Search

Your search keyword '"De Martini, Paolo Marco"' showing total 48 results
Start Over Author "De Martini, Paolo Marco"
48 results on '"De Martini, Paolo Marco"'

1. Multidisciplinary high resolution Geophysical Imaging of Pantano Ripa Rossa Segment of the Irpinia Fault (Southern Italy)

Author

Bruno, Pier Paolo G., Ferrara, Giuseppe, Zambrano, Miller, Maraio, Stefano, Improta, Luigi, Volatili, Tiziano, Di Fiore, Vincenzo, Florio, Giovanni, Iacopini, David, Accomando, Filippo, Tarallo, Daniela, De Martini, Paolo Marco, Muccini, Filippo, Punzo, Michele, Paoletti, Valeria, Albanese, Stefano, Iannone, Antonio, Pacifico, Lucia Rita, Vicari, Annamaria, Famiglietti, Nicola Angelo, Memmolo, Antonino, Cavuoto, Giuseppe, and Milano, Maurizio

Published
2024
Full Text
View/download PDF

3. Blast-induced liquefaction in silty sands for full-scale testing of ground improvement methods: Insights from a multidisciplinary study

Author

Amoroso, Sara, Rollins, Kyle M., Andersen, Paul, Gottardi, Guido, Tonni, Laura, García Martínez, Maria F., Wissmann, Kord, Minarelli, Luca, Comina, Cesare, Fontana, Daniela, De Martini, Paolo Marco, Monaco, Paola, Pesci, Arianna, Sapia, Vincenzo, Vassallo, Maurizio, Anzidei, Marco, Carpena, Andrea, Cinti, Francesca, Civico, Riccardo, Coco, Igino, Conforti, Dario, Doumaz, Fawzi, Giannattasio, Fabio, Di Giulio, Giuseppe, Foti, Sebastiano, Loddo, Fabiana, Lugli, Stefano, Manuel, Maria R., Marchetti, Diego, Mariotti, Mauro, Materni, Valerio, Metcalfe, Brian, Milana, Giuliano, Pantosti, Daniela, Pesce, Antonio, Salocchi, Aura C., Smedile, Alessandra, Stefani, Marco, Tarabusi, Gabriele, and Teza, Giordano

Published
2020
Full Text
View/download PDF

4. Tsunamis in the Mediterranean Sea

Author

De Martini, Paolo Marco, primary, Graziani, Laura, additional, Maramai, Alessandra, additional, Orefice, Simone, additional, Pantosti, Daniela, additional, and Smedile, Alessandra, additional

Published
2020
Full Text
View/download PDF

7. High-resolution 3-D geophysical imaging across a seismogenic fault: the TEst Site IRpinia fAult (TESIRA) project

Author

Bruno, Pier Paolo Gennaro, primary, Ferrara, Giuseppe, additional, Improta, Luigi, additional, Maraio, Stefano, additional, Di Fiore, Vincenzo, additional, Iacopini, David, additional, Fusco, Mario, additional, Punzo, Michele, additional, Paoletti, Valeria, additional, Cavuoto, Giuseppe, additional, and De Martini, Paolo Marco, additional

Published
2023
Full Text
View/download PDF

8. A multidisciplinary approach gives new insights into the shallow structural setting of the Val d’Agri oilfield (Basilicata, southern Apennines, Italy) 

Author

Maffucci, Roberta, primary, Caciagli, Marco, additional, Braun, Thomas, additional, Buttinelli, Mauro, additional, Cinti, Francesca, additional, Danesi, Stefania, additional, De Martini, Paolo Marco, additional, Errico, Maddalena, additional, Famiani, Daniela, additional, Materni, Valerio, additional, Pantosti, Daniela, additional, Pucci, Stefano, additional, Salimbeni, Simone, additional, and Sapia, Vincenzo, additional

Published
2023
Full Text
View/download PDF

10. Historical and pre-historical tsunamis in the Mediterranean and its connected seas: Geological signatures, generation mechanisms and coastal impacts

Author

Papadopoulos, Gerassimos A., Gràcia, Eulàlia, Urgeles, Roger, Sallares, Valenti, De Martini, Paolo Marco, Pantosti, Daniela, González, Mauricio, Yalciner, Ahmet C., Mascle, Jean, Sakellariou, Dimitris, Salamon, Amos, Tinti, Stefano, Karastathis, Vassilis, Fokaefs, Anna, Camerlenghi, Angelo, Novikova, Tatyana, and Papageorgiou, Antonia

Published
2014
Full Text
View/download PDF

11. Publicity waves based on manipulated geoscientific data suggesting climatic trigger for majority of tsunami findings in the Mediterranean – Response to 'Tsunamis in the geological record: Making waves with a cautionary tale from the Mediterranean' by Marriner et al. (2017)

Author

Vött, Andreas, Bruins, Hendrik J., Gawehn, Matthijs, Goodman-Tchernov, Beverly N., De Martini, Paolo Marco, Kelletat, Dieter, Mastronuzzi, Giuseppe, Reicherter, Klaus, Röbke, Björn R., Scheffers, Anja, Willershäuser, Timo, Avramidis, Pavlos, Bellanova, Piero, Costa, Pedro J.M., Finkler, Claudia, Hadler, Hanna, Koster, Benjamin, Lario, Javier, Reinhardt, Eduard, Mathes-Schmidt, Margret, Ntageretzis, Konstantin, Pantosti, Daniela, Papanikolaou, Ioannis, Sansò, Paolo, Scicchitano, Giovanni, Smedile, Alessandra, Szczuciński, Witek, Rötbke, Bjötrn R., and Willershätuser, Timo

Subjects
Mediterranean climate, Mediterranean sea, Geographie, Context (language use), Storm, Physical geography, Storm Data, Geologic record, Coastal flood, Holocene, Geology, ddc:910
Abstract

Zeitschrift für Geomorphologie (2018). doi:10.1127/zfg_suppl/2018/0547, Published by Schweizerbart, Stuttgart

Published
2019
Full Text
View/download PDF

13. High‐Resolution Seismic Profiling in the Hanging Wall of the Southern Fault Section Ruptured During the 2016 Mw 6.5 Central Italy Earthquake

Author

Villani, Fabio, primary, Maraio, Stefano, additional, Bruno, Pier Paolo, additional, Improta, Luigi, additional, Wood, Kieran, additional, Pucci, Stefano, additional, Civico, Riccardo, additional, Sapia, Vincenzo, additional, De Martini, Paolo Marco, additional, Brunori, Carlo Alberto, additional, Doglioni, Carlo, additional, and Pantosti, Daniela, additional

Published
2021
Full Text
View/download PDF

15. Surface faulting during the 29 December 2020 Mw 6.4 Petrinja earthquake (Croatia)

Author

Boncio, Paolo, primary, Amoroso, Sara, additional, Atanackov, Jure, additional, Baize, Stéphane, additional, Barbača, Josip, additional, Bavec, Miloš, additional, Belić, Nikola, additional, Benedetti, Lucilla, additional, Brajkovič, Rok, additional, Brčić, Vlatko, additional, Budić, Marko, additional, Caciagli, Marco, additional, Celarc, Bogomor, additional, Civico, Riccardo, additional, Cinti, Francesca R., additional, De Martini, Paolo Marco, additional, Filjak, Radovan, additional, Henriquet, Maxime, additional, Kordić, Branko, additional, Iezzi, Francesco, additional, Minarelli, Lua, additional, Moulin, Adrien, additional, Nappi, Rosa, additional, Novak, Ana, additional, Novak, Matevž, additional, Pace, Bruno, additional, Palenik, Damir, additional, Pantosti, Daniela, additional, Pucci, Stefano, additional, Jamšek Rupnik, Petra, additional, Špelić, Marko, additional, Testa, Alessio, additional, Valkaniotis, Sotiris, additional, and Vukovski, Martija, additional

