{"items":[{"link":[{"url":"http:\/\/www.jcheminf.com\/content\/3\/1\/47"}],"type":"article","year":"2011","title":"Open Bibliography for Science, Technology and Medicine","author":[{"name":"Richard Jones"},{"name":"Mark MacGillivray"},{"name":"Peter Murray-Rust"},{"name":"Jim Pitman"},{"name":"Peter Sefton"},{"name":"Ben O'Steen"},{"name":"William Waites"}],"journal":{"name":"Journal of Cheminformatics"},"identifier":[{"id":"10.1186\/1758-2946-3-47","type":"doi"}],"id":1},{"link":[{"url":"http:\/\/www.jcheminf.com\/content\/3\/1\/47"}],"type":"book","year":"2016","title":"Open Architecture","author":[{"name":"Richard Jones"},{"name":"Mark MacGillivray"},{"name":"William Waites"}],"journal":{"name":"Journal of Cheminformatics"},"identifier":[{"id":"10.1186\/1758-2946-3-47","type":"doi"}],"id":2},{"link":[{"url":"10.5281\/zenodo.2359019"}],"type":"","year":"2018","title":"Geological report at the seismic station IV. MODE- MODENA","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d"},"identifier":[{"id":"10.5281\/zenodo.2359019","type":"DOI"}],"id":1224},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/12983"}],"type":"article","year":"2019","title":"Geological report at the seismic station IV.BIOG \u2013 Ariano Irpino (AV) . ","author":[{"name":"Luigi ZARRILLI"},{"name":"Raffaele MOSCHILLO"},{"name":"Gaetano RICCIO"},{"name":"Stefania PUCILLO"},{"name":""},{"name":""}],"journal":{"name":"Earth-Prints"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12983","type":"ISRC"}],"id":1240},{"link":[{"url":""}],"type":"","year":"2013","title":"Studio sismologico per la caratterizzazione della risposta sismica di sito ai fini della microzonazione sismica di alcuni comuni della regione Emilia-Romagna. ","author":[{"name":"Laurenzano G."},{"name":"Priolo E."},{"name":"Barnaba C."},{"name":"Gallipoli M. R."},{"name":"Klin P."},{"name":"Martelli L., Mucciarelli M., Romanelli M."}],"journal":{"name":"Rel. OGS 2013\/74 Sez. CRS 26, dd. 31 luglio 2013."},"identifier":[{"id":"","type":""}],"id":1251},{"link":[{"url":" https:\/\/doi.org\/10.1144\/EGSP27.13"}],"type":"article","year":"2016","pages":"147--158","title":"Site classification map of Italy based on surface geology","author":"Di Capua G.,  Peppoloni S.,  Amanti M.,  Cipolloni C.,  Conte G.","number":"1","volume":"27","journal":"Geological Society, London, Engineering Geology Special Publications","publisher":"Geological Society of London","identifier":[{"id":" https:\/\/doi.org\/10.1144\/EGSP27.13","type":"ISRC"}],"unique_name":"di2016site","id":1264},{"link":[{"url":""}],"year":"","title":"prova 19\/07\/2021","author":[{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":""},"identifier":[{"id":"http:\/\/doi.org\/10.20.55","type":"DOI"}],"id":1253},{"link":[{"url":""}],"year":"2021","title":"non funziona il bottone ADD+ della Bliblio. ","author":[{"name":"rossi A."},{"name":"Alessia"},{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":""},"identifier":[{"id":"bla bla bla","type":""}],"id":1254},{"type":"article","year":"1997","pages":"710--730","title":"Site amplification in the San Fernando Valley, California: variability of site-effect estimation using the S-wave, coda, and H\/V methods","author":"Bonilla, Luis Fabian and Steidl, Jamison H and Lindley, Grant T and Tumarkin, Alexei G and Archuleta, Ralph J","number":"3","volume":"87","journal":"Bulletin of the Seismological Society of America","publisher":"The Seismological Society of America","unique_name":"bonilla1997site","id":1255},{"link":[{"url":""}],"year":"","title":"Site characterization report at the seismic station \u200b IV.TRTR\u2013 Tortoreto Teramo \u200b","author":[{"name":""},{"name":""},{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":""},"identifier":[{"id":"\u200b http:\/\/hdl.handle.net\/2122\/14051","type":"DOI"}],"id":1258},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/14054"}],"year":"2020","title":"Site characterization report at the seismic station IV.INTR \u2013 Introdacqua (AQ)","author":[{"name":"Geology: Pischiutta M."},{"name":"Minarelli L."},{"name":"Geophysics: Vassallo M."},{"name":"Di Giulio G."},{"name":"Mercuri A."},{"name":"Minarelli L."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/14054","type":"ISRC"}],"id":1260},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/14052"}],"year":"2020","title":"Site characterization report at the seismic station IV.LNSS -Leonessa (RI)","author":[{"name":"Geology: Minarelli L"},{"name":"Falcucci E"},{"name":"Geophysics: Di Giulio G"},{"name":"Vassallo M"},{"name":"Cultrera G"},{"name":"Mercuri A"}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/14052","type":"DOI"}],"id":1256},{"link":[{"url":""}],"year":"2017","title":"Final Report Development of a conceptual geological model for five seismic station  with accelerometer of the INGV Seismic Network","author":[{"name":"BONOMO R., D\u2019AMBROGI C., D\u2019OREFICE M."},{"name":"FIORENZA D., GAF\u00c0 R. M. MONTI G.M."},{"name":"Di MANNA M., ROMA M., VITA L."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Internal Report ISPRA-INGV"},"identifier":[{"id":"","type":""}],"id":1266},{"url":"http:\/\/hdl.handle.net\/2122\/12955","type":"misc","title":"Velocity profile report at the seismic station IV.BIOG \u2013 Camporeale-Ariano Irpino (AV)","author":"Stefania Pucillo and Rocco Cogliano and Gaetano Riccio and Antonio Fodarella and Gianpaolo Cecere and Antonino Memmolo and Fabrizio Cara","identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12955","type":"DOI"}],"unique_name":"2122_12955","id":1262},{"link":[{"url":"10.5281\/zenodo.2430497"}],"year":"2018","title":"Geological report at the seismic station IV.NRCA\u2013Norcia (PG)","author":[{"name":"Di Naccio D."},{"name":"Bordoni P."},{"name":"Famiani D."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d"},"identifier":[{"id":"10.5281\/zenodo.2430497","type":"DOI"}],"id":1281},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/14044"}],"year":"2020","title":"Site characterization report at the seismic station IV.NEVI \u2013 Neviano degli Arduini (PR)","author":[{"name":"Geology: Lovati S., Manganello P."},{"name":"Geophysics: Lovati S., Manganello P."},{"name":"Lorenzetti A."},{"name":"Puglia R."},{"name":"Massa M."