correction for Qp and S over the whole spectrum could not be performed, a new approach to estimate spectral parameters was applied. We defined the new notion of "holed spectrum" to specify a spectrum lacking corrected spectral amplitude values within a certain frequency range, whereas we referred to a "whole spectrum" to specify when the entire analyzed frequency band was used. A detailed statistical analysis showed that dealing with the holed spectrum did not lead to significant differences in the estimate of spectral parameters. Displacement holed spectra, corrected by the attenuation and site response, were then used to estimate source parameters. Seismic moments ranged from 1017 to 1020 dyne cm, and source dimensions from 150 to 500 m. In general, the stress-drop values obtained analyzing P-wave spectra were very low, because they mainly span the range of 0.05–5 bars.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
A. Brancato, J. A. Hole, S. Gresta, and J. N. Beale
Determination of Seismogenic Structures in Southeastern Sicily (Italy) by High-Precision Relative Relocation of Microearthquakes
Bulletin of the Seismological Society of America, June 1, 2009; 99(3): 1921 - 1936.
[Abstract] [Full Text] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
G. Tusa and S. Gresta
Frequency-Dependent Attenuation of P Waves and Estimation of Earthquake Source Parameters in Southeastern Sicily, Italy
Bulletin of the Seismological Society of America, December 1, 2008; 98(6): 2772 - 2794.
[Abstract] [Full Text] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
E. Giampiccolo, S. D'Amico, D. Patane, and S. Gresta
Attenuation and Source Parameters of Shallow Microearthquakes at Mt. Etna Volcano, Italy
Bulletin of the Seismological Society of America, February 1, 2007; 97(1B): 184 - 197.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Seismological Society of America