Published
2021
Full Text
View/download PDF

16. Liquefaction field reconnaissance following the 29th December 2020 Mw 6.4 Petrinja earthquake (Croatia)

Author

Amoroso, Sara, primary, Barbača, Josip, additional, Belić, Nikola, additional, Kordić, Branko, additional, Brčić, Vlatko, additional, Budić, Marko, additional, Civico, Riccardo, additional, De Martini, Paolo Marco, additional, Hećej, Nina, additional, Kurečić, Tomislav, additional, Minarelli, Luca, additional, Novosel, Tomislav, additional, Palenik, Damir, additional, Pantosti, Daniela, additional, Pucci, Stefano, additional, Filjak, Radovan, additional, Ricci, Tullio, additional, Špelić, Marko, additional, and Vukovski, Matija, additional

Published
2021
Full Text
View/download PDF

19. A deep resistivity Full Waver survey unravels the 3D structure of the Castelluccio basin in relation to the source of the 2016 Mw 6.5 Norcia earthquake (central Italy)

Author

Sapia, Vincenzo, primary, Villani, Fabio, additional, Fischanger, Federico, additional, Lupi, Matteo, additional, Baccheschi, Paola, additional, Brunori, Carlo Alberto, additional, Civico, Riccardo, additional, Coco, Igino, additional, De Martini, Paolo Marco, additional, Giannattasio, Fabio, additional, Improta, Luigi, additional, Materni, Valerio, additional, Murgia, Federica, additional, Pantosti, Daniela, additional, Pizzimenti, Luca, additional, Pucci, Stefano, additional, Ricci, Tullio, additional, Romano, Valentina, additional, Sciarra, Alessandra, additional, and Smedile, Alessandra, additional

Published
2020
Full Text
View/download PDF

22. High‐Resolution Seismic Profiling in the Hanging Wall of the Southern Fault Section Ruptured During the 2016 Mw 6.5 Central Italy Earthquake.

Author

Villani, Fabio, Maraio, Stefano, Bruno, Pier Paolo, Improta, Luigi, Wood, Kieran, Pucci, Stefano, Civico, Riccardo, Sapia, Vincenzo, De Martini, Paolo Marco, Brunori, Carlo Alberto, Doglioni, Carlo, and Pantosti, Daniela

Abstract

The Vettore–Bove normal fault system in central Italy ruptured during the 2016 MW 6.5 Norcia earthquake causing extensive surface faulting. At the Pian Grande di Castelluccio hanging wall basin, along the southern section of the fault ruptured during the MW 6.5 mainshock, we performed a high‐resolution seismic reflection/refraction experiment aimed at (a) imaging the shallow pattern of the fault system, and (b) reconstructing the architecture of the continental infill. We collected three profiles for a total length of ∼8 km. We used a reflection processing flow and non‐linear refraction tomography to obtain migrated stack sections and P‐wave velocity images resolved down to the depth of the pre‐Quaternary substratum. The main profile in the northern part of the basin crosses the westernmost splays of the ruptured fault zone striking N150°–170°. Seismic imaging unravels a ∼1 km‐wide fault zone comprising three W‐throwing splays and subsidiary faults, which affect the continental infill and produce a minimum aggregate Quaternary throw of ∼400 ± 100 m. Recent deformation is localized in this part of the surveyed fault section, attesting active displacement accumulation of the Vettore–Bove fault system. The other profiles in the central‐southern part of the basin show additional faults, likely striking N20°–40° and which concurred to generate a ∼500 m‐deep depocenter. These faults were mostly active during an early extensional phase; however, one of them likely displaces shallow layers with a throw close to the resolution limit of seismic data (<10 m), suggesting activity in the Late Pleistocene. Key Points: Three high resolution seismic profiles image the hanging wall of southern part of the 2016 MW 6.5 central Italy earthquake fault zoneThe surveyed ∼1 km‐wide hidden fault section displays three active W‐dipping splays with a minimum aggregate Quaternary throw of ∼400 mP‐wave velocity tomographic images and migrated sections depict a ∼500 m‐deep Quaternary depocenter in the earthquake fault hanging wall [ABSTRACT FROM AUTHOR]

Published
2021
Full Text
View/download PDF

23. Surface ruptures following the 26 December 2018, Mw 4.9, Mt. Etna earthquake, Sicily (Italy)

Author

Civico, Riccardo, Pucci, Stefano, Nappi, Rosa, Azzaro, Raffaele, Villani, Fabio, Pantosti, Daniela, Cinti, Francesca R., Pizzimenti, Luca, Branca, Stefano, Brunori, Carlo Alberto, Caciagli, Marco, Cantarero, Massimo, Cucci, Luigi, D’Amico, Salvatore, De Beni, Emanuela, De Martini, Paolo Marco, Mariucci, Maria Teresa, Montone, Paola, Nave, Rosella, Ricci, Tullio, Sapia, Vincenzo, Smedile, Alessandra, Tarabusi, Gabriele, Vallone, Roberto, and Venuti, Alessandra

Abstract

We present a 1:10,000 scale map of the coseismic surface ruptures following the 26 December 2018 Mw 4.9 earthquake that struck the eastern flank of Mt. Etna volcano (southern Italy). Detailed rupture mapping is based on extensive field surveys in the epicentral region. Despite the small size of the event, we were able to document surface faulting for about 8 km along the trace of the NNW-trending active Fiandaca Fault, belonging to the Timpe tectonic system in the eastern flank of the volcano. The mapped ruptures are characterized in most cases by perceivable opening and by a dominant right-oblique sense of slip, with an average slip of about 0.09 m and a peak value of 0.35 m. It is also noteworthy that the ruptures vary significantly in their kinematic expression, denoting locally high degree of complexity of the surface faulting.