},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/14044","type":"DOI"}],"id":1259},{"link":[{"url":"10.5281\/zenodo.1145726"}],"year":"2017","title":"Site characterization of the INGV station IV.OPPE OPPEANO","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Convenzione DPC-INGV 2017 Allegato B2, Obiettivo 1 - TASK B: Caratterizzazione siti accelerometrici\u201d, "},"identifier":[{"id":"10.5281\/zenodo.1145726","type":""}],"id":1282},{"link":[{"url":"10.5281\/zenodo.806779"}],"year":"2016","title":"Site characterization of the INGV station IV.ROM9 \u2013 ROMA (INGV garden)","author":[{"name":"Di Giulio G., Vassallo M."},{"name":"Bordoni P., Cultrera G.,"},{"name":"Milano G., Amoroso S."},{"name":"Famiani D., Cara F."},{"name":"Carlucci G., Attolico D."},{"name":""}],"journal":{"name":"Working group INGV of DPC-INGV 2016 agreement All. B2 Task B"},"identifier":[{"id":"10.5281\/zenodo.806779","type":""}],"id":1283},{"link":[{"url":"10.5281\/zenodo.2222307"}],"year":"2018","title":"Velocity profile report at the seismic station IV.CIMA-CIVITANOVA MARCHE","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":"Ladina C.,  Frapiccini M."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d, (2018)"},"identifier":[{"id":"10.5281\/zenodo.2222307","type":"ISRC"}],"id":1269},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/12967"}],"year":"2019","title":"Geological report at the seismic station IV.FERS \u2013 Casaglia, Ferrara","author":[{"name":"Minarelli L."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12967","type":""}],"id":1272},{"link":[{"url":"10.5281\/zenodo.2281845"}],"year":"2018","title":"Velocity profile report at the seismic stations IV.IOCA and IT.CML-Casamicciola Terme, Ischia","author":[{"name":"Vassallo M., Milana G."},{"name":"Di Giulio G., Bordoni P."},{"name":"Cogliano R., Fodarella A."},{"name":"Pucillo S., Riccio G."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d"},"identifier":[{"id":"10.5281\/zenodo.2281845","type":"ISRC"}],"id":1273},{"link":[{"url":"10.5281\/zenodo.2399252"}],"year":"2018","title":"Geological report at the seismic station IV.CIMA  - Civitanova Marche (MC).","author":[{"name":"Ladina C. "},{"name":"Famiani D."},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d, (2018). "},"identifier":[{"id":"10.5281\/zenodo.2399252","type":"DOI"}],"id":1268},{"doi":"10.5281\/zenodo.807785","url":"https:\/\/doi.org\/10.5281\/zenodo.807785","month":"jun, 2017","title":"Site characterization of the INGV seismic station IV.CDCA Citta di Castello. Working group INGV of DPC-INGV 2016 agreement All. B2 Task B","author":"Di Giulio G., M. Vassallo, P. Bordoni, G. Cultrera, D. Famiani, G. Milana, L. Cantore (INGV)","identifier":[{"id":"https:\/\/doi.org\/10.5281\/zenodo.807785","type":""}],"id":1267},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/12951"}],"year":"2019","title":"Velocity profile report at the seismic station IV.MILN\u2013 Milano","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12951","type":""}],"id":1276},{"link":[{"url":"10.5281\/zenodo.807793"}],"year":"2016","title":"Seismic characterization of accelerometric sites. Site characterization of the INGV station IV.CMPO \u2013 Campotto Po (Municipality Argenta, Ferrara)","author":[{"name":"Di Giulio G., Vassallo M."},{"name":"Bordoni P., Cultrera G."},{"name":"Milana G., Cantore L., Cogliano R."},{"name":"Fodarella A., Riccio G."}],"journal":{"name":"Working group INGV of DPC-INGV 2016 agreement All. B2 Task B"},"identifier":[{"id":"10.5281\/zenodo.807793","type":"DOI"}],"id":1270},{"link":[{"url":"10.5281\/zenodo.1145741"}],"year":"2017","title":"Site characterization of the INGV station IV.EUCT PAVIA","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":""}],"journal":{"name":"Working group INGV \"Convenzione DPC-INGV 2017 Allegato B2, Obiettivo 1 - TASK B: Caratterizzazione siti accelerometrici\u201d, "},"identifier":[{"id":"10.5281\/zenodo.1145741","type":"DOI"}],"id":1271},{"link":[{"url":"10.5281\/zenodo.2451187"}],"year":"2018","title":"Geological report at the seismic stations IV.IOCA and IT.CML-Casamicciola Terme (NA)","author":[{"name":"Famiani D. "},{"name":"Di Naccio D."},{"name":"Bordoni P."},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d"},"identifier":[{"id":"10.5281\/zenodo.2451187","type":"ISRC"}],"id":1274},{"link":[{"url":"10.5281\/zenodo.824019"}],"year":"2016","title":"Site characterization of station IV.LAV9 (LANUVIO) of Italian National Seismic Network","author":[{"name":"Cara F., Di Giulio G."},{"name":"Vassallo M., Milana G."},{"name":"Bordoni P., Cultrera G."},{"name":"Mercuri A."},{"name":"Famiani D."},{"name":"Carlucci G."}],"journal":{"name":"Working group INGV of DPC-INGV 2016 agreement All. B2 Task B"},"identifier":[{"id":"10.5281\/zenodo.824019","type":""}],"id":1275},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/12935"}],"year":"2019","title":"Geological report at the seismic station IV.MILN -Milano","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12935","type":"DOI"}],"id":1277},{"link":[{"url":"10.5281\/zenodo.1145734"}],"year":"2017","title":"Site characterization of the INGV station IV.MNTV MANTOVA.","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Convenzione DPC-INGV 2017 Allegato B2, Obiettivo 1 - TASK B: Caratterizzazione siti accelerometrici\u201d, "},"identifier":[{"id":"10.5281\/zenodo.1145734","type":""}],"id":1278},{"link":[{"url":"10.5281\/zenodo.2222319"}],"year":"2018","title":"Velocity profile report at the seismic station IV.MODE-MODENA","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d"},"identifier":[{"id":"10.5281\/zenodo.2222319","type":"DOI"}],"id":1279},{"link":[{"url":"10.5281\/zenodo.2358257"}],"year":"2018","title":"Velocity profile report at the seismic station IV.NRCA-NORCIA","author":[{"name":"Di Giulio G., Vassallo M."},{"name":"Milana G."},{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d"},"identifier":[{"id":"10.5281\/zenodo.2358257","type":"DOI"}],"id":1280},{"link":[{"url":"10.5281\/zenodo.803945"}],"year":"2016","title":"Site characterization of the INGV station IV.SANR \u2013SANDRIGO","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Santulin M."},{"name":"Massa M."