Το μέγεθος υπολογίστηκε M=7.4 με βάση τη σχέση του Hara T., 2007

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Slip model by Agalos A. email: aagalos@geol.uoa.gr

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References

Agalos A., Papadimitriou P., Makropoulos K., 2008. Rupture Histories of Strong Earthquakes. 31st General
Assembly of the European Seismological Commission, held at the Creta Maris
Conference Center, Hersonissos, Crete Greece, Book of Short papers, p 9-16.

Bassin, C., Laske, G. and Masters, G., 2000. The Current Limits of Resolution for Surface Wave Tomography
in North America, EOS Trans AGU, 81, F897.

Bouchon Michel, (1981). A simple method to calculate Green's functions for elastic layered media. BSSA, 71, 4, 959-971.

Hara, T., Measurement of duration of high-frequency energy radiation and its application to determination of
magnitudes of large shallow earthquakes, Earth Planets Space, 59, 227-231, 2007a.

Hara, T., Magnitude determination using duration of high frequency energy radiation and displacement amplitude:
application to tsunami earthquakes, Earth Planets Space, 59, 561-565, 2007b.

Harris, R., A., and Simpson R., W., (2002). The 1999 MW 7.1 Hector Mine, California Earthquake - A test of the stress
shadow hypothesis? BSSA, 92, 4, 1497-1512.

Hartzell S. H., and Heaton T. H., 1983. Inversion of strong ground motion and teleseismic waveform
data for the fault rupture history of the 1979 Imperial Valley, California, earthquake. BSSA, 73, 1553_1583.

Moshou A., Papadimitriou P., Makropoulos K., 2008. Waveform Inversion using Teleseismic and
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Seismological Commission, held at the Creta Maris Conference Center, Hersonissos, Crete Greece,
Book of abstracts, p 95.

Wessel, P. and W. H. F. Smith., 1991. Free software helps map and display data, EOS Trans. AGU, 72, 441.