2004
DOI: 10.1023/b:jose.0000038449.78801.05
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Defining a model of 3D seismogenic sources for Seismic Hazard Assessment applications: The case of central Apennines (Italy)

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Cited by 264 publications
(239 citation statements)
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“…This earthquake has activated one of the fault segments of the L'Aquila fault that bounds the northern part of the Aterno valley in Paganica . Boncio et al (2004) estimated a maximum expected earthquake magnitude of 6.1-6.4 for this segment in Paganica (named it Aquilano fault), which is similar to the mainshock event. Herein, it has to be noted that other fault segments of the same fault system (such as the Mt.…”
Section: Discussionmentioning
confidence: 90%
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“…This earthquake has activated one of the fault segments of the L'Aquila fault that bounds the northern part of the Aterno valley in Paganica . Boncio et al (2004) estimated a maximum expected earthquake magnitude of 6.1-6.4 for this segment in Paganica (named it Aquilano fault), which is similar to the mainshock event. Herein, it has to be noted that other fault segments of the same fault system (such as the Mt.…”
Section: Discussionmentioning
confidence: 90%
“…Romeo and Pugliese (2000) using a Poissonian approach estimated a high probability for a peak ground acceleration of 0.25 g in a 50 year period and estimated a very high time-dependent probability of 23.6% in the next 30 years of a M s > 6.3 in L'Aquila. Boncio et al (2004) assessed a maximum expected magnitude between 6.1 and 6.4 for the L'Aquilano fault that bounds the Aterno basin. Moreover, Pace et al (2006) based on time dependent probabilities and a BPT distribution estimated for the year 2004 about 10% the probability for the next 50 years of rupturing of the Paganica segment that neighbours the town of L'Aquila and estimated a high probability of a peak acceleration exceeding 0.30 g in a 50 year period.…”
Section: Historical Record and Seismic Hazard Of L'aquilamentioning
confidence: 99%
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“…The fault system bounding the eastern flank of the Middle Aterno Valley was roughly depicted, or even completely missing, in several of the pre 2009 L'Aquila earthquake maps (Bagnaia, D'Epifanio, & Sylos Labini, 1992;Bertini & Bosi, 1993;Boncio, Lavecchia, & Pace, 2004;ISPRA, 2009;Vezzani & Ghisetti, 1998). Therefore, the fault system was ignored by the researchers dealing with active tectonics.…”
Section: Introductionmentioning
confidence: 99%
“…Seismic hazard maps based on geological fault slip-rate data show that strong events (intensities ~IX) can hit L'Aquila with short recurrence time of approximately 250±50 years (Roberts et al, 2004). Boncio et al (2004) estimated a maximum expected earthquake magnitude of 6.1-6.4 for the L'Aquila fault segment in Paganica, and stronger events are expected for other segments of the same fault system or other neighboring faults for their impressive post-glacial fault scarps (Papanikolaou et al, 2010 and references therein). Based on trenching investigations, Galli et al (2002) support that the Campo Imperatore fault, only 20 km away from L'Aquila, can give a Magnitude 7.0 earthquake.…”
Section: Introductionmentioning
confidence: 99%