},{"name":""},{"name":""}],"journal":{"name":"Working group INGV of DPC-INGV 2016 agreement All. B2 Task B"},"identifier":[{"id":"10.5281\/zenodo.803945","type":""}],"id":1284},{"link":[{"url":"10.5281\/zenodo.2399636"}],"year":"2018","title":"Geological report at the seismic station IV.SEF1 \u2013 SEFRO (MC)","author":[{"name":"Ladina C. "},{"name":"Famiani D. "},{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d"},"identifier":[{"id":"10.5281\/zenodo.2399636","type":""}],"id":1285},{"link":[{"url":"10.5281\/zenodo.2222327"}],"year":"2018","title":"Velocity profile report at the seismic station IV.SEF1-SEFRO","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":"Ladina C. "},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d, (2018)"},"identifier":[{"id":"10.5281\/zenodo.2222327","type":""}],"id":1286},{"link":[{"url":"https:\/\/www.researchgate.net\/publication\/265482961_Caratterizzazione_dinamica_dei_terreni_di_Senigallia_e_analisi_della_risposta_sismica_locale"}],"year":"2007","title":"Scenari di pericolosit\u00e0 sismica della fascia costiera marchigiana. La Microzonazione sismica di Senigallia","author":[{"name":"Mucciarelli M."},{"name":"Tiberi P."},{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":""},"identifier":[{"id":"","type":""}],"id":1287},{"link":[{"url":"10.5281\/zenodo.2399932"}],"year":"2018","title":"Geological report at the seismic station IV.SENI-Senigallia (AN)","author":[{"name":"Ladina C. "},{"name":"Famiani D. "},{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2018, Allegato B2, Obiettivo 1 - TASK B\u201d, (2018)"},"identifier":[{"id":"10.5281\/zenodo.2399932","type":""}],"id":1288},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/12959"}],"year":"2019","title":"Geological report at the seismic station IV.TERO \u2013 Teramo","author":[{"name":"Di Naccio D."},{"name":"Famiani D. "},{"name":"Minarelli L."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12959","type":""}],"id":1289},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/12948"}],"year":"2019","title":"Velocity profile report at the seismic station IV.TERO \u2013 TERAMO","author":[{"name":"Di Giulio G., Vassallo M."},{"name":"Cultrera G."},{"name":"Minarelli L."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12948","type":"DOI"}],"id":1290},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/14051"}],"year":"2020","title":"Site characterization report at the seismic station IV.TRTR\u2013 Tortoreto Teramo","author":[{"name":"Geology: Di Naccio D."},{"name":"Geophysics: Di Giulio G."},{"name":"Vassallo M."},{"name":"Minarelli L."},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/14051","type":"DOI"}],"id":1291},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/12909"}],"year":"2019","title":"Geological report at the seismic station IV.VOBA - Vobarno","author":[{"name":"Lovati C."},{"name":"Mascandola C."},{"name":"Massa M."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12909","type":""}],"id":1292},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/12907"}],"year":"2019","title":"Velocity profile report at the seismic station IV.VOBA\u2013 Vobarno","author":[{"name":"Mascandola C."},{"name":"Lovati S."},{"name":"Massa M."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/12907","type":"DOI"}],"id":1293},{"doi":"10.1111\/j.1365-246X.2009.04451.x","url":"https:\/\/doi.org\/10.1111\/j.1365-246X.2009.04451.x","issn":"0956-540X","type":"article","year":"2010","month":"02","pages":"820-828","title":"Ambient vibration analysis of an unstable mountain slope","author":"Burj\u00e1nek, Jan and Gassner-Stamm, Gabriela and Poggi, Valerio and Moore, Jeffrey R. and F\u00e4h, Donat","eprint":"https:\/\/academic.oup.com\/gji\/article-pdf\/180\/2\/820\/6047841\/180-2-820.pdf","number":"2","volume":"180","journal":"Geophysical Journal International","abstract":"A field experiment with small aperture seismic arrays was performed on the unstable rock slope above the village of Randa in the southern Swiss Alps. The aim of this experiment was to constrain the seismic response of a potential future rockslide using ambient vibration recordings. Weak seismic events were identified on the recordings and site-to-reference spectral ratios were calculated using a reference site located on the stable part of the slope. Spectral ratios of up to 30 were observed at sites located within the unstable portion of the slope. A strong variation of spectral ratios with azimuth indicates a directional site effect. Neither amplification nor directionality were observed at sites located in the stable part of the slope. Furthermore, time-frequency polarization analysis of the ambient noise was performed to provide robust estimates of frequency dependent directions of the maximum polarization. It was found that the unstable part of the slope vibrates within a narrow range of directions (130 \u00b1 10\u00b0) for the frequency range centred around 5 Hz. The polarization directions estimated from ambient seismic vibrations are in good agreement with the deformation directions obtained by geodetic and in situ measurements. No directionality of ambient vibrations was observed at sites within the stable part of the slope.","identifier":[{"id":"","type":"DOI"}],"unique_name":"10.1111\/j.1365-246X.2009.04451.x","id":1294},{"doi":"10.1093\/gji\/ggy133","url":"https:\/\/doi.org\/10.1093\/gji\/ggy133","issn":"0956-540X","type":"article","year":"2018","month":"03","pages":"635-650","title":"A systematic analysis of directional site effects at stations of the Italian seismic network to test the role of local topography","author":"Pischiutta, Marta and Cianfarra, Paola and Salvini, Francesco and Cara, Fabrizio and Vannoli, Paola","eprint":"https:\/\/academic.oup.com\/gji\/article-pdf\/214\/1\/635\/25012513\/ggy133.pdf","number":"1","volume":"214","journal":"Geophysical Journal International","abstract":"Directional site effects observed at seismological stations on pronounced relief are analysed. We investigate the ground motion properties calculating horizontal-to-vertical spectral ratios and horizontal polarization of both ambient vibrations and earthquake records using broad-band seismograms of the Italian seismic network. We find that a subset of 47 stations with pronounced relief results in a significant (\\\\>2) directional amplification of the horizontal component, with a well-defined, site-specific direction of motion. However, the horizontal spectral response of sites is not uniform, varying from an isolated (resonant) frequency peak to a broad-band amplification, interesting frequency bands as large as 1\u201310\u00a0Hz in many cases. Using 47 selected stations, we have tried to establish a relation between directional amplification and topography geometry in a 2-D vision, when applicable, through a morphological