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D. Gordienko, Y. Kopnichev, I. Sokolova (2006)
Spatiotemporal variations of short-period S-wave attenuation field in source zones of large and great earthquakesDoklady Earth Sciences, 408
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ISSN 1028-334X, Doklady Earth Sciences, 2008, Vol. 423, No. 8, pp. 1257â1261. © Pleiades Publishing, Ltd., 2008. Original Russian Text © Yu.F. Kopnichev, I.N. Sokolova, 2008, published in Doklady Akademii Nauk, 2008, Vol. 422, No. 5, pp. 672â676. GEOPHYSICS Yu. F. Kopnicheva and I. N. Sokolovab Presented by Academician V.N. Strakhov March 17, 2008 Received March 18, 2008 DOI: 10.1134/S1028334X08080163 Characteristics of the seismicity and absorption ï¬eld of short-period transversal waves are studied in the source region of the Sumatra earthquake of December 26, 2004 (Mw = 9.0). A ring structure was distinguished west of Sumatra Island, which was formed by the epicenters of shallow earthquakes with M ⥠5.5 that occurred in the period from January 1, 1969, to December 25, 2004, in the region between 1° and 7° N. The majority of relatively strong (M ⥠5.5) deep aftershocks of the Sumatra earthquake was conï¬ned to the boundaries of this structure. Mapping of the absorption ï¬eld in the source zone and nearby vicinities was made on the basis of records at the PSI station at epicentral distances ~250â700 km. We used the method based on the analysis of the attenuation rate of the early coda Sn
Doklady Earth Sciences – Springer Journals
Published: Nov 1, 2008
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