Published
2019
Full Text
View/download PDF

24. A database of the coseismic effects following the 30 October 2016 Norcia earthquake in Central Italy

Author

Villani, Fabio, Civico, Riccardo, Pucci, Stefano, Pizzimenti, Luca, Nappi, Rosa, De Martini, Paolo Marco, Agosta, F., Alessio, G., Alfonsi, L., Amanti, M., Amoroso, S., Aringoli, D., Auciello, E., Azzaro, R., Baize, S., Bello, S., Benedetti, L., Bertagnini, A., Binda, G., Bisson, M., Blumetti, A.M., Bonadeo, L., Boncio, P., Bornemann, P., Branca, S., Braun, T., Brozzetti, F., Brunori, C.A., Burrato, P., Caciagli, M., Campobasso, C., Carafa, M., Cinti, F.R., Cirillo, D., Comerci, V., Cucci, L., De Ritis, R., Deiana, G., Del Carlo, P., Del Rio, L., Delorme, A., Di Manna, P., Di Naccio, D., Falconi, L., Falcucci, E., Farabollini, P., Faure Walker, J.P., Ferrarini, F., Ferrario, M.F., Ferry, M., Feuillet, N., Fleury, J., Fracassi, U., Frigerio, C., Galluzzo, F., Gambillara, R., Gaudiosi, G., Goodall, H., Gori, S., Gregory, L.C., Guerrieri, L., Hailemikael, S., Hollingsworth, J., Iezzi, F., Invernizzi, C., Jablonská, D., Jacques, E., Jomard, H., Kastelic, V., Klinger, Y., Lavecchia, G., Leclerc, F., Liberi, F., Lisi, A., Livio, F., Lo Sardo, L., Malet, J.P., Mariucci, M.T., Materazzi, M., Maubant, L., Mazzarini, F., McCaffrey, K.J.W., Michetti, A.M., Mildon, Z.K., Montone, P., Moro, M., Nave, R., Odin, M., Pace, B., Paggi, S., Pagliuca, N., Pambianchi, G., Pantosti, D., Patera, A., Pérouse, E., Pezzo, G., Piccardi, L., Pierantoni, P.P., Pignone, M., Pinzi, S., Pistolesi, E., Point, J., Pousse, L., Pozzi, A., Proposito, M., Puglisi, C., Puliti, I., Ricci, T., Ripamonti, L., Rizza, M., Roberts, G.P., Roncoroni, M., Sapia, V., Saroli, M., Sciarra, A., Scotti, O., Skupinski, G., Smedile, A., Soquet, A., Tarabusi, G., Tarquini, S., Terrana, S., Tesson, J., Tondi, E., Valentini, A., Vallone, R., Van der Woerd, J., Vannoli, P., Venuti, A., Vittori, E., Volatili, T., Wedmore, L.N.J., Wilkinson, M., Zambrano, M., Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Roma (INGV), Istituto Nazionale di Geofisica e Vulcanologia, Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Palermo (INGV), Istituto sull’Inquinamento Atmosferico (CNR-IIA), Consiglio Nazionale delle Ricerche (CNR), Institut de Radioprotection et de Sûreté Nucléaire (IRSN), Università degli studi 'G. d'Annunzio' Chieti-Pescara [Chieti-Pescara] (Ud'A), Laboratoire Image, Ville, Environnement (LIVE), Université de Strasbourg (UNISTRA)-Centre National de la Recherche Scientifique (CNRS), Littoral, Environnement, Télédétection, Géomatique (LETG - Caen), Littoral, Environnement, Télédétection, Géomatique UMR 6554 (LETG), Université de Caen Normandie (UNICAEN), Normandie Université (NU)-Normandie Université (NU)-Université d'Angers (UA)-Université de Nantes (UN)-École pratique des hautes études (EPHE)-Université de Brest (UBO)-Université de Rennes 2 (UR2), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Centre National de la Recherche Scientifique (CNRS)-Université de Caen Normandie (UNICAEN), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Centre National de la Recherche Scientifique (CNRS), Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS), Dipartimento di Scienze Fisiche, Informatiche e Matematiche [Modena], Università degli Studi di Modena e Reggio Emilia (UNIMORE), Géosciences Montpellier, Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Université des Antilles (UA), Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Collège de France (CdF)-Institut national des sciences de l'Univers (INSU - CNRS)-Aix Marseille Université (AMU)-Institut National de la Recherche Agronomique (INRA), Géoazur (GEOAZUR 7329), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud]), Institut de physique du globe de Strasbourg (IPGS), Université de Strasbourg (UNISTRA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Istituto Nazionale di Geofisica e Vulcanologia – Sezione di Pisa (INGV), Laboratoire de géologie de l'ENS (LGE), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris)-École normale supérieure - Paris (ENS Paris), Institut des Sciences de la Terre (ISTerre), Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-PRES Université de Grenoble-Institut de recherche pour le développement [IRD] : UR219-Institut national des sciences de l'Univers (INSU - CNRS)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Université Joseph Fourier - Grenoble 1 (UJF), Italian National agency for new technologies, Energy and sustainable economic development [Frascati] (ENEA), Departimento di Scienze della Terra [Camerino], Università di Camerino (UNICAM), Laboratoire d'Ecologie Alpine (LECA), Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Université Joseph Fourier - Grenoble 1 (UJF)-Université Grenoble Alpes (UGA), Dynamique globale et déformation active (IPGS) (IPGS-DGDA), Université de Strasbourg (UNISTRA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Strasbourg (UNISTRA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), National Research Council of Italy | Consiglio Nazionale delle Ricerche (CNR), Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Normandie Université (NU)-Normandie Université (NU)-Université d'Angers (UA)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (IGARUN), Université de Nantes (UN)-Université de Nantes (UN)-Université de Caen Normandie (UNICAEN), Université de Nantes (UN)-Université de Nantes (UN), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Università degli Studi di Modena e Reggio Emilia = University of Modena and Reggio Emilia (UNIMORE), COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud]), Laboratoire de géologie de l'ENS (LGENS), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement [IRD] : UR219-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Università degli Studi di Camerino = University of Camerino (UNICAM), Laboratoire d'Ecologie Alpine (LECA ), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA), Normandie Université (NU)-Normandie Université (NU)-Université d'Angers (UA)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Brest (UBO)-Université de Rennes 2 (UR2), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (IGARUN), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Université des Antilles (UA)-Centre National de la Recherche Scientifique (CNRS), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Università degli Studi di Camerino (UNICAM), Puglisi, C., Proposito, M., Hailemikael, S., Falconi, L., Centre National de la Recherche Scientifique (CNRS)-Université de Rennes 2 (UR2), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Université de Brest (UBO)-École pratique des hautes études (EPHE)-Université de Nantes (UN)-Université d'Angers (UA)-Université de Caen Normandie (UNICAEN), Normandie Université (NU)-Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS)-Université de Rennes 2 (UR2), Normandie Université (NU)-Normandie Université (NU), Centre National de la Recherche Scientifique (CNRS)-Université de La Réunion (UR)-Université Paris Diderot - Paris 7 (UPD7)-IPG PARIS-Institut national des sciences de l'Univers (INSU - CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA), Villani, F., Civico, R., Pucci, S., Pizzimenti, L., Nappi, R., De Martini, P. M., Agosta, F., Alessio, G., Alfonsi, L., Amanti, M., Amoroso, S., Aringoli, D., Auciello, E., Azzaro, R., Baize, S., Bello, S., Benedetti, L., Bertagnini, A., Binda, G., Bisson, M., Blumetti, A. M., Bonadeo, L., Boncio, P., Bornemann, P., Branca, S., Braun, T., Brozzetti, F., Brunori, C. A., Burrato, P., Caciagli, M., Campobasso, C., Carafa, M., Cinti, F. R., Cirillo, D., Comerci, V., Cucci, L., De Ritis, R., Deiana, G., Del Carlo, P., Del Rio, L., Delorme, A., Di Manna, P., Di Naccio, D., Falcucci, E., Farabollini, P., Faure Walker, J. P., Ferrarini, F., Ferrario, M. F., Ferry, M., Feuillet, N., Fleury, J., Fracassi, U., Frigerio, C., Galluzzo, F., Gambillara, R., Gaudiosi, G., Goodall, H., Gori, S., Gregory, L. C., Guerrieri, L., Hollingsworth, J., Iezzi, F., Invernizzi, C., Jablonska, D., Jacques, E., Jomard, H., Kastelic, V., Klinger, Y., Lavecchia, G., Leclerc, F., Liberi, F., Lisi, A., Livio, F., Sardo, L., Malet, J. P., Mariucci, M. T., Materazzi, M., Maubant, L., Mazzarini, F., Mccaffrey, K. J. W., Michetti, A. M., Mildon, Z. K., Montone, P., Moro, M., Nave, R., Odin, M., Pace, B., Paggi, S., Pagliuca, N., Pambianchi, G., Pantosti, D., Patera, A., Perouse, E., Pezzo, G., Piccardi, L., Pierantoni, P. P., Pignone, M., Pinzi, S., Pistolesi, E., Point, J., Pousse, L., Pozzi, A., Puliti, I., Ricci, T., Ripamonti, L., Rizza, M., Roberts, G. P., Roncoroni, M., Sapia, V., Saroli, M., Sciarra, A., Scotti, O., Skupinski, G., Smedile, A., Soquet, A., Tarabusi, G., Tarquini, S., Terrana, S., Tesson, J., Tondi, E., Valentini, A., Vallone, R., Van Der Woerd, J., Vannoli, P., Venuti, A., Vittori, E., Volatili, T., Wedmore, L. N. J., Wilkinson, M., and Zambrano, M.