analysis of the digital elevation model using geographic information systems. The procedure computes the parameters that characterize the geometry of topographic irregularities (size and slope), in combination with a principal component analysis that automatically yields the orientation of the elongated ridges. In seeking a relation between directional amplification and the surface morphology, we have found that it is impossible to fit the variety of observations with a resonant topography model as well as to identify common features in the ground motion behaviour for stations with similar topography typologies. We conclude that, rather than the shape of the topography, local structural complexities and details of the near-surface structure must play a predominant role in controlling ground motion properties at sites with pronounced relief.","identifier":[{"id":"","type":"DOI"}],"unique_name":"10.1093\/gji\/ggy133","id":1295},{"link":[{"url":""}],"type":"article","year":"2020","title":"topolino","author":[{"name":"pippo"},{"name":"pluto"},{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":"BSSA"},"identifier":[{"id":"http:\/\/doi.org\/10.20.55","type":"DOI"}],"id":1252},{"doi":"10.1785\/012003001","url":"https:\/\/doi.org\/10.1785\/012003001","issn":"0037-1106","type":"article","year":"2004","month":"08","pages":"1517-1527","title":"Ambient Noise Levels in the Continental United States","author":"McNamara, Daniel E. and Buland, Raymond P.","eprint":"https:\/\/pubs.geoscienceworld.org\/ssa\/bssa\/article-pdf\/94\/4\/1517\/2720935\/1517\\_ssa03001.pdf","number":"4","volume":"94","journal":"Bulletin of the Seismological Society of America","abstract":"We present a new approach to characterize the background seismic noise across the continental United States. Using this approach, power spectral density (PSD) is estimated at broadband seismic stations for frequencies ranging from \u223c0.01 to 16 Hz. We selected a large number of 1-hr waveform segments during a 3-yr period, from 2001 to 2003, from continuous data collected by the U.S. National Seismograph Network and the Advanced National Seismic System (ANSS).For each segment of continuous data, the PSD is estimated and smoothed in full-octave averages at 1\/8 octave intervals. Powers for each 1\/8 period interval were then accumulated in 1-dB power bins. A statistical analysis of power bins yields probability density functions (PDFs) as a function of noise power for each of the octave bands at each station and component. There is no need to account for earthquakes since they map into a background probability level. A comparison of day and night PDFs and an examination of artifacts related to station operation and episodic cultural noise allow us to estimate both the overall station quality and the level of earth noise at each site. Percentage points of the PDFs have been derived to form the basis for noise maps of the contiguous United States at body-wave frequencies.The results of our noise analysis are useful for characterizing the performance of existing broadband stations and for detecting operational problems and should be relevant to the future siting of ANSS backbone stations. The noise maps at body-wave frequencies should be useful for estimating the magnitude threshold for the ANSS backbone and regional networks or conversely for optimizing the distribution of regional network stations.","identifier":[{"id":"","type":"DOI"}],"unique_name":"10.1785\/012003001","id":1307},{"doi":"10.1016\/j.jog.2014.09.006","link":[{"url":"https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S0264370714001306"}],"type":"article","year":"2014","pages":"16-25","title":"The lithosphere and asthenosphere system in Italy as inferred from the Vp and Vs 3D velocity model and Moho map","author":"Di Stefano, R. and Ciaccio, M.G.","number":"Complete","volume":"82","journal":"Journal of Geodynamics","abstract":"We present an updated high-resolution tomographic P- and S-wave velocity model of the lithosphere and asthenosphere system in Italy, obtained by adding the observations from \u223c25,000 earthquakes (recorded between 2003 and April 2012 at three-component stations) to the previously inverted dataset (165,000 P-wave phases from \u223c8000 events recorded between 1988 and 2002 at single-component). The final dataset includes \u223c586,000 P- and \u223c290,000 S-wave arrival times. The main strength of this research is the use of a method able to model P- and S-seismic phases refracted at the Moho discontinuity. We use a new and original map of the 3D Moho geometry obtained by integrating selected high quality controlled source seismology (CSS) and teleseismic receiver function data. Resolution strongly benefits also from the fast increase in number and quality of INGV National Seismic Network since year 2003 and from its integration with several permanent regional seismic networks. This study confirms the main structural features in the best-resolved parts of the inverted volume and much better images details in the less resolved areas of previous Vp models, due to both the larger number of inverted phases and the more even distribution of seismic stations. A new 3D Vp\/Vs model is presented and discussed. Shallow structures and the relationships between the Adriatic, Tyrrhenian, and Adria plates are better imaged.","keywords":"Tomography; Vp\/Vs; Moho topography; Italy region","language":"English","identifier":[{"id":"","type":"DOI"}],"affiliation":"Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy","unique_name":"DiStefano2014","id":1303},{"doi":"10.1016\/j.soildyn.2014.04.002","link":[{"url":"https:\/\/doi.org\/10.1016\/j.soildyn.2014.04.002"}],"type":"article","year":"2014","month":"08","pages":"248\u2013258","title":"A GIS procedure for fast topographic characterization of seismic recording stations","author":"V. Pessina and E. Fiorini","volume":"63","journal":"Soil Dynamics and Earthquake Engineering","identifier":[{"id":"https:\/\/doi.org\/10.1016\/j.soildyn.2014.04.002","type":"DOI"}],"unique_name":"article","id":1296},{"doi":"https:\/\/doi.org\/10.1016\/S0924-2716(02)00164-8","url":"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0924271602001648","issn":"0924-2716","note":"Challenges in Geospatial Analysis and Visualization","type":"article","year":"2003","pages":"356-370","title":"Mapping from ASTER stereo image data: DEM validation and accuracy