http://www.cnr.it/ontology/cnr/individuo/prodotto/ID306681
Statistical tools in the analysis of macroseismic fields for probability modelling of the attenuation analysis of macroseismic (Contributo in atti di convegno)
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- Statistical tools in the analysis of macroseismic fields for probability modelling of the attenuation analysis of macroseismic (Contributo in atti di convegno) (literal)
- Anno
- 2013-01-01T00:00:00+01:00 (literal)
- Alternative label
Rotondi R. (2013)
Statistical tools in the analysis of macroseismic fields for probability modelling of the attenuation analysis of macroseismic
in 4th General Meeting UPStrat-MAFA ``Disaster Prevention Strategies Using MAcroseismic Fields and FAult Sources'' EU Project, Catania, December 11-14, 2013
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- This study is co-financed by the EU-Civil Protection Financial Instrument, in the framework of the European project \"Urban disaster
Prevention Strategies using MAcroseismic Fields and FAult Sources\" (UPStrat-MAFA - Num.230301/2011/613486/SUB/A5), DG ECHO Unit A5. (literal)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
- 4th General Meeting UPStrat-MAFA Urban Disaster Prevention Strategies Using Macroseismic Fields and FAult Sources, Catania 11-14 December 2013 (literal)
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- CNR - IMATI sezione di Milano (literal)
- Titolo
- Statistical tools in the analysis of macroseismic fields for probability modelling of the attenuation analysis of macroseismic (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#curatoriVolume
- Susanna Falsaperla, Horst Langer, Salvatore Mangiagli, Luciano Scarfì (literal)
- Abstract
- Information content of a macroseismic field is generally summarized by tracing the isoseismals. A simple
examination of a series of fields on the basis of these curves fully proves the complexity of the problem to
identify a global pattern among the trends of decay of the macroseismic intensity shown by the various
earthquakes. This investigation raises some questions on: 1) the dependence of the decay pattern on the
epicentral intensity; 2) the existence of a specific shape for the isoseismals in a seismogenic zone; 3) the way
in which the velocity of the decay changes as a function of the epicentre-site distance; 4) the possible
correlation among shape of the isoseismals and some tectonic features; 5) how to quantify and include into
the model the various sources of uncertainty inherent in the phenomenon. (literal)
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