Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1838
AuthorsKiratzi, A. A. 
TitleActive seismic deformation in the Italian peninsula and Sicily
Issue DateApr-1994
Series/Report no.37/1
URIhttp://hdl.handle.net/2122/1838
KeywordsDeformation
seismicity
Italy
Sicily
Tyrrhenian Sea
Subject Classification04. Solid Earth::04.07. Tectonophysics::04.07.04. Plate boundaries, motion, and tectonics 
05. General::05.02. Data dissemination::05.02.02. Seismological data 
AbstractRecent and historical seismicity as well as reliable fault plane solutions are used in order to perform a moment tensor analysis and estimate the active crustal and sub-crustal deformation of the Italian peninsula and Sicily. The results show that in Northern Italy, along the Alps, the deformation is taken up by compression at N162°E and a rate of 1 mm/yr. The thickening of the seismogenic layer is taking place at a rate of 0.1 mm/yr. In Central Italy, along the Apennines, extension is prevailing at N28°E and a rate of 3 mm/yr which causes thinning of the seismogenic layer at a rate 0.5 mm/yr. In Southern Italy, at Calabria, the deformation is taken up as extension at N40°E and a rate of 11 mm/yr. At the island of Sicily, compression is occurring at N25°E and a rate of 1 mm/yr. These results are in agreement with plate motion models for the area. The analysis of the deep seismicity of the Tyrrhenian Sea showed that the descending slab is in a state of down dip compression at N146°E and a rate of 2 mm/yr.
Appears in Collections:Annals of Geophysics

Files in This Item:
File Description SizeFormat 
03 kiratzi.pdf5.01 MBAdobe PDFView/Open
Show full item record

Page view(s)

69
checked on Apr 29, 2017

Download(s)

99
checked on Apr 29, 2017

Google ScholarTM

Check