Subjects
Statistics and Probability, data collection, 010504 meteorology & atmospheric sciences, [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph], Library and Information Sciences, 010502 geochemistry & geophysics, computer.software_genre, 01 natural sciences, Education, 30 October 2016 Norcia earthquake, Earthquakes, ground deformation process, 0105 earth and related environmental sciences, [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics, surface faulting hazard, Central Apennines, Database, Landslide, data acquisition system, Extensional definition, Computer Science Applications, 13. Climate action, Homogeneous, Georeference, ground deformation process, data acquisition system, Central Apennines, 30 October 2016 Norcia earthquake, Statistics, Probability and Uncertainty, computer, Relevant information, Geology, Information Systems
Abstract

We provide a database of the coseismic geological surface effects following the Mw 6.5 Norcia earthquake that hit central Italy on 30 October 2016. This was one of the strongest seismic events to occur in Europe in the past thirty years, causing complex surface ruptures over an area of >400 km2. The database originated from the collaboration of several European teams (Open EMERGEO Working Group; about 130 researchers) coordinated by the Istituto Nazionale di Geofisica e Vulcanologia. The observations were collected by performing detailed field surveys in the epicentral region in order to describe the geometry and kinematics of surface faulting, and subsequently of landslides and other secondary coseismic effects. The resulting database consists of homogeneous georeferenced records identifying 7323 observation points, each of which contains 18 numeric and string fields of relevant information. This database will impact future earthquake studies focused on modelling of the seismic processes in active extensional settings, updating probabilistic estimates of slip distribution, and assessing the hazard of surface faulting.

Published
2018
Full Text
View/download PDF

25. Surface ruptures following the 26 December 2018, Mw 4.9, Mt. Etna earthquake, Sicily (Italy)

Author

Civico, Riccardo, primary, Pucci, Stefano, additional, Nappi, Rosa, additional, Azzaro, Raffaele, additional, Villani, Fabio, additional, Pantosti, Daniela, additional, Cinti, Francesca R., additional, Pizzimenti, Luca, additional, Branca, Stefano, additional, Brunori, Carlo Alberto, additional, Caciagli, Marco, additional, Cantarero, Massimo, additional, Cucci, Luigi, additional, D’Amico, Salvatore, additional, De Beni, Emanuela, additional, De Martini, Paolo Marco, additional, Mariucci, Maria Teresa, additional, Montone, Paola, additional, Nave, Rosella, additional, Ricci, Tullio, additional, Sapia, Vincenzo, additional, Smedile, Alessandra, additional, Tarabusi, Gabriele, additional, Vallone, Roberto, additional, and Venuti, Alessandra, additional

Published
2019
Full Text
View/download PDF

26. Ricostruzione tridimensionale dei principali rilievi interessati dai fenomeni di fagliazione superficiale tra Arquata del Tronto (AP) e Cupi (MC), Sequenza Sismica in Italia centrale, gruppo EMERGEO INGV: Parte 1

Author

Civico Riccardo, Pucci Stefano, Cinti Francesca Romana, and De Martini Paolo Marco

Subjects
Coseismic ruptures, seismic sequence central Italy 2016, Structure for Motion
Abstract

Costruzione di modelli tridimensionali del terreno tramite tecnica fotogrammetrica (Structure for Motion - SfM) e immagini ortorettificate delle principali aree interessate degli effetti cosismici di superficie relativi agli eventi sismici avvenuti tra il 24 agosto ed il 23 novembre 2016. L’area d’interesse primaria è quella delle sommità morfologiche prive di vegetazione dell’allineamento disposto NO-SE comprendente le vette dei monti Vettore, Argentella, Porche, Bove e Rotondo e, subordinatamente, dei rilievi dei monti Val di Fibbia-Macereto, Cornaccione e Lieto.

Published
2017
Full Text
View/download PDF

28. The first Italian blast-induced liquefaction test (Mirabello, Emilia-Romagna, Italy): description of the experiment and preliminary results

Author

Amoroso, Sara, Milana, Giuliano, Rollins, Kyle M., Comina, Cesare, Minarelli, Luca, Manuel, Maria, R., Monaco, Paola, Franceschini, Marco, Anzidei, Marco, Lusvardi, Cameron, Cantore, Luciana, Carpena, Andrea, Casadei, Stefano, Cinti, Francesca R., Civico, Riccardo, Cox, Brady R., De Martini, Paolo Marco, Di Giulio, Giuseppe, Di Naccio, Deborah, Di Stefano, Giuseppe, Facciorusso, Johann, Famiani, Daniela, Fiorelli, Federico, Fontana, Daniela, Foti, Sebastiano, Madiai, Claudia, Marangoni, Valeria, Marchetti, Diego, Marchetti, Silvano L., Martelli, Luca, Mariotti, Mauro, Muscolino, Elena, Pancaldi, Davide, Pantosti, Daniela, Passeri, Federico, Pesci, Arianna, Romeo, Giovanni, Sapia, Vincenzo, Smedile, Alessandra, Stefani, Marco, Tarabusi, Gabriele, Teza, Giordano, Vassallo, Maurizio, Villani, Fabio, Amoroso S., Milana G., Rollins K.M., Comina C., Minarelli L., Manuel M.R., Monaco P., Franceschini M., Anzidei M., Lusvardi C., Cantore L., Carpena A., Casadei S., Cinti F.R., Civico R., Cox B.R., De Martini P.M., Di Giulio G., Di Naccio D., Di Stefano G., Facciorusso J., Famiani D., Fiorelli F., Fontana D., Foti S., Madiai C., Marangoni V., Marchetti D., Marchetti S.L., Martelli L., Mariotti M., Muscolino E., Pancaldi D., Pantosti D., Passeri F., Pesci A., Romeo G., Sapia V., Smedile A., Stefani M., Tarabusi G., Teza G., Vassallo M., and Villani F.

Subjects
Scale (ratio), liquefaction, Stratigraphy, geotechnical and geophysical surveys, 0211 other engineering and technologies, Emilia-Romagna earthquake, Stratigrafia, 02 engineering and technology, Quaternario, 010502 geochemistry & geophysics, 01 natural sciences, Seismic analysis, Quaternary, Pore water pressure, Seismic Liquefaction, Geotechnical engineering, Fluvia Sedimentation, Geothenics, Geologia, Soil liquefaction, Strain gauge, liquefaction, blast test, geotechnical and geophysical surveys, Emilia-Romagna earthquake, seismic design, 021101 geological & geomatics engineering, 0105 earth and related environmental sciences, Liquefazione Simisca, blast test, Settlement (structural), Po Plain, seismic design, Ambientale, Liquefaction, Geology, Sedimentologia Fluviale, Geologia, Stratigrafia, Geotecnica, Liquefazione Simisca, Quaternario, Sedimentologia Fluviale, Pianura Padana, Geotecnica, Pianura Padana, Geophysics, Soil water, Blast test, Geotechnical and geophysical surveys, Seismic design, Geology, Stratigraphy, Geothenics, Seismic Liquefaction, Quaternary, Fluvia Sedimentation, Po Plain, Geotechnical and geophysical survey
Abstract

Soil liquefaction can result in significant settlement and reduction of load-bearing capacity. Moreover, the increase and the accumulation of pore pressure during an earthquake and its post-seismic dissipation can generate permanent deformations and settlements. The quantitative evaluation of post-liquefaction settlements is of extreme importance for engineering purposes, i.e. for earthquake-resistant design of new buildings and safety evaluation of existing ones. Quantifying the extent of these phenomena is, however, rather difficult. Uncertainties arise from the stochastic nature of the earthquake loading, from the simplifications of soil models, and from the difficulty in establishing correlations between the pre-earthquake soil state and the post-seismic deformations. Field scale liquefaction tests, under controlled conditions, are therefore important for a correct quantification of these phenomena. Recent experiences (e.g. New Zealand, United States) show that liquefaction can be induced and monitored with field scale blast tests to study the related effects on soil geotechnical properties. Within this framework this paper introduces the preliminary results obtained from a research project on blast-induced liquefaction at the field scale; tests were performed at a trial site located in Mirabello (Ferrara, Italy), a village strongly affected by liquefaction phenomena during the 2012 Emilia Romagna earthquake. Invasive tests, such as piezocone, seismic dilatometer and down-hole tests, and non-invasive tests were carried out before and after the execution of two blast test sequences to study the variation in physical properties of the soils. Pore pressure transducers, settlement profilometers, accelerometers and an instrumented micropile were installed with the objective of measuring, during and after the detonations, the generation and subsequent dissipation of the pore pressure, the vertical deformations, and the blast-induced ground motions respectively. Variations in load distribution on deep foundations due to soil liquefaction were also evaluated on a test micropile instrumented with a strain gauge chain. Topographical surveys were carried out to measure ground surface settlements. Laboratory tests and trenches also provided increase understanding of the site characteristics.

