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New paleoseismological data from the Gran Sasso d'Italia area (central Apennines)

TitoloNew paleoseismological data from the Gran Sasso d'Italia area (central Apennines)
Tipo di pubblicazioneArticolo su Rivista peer-reviewed
Anno di Pubblicazione2002
AutoriGalli, P., Galadini F., Moro M., and Giraudi C.
RivistaGeophysical Research Letters
Volume29
Paginazione38-1 - 38-4
ISSN00948276
Parole chiaveactive fault, earthquake rupture, Earthquakes, fault slip, Geophysics, Italy, paleoseismicity, Paleoseismology, seismic hazard, Seismology, Surface faulting
Abstract

Paleoseismological analyses along the Campo Imperatore normal fault (CIF) in the Gran Sasso massif, which is an area characterized by the absence of significant historical earthquakes, highlight the occurrence of surface faulting after the 5th-3rd cent. BC and around the 6th-5th millenium BC. These ages agree with those reported by Giraudi and Frezzotti [1995] on the western tip of the CIF, thus suggesting the possible entire rupture of the 30-km-long CIF during M ∼ 7 events. These data contribute to the re-evaluation of the seismic hazard of a large surrounding area, including the city of L'Aquila (∼100,000 inhabitants), which is located 20 km from the CIF, in the hangingwall side.

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cited By 29

URLhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-0036555041&partnerID=40&md5=ed8593ead940e3115bf0ff32e2e42df6
Citation KeyGalli2002