Combining 3-D Deep Electrical Resistivity Tomography With Magnetic Surveys to Investigate Complex Tectonic Basins: A Case Study From the Central Apennines Seismic Belt (Italy) V. Sapia, F. Villani, L. Improta, F. Fischanger, P. M. De Martini, V. Romano, V. Materni, P. Baccheschi, A. Smedile, I. Nicolosi, L. Minelli, F. D’Ajello Caracciolo, R. Carluccio, S. Maraio, G. Di Giulio, L. Ruggiero, A. Sciarra, D. Pantosti, M. Pischiutta, T. Ricci, R. Civico, M. Vassallo, C. A. Brunori, M. Lupi Tectonics, 2025 We use an innovative geophysical approach to reconstruct the deep structure of Campo Felice, an important extensional basin in the central Apennines (Italy) where active crustal extension is accommodated by normal faults capable of generating earthquakes of magnitude MW 6+. To this end, we combine 3‐D Deep Electrical Resistivity Tomography with Unmanned Aerial Vehicle aeromagnetic survey. Before this study, the knowledge of the subsurface was limited to a small sector of the basin investigated by two seismic reflection profiles and shallow scientific drillings. Our resistivity model unravels for the first time a complex subsurface structure, due to two SW‐dipping and left‐stepping normal faults (Mt Cefalone‐Serralunga and Mt Orsello), with antithetic and relay faults. Altogether, they favored the generation of two distinct sub‐basins ∼400–450 and ∼250–300 m‐deep, filled with alluvial, lacustrine and glacial deposits. Aeromagnetic data further constrain the extent and thickness of fine‐grained infill sediments, while previous drillings and seismic reflection profiles are useful to constrain geological interpretation. We provide a model of basin evolution covering approximately the last million years, improving the knowledge of the Quaternary kinematics and structure of this sector of the chain. Furthermore, this cost‐effective approach can be safely exported to similar tectonic contexts elsewhere.
Subsurface characterization of crystalline rocks at the Einstein Telescope candidate site (Italy): Insights from seismic tomography, geoelectrical and morphostructural analyses F. Villani, S. Maraio, L. Improta, P.M. De Martini, D. Cavallaro, M. Firetto Carlino, C.A. Brunori, V. Longo, L. Casini, M.C. Caradonna, C. Zei, S. Rapisarda, G. Oggiano, C. Giunchi, G. Saccorotti, M. Coltelli, D. D'Urso, L. Naticchioni, F. Ricci, G. Schillaci, D. Cittadino, M. Marsella, Q. Napoleoni, C. Rossini, G.L. Cardello Tectonophysics, 2025 The Einstein Telescope (ET) will be the first European underground observatory of gravitational waves. The observatory's interferometric detectors will be housed in a large underground infrastructure,which necessitates a stable and quiet geological context. We present the results of a geognostic campaign conducted for the Italian candidate site in Sardinia, during which two ~270 m-deep boreholes were drilled in granites and orthogneiss at two sites that are possible locations of the ET infrastructure. We acquired high-resolution, dense seismic and electrical resistivity tomography (ERT) profiles to complement borehole data, constraining the thickness of the weathered layer and characterizing the rock properties in terms of intact versus fractured zones down to depths of 100–240 m. At depths >50 m, we observed high P-wave velocity (Vp ~ 5000–5500 m/s, while very high Vp (~6000 m/s) paired with very high resistivity (ρ > 1000 Ωm) was found at depths of 150–200 m, suggesting unfractured or weakly fractured rocks consistent with borehole logs and literature data on geophysical surveys on crystalline rocks. We recognized a couple of sub-vertical low-Vp (~4250–4500 m/s) and low-resistivity anomalies (ρ < 500 Ωm), up to ~15–35 m-wide, suggesting the occurrence of fracture zones with groundwater, matching the intersection with fault zones mapped at the surface. Comparison with co-located resistivity sections, downhole seismic surveys, well logs, and field-based structural and morphostructural analyses allowed us to attribute these anomalies to fault zones ~0.3–0.5 km-long that belong to an immature fault network with shallow water circulation. This methodological approach highlights the utility of tomographic techniques combined with structural investigations and represents a guideline that can be applied in similar contexts characterized by poorly fractured crystalline rocks.
Multi-Temporal Relative Sea Level Rise Scenarios up to 2150 for the Venice Lagoon (Italy) Marco Anzidei, Cristiano Tolomei, Daniele Trippanera, Tommaso Alberti, Alessandro Bosman, Carlo Alberto Brunori, Enrico Serpelloni, Antonio Vecchio, Antonio Falciano, Giuliana Deli Remote Sensing, 2025 The historical City of Venice, with its lagoon, has been severely exposed to repeated marine flooding since historical times due to the combined effects of sea level rise (SLR) and land subsidence (LS) by natural and anthropogenic causes. Although the sea level change in this area has been studied for several years, no detailed flooding scenarios have yet been realized to predict the effects of