Published
2017

29. The first Italian blast-induced liquefaction test 1 (Mirabello, Emilia-Romagna, Italy): description of the experiment and preliminary results

Author

Amoroso, Sara, Milana, Giuliano, Rollins, KYLE M, Comina, Cesare, Minarelli, Luca, Manuel, MARIA R, Monaco, Paola, Franceschini, Marco, Anzidei, Marco, Lusvardi, Cameron, Cantore, Luciana, Carpena, Andrea, Casadei, Stefano, Cinti, FRANCESCA R, Civico, Riccardo, Cox, BRADY R, DE MARTINI, PAOLO MARCO, DI GIULIO, Giuseppe, DI NACCIO, Deborah, DI STEFANO, Giuseppe, Facciorusso, Johann, Famiani, Daniela, Fiorelli, Federico, Fontana, Daniela, Foti, Sebastiano, Madiai, Claudia, Marangoni, Valeria, Marchetti, Diego, Marchetti, SILVANO L, Martelli, Luca, Mariotti, Mauro, Muscolino, Elena, Pancaldi, Davide, Pantosti, Daniela, Passeri, Federico, Pesci, Arianna, Romeo, Giovanni, Sapia, Vincenzo, Smedile, Alessandra, Stefani, Marco, Tarabusi, Gabriele, Teza, Giordano, Vassallo, Maurizio1, and Villani, Fabio

Subjects
Blast test Emilia-Romagna earthquake Geotechnical and geophysical surveys Liquefaction Seismic design
Published
2017

30. GdL ‘’MODELLO DI SOTTOSUOLO SEQUENZA DI AMATRICE’’

Author

Buttinelli, Mauro, Anselmi, Mario, Maesano, Francesco Emanuele, Doglioni, Carlo, Pantosti, Daniela, Di Bucci, Daniela, D'Ambrogi, Chiara, Bigi, Sabina, Improta, Luigi, Scrocca, Davide, Petracchini, Lorenzo, Mariucci, Maria Teresa, De Martini, Paolo Marco, Pucci, Stefano, Billi, Andrea, Ferri, Fernando, Bonini, Lorenzo, Tiberti, Mara Monica, Montone, Paola, Vannoli, Paola, Burrato, Pierfrancesco, Civico, Riccardo, Basili, Roberto, Fracassi, Umberto, Cavinato, Giampaolo, and Moscatelli, Massimiliano

Subjects
3D modelling, dati di sottosuolo, modelli geologici
Abstract

Gruppo composto da ricercatori e tecnologi di diversi enti di ricerca italiani con competenze sull’analisi di dati geologici di superficie e di sottosuolo per la ricostruzione di un modello geologico dell'area interessata dalla sequenza sismica del 24 agosto

Published
2016
Full Text
View/download PDF

31. Abstracts Volume 6th International INQUA Meeting on Paleoseismology, Active Tectonics and Archaeoseismology. 19 | 24 April 2015, Pescina, Fucino Basin, Italy

Author

Blumetti, Anna Maria, Cinti, Francesca Romana, De Martini, Paolo Marco, Galadini, Fabrizio, Guerrieri, Luca, Michetti, Alessandro Maria, Pantosti, Daniela, and Vittori, E. (Eds.)

Abstract

Dear Participant, we are very happy to welcome you in Pescina (Abruzzi, Italy) for the 6th INQUA International Workshop on Active Tectonics, Paleoseismology and Archaeoseismology (“6th PATA Days”). In the last six years, INQUA TERPRO Focus Group on Paleoseismology and Active Tectonics (PALACTE), supported very successful Workshops annually held in Europe and Overseas, the last in Korea in 2014. The 6th joint meeting locates in the central Apennines, one of the most tectonically active area in the Mediterranean. In fact, the scientific sessions will be attended in the Pescina village that was completely destroyed by the 1915 M7 Fucino earthquake, one of the most devastating earthquakes ever occurred in Italy. This event is also one of the first to be well documented in the Mediterranean, with surface ruptures and other effects on the environment. We will commemorate the Centenary of this event occurrence. We will be also very close to the source of the 2009 M6.3 L’Aquila event, located about 50 km to the north. The two-days field trip will be dedicated to both the earthquake areas. We are expecting a very intense and worldwide scientific meeting with over 180 participants from 25 different countries, and about 150 studies to be presented and discussed. All this will occur in the unique historical atmosphere of the ancient Pescina village at the Centro Studi “Ignazio Silone”, a cultural center devoted to the fellow citizen, world-famous writer. During the Fucino 2015 event we will discuss the final results of the INQUA Project 1299 – EEE METRICS Parametrization of Earthquake Environmental Effects (2011-2015) that will be formally presented on July 2015 at the XIX INQUA Congress in Nagoya (Japan). This will be also the occasion to further discuss future joint research projects for the 2015-2019 intercongress period. Two major research areas have been identified in the PALACTE meeting held in Madrid last year (2628 February 2014), i.e., 1) Minimum Magnitude Surface Rupture (MMR) and Maximum Potential Earthquake (MPE) from paleoseismic Quaternary records, and 2) Geological Earthquake Mapping of recent, historical and paleoseismic events: Quaternary Geology for Seismic Hazard Analyses. Preliminary community projects covering these areas will be discussed during the INQUA Business Meeting in Pescina. You are also kindly invited to the workshop between the European Plate Observing System (EPOS, an integrated solid Earth Sciences research infrastructure), and EuroGeoSurveys (EGS, an organization representing 37 National Geological Surveys and some regional Surveys in Europe). During the workshop, an open debate involving the Fucino 2015 participants will be focused on the integration of geological and geophysical data for scientific research purposes, as well as on common data policies in order to access to harmonized multidisciplinary data. We wish to acknowledge all the people who supported this event and in particular, the Mayor of Pescina Municipality Antonio Iulianella and the Comitato Pescina 2015 for their invaluable work with the organization, the members of the Scientific Committee, the Sponsors, and all the Colleagues who handled the abstracts. We wish you a fruitful conference with constructive scientific discussion but also the discovery of history, tradition and food of the Abruzzi region in the central Italy. “GRAZIE” for your contribution to Fucino 2015! The Fucino 2015 Organizing Committee Anna Maria Blumetti Francesca Romana Cinti Paolo Marco De Martini Fabrizio Galadini Luca Guerrieri Alessandro Maria Michetti Daniela Pantosti Eutizio Vittori

Published
2015
Full Text
View/download PDF

32. Deep electrical resistivity tomography along the tectonically active Middle Aterno Valley (2009 L'Aquila earthquake area, central Italy)

