Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1452
AuthorsTosi, P. 
TitleSeismogenic structure behaviour revealed by spatial clustering of seismicity in the Umbria-Marche Region (Central Italy)
Issue DateJun-1998
Series/Report no.41/2
URIhttp://hdl.handle.net/2122/1452
Keywordsseismogenic structure
fractal dimension
spatial clustering
foreshock
Central Italy
Subject Classification04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics 
AbstractTime variations in the spatial distribution of earthquake epicentres are analyzed by application of the fractal correlation dimension method. The zone under investigation is located in Central Italy, bounded in longitude by 12.0 and 14.4 degrees east and in latitude by 42.0 and 43.6 degrees north. From 1st January 1978 to 5th October 1997, 2028 events with a magnitude above Ml= 2.5 constitute the database.Evolution of the spatial fractal dimension Ds permits the identification of seismic cycles that are connected to the occurrence of main earthquakes.In particular, it is possible to recognize a division within each cycle, between a period of random background seismicity and a spatial clustering of events where shocks of magnitude Ml ┬│occur. Moreover, the decrease in Ds prior to such events, evidences a structural relationship between foreshocks and the occurrence of a main shock, even if not in close territorial proximity.This feature indicates a new, more extensive definition of seismogenic structure which can includes several interconnected structures within a large area.
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Annals of Geophysics
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