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GEOPHYSICAL RESEARCH LETTERS,
VOL. 30, NO. 24,
8042,
doi:10.1029/2003GL018020,
2003
Sn attenuation in the Anatolian and Iranian plateau and surrounding regions
Rengin Gök
Kandilli Observatory and Earthquake Research Institute, Bogaziçi University, Istanbul, Turkey
Eric Sandvol
Department of Geological Sciences, University of Missouri, Columbia, Missouri, USA
Niyazi Türkelli
Kandilli Observatory and Earthquake Research Institute, Bogaziçi University, Istanbul, Turkey
Dogan Seber
Institute for the Study of the Continents, Cornell University, Ithaca, New York, USA
Muawia Barazangi
Institute for the Study of the Continents, Cornell University, Ithaca, New York, USA
Abstract
The propagation characteristics of the regional Sn shear waves have been mapped to provide insight into the lithospheric structure
of the Anatolian and Iranian plateau and the surrounding regions. Thousands of regional earthquakes within the distance range
of 2–15 degrees were recorded by broadband and short period stations located in Turkey and nearby regions, especially new
data recorded by 29 broadband stations in the Eastern Turkey Seismic Experiment network. The propagation efficiencies of Sn
were determined visually using their amplitude and frequency content. Attenuation maps were then tomographically constructed
using the observed propagation efficiencies. Our results confirm that Sn propagates efficiently in the uppermost mantle beneath
the Mediterranean Sea, the Black Sea, and the Caspian Sea and along the Zagros fold and thrust belt. Sn is not observed in
eastern Turkey, northwestern Iran, or central Anatolia. In contrast to previous available studies, this study considerably
improved the mapped location of the boundaries between the zones of efficient and attenuated Sn. Our results are best explained
by an absence of lithospheric mantle, or the presence of thin and hot lithospheric mantle beneath most of the Anatolian and
Iranian plateau.
Received 20
June
2003;
accepted 14
October
2003;
published 22
November
2003.
Index Terms: 7218 Seismology: Lithosphere and upper mantle; 7299 Seismology: General or miscellaneous; 8102 Tectonophysics: Continental contractional orogenic belts; 8120 Tectonophysics: Dynamics of lithosphere and mantle—general.
Read Full Article (file size: 362093 bytes) Cited by
Citation: Gök, R., E. Sandvol, N. Türkelli, D. Seber, and M. Barazangi
(2003),
Sn attenuation in the Anatolian and Iranian plateau and surrounding regions,
Geophys. Res. Lett.,
30(24),
8042,
doi:10.1029/2003GL018020.
Copyright 2003 by the American Geophysical Union.
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