Author

Pucci, Stefano, primary, Civico, Riccardo, additional, Villani, Fabio, additional, Ricci, Tullio, additional, Delcher, Eric, additional, Finizola, Anthony, additional, Sapia, Vincenzo, additional, De Martini, Paolo Marco, additional, Pantosti, Daniela, additional, Barde-Cabusson, Stéphanie, additional, Brothelande, Elodie, additional, Gusset, Rachel, additional, Mezon, Cécile, additional, Orefice, Simone, additional, Peltier, Aline, additional, Poret, Matthieu, additional, Torres, Liliana, additional, and Suski, Barbara, additional

Published
2016
Full Text
View/download PDF

33. Imaging the structural style of an active normal fault through multidisciplinary geophysical investigation: a case study from the Mw 6.1, 2009 L'Aquila earthquake region (central Italy)

Author

Villani, Fabio, primary, Pucci, Stefano, additional, Civico, Riccardo, additional, De Martini, Paolo Marco, additional, Nicolosi, Iacopo, additional, D'Ajello Caracciolo, Francesca, additional, Carluccio, Roberto, additional, Di Giulio, Giuseppe, additional, Vassallo, Maurizio, additional, Smedile, Alessandra, additional, and Pantosti, Daniela, additional

Published
2015
Full Text
View/download PDF

34. The L'Aquila trial

Author

Cocco, Massimo, primary, Cultrera, Giovanna, additional, Amato, Alessandro, additional, Braun, Thomas, additional, Cerase, Andrea, additional, Margheriti, Lucia, additional, Bonaccorso, Alessandro, additional, Demartin, Martina, additional, De Martini, Paolo Marco, additional, Galadini, Fabrizio, additional, Meletti, Carlo, additional, Nostro, Concetta, additional, Pacor, Francesca, additional, Pantosti, Daniela, additional, Pondrelli, Silvia, additional, Quareni, Francesca, additional, and Todesco, Micol, additional

Published
2015
Full Text
View/download PDF

35. Integrating new and traditional approaches for the estimate of slip-rates of active faults: examples from the Mw 6.3, 2009 L’Aquila earthquake area, Central Italy

Author

De Martini, Paolo Marco, Civico, Riccardo <1980>, De Martini, Paolo Marco, and Civico, Riccardo <1980>

Abstract

This thesis is based on the integration of traditional and innovative approaches aimed at improving the normal faults seimogenic identification and characterization, focusing mainly on slip-rate estimate as a measure of the fault activity. The L’Aquila Mw 6.3 April 6, 2009 earthquake causative fault, namely the Paganica - San Demetrio fault system (PSDFS), was used as a test site. We developed a multidisciplinary and scale‐based strategy consisting of paleoseismological investigations, detailed geomorphological and geological field studies, as well as shallow geophysical imaging and an innovative application of physical properties measurements. We produced a detailed geomorphological and geological map of the PSDFS, defining its tectonic style, arrangement, kinematics, extent, geometry and internal complexities. The PSDFS is a 19 km-long tectonic structure, characterized by a complex structural setting and arranged in two main sectors: the Paganica sector to the NW, characterized by a narrow deformation zone, and the San Demetrio sector to SE, where the strain is accommodated by several tectonic structures, exhuming and dissecting a wide Quaternary basin, suggesting the occurrence of strain migration through time. The integration of all the fault displacement data and age constraints (radiocarbon dating, optically stimulated luminescence (OSL) and tephrochronology) helped in calculating an average Quaternary slip-rate representative for the PSDFS of 0.27 - 0.48 mm/yr. On the basis of its length (ca. 20 km) and slip per event (up to 0.8 m) we also estimated a max expected Magnitude of 6.3-6.8 for this fault. All these topics have a significant implication in terms of surface faulting hazard in the area and may contribute also to the understanding of the PSDFS seismic behavior and of the local seismic hazard.

Published
2012

41. A continuous palaeosecular variation record of the last four millennia from the Augusta Bay (Sicily, Italy).

Author

Sagnotti, Leonardo, Smedile, Alessandra, De Martini, Paolo Marco, Pantosti, Daniela, Speranza, Fabio, Winkler, Aldo, Carlo, Paola Del, Bellucci, Luca Giorgio, and Gasperini, Luca

Subjects
DIURNAL variations of geomagnetism, SEA level, HIGH resolution imaging, GEOPHYSICS, SEQUENCE stratigraphy, ANTHROPOGENIC effects on nature
Abstract

We present a high-resolution palaeomagnetic and rock magnetic study of two cores, MS06 and MS06-SW (6.7 and 1.1 m long, respectively), collected at 72 m below sea level in the Augusta Bay shelf (Eastern Sicily, Ionian Sea, Italy) about 2.3 km from the coastline. Geophysical surveying carried out in the sampling area highlighted the presence of a homogeneous sedimentary sequence that most likely was deposited after the Last Glacial Maximum and was not affected by anthropogenic disturbances. The two cores penetrated a monotonous mud sedimentary sequence, interrupted at ∼3 m depth by a 3-4-cm-thick volcanic sandy layer that is correlated with the tephra fallout deposit produced by the 122 BC plinian eruption of Mt Etna. This tephra, along with radiocarbon dating of nine marine shells and with radioactive tracers for the uppermost 0.3 m (Pb and Cs), provide the chronological constraints for the stratigraphic sequence that resulted younger than 4500 yr BP. Palaeomagnetic and rock magnetic data show that the sample sequence is magnetically homogeneous. A single peak of high magnetic mineral concentration is present and corresponds to the volcanic sandy layer. Palaeomagnetic data allowed the identification of a well-defined characteristic remanent magnetization that provides a high-resolution record of palaeosecular variation (PSV) at the sampling site. The reconstructed PSV curve is in good agreement with the available regional reference PSV curves and with the prediction from recent PSV modelling for Europe. The palaeomagnetic data obtained in this study on the one hand support and refine the age model for the cores, derived from other independent constraints, and on the other hand provide an original high-resolution PSV curve that can serve as a reference for the central Mediterranean over the last 4 ka. [ABSTRACT FROM AUTHOR]

Published
2011
Full Text
View/download PDF

42. Discrimination of Tsunami Sources (Earthquake versus Landslide) on the Basis of Historical Data in Eastern Sicily and Southern Calabria.

Author

Gerardi, Flavia, Barbano, Maria Serafina, De Martini, Paolo Marco, and Pantosti, Daniela

Subjects
TSUNAMIS, OCEAN waves, EARTHQUAKES, SHORELINES
Abstract

The source mechanisms responsible for large historical tsunamis that have struck eastern Sicily and southern Calabria are a topic of robust debate. We have compiled a database of historical coeval descriptions of three large tsunamis: 11 January 1693, 6 February 1783, and 28 December 1908. By using accounts of run-up and inundation and employing an approach proposed by Okal and Synolakis in 2004, we can provide discriminants to define the nature of the near-field tsunami sources (fault dislocation or landslide). Historical reports for the 1908 event describe affected localities, maximum run-ups, and inundation areas. However, for the 1693 and 1783 tsunamis, reports are limited to inundation and occasional run-up estimates. We calculate run-up values for these events using available relations between inundation and run-up. We employed the model of Okal and Synolakis to the obtained profiles of tsunami run-up along the inundated shorelines. The 1908 run-up data distribution confirms that the tsunami is compatible with a seismic dislocation source, whereas the 1783 data supports contemporary observations and recent offshore investigations suggesting that the tsunami was produced by an earthquake-triggered submarine landslide. Analysis of the 1693 event data suggests that the tsunami was generated during a tectonic event and thus a seismogenic source should be found offshore. [ABSTRACT FROM AUTHOR]

Published
2008
Full Text
View/download PDF

43. Geomorphological, paleontological and 87Sr/86Sr isotope analyses of early Pleistocene paleoshorelines to define the uplift of Central Apennines (Italy)

Author

Mancini, Marco, D'Anastasio, Elisabetta, Barbieri, Mario, and De Martini, Paolo Marco

