Indexes and physical parameters for the litho-stratigraphic model of Venice

Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in t...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Boaga, Jacopo [verfasserIn] Iliceto, Vittorio Zezza, Fulvio

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2010

Schlagwörter:	Seismic parameters Shear waves Compressional waves Passive seismic surveys

Anmerkung:	© Springer-Verlag 2010

Übergeordnetes Werk:	Enthalten in: Rendiconti lincei - Heidelberg : Springer, 1990, 21(2010), Suppl 1 vom: 27. Juli, Seite 229-238
Übergeordnetes Werk:	volume:21 ; year:2010 ; number:Suppl 1 ; day:27 ; month:07 ; pages:229-238

Links:	Volltext

DOI / URN:	10.1007/s12210-010-0092-2

Katalog-ID:	SPR025366564

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allfields	10.1007/s12210-010-0092-2 doi (DE-627)SPR025366564 (SPR)s12210-010-0092-2-e DE-627 ger DE-627 rakwb eng Boaga, Jacopo verfasserin aut Indexes and physical parameters for the litho-stratigraphic model of Venice 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2010 Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. The measurements campaign furnished, moreover, indexes and physical parameters quantification for the litho-stratigraphic model of the Venetian subsoil. Seismic parameters (dpeaa)DE-He213 Shear waves (dpeaa)DE-He213 Compressional waves (dpeaa)DE-He213 Passive seismic surveys (dpeaa)DE-He213 Iliceto, Vittorio aut Zezza, Fulvio aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 21(2010), Suppl 1 vom: 27. Juli, Seite 229-238 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:21 year:2010 number:Suppl 1 day:27 month:07 pages:229-238 https://dx.doi.org/10.1007/s12210-010-0092-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 21 2010 Suppl 1 27 07 229-238
spelling	10.1007/s12210-010-0092-2 doi (DE-627)SPR025366564 (SPR)s12210-010-0092-2-e DE-627 ger DE-627 rakwb eng Boaga, Jacopo verfasserin aut Indexes and physical parameters for the litho-stratigraphic model of Venice 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2010 Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. The measurements campaign furnished, moreover, indexes and physical parameters quantification for the litho-stratigraphic model of the Venetian subsoil. Seismic parameters (dpeaa)DE-He213 Shear waves (dpeaa)DE-He213 Compressional waves (dpeaa)DE-He213 Passive seismic surveys (dpeaa)DE-He213 Iliceto, Vittorio aut Zezza, Fulvio aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 21(2010), Suppl 1 vom: 27. Juli, Seite 229-238 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:21 year:2010 number:Suppl 1 day:27 month:07 pages:229-238 https://dx.doi.org/10.1007/s12210-010-0092-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 21 2010 Suppl 1 27 07 229-238
allfields_unstemmed	10.1007/s12210-010-0092-2 doi (DE-627)SPR025366564 (SPR)s12210-010-0092-2-e DE-627 ger DE-627 rakwb eng Boaga, Jacopo verfasserin aut Indexes and physical parameters for the litho-stratigraphic model of Venice 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2010 Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. The measurements campaign furnished, moreover, indexes and physical parameters quantification for the litho-stratigraphic model of the Venetian subsoil. Seismic parameters (dpeaa)DE-He213 Shear waves (dpeaa)DE-He213 Compressional waves (dpeaa)DE-He213 Passive seismic surveys (dpeaa)DE-He213 Iliceto, Vittorio aut Zezza, Fulvio aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 21(2010), Suppl 1 vom: 27. Juli, Seite 229-238 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:21 year:2010 number:Suppl 1 day:27 month:07 pages:229-238 https://dx.doi.org/10.1007/s12210-010-0092-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 21 2010 Suppl 1 27 07 229-238
allfieldsGer	10.1007/s12210-010-0092-2 doi (DE-627)SPR025366564 (SPR)s12210-010-0092-2-e DE-627 ger DE-627 rakwb eng Boaga, Jacopo verfasserin aut Indexes and physical parameters for the litho-stratigraphic model of Venice 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2010 Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. The measurements campaign furnished, moreover, indexes and physical parameters quantification for the litho-stratigraphic model of the Venetian subsoil. Seismic parameters (dpeaa)DE-He213 Shear waves (dpeaa)DE-He213 Compressional waves (dpeaa)DE-He213 Passive seismic surveys (dpeaa)DE-He213 Iliceto, Vittorio aut Zezza, Fulvio aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 21(2010), Suppl 1 vom: 27. Juli, Seite 229-238 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:21 year:2010 number:Suppl 1 day:27 month:07 pages:229-238 https://dx.doi.org/10.1007/s12210-010-0092-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 21 2010 Suppl 1 27 07 229-238
