Lithospheric rheology in southern Italy inferred from postseismic viscoelastic relaxation following the 1980 Irpinia earthquake

Author:

Dalla Via G.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference35 articles.

1. Ground movements and faulting mechanism associated to the November 23, 1980 southern Italy earthquake;Arca;Boll. Geod. Sci. Affini,1983

2. Details of the rupture kinematics and mechanism of the 1980 Irpinia earthquake: New results and remaining questions;Bernard;Ann. Geofis.,1993

3. Time-dependent distributed afterslip on and deep below the Izmit earthquake rupture;Bürgmann;Bull. Seismol. Soc. Am.,2002

4. Avarage strain rate in the Italian crust inferred from a permanent GPS network- II. Strain rate versus seismicity and structural geology;Caporali;Geophys. J. Int.,2003

5. Occam's inversion: A pratical algorithm for generating smooth models from electromagnetic sounding data;Constable;Geophysics,1987

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