Subjects
RIVERS, GEOMORPHOLOGY, STRATIGRAPHIC geology
Abstract

Abstract: The eastern border of the Middle Valley of the Tiber River is characterized by several Plio-Pleistocene paleoshorelines, which extend for about 100 km along the western margin of the Central Apennines (Italy). We studied these paleoshorelines by the means of geological and paleontological analyses and new 87Sr/86Sr isotope analyses. The youngest and uppermost paleoshorelines have been detected and mapped through detailed geologic and stratigraphic surveys, which led to the recognition of nearshore deposits, cliff breccias, alignments of Lithophaga borings, fossil abrasion notches and wave-cut platforms. The altitude of these paleoshorelines decreases almost regularly in the NNW–SSE direction from 480 to 220 m a.s.l. Measurements of the 87Sr/86Sr isotope ratio have been conducted on corals and mollusks collected from sediments outcropping close to the paleoshorelines. The isotopic dating results indicate numerical values that range between 0.70907 and 0.70910 all over the 100-km outcrop. These results, together with biostratigraphic data, constrain the age of the youngest paleoshorelines to 1.65–1.50 Ma. These paleoshorelines are thus considered almost isochronous, giving an estimated uplift rate of 0.34–0.17±0.03 mm/a moving from NNW to SSE. Shape, length and continuity of the 100-km-long observed movements indicate that the studied paleoshorelines are an important marker of the Quaternary uplift of the Central Apennines. [Copyright &y& Elsevier]

Published
2007
Full Text
View/download PDF

44. Geodetic and seismologic evidence for slip variability along a blind normal fault in the Umbria-Marche 1997–1998 earthquakes (central Italy).

Author

De Martini, Paolo Marco, Pino, Nicola Alessandro, Valensise, Gianluca, and Mazza, Salvatore

Subjects
*EARTHQUAKES, *GEODESY, *SEISMOLOGY
Abstract

We analysed elevation changes induced by the 1997–1998 Umbria-Marche, central Apennines (Italy) earthquakes. We employed data from a first-order geodetic levelling line measured in 1951, 1992 and 1998. The line bears a record of pre-seismic and coseismic strains associated with the causative fault of the 1997 September 26, 09:40 mainshock . A first level analysis performed under the assumption of slip homogeneity of coseismic slip shows misfits that cannot be reduced simply by altering the fault size and geometry. A more detailed analysis based on a distribution of coseismic slip obtained from broad-band seismograms provides a better fit and is in agreement with 1951–1992 elevation changes interpreted as precursory slip by previous investigators. The levelling data sets new constraints on the location, extent, dip and depth of the fault, in full agreement with seismological evidence and images from SAR interferometry. The data show no evidence for slip in the uppermost 3 km of the crust, suggesting that a major and widely recognized normal fault that exists in the area is no longer active and showing a tendency of present tectonic strains to revert the current topographic setting. [ABSTRACT FROM AUTHOR]

Published
2003
Full Text
View/download PDF

45. High‐Resolution Seismic Profiling in the Hanging Wall of the Southern Fault Section Ruptured During the 2016 Mw6.5 Central Italy Earthquake

Author

Villani, Fabio, Maraio, Stefano, Bruno, Pier Paolo, Improta, Luigi, Wood, Kieran, Pucci, Stefano, Civico, Riccardo, Sapia, Vincenzo, De Martini, Paolo Marco, Brunori, Carlo Alberto, Doglioni, Carlo, and Pantosti, Daniela

Abstract

The Vettore–Bove normal fault system in central Italy ruptured during the 2016 MW6.5 Norcia earthquake causing extensive surface faulting. At the Pian Grande di Castelluccio hanging wall basin, along the southern section of the fault ruptured during the MW6.5 mainshock, we performed a high‐resolution seismic reflection/refraction experiment aimed at (a) imaging the shallow pattern of the fault system, and (b) reconstructing the architecture of the continental infill. We collected three profiles for a total length of ∼8 km. We used a reflection processing flow and non‐linear refraction tomography to obtain migrated stack sections and P‐wave velocity images resolved down to the depth of the pre‐Quaternary substratum. The main profile in the northern part of the basin crosses the westernmost splays of the ruptured fault zone striking N150°–170°. Seismic imaging unravels a ∼1 km‐wide fault zone comprising three W‐throwing splays and subsidiary faults, which affect the continental infill and produce a minimum aggregate Quaternary throw of ∼400 ± 100 m. Recent deformation is localized in this part of the surveyed fault section, attesting active displacement accumulation of the Vettore–Bove fault system. The other profiles in the central‐southern part of the basin show additional faults, likely striking N20°–40° and which concurred to generate a ∼500 m‐deep depocenter. These faults were mostly active during an early extensional phase; however, one of them likely displaces shallow layers with a throw close to the resolution limit of seismic data (<10 m), suggesting activity in the Late Pleistocene. Three high resolution seismic profiles image the hanging wall of southern part of the 2016 MW6.5 central Italy earthquake fault zoneThe surveyed ∼1 km‐wide hidden fault section displays three active W‐dipping splays with a minimum aggregate Quaternary throw of ∼400 mP‐wave velocity tomographic images and migrated sections depict a ∼500 m‐deep Quaternary depocenter in the earthquake fault hanging wall Three high resolution seismic profiles image the hanging wall of southern part of the 2016 MW6.5 central Italy earthquake fault zone The surveyed ∼1 km‐wide hidden fault section displays three active W‐dipping splays with a minimum aggregate Quaternary throw of ∼400 m P‐wave velocity tomographic images and migrated sections depict a ∼500 m‐deep Quaternary depocenter in the earthquake fault hanging wall

Published
2021
Full Text
View/download PDF

47. Progetto RETRACE-3D - centRal italy EarThquakes integRAted Crustal modEl - Rapporto Finale

Author

RETRACE-3D Working Group, Buttinelli, Mauro, Di Bucci, Daniela, D'Ambrogi, Chiara, Scrocca, Davide, Maesano, Francesco, Petracchini, Lorenzo, Basili, Roberto, Cara, Pierluigi, Castenetto, Sergio, Giuliani, Roberta, Salvi, Ilaria, Bigi, Sabina, Cavinato, Gian Paolo, Di Filippo, Michele, Messina, Paolo, Castaldo, Raffaele, De Novellis, Vincenzo, Pepe, Susi, Solaro, Giuseppe, Tizzani, Pietro, Anzidei, Marco, Bignami, Christian, Bonini, Lorenzo, Burrato, Pierfrancesco, Cheloni, Daniele, Chiappini, Massimo, Cinti, Francesca, De Gori, Pasquale, De Martini, Paolo Marco, Devoti, Roberto, Di Naccio, Deborah, Di Nezza Maria, Falcucci, Emanuela, Fracassi, Umberto, Galadini, Fabrizio, Gori, Stefano, Improta, Luigi, Kastelic, Vanja, Marchetti, Marco, Mariucci, Maria Teresa, Minelli, Liliana, Montone, Paola, Moro, Marco, Pantosti, Daniela, Pignatelli, Alessandro, Sapia, Vincenzo, Saroli, Michele, Tertulliani, Andrea, Tiberti, Mara, Vallone, Roberto, Vannoli, Paola, Villani, Fabio, Bonomo, Roberto, Calcaterra, Stefano, Congi, Maria Pia, Capotorti, Franco, Di Manna, Pio, Ferri, Fernando, Gambino, Piera, Marino Maurizio, and Ventura, Renato

Subjects
Central Apennines, Appennino centrale, 3D geological model, 2016 seismic sequence, Sequenza sismica 2016, Sismotettonica, Seismotectonics, Modello geologico 3D
Abstract

