A fractal approach to the temporal distribution of microseismicity at the low eastern flank of Mt. Etna during 1989-1994

Details A fractal approach to the temporal distribution of microseismicity at the low eastern flank of Mt. Etna during 1989-1994 A fractal approach to the temporal distribution of microseismicity at the low eastern flank of Mt. Etna during 1989-1994

Dec 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998pepi..109..115l&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 109, Issue 3-4, p. 115-127.

Physics

2

Scientific paper

Seismicity affecting the low eastern flank of Mt. Etna shows clustering in time. We analysed a catalog of microearthquakes recorded by the four stations of the Osservatorio Sismologico di Protezione Civile di Acireale during the period 1989-1994. In general a strong deviation from periodic and random distribution was found. The temporal clustering is scale invariant and a fractal dimension can be derived to characterize it. Fractal dimensions seem to be correlated to the beginning of two major eruptions.

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