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Seismicity at the border between Central and Southern Apennines (Italy): Re-evaluation of the early 1984 instrumental earthquake
Language
English
Obiettivo Specifico
3.1. Fisica dei terremoti
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Title of the book
Issue/vol(year)
1-4/ 499(2011)
Publisher
Elsevier
Pages (printed)
92-104
Issued date
January 2011
Alternative Location
Abstract
We re-evaluate the 1984 Abruzzo-Lazio Earthquake on the basis of original seismological data discussed in
light of previous interpretations from other authors. This sequence, characterized by two distinct mainshocks
(Ms=5.8 and Ms=5.2; NEIS) having low spatial and temporal separation, developed at the border between
Central and Southern Apennines. The sequence originated in a narrow area, adjacent to the main NW–SE
structures belonging to the Apenninic Chain, crossed by fault segments with different orientation. The spatiotemporal
evolution of the seismicity, the focal mechanisms of some aftershocks, never obtained before, and
waveform analysis suggest that the sequence developed in several stages. The beginning of the two main
stages was marked by two events (Ms=5.8 and Ms=5.2), and the entire sequence was strongly controlled
by the structural heterogeneity in the medium involved in the stress release process. The ruptures nucleated
on a ENE–WSW striking fault segment belonging to the NNE-striking Ortona-Roccamonfina tectonic line and
propagated towards ENE. The presence of the NW–SE structures belonging to the Apennine Chain and their
geometry acted as a barrier to the spread of the aftershocks northeastward. As a consequence, a local
concentration of static stress in the area enclosed between the northern edge of the rupture segment of the
first mainshock and the NW-striking structures triggered the Ms=5.2 event on a W–E pre-existing fault
segment. In turn, the static stress changes due to the second mainshock activated adjacent NE–SW and NW–
SE fault segments. The NW-striking structures belonging to the Apennines acted as a structural barrier, halting
the propagation of the ruptures nucleating on a fault segment that belongs to the NNE-striking Ortona-
Roccamonfina tectonic line.
light of previous interpretations from other authors. This sequence, characterized by two distinct mainshocks
(Ms=5.8 and Ms=5.2; NEIS) having low spatial and temporal separation, developed at the border between
Central and Southern Apennines. The sequence originated in a narrow area, adjacent to the main NW–SE
structures belonging to the Apenninic Chain, crossed by fault segments with different orientation. The spatiotemporal
evolution of the seismicity, the focal mechanisms of some aftershocks, never obtained before, and
waveform analysis suggest that the sequence developed in several stages. The beginning of the two main
stages was marked by two events (Ms=5.8 and Ms=5.2), and the entire sequence was strongly controlled
by the structural heterogeneity in the medium involved in the stress release process. The ruptures nucleated
on a ENE–WSW striking fault segment belonging to the NNE-striking Ortona-Roccamonfina tectonic line and
propagated towards ENE. The presence of the NW–SE structures belonging to the Apennine Chain and their
geometry acted as a barrier to the spread of the aftershocks northeastward. As a consequence, a local
concentration of static stress in the area enclosed between the northern edge of the rupture segment of the
first mainshock and the NW-striking structures triggered the Ms=5.2 event on a W–E pre-existing fault
segment. In turn, the static stress changes due to the second mainshock activated adjacent NE–SW and NW–
SE fault segments. The NW-striking structures belonging to the Apennines acted as a structural barrier, halting
the propagation of the ruptures nucleating on a fault segment that belongs to the NNE-striking Ortona-
Roccamonfina tectonic line.
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