allfieldsSound	10.1007/s12210-010-0092-2 doi (DE-627)SPR025366564 (SPR)s12210-010-0092-2-e DE-627 ger DE-627 rakwb eng Boaga, Jacopo verfasserin aut Indexes and physical parameters for the litho-stratigraphic model of Venice 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2010 Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. The measurements campaign furnished, moreover, indexes and physical parameters quantification for the litho-stratigraphic model of the Venetian subsoil. Seismic parameters (dpeaa)DE-He213 Shear waves (dpeaa)DE-He213 Compressional waves (dpeaa)DE-He213 Passive seismic surveys (dpeaa)DE-He213 Iliceto, Vittorio aut Zezza, Fulvio aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 21(2010), Suppl 1 vom: 27. Juli, Seite 229-238 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:21 year:2010 number:Suppl 1 day:27 month:07 pages:229-238 https://dx.doi.org/10.1007/s12210-010-0092-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 21 2010 Suppl 1 27 07 229-238
language	English
source	Enthalten in Rendiconti lincei 21(2010), Suppl 1 vom: 27. Juli, Seite 229-238 volume:21 year:2010 number:Suppl 1 day:27 month:07 pages:229-238
sourceStr	Enthalten in Rendiconti lincei 21(2010), Suppl 1 vom: 27. Juli, Seite 229-238 volume:21 year:2010 number:Suppl 1 day:27 month:07 pages:229-238
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Seismic parameters Shear waves Compressional waves Passive seismic surveys
isfreeaccess_bool	false
container_title	Rendiconti lincei
authorswithroles_txt_mv	Boaga, Jacopo @@aut@@ Iliceto, Vittorio @@aut@@ Zezza, Fulvio @@aut@@
publishDateDaySort_date	2010-07-27T00:00:00Z
hierarchy_top_id	385615477
id	SPR025366564
language_de	englisch
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author	Boaga, Jacopo
spellingShingle	Boaga, Jacopo misc Seismic parameters misc Shear waves misc Compressional waves misc Passive seismic surveys Indexes and physical parameters for the litho-stratigraphic model of Venice
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topic_title	Indexes and physical parameters for the litho-stratigraphic model of Venice Seismic parameters (dpeaa)DE-He213 Shear waves (dpeaa)DE-He213 Compressional waves (dpeaa)DE-He213 Passive seismic surveys (dpeaa)DE-He213
topic	misc Seismic parameters misc Shear waves misc Compressional waves misc Passive seismic surveys
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title	Indexes and physical parameters for the litho-stratigraphic model of Venice
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title_full	Indexes and physical parameters for the litho-stratigraphic model of Venice
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author_browse	Boaga, Jacopo Iliceto, Vittorio Zezza, Fulvio
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title_sort	indexes and physical parameters for the litho-stratigraphic model of venice
title_auth	Indexes and physical parameters for the litho-stratigraphic model of Venice
abstract	Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. The measurements campaign furnished, moreover, indexes and physical parameters quantification for the litho-stratigraphic model of the Venetian subsoil. © Springer-Verlag 2010
abstractGer	Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. The measurements campaign furnished, moreover, indexes and physical parameters quantification for the litho-stratigraphic model of the Venetian subsoil. © Springer-Verlag 2010
abstract_unstemmed	Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. The measurements campaign furnished, moreover, indexes and physical parameters quantification for the litho-stratigraphic model of the Venetian subsoil. © Springer-Verlag 2010
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title_short	Indexes and physical parameters for the litho-stratigraphic model of Venice
url	https://dx.doi.org/10.1007/s12210-010-0092-2
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fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR025366564</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230403065948.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2010 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s12210-010-0092-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR025366564</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s12210-010-0092-2-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Boaga, Jacopo</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Indexes and physical parameters for the litho-stratigraphic model of Venice</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2010</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 2010</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract We performed passive and controlled source seismic surveys in the historical center of Venice to characterize subsoil layers, seismic indexes and physical parameters of subsoil. The adopted techniques allowed us to identify two main different seismic responses for the Venetian subsoil, in terms of both elastic earth parameters and seismic characteristics. In particular, the horizontal to vertical spectral ratio technique was applied, highlighting a substantial relevant heterogeneity. This is due to the presence of relatively strong acoustic impedance contrast in the shallow subsoil (8–10 m deep), detected only in some sites of historical city center. With the aid of a geological reconstruction, seismic surveys interpretation was able to highlight the presence of a particular alluvial complex, identified as a ‘multistorey sandbody’. 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Indexes and physical parameters for the litho-stratigraphic model of Venice

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