Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; June 2004; v. 94; no. 3; p. 1166-1171; DOI: 10.1785/0120020161
© 2004 Seismological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via ISI Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Gurbuz, C.
Right arrow Articles by Barazangi, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Short Note

Seismic Event Location Calibration Using the Eastern Turkey Broadband Seismic Network: Analysis of the Agri Dam Explosion

Cemil Gurbuz, Niyazi Turkelli, Tolga Bekler, Rengin Gok, Eric Sandvol, Dogan Seber and Muawia Barazangi

Bogazici University
Kandilli Observatory and Earthquake Research Institute
Istanbul, Turkey
gurbuz{at}boun.edu.tr
(C.G., N.T., T.B., R.G.)

University of Missouri
Department of Geological Sciences
Columbia, Missouri 65211
sandvole{at}missouri.edu
(E.S.)

Cornell University
Institute for the Study of the Continents
Ithaca, New York 14853
(D.S., M.B.)

A 12-ton controlled source explosion took place in eastern Turkey on 5 June 2001 and was recorded by 18 stations of the Eastern Turkey Seismic Experiment (ETSE) PASSCAL broadband network. This is a unique recording obtained for the first time in this region. Due to the blasting type and extremely high Lg and Sn attenuation in eastern Turkey, the blast is only observed out to a distance of about 300 km. We have used travel-time data from this explosion to obtain average crustal structure and site correction terms for the stations. The explosion was located using two new regional velocity models and the IASP91 velocity model to test the location capabilities of the ETSE network. We found that for surface focus events, the ETSE network is able to locate events to within 1–2 km of the true epicenter.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2004 by the Seismological Society of America.