ABSTRACT: The Municipalities of Gatteo, Savignano and San Mauro Pascoli are located in the south-eastern pan of Emilia-Romagna Region. Seismic hazard of the area has been computed using the GNDT National Seismic Catalogue and the ONDT Seismotectonic Zonation. The seismicity can be considered moderate: in the past the zone has been stricken by several earthquakes (for ex¬ample in 1786, 1672, 1875 and 1916) with maximum Intensity around VIII MCS. As computed as¬suming interarrival times exponentially distributed and magnitude characterized by negative expo¬nentially distribution, seismic hazard is quite similar for the three Municipalities (with PGA per 474 years Return Period around 2S0 gals). The significant level of risk, particularly relevant in summertime, when the whole region becomes an overpopulated area because of tourism, urged the Emilia-Romagna Administration, in agreement with local Municipalities, to start a microzonation project. The analyzed area is situated along the coast of the Adriatic sea, and is nearly flat: from a geological point of view the sequence is continued by continental to marine deposits, laying in dis¬cordance on the last marine formations (Sabbie Gialle, lower and middle Pleistocene). It should be pointed out that the geotechnical parameters indicate very poor soils, with Nsn of clay formations less than 5, and of sandy formations less than 10. The presence of strata characterized by low Vs (less than 100 m/s) could induce severe non-linear behavior of soils under earthquake loading. In addition sandy beaches are (in some parts) susceptible of liquefaction. The output of the microzo-nation investigation consists on the evaluation of expected response spectra, identification of sus¬ceptible liquefaction areas and zones exposed to the possibility of non-linear behavior of soils. These results will be used for the preparation of the master plan of the Rubicone area (the master plan can be referred to as an intermunicipalities land-use planning).
Seismic microzonation of some Municipalities of the Rubicone area (Emilia-Romagna Region) / A. MARCELLINI;R. DAMINELLI; M. PAGANI; F. RIVA; T. CRESPELLANI; C. MADIAI; G. VANNUCCHI; G. FRASSINETI; L. MARTELLI; D. PALUMBO; G. VIEL. - STAMPA. - (1999), pp. 339-350. (Intervento presentato al convegno 11th European Conference on Earthquake Engineering tenutosi a Paris nel 6-11 September 1998).
Seismic microzonation of some Municipalities of the Rubicone area (Emilia-Romagna Region)
CRESPELLANI, TERESA;MADIAI, CLAUDIA;VANNUCCHI, GIOVANNI;
1999
Abstract
ABSTRACT: The Municipalities of Gatteo, Savignano and San Mauro Pascoli are located in the south-eastern pan of Emilia-Romagna Region. Seismic hazard of the area has been computed using the GNDT National Seismic Catalogue and the ONDT Seismotectonic Zonation. The seismicity can be considered moderate: in the past the zone has been stricken by several earthquakes (for ex¬ample in 1786, 1672, 1875 and 1916) with maximum Intensity around VIII MCS. As computed as¬suming interarrival times exponentially distributed and magnitude characterized by negative expo¬nentially distribution, seismic hazard is quite similar for the three Municipalities (with PGA per 474 years Return Period around 2S0 gals). The significant level of risk, particularly relevant in summertime, when the whole region becomes an overpopulated area because of tourism, urged the Emilia-Romagna Administration, in agreement with local Municipalities, to start a microzonation project. The analyzed area is situated along the coast of the Adriatic sea, and is nearly flat: from a geological point of view the sequence is continued by continental to marine deposits, laying in dis¬cordance on the last marine formations (Sabbie Gialle, lower and middle Pleistocene). It should be pointed out that the geotechnical parameters indicate very poor soils, with Nsn of clay formations less than 5, and of sandy formations less than 10. The presence of strata characterized by low Vs (less than 100 m/s) could induce severe non-linear behavior of soils under earthquake loading. In addition sandy beaches are (in some parts) susceptible of liquefaction. The output of the microzo-nation investigation consists on the evaluation of expected response spectra, identification of sus¬ceptible liquefaction areas and zones exposed to the possibility of non-linear behavior of soils. These results will be used for the preparation of the master plan of the Rubicone area (the master plan can be referred to as an intermunicipalities land-use planning).
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