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  5. The 2012 Emilia earthquake sequence: an attempt of historical reading
 
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The 2012 Emilia earthquake sequence: an attempt of historical reading

Author(s)
Graziani, L.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Bernardini, F.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia  
Castellano, C.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Del Mese, S.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Ercolani, E.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia  
Rossi, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Tertulliani, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Vecchi, M.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Language
English
Obiettivo Specifico
3T. Pericolosità sismica e contributo alla definizione del rischio
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Journal of Seismology  
Issue/vol(year)
/19 (2015)
ISSN
1383-4649
Electronic ISSN
1573-157X
Publisher
Springer Science+Business Media B.V.
Pages (printed)
371-387
Date Issued
2015
DOI
10.1007/s10950-014-9471-y
URI
https://www.earth-prints.org/handle/2122/9283
Subjects
04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology  
Subjects

mcs scale

EMS98

Emilia 2012

historical seismology...

Abstract
In May-June 2012 the Po Valley (Northern Italy) was struck by an earthquake sequence whose strongest event occurred on 20 May (Mw 5.9). The intensity values (Imax 7-8 EMS98) assessed through macroseismic field surveys seemed inappropriate to describe the whole range of effects observed, especially those to monumental heritage, that suffered very heavy damage and destruction. The observed intensities in fact were significantly lower than those we could have expected after a Mw 5.9 event for Italy. As magnitude-intensity regressions are mainly based on historical earthquakes data, we handle this issue going back in time and debating the following hypotheses:
a) the 2012 Emilia earthquake sequence shows lower intensity values than expected because the affected urban context is more heterogeneous and much less vulnerable than in the past;
b) some historical earthquakes, especially those that occurred centuries ago and are provided with little information, could show a tendency to be overestimated in intensity, and consequently in magnitude.
In order to give consistency to such hypotheses we have introduced, as a test, a dual historical reading of the 2012 Emilia earthquake sequence as if it had occurred in the past: the first reading refers to a period prior to the introduction of concrete in buildings assessing the intensity on traditional masonry buildings only. A further historical reading, assessed by using information on monumental buildings only, was performed and it can be roughly referred to the XVI-XVII centuries. In both cases intensity values tend to grow significantly. The results could have a relevant impact when considered for seismic hazard assessments if confirmed on a large scale.
Type
article
File(s)
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manuscript_final.docx

Description
revised version
Size

90.89 KB

Format

Microsoft Word

Checksum (MD5)

da385494a6d4db41d704190950ab6b1d

rome library|catania library|milano library|napoli library|pisa library|palermo library
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