Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1620
Authors: Patanè, G.* 
Centamore, C.* 
La Delfa, S.* 
Title: Isochronal maps at Mt. Etna volcano (Italy): a simple and reliable tool for investigating large-scale heterogeneities
Issue Date: Oct-1997
Series/Report no.: 40/5
URI: http://hdl.handle.net/2122/1620
Keywords: Mt. Etna
isochronal curves
Subject Classification04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology 
Abstract: This paper analyses twelve etnean earthquakes which occurred at various depths and recorded at least by eleven stations. The seismic stations span a wide part of the volcanic edifice; therefore each set of direct P-wave arrival times at these stations can be considered appropriate for tracing isochronal curves. Using this simple methodology and the results obtained by previous studies the authors make a reconstruction of the geometry of the bodies inside the crust beneath Mt. Etna. These bodies are interpreted as a set of cooled magmatic masses, delimited by low-velocity discontinuities which can be considered, at present, the major feeding systems of the volcano.
Appears in Collections:Annals of Geophysics

Files in This Item:
File Description SizeFormat 
36 patane.pdf2.8 MBAdobe PDFView/Open
Show full item record

Page view(s)

73
Last Week
0
Last month
0
checked on Aug 14, 2018

Download(s)

63
checked on Aug 14, 2018

Google ScholarTM

Check