Il progetto RETRACE-3D (centRal italy EarThquakes integRAted Crustal modEl) è volto alla caratterizzazione tridimensionale, geologica e sismotettonica, del volume di crosta terrestre che a partire dal 24 agosto 2016 è stato interessato dai terremoti di Amatrice, Visso e Norcia, e dalla relativa sequenza sismica. Il progetto è il risultato di una collaborazione tra il Dipartimento della Protezione Civile, l’Istituto Nazionale di Geofisica e Vulcanologia (INGV), il Consiglio Nazionale delle Ricerche che partecipa con l’Istituto di Geologia Ambientale e Geoingegneria (CNR-IGAG) e l’Istituto per il Rilevamento Elettromagnetico dell’Ambiente (CNR-IREA) e l’Istituto Superiore per la Protezione e la Ricerca Ambientale (ISPRA), con la collaborazione di Eni e Total, realtà private ma anch’esse parte del Servizio nazionale della Protezione Civile, che hanno messo a disposizione i propri dati di sottosuolo. La finalità principale del progetto è stata ricostruire un quadro 3D di alta qualità della distribuzione dei diversi tipi di rocce nel sottosuolo in questa porzione di Appennino centralee delle possibili sorgenti sismogenetiche presenti in quel settore di crosta terrestre. Il progetto RETRACE-3D è stata un’occasione di lavoro multidisciplinare unica nel suo genere, alla quale hanno partecipato esperte ed esperti del Dipartimento della Protezione Civile e ricercatrici e ricercatori appartenenti ai Centri di Competenza del Dipartimento stesso, contribuendo al miglioramento delle conoscenze sui terremoti e ad una migliore valutazione della pericolosità sismica del territorio italiano. I percorsi di lavoro seguiti e le collaborazioni sviluppate all’interno del progetto sono da considerarsi di valore confrontabile con i risultati scientifici ottenuti, esi intende sottolineare come esperienze positive e propositive come quelle realizzate nel progetto RETRACE-3Dpossano costituire, in futuro, uno standard di azione e interazione tra i singoli ricercatori di diverse Istituzioni scientifiche e gli esperti del Dipartimento della Protezione Civile, anche al di fuori delle fasi emergenziali e post-emergenziali di una sequenza sismica. Il presente Rapporto finale è frutto dell’attività e dell’opinione degli autori. I contenuti non rappresentano necessariamente l’opinione generale delle istituzioni di cui i singoli autori fanno parte. La proprietà intellettuale dei risultati qui riportati è degli autori. Sebbene sia stato fatto ogni sforzo possibile per integrare i dati disponibili, non viene fornita alcuna garanzia, esplicita o implicita, in merito all'accuratezza e all'affidabilità dei dati forniti in RETRACE-3D GEOMOD. Gli utenti sono invitati a considerare l'incertezza epistemica intrinseca di tale prodotto per ogni suo possibile utilizzo e a tenere conto che il modello ha una scala equivalente a 1:250.000. RETRACE-3D GEOMOD è stato progettato per analisi a scala regionale; per studi e utilizzi diversi, a scale più locali (dettaglio superiore alla scala 1:250.000), andranno previste da parte degli utilizzatori indagini locali e sito specifiche. Gli utenti sono invitati a considerare attentamente la natura e la scala del contenuto di RETRACE-3D GEOMOD prima qualunque utilizzo. Gli autori di RETRACE-3D GEOMOD non sono responsabili per utilizzi diversi da quelli dichiarati.

Published
2021
Full Text
View/download PDF

48. New insights into active tectonics and seismogenic potential of the Italian Southern Alps from vertical geodetic velocities

Author

Letizia Anderlini, Enrico Serpelloni, Cristiano Tolomei, Paolo Marco De Martini, Giuseppe Pezzo, Adriano Gualandi, Giorgio Spada, Anderlini, Letizia, Serpelloni, Enrico, Tolomei, Cristiano, De Martini, Paolo Marco, Pezzo, Giuseppe, Gualandi, Adriano, Spada, Giorgio, ARAG - AREA FINANZA E PARTECIPATE, DIP. DI FISICA, DIP. DI SCIENZE DELLA TERRA E GEOLOGICO-AMBIENTALI, and DIPARTIMENTO DI FISICA E ASTRONOMIA 'AUGUSTO RIGHI'

Subjects
Horizontal and vertical, Stratigraphy, EASTERN ALPS, Soil Science, SURFACE DEFORMATION, Fault (geology), Induced seismicity, FAULT SLIP DISTRIBUTION, LAGOON-OF-VENICE, 1989 LOMA-PRIETA, INTERSEISMIC DEFORMATION, CRUSTAL DEFORMATION, LATERAL EXTRUSION, EUROPEAN ALPS, PO PLAIN, lcsh:Stratigraphy, Geochemistry and Petrology, Interferometric synthetic aperture radar, Glacial period, lcsh:QE640-699, Earth-Surface Processes, geography, geography.geographical_feature_category, lcsh:QE1-996.5, Front (oceanography), Paleontology, Geodetic datum, Geology, Geodesy, lcsh:Geology, Tectonics, Geophysics
Abstract

open 7 no This study presents and discusses horizontal and vertical geodetic velocities for a low strain rate region of the south Alpine thrust front in northeastern Italy obtained by integrating GPS, interferometric synthetic aperture radar (InSAR) and leveling data. The area is characterized by the presence of subparallel, south-verging thrusts whose seismogenic potential is still poorly known. Horizontal GPS velocities show that this sector of the eastern Southern Alps is undergoing ∼1 mm a−1 of NW–SE shortening associated with the Adria–Eurasia plate convergence, but the horizontal GPS velocity gradient across the mountain front provides limited constraints on the geometry and slip rate of the several subparallel thrusts. In terms of vertical velocities, the three geodetic methods provide consistent results showing a positive velocity gradient, of ∼ 1.5 mm a−1, across the mountain front, which can hardly be explained solely by isostatic processes. We developed an interseismic dislocation model whose geometry is constrained by available subsurface geological reconstructions and instrumental seismicity. While a fraction of the measured uplift can be attributed to glacial and erosional isostatic processes, our results suggest that interseismic strain accumulation at the Montello and the Bassano–Valdobbiadene thrusts it significantly contributing to the measured uplift. The seismogenic potential of the Montello thrust turns out to be smaller than that of the Bassano–Valdobbiadene fault, whose estimated parameters (locking depth equals 9.1 km and slip rate equals 2.1 mm a−1) indicate a structure capable of potentially generating a Mw>6.5 earthquake. These results demonstrate the importance of precise vertical ground velocity data for modeling interseismic strain accumulation in slowly deforming regions where seismological and geomorphological evidence of active tectonics is often scarce or not conclusive. Financial support. Letizia Anderlini is supported by INGV-MISE-DGS 2018 project funded by the Italian Ministry of the Economic Development. Giorgio Spada is funded by a FFABR (Finanziamento delle Attività Base di Ricerca) grant from MIUR (Ministero dell'Istruzione, dell'Università e della Ricerca), and by a DiSPeA research grant. This study has been partially supported by the project TRANSIENTI, by the MIUR “Premiale 2014” project, by the Italian Presidenza del Consiglio dei Ministri, Dipartimento di Protezione Civile (project no. S1 2013–2014 INGV-DPC agreement), and by the MIUR “Pianeta Dinamico” institutional project. open Anderlini, Letizia; Serpelloni, Enrico; Tolomei, Cristiano; De Martini, Paolo Marco; Pezzo, Giuseppe; Gualandi, Adriano; Spada, Giorgio Anderlini, Letizia; Serpelloni, Enrico; Tolomei, Cristiano; De Martini, Paolo Marco; Pezzo, Giuseppe; Gualandi, Adriano; Spada, Giorgio

Published
2020

Catalog

Books, media, physical & digital resources
See catalog results