z-logo
Premium
Coseismic and postseismic displacements related with the 1997 Earthquake Sequence in Umbria‐Marche (Central Italy)
Author(s) -
Basili Roberto,
Meghraoui Mustapha
Publication year - 2001
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2000gl012102
Subject(s) - geology , seismology , geodesy , slip (aerodynamics) , fault (geology) , displacement (psychology) , aqueduct , deformation (meteorology) , surface rupture , vertical displacement , geomorphology , psychology , history , oceanography , physics , archaeology , psychotherapist , thermodynamics
We study the coseismic and postseismic displacements related with the 1997 Umbria‐Marche earthquake sequence by means of leveling lines along a deformed aqueduct located in the epicentral area. Comparing the 1960 and 10/1997 measurements we obtain 0.49±0.10 m of coseismic displacement distributed along 3 km across the normal fault zone. Modeling of the coseismic surface dislocation is obtained from a combination of low angle (38°) faults at depth and high angle (80°) upper fault branches. The best fit model indicates that the upper branches stop at 0.4 km below the ground surface and have 60% of slip with respect to the lower faults. The postseismic displacement measured during 1998 is 0.18 m and represents 36% of the apparent coseismic deformation. Moderate earthquakes in the Apennines and related surface deformation may thus result from curved faults that reflect the brittle‐elastic properties of the uppermost crustal structures.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here