Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2936
AuthorsBraun, T.* 
Cesca, S.* 
Piccinini, D.* 
Spinelli, E.* 
Fiordelisi, A.* 
TitleOrigin of Micro-Earthquakes in Geothermal Areas (OMEGA): Source inversion of seismic events recorded in the Larderello geothermal area
Issue DateNov-2006
URIhttp://hdl.handle.net/2122/2936
Keywordssource inversion
geothermal area
Larderello
Subject Classification04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics 
AbstractThe Larderello geothermal area is located in the northern part of a volcanic zone that extends along the Italian Tyrrhenian coast. Geophysical investigations in this area suggest a crustal thinning and intrusion of hot mantle material into the crust. The local seismicity, monitored since 1978 by a network of 26 shortperiod almost vertical seismic stations, is characterized by a several hundred of M ≤ 1.5 events per year, never exceeding M=3.2 in the past 25 years.
Appears in Collections:Conference materials

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