assessment","author":"Akira Hirano and Roy Welch and Harold Lang","number":"5","volume":"57","journal":"ISPRS Journal of Photogrammetry and Remote Sensing","abstract":"The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on-board the National Aeronautics and Space Administration's (NASA's) Terra spacecraft provides along-track digital stereo image data at 15-m resolution. As part of ASTER digital elevation model (DEM) accuracy evaluation efforts by the US\/Japan ASTER Science Team, stereo image data for four study sites around the world have been employed to validate prelaunch estimates of heighting accuracy. Automated stereocorrelation procedures were implemented using the Desktop Mapping System (DMS) software on a personal computer to derive DEMs with 30- to 150-m postings. Results indicate that a root-mean-square error (RMSE) in elevation between \u00b17 and \u00b115 m can be achieved with ASTER stereo image data of good quality. An evaluation of an ASTER DEM data product produced at the US Geological Survey (USGS) EROS Data Center (EDC) yielded an RMSE of \u00b18.6 m. Overall, the ability to extract elevations from ASTER stereopairs using stereocorrelation techniques meets expectations.","keywords":"ASTER, DEM, stereocorrelation, validation","identifier":[{"id":"https:\/\/doi.org\/10.1016\/S0924-2716(02)00164-8","type":"DOI"}],"unique_name":"HIRANO2003356","id":1297},{"link":[{"url":"http:\/\/tinitaly.pi.ingv.it\/"}],"year":"2007","title":"TINITALY, a digital elevation model of Italy with a 10 meters cell size (Version 1.0)","author":[{"name":"Tarquini S."},{"name":"Isola I."},{"name":" Favalli M."},{"name":"Battistini A. "}],"journal":{"name":"Istituto Nazionale di Geofisica e Vulcanologia (INGV)"},"identifier":[{"id":"https:\/\/doi.org\/10.13127\/TINITALY\/1.0.","type":"DOI"}],"id":1298},{"link":[{"url":""}],"year":"","title":"Quality assessment for site characterization at seismic stations. ","author":[{"name":"Di Giulio, G."},{"name":"Cultrera, G. "},{"name":"Cornou, C."},{"name":"Bard, P.Y."},{"name":"Al Tfaily, B."},{"name":""}],"journal":{"name":"Bulletin of Earthquake Engineering, pp.1-49."},"identifier":[{"id":"https:\/\/doi.org\/10.1007\/s10518-021-01137-6","type":"ISRC"}],"id":1299},{"link":[{"url":"https:\/\/www.gazzettaufficiale.it\/eli\/gu\/2018\/02\/20\/42\/so\/8\/sg\/pdf"}],"year":"2018","title":"Aggiornamento delle \u00abNorme tecniche per le costruzioni\u00bb.","author":[{"name":"MINISTERO DELLE INFRASTRUTTURE E DEI TRASPORTI"},{"name":""},{"name":""},{"name":""}],"journal":{"name":""},"identifier":[{"id":"","type":""}],"id":1301},{"link":[{"url":"https:\/\/www.gazzettaufficiale.it\/eli\/gu\/2009\/02\/26\/47\/so\/27\/sg\/pdf"}],"year":"2008","title":"Istruzioni per l\u2019applicazione delle \u00abNuove norme tecniche per le costruzioni\u00bb ","author":[{"name":"MINISTERO DELLE INFRASTRUTTURE E DEI TRASPORTI"},{"name":""},{"name":""},{"name":""}],"journal":{"name":""},"identifier":[{"id":"","type":""}],"id":1300},{"link":[{"url":"https:\/\/www.nehrp.gov\/"}],"year":"2009","title":"NEHRP Recommended Seismic Provisions for New Buildings and Other Structures FEMA P-750\/2009 ed","author":[{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":"National Earthquake Hazards Reduction Program"},"identifier":[{"id":"","type":""}],"id":1302},{"link":[{"url":"https:\/\/eurocodes.jrc.ec.europa.eu\/"}],"year":" 2004","title":"Eurocode 8: Design of structures for earthquake resistance\u2014Part 1: General rules, seismic actions and rules for buildings, European Standard EN 1998-1:2004. European Committee for Standardisation, Brussels ","author":[{"name":"CEN"},{"name":""},{"name":""},{"name":""}],"journal":{"name":""},"identifier":[{"id":"","type":""}],"id":1265},{"doi":"10.1785\/0220190360","url":"https:\/\/doi.org\/10.1785\/0220190360","issn":"0895-0695","type":"article","year":"2020","month":"04","pages":"1878-1889","title":"Geopsy: A User\u2010Friendly Open\u2010Source Tool Set for Ambient Vibration Processing","author":"Wathelet, Marc and Chatelain, Jean\u2010Luc and Cornou, C\u00e9cile and Giulio, Giuseppe Di and Guillier, Bertrand and Ohrnberger, Matthias and Savvaidis, Alexandros","eprint":"https:\/\/pubs.geoscienceworld.org\/ssa\/srl\/article-pdf\/91\/3\/1878\/4988673\/srl-2019360.1.pdf","number":"3","volume":"91","journal":"Seismological Research Letters","abstract":"Ambient vibrations are nowadays considerably used worldwide for numerous types of engineering applications and scientific research. Geopsy and its companion tools are part of that landscape. Since the first release of the program package in 2005, as outcome of the European Union project Site Effects aSsessment from AMbient noisE, Geopsy has become a mature multiplatform open\u2010source package (released under GNU Public License version 3) that has already been recognized as a reference tool for analyzing ambient vibration data in the context of site characterization studies. The community of users has grown from a core group of researchers up to thousands of seismologists and engineers on every career level and on all continents. The versatility of geopsy allows for the processing of all kinds of data needed in site characterization studies, that is, from single station single trace to three\u2010component array recordings. In all of the aforementioned cases, the steps from field acquisition to the production of publication\u2010ready figures are covered and supported by user\u2010friendly graphical user interfaces or corresponding command\u2010line tools for the automation of the complete processing chain. To avoid black\u2010box usage, a number of lower\u2010level tools guarantee maximum flexibility in accessing and controlling processing results at any stage of the analysis.","identifier":[{"id":"","type":"DOI"}],"unique_name":"10.1785\/0220190360","id":1304},{"link":[{"url":"10.1016\/J.SOILDYN.2021.106848"}],"type":"article","year":"2021","pages":"106848","title":"A GIS procedure for the topographic classification of Italy, according to the seismic code provisions","author":"C. Mascandola, L. Luzi, C. Felicetta and F. Pacor","volume":"148","journal":"Soil Dynamics and Earthquake Engineering","identifier":[{"id":"10.1016\/J.SOILDYN.2021.106848","type":"DOI"}],"unique_name":"Mascandola2021AGP","id":1331},{"link":[{"url":"https:\/\/pubs.usgs.gov\/of\/1993\/0322\/ofr93-322.pdf"}],"year":"1993","title":"Observations and modeling of seismic background noise","author":[{"name":"Jon R. Peterson"},{"name":""},{"name":""},{"name":""}],"journal":{"name":"\tU.S. Geological Survey - Albuquerque Seismological Laboratory"},"identifier":[{"id":"10.3133\/ofr93322","type":"DOI"}],"id":1306},{"link":[{"url":"http:\/\/editoria.rm.ingv.it\/rapporti\/2015\/rapporto297\/"}],"year":"2015","title":" SQLX: Test di Installazione e Funzionamento","author":[{"name":"Marzorati s."},{"name":"Lauciani V."},{"name":""},{"name":""}],"journal":{"name":"Rapporti Tecnici INGV"},"identifier":[{"id":"","type":""}],"id":1308},{"link":[{"url":"http:\/\/editoria.rm.ingv.it\/archivio_pdf\/rapporti\/217\/pdf\/rapporti_218.pdf"}],"year":"2012","title":"SEISFACE: interfaccia di gestione delle informazioni della rete sismica nazionale centralizzata","author":[{"name":"Pintore S."},{"name":"Marcocci C."},{"name":"Bono A."},{"name":"Lauciani V., Quintiliani M."}],"journal":{"name":"Rapporti Tecnici INGV"},"identifier":[{"id":"","type":""}],"id":1309},{"link":[{"url":"https:\/\/pubs.usgs.gov\/of\/2002\/ofr-02-0144\/ofr-02-0144.pdf"}],"year":"2002","title":"Methods of Installing United States National Seismographic Network (USNSN) Stations -- A Construction Manual","author":[{"name":"McMillan John R."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"U.S. Geological Survey"},"identifier":[{"id":"","type":""}],"id":1310},{"link":[{"url":""}],"year":"2022","title":" HV Noise and Earthquake Automatic Analysis (HVNEA)","author":[{"name":"Vassallo M."},{"name":"Riccio G."},{"name":"Mercuri A., Cultrera G.,"},{"name":"Di Giulio g."}],"journal":{"name":"Seismological Research Letters"},"identifier":[{"id":"10.1785\/0220220115","type":"DOI"}],"id":1305},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/15106"}],"year":"2021","title":"Site characterization report at the seismic station IV.CAPR \u2013 Capriolo (BS)","author":[{"name":"Manganello P., Lovati S."},{"name":"Puglia R."},{"name":"Brunelli G., Lorenzetti A."},{"name":"Massa M."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/15106","type":"DOI"}],"id":1321},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/15101"}],"year":"2021","title":"Site characterization report at the seismic station IV.MOCO \u2013 Biccari Monte Cornacchia (FG)","author":[{"name":"Zarrilli L., Moschillo R."},{"name":"Vassallo M., Di Giulio G."},{"name":"Pucillo S., Cogliano R."},{"name":"Riccio G."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/15101","type":"DOI"}],"id":1316},{"link":[{"url":"https:\/\/adgeo.copernicus.org\/articles\/43\/31\/2016\/"}],"year":"2016","title":"The Italian National Seismic Network and the earthquake and tsunami monitoring and surveillance systems","author":[{"name":"Michelini A., Margheriti L., Cattaneo M., Cecere G., D'Anna G., Delladio A., Moretti M."},{"name":"Pintore S., Amato A., Basili A., Bono A., Casale P., Danecek P., Demartin M., Faenza L."},{"name":"Lauciani V., Mandiello A. G., Marchetti A., Marcocci C., Mazza S., Mele, F. M. , Nardi A., Nostro C."},{"name":"Pignone M., Quintiliani M., Rao S., Scognamiglio L., Selvaggi, G."}],"journal":{"name":"Advances in Geosciences"},"identifier":[{"id":"https:\/\/doi.org\/10.5194\/adgeo-43-31-2016","type":"DOI"}],"id":1312},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/15102"}],"year":"2021","title":"Site characterization report at the seismic station IV.VENL \u2013 Venezia Lido (VE)","author":[{"name":"Manganello P., Lovati S."},{"name":"Puglia R., Brunelli G."},{"name":"Lorenzetti A."},{"name":"Massa M."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/15102","type":""}],"id":1317},{"link":[{"url":" http:\/\/hdl.handle.net\/2122\/15220"}],"year":"2021","title":"Site characterization report at the seismic station IV.TREG \u2013 Tregnago (VR)","author":[{"name":"Manganello P., Lovati S."},{"name":"Puglia R., Brunelli G."},{"name":"Lorenzetti A."},{"name":"Massa M."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/15220","type":"DOI"}],"id":1318},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/15054"}],"year":"2021","title":"Site characterization report at the seismic station IV.POFI \u2013 Posta Fibreno (FR)","author":[{"name":"Falcucci M., Maceroni D."},{"name":"Dixit Dominus G., "},{"name":"Vassallo M."},{"name":"Di Giulio G., De Luca G."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/15054","type":"DOI"}],"id":1319},{"link":[{"url":""}],"type":"inproceedings","year":"2008","title":"The Lithological map of Italy at 1: 100.000 scale: An example of re-use of an existing paper geological map","author":"Amanti M., Battaglini L., Campo V., Cipolloni C., Congi M.P., Conte G., Delogu D., Ventura R., Zonetti,C.","booktitle":"33rd International Geological Conference, IEI02310L--6-14th August, Oslo (Norway)","identifier":[{"id":"","type":""}],"unique_name":"amanti2008lithological","id":1314},{"link":[{"url":""}],"year":"2016","title":" Agreement between INGV (Istituto Nazionale di Geofisica e Vulcanologia) and ISPRA (Istituto Superiore per la Protezione e la Ricerca Ambientale) for a technical-scientific collaboration aimed at the geolithological characterization of the sites on which the stations of the INGV national seismic network. March 30th, 2016.","author":[{"name":""},{"name":""},{"name":""},{"name":""}],"journal":{"name":""},"identifier":[{"id":"Agreement INGV-ISPRA","type":""}],"id":1315},{"doi":"10.1785\/0220200380","url":"https:\/\/doi.org\/10.1785\/0220200380","issn":"0895-0695","type":"article","year":"2021","month":"03","pages":"1659-1671","title":"Seismic Surveillance and Earthquake Monitoring in Italy","author":"Margheriti L., Nostro C., Cocina O., Castellano M., Moretti M., Lauciani V., Quintiliani M., Bono A., Mele F. M., Pintore S., Montalto P., Peluso R., Scarpato G., Rao S., Alparone S., Di Prima S., Orazi M., Piersanti A., Cecere G., Cattaneo M., Vicari A., Sepe V., Bignami C., Valoroso L., Aliotta M., Azzarone A., Baccheschi P., Benincasa A., Bernardi F., Carluccio I., Casarotti E., Cassisi C., Castello B., Cirilli F., D'Agostino M., D'Ambrosio C., Danecek P., De Cesare W., Della Bina E., Di Filippo A., Di Stefano R., Faenza L., Falco L., Fares M., Ficeli P., Latorre D., Lorenzino M. C., Mandiello A., Marchetti A., Mazza S., Michelini A., Nardi A., Pastori M., Pignone M., Prestifilippo M., Ricciolino P., Sensale G., Scognamiglio L., Selvaggi G., Torrisi O., Zanolin F., Amato A., Bianco F., Branca S., Privitera E., Stramondo S.","eprint":"https:\/\/pubs.geoscienceworld.org\/ssa\/srl\/article-pdf\/92\/3\/1659\/5285951\/srl-2020380.1.pdf","number":"3","volume":"92","journal":"Seismological Research Letters","abstract":"The Istituto Nazionale di Geofisica e Vulcanologia (INGV) is an Italian research institution with focus on earth sciences. Moreover, the INGV is the operational center for seismic surveillance and earthquake monitoring in Italy and is a part of the civil protection system as a center of expertise on seismic, volcanic, and tsunami risks.INGV operates the Italian National Seismic Network and other networks at national scale and is a primary node of the European Integrated Data Archive for archiving and distributing strong\u2010motion and weak\u2010motion seismic recordings.In the control room in Rome, INGV staff performs seismic surveillance and tsunami warning services; in Catania and Naples, the control rooms are devoted to volcanic surveillance. Volcano monitoring includes locating earthquakes in the regions around the Sicilian (Etna, Eolian Islands, and Pantelleria) and the Campanian (Vesuvius, Campi Fregrei, and Ischia) active volcanoes. The tsunami warning is based on earthquake location and magnitude (M) evaluation for moderate to large events in the Mediterranean region and also around the world.The technologists of the institute tuned the data acquisition system to accomplish, in near real time, automatic earthquake detection, hypocenter and magnitude determination, and evaluation of several seismological products (e.g., moment tensors and ShakeMaps).Database archiving of all parametric results is closely linked to the existing procedures of the INGV seismic surveillance environment and surveillance procedures. Earthquake information is routinely revised by the analysts of the Italian seismic bulletin.INGV provides earthquake information to the Department of Civil Protection (Dipartimento di Protezione Civile) to the scientific community and to the public through the web and social media. We aim at illustrating different aspects of earthquake monitoring at INGV: (1)\u00a0network operations; (2)\u00a0organizational structure and the hardware and software used; and (3)\u00a0communication, including recent developments and planned improvements.","identifier":[{"id":"","type":"DOI"}],"unique_name":"10.1785\/0220200380","id":1313},{"link":[{"url":"http:\/\/hdl.handle.net\/2122\/15017"}],"year":"2021","title":"Site characterization report at the seismic station IV.CNCS \u2013 Concesio (BS)","author":[{"name":"Manganello P., Lovati S."},{"name":"Puglia R., Brunelli G."},{"name":"Lorenzetti A. "},{"name":"Massa M."}],"journal":{"name":"Working group INGV \"Agreement DPC-INGV 2019-21, All.B2- WP1, Task 2\u201d"},"identifier":[{"id":"http:\/\/hdl.handle.net\/2122\/15017","type":"DOI"}],"id":1320},{"doi":"https:\/\/doi.org\/10.1016\/j.soildyn.2019.04.002","url":"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0267726118311114","issn":"0267-7261","type":"article","year":"2019","pages":"79-93","title":"Seismic soil classification of Italy based on surface geology and shear-wave velocity measurements","author":"Forte G., Chioccarelli E., De Falco M., Cito P., Santo A., Iervolino I.","volume":"122","journal":"Soil Dynamics and Earthquake Engineering","abstract":"During an earthquake the seismic wave amplification related to local site conditions can have a significant impact on the ground motion. In order to account for these local effects some proxies for the soil characteristics exist; e.g., the average shear-wave velocity of the upper 30\u202fm (VS,30), or the equivalent shear-wave velocity from the ground to the depth of the seismic bedrock when this is less than 30\u202fm VS,eq. The aim of this paper is to provide maps of seismic shallow soil classification for Italy accounting for two sources of information: site-specific measurements and large-scale geological maps. The soil maps are obtained via a four-step procedure: (1) a database of available site-specific investigations is built, covering (unevenly) the whole national territory; (2) twenty geo-lithological complexes are identified from the available geological maps; (3) the investigations are grouped as a function of the geo-lithological complex and the distribution of measured VS,30 and VS,eq are estimated; (4) medians and standard deviations of such distributions are assumed to be representative of the corresponding complexes. The statistics of investigations are used to derive the large-scale soil maps. To make the results of the study available, a stand-alone software has been developed. Despite not being adequate substitutes of site-specific studies such as microzonation and local site response analyses, the provided results can be useful for large-scale seismic risk studies.","keywords":"Probabilistic seismic hazard assessment, Regional seismic risk, Site classification, Soil classes, Seismic soil response","identifier":[{"id":"https:\/\/doi.org\/10.1016\/j.soildyn.2019.04.002","type":"DOI"}],"unique_name":"FORTE201979","id":1322},{"link":[{"url":"http:\/\/www.fdsn.org\/pdf\/SEEDManual_V2.4.pdf"}],"year":"2012","title":"SEED Reference Manual","author":[{"name":"IRIS"},{"name":""},{"name":""},{"name":""}],"journal":{"name":"USGS"},"identifier":[{"id":"","type":""}],"id":1325},{"link":[{"url":""}],"year":"2018","title":"Risultati delle prove geofisiche in foro di tipo Down-Hole (DH) Sede INGV - Via di Vigna Murata 605 (RM)","author":[{"name":"Cercato M, Desideri F.S., Pugliese F."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"DICEA- Univ. La Sapienza (Agreement DPCINGV 2018, All. B2: Obiettivo 1 - TASKB)"},"identifier":[{"id":"","type":""}],"id":1326},{"link":[{"url":" https:\/\/gfzpublic.gfz-potsdam.de\/pubman\/item\/item_227033"}],"year":"1998","title":"European Macroseismic Scale 1998 (EMS-98)","author":[{"name":"ESC Working Group Macroseismic Scales"},{"name":""},{"name":""},{"name":""}],"journal":{"name":"G. Gr\u00fcnthal (Ed.), ISBN N\u00b0 2-87977-008-4, Luxembourg "},"identifier":[{"id":"https:\/\/doi.org\/10.2312\/EMS-98.full.en","type":"DOI"}],"id":1324},{"link":[{"url":""}],"year":"2016","title":"Caratterizzazione geolitologica dei siti su cui ricadono le stazioni della Rete Sismica Nazionale dell\u2019INGV","author":[{"name":"Monti G. M."},{"name":"Martarelli L."},{"name":"Gaf\u00e0 R. M."},{"name":"Olivetta L."}],"journal":{"name":"INGV- ISPRA 2016-17 Agreement (protocol INGV 2016\/0003777 of 04\/04\/2016): \"Scientific and technical collaboration aimed at the geolithological characterization of the sites of the stations of the national INGV seismic network \"(Scientific Coordinators: P. Bordoni and G.M. Monti)"},"identifier":[{"id":"","type":""}],"id":1328},{"link":[{"url":""}],"year":"2017","title":"RELAZIONE TECNICA  In merito ai lavori di  \u201c Realizzazione di n. 1 sondaggio geognostico a profondit\u00e0 di 75 mt.\u201d   \u201cIn localit\u00e0 Via di Vigna Murata 605 _ INGV\u201d","author":[{"name":"M. Gizi"},{"name":""},{"name":""},{"name":""}],"journal":{"name":"UNIGEO s.r.l"},"identifier":[{"id":"","type":""}],"id":1330},{"link":[{"url":"http:\/\/people.dicea.unifi.it\/johannf\/Senigallia_2007.pdf"}],"year":"2007","title":"Caratterizzazione dinamica dei terreni di Senigallia e analisi della risposta sismica locale ","author":[{"name":"Crespellani T."},{"name":"Facciorusso J."},{"name":"Madiai C."},{"name":"Simoni G."}],"journal":{"name":""},"identifier":[{"id":"","type":""}],"id":1329},{"link":[{"url":""}],"year":"2018","title":"Risultati delle prove geofisiche in foro di tipo Cross-Hole (CH) Sede INGV - Via di Vigna Murata 605 (RM)","author":[{"name":"Cercato M., Desideri F.S., Pugliese F."},{"name":""},{"name":""},{"name":""}],"journal":{"name":"DICEA- Univ. La Sapienza (Agreement DPCINGV 2018, All. B2: Obiettivo 1 - TASKB)"},"identifier":[{"id":"","type":""}],"id":1327},{"doi":"https:\/\/doi.org\/10.1016\/j.enggeo.2020.105745","url":"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0013795220304713","issn":"0013-7952","type":"article","year":"2020","pages":"105745","title":"A new Vs30 map for Italy based on the seismic microzonation dataset","author":"Mori F., Mendicelli A., Moscatelli M., Romagnoli G., Peronace E., Naso G.","volume":"275","journal":"Engineering Geology","abstract":"In this study, we derive a large-scale Vs30 map for Italy starting from the global terrain geomorphological classification based on normalized slope, local convexity, and surface texture (after Iwahashi et al., 2018). The novelty of the present work is the integration of a large amount of data from the Italian seismic microzonation dataset, consisting in about 35,000 borehole logs and 11,300 Vs profiles. The results of our analysis suggest that the geomorphological classes are correlated to subsoil lithologies and Vs30 values more than surface lithological types (after Amanti et al., 2008). As already done in Japan (Matsuoka and Wakamatsu, 2006), Greece (Stewart et al., 2014), Central and Eastern North America (Parker et al., 2017), and Pacific Northwest Region of North America (Ahdi et al., 2017), we found a proxy dependence of Vs30 from slope gradient and elevation through a lognormal linear regression model for each geomorphological class. A stepwise method allowed us to give meaning and statistical robustness to the regression model dependencies. The polygons inconsistent with the Iwahashi et al. (2018) approach (e.g., Meso-Cenozoic carbonate units of Apulian block and Hyblean Plateau related to the foreland domain) were replaced with the polygons of the lithological map (Amanti et al., 2008) and the associated Vs30 lognormal average values. Therefore, a hybrid raster Vs30 map was created with a spatial resolution of 50\u00a0\u00d7\u00a050 m. The comparison with other previous maps shows how the forecast improves in terms of both accuracy and precision. For these reasons, the new Vs30 proxy-based map for Italy based on the seismic microzonation dataset represents a useful tool for improving several applications: ShakeMaps, stochastic event based hazard map, total hazard map, assessment of coseismic instabilities, seismic risk assessment for spatially distributed emergency and resilience systems. Vs30 raster maps and supplementary material are available in the Research Data (doi:10.17632\/8458tgzc73.1).","keywords":"V map, Seismic microzonation, Geomorphological classes, Proxy-based map, Italy","identifier":[{"id":"https:\/\/doi.org\/10.1016\/j.enggeo.2020.105745","type":"DOI"}],"unique_name":"MORI2020105745","id":1323},{"doi":"https:\/\/doi.org\/10.1016\/j.jappgeo.2017.07.016","url":"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0926985117304901","issn":"0926-9851","type":"article","year":"2017","pages":"17-27","title":"Geophysical and geologic surveys of the areas struck by the August 26th 2016 Central Italy earthquake: The study case of Pretare and Piedilama","author":"S. Imposa and F. Panzera and S. Grassi and G. Lombardo and S. Catalano and G. Romagnoli and G. Tortorici","volume":"145","journal":"Journal of Applied Geophysics","abstract":"A MW6.0 earthquake struck the Central Italian Apennines on August 24th 2016, followed by an important seismic sequence characterized by hundreds of aftershocks. The earthquake caused fatalities and partially destroyed several towns surrounding the epicentral area. In this context the Italian Centre for Seismic Microzonation and its applications was involved for the seismic characterization of the struck area. Using ambient vibrations spectral ratios at seventy-five sites and shear wave velocity profiles obtained through surface waves dispersion properties we assessed seismic site response properties in the Pretare and Piedilama villages located in the territory of Arquata del Tronto. The survey performed inside the valley in which the two villages are located set into evidence that the spectral ratios often show a predominant frequency ranging between 3.0 and 5.0Hz or several peaks that can be related to some alternating layers with different velocities. Conversely, along the valley flanks, where the geological substratum outcrop, spectral ratios tend towards low amplitude values. The soft sediments inside the valley are characterized by shear wave velocity lower than 350m\/s, whereas the geological substratum has shear wave velocity ranging between 600 and 1200m\/s. The integrated interpretation of both geophysical and geological data, made possible to infer subsoil models of the investigated areas identifying the depth of the seismic bedrock and characterizing the buried morphology.","keywords":"Microzonation, Spectral ratio, Central Italy earthquake, Shear wave velocity","identifier":[{"id":"https:\/\/doi.org\/10.1016\/j.jappgeo.2017.07.016","type":"DOI"}],"unique_name":"IMPOSA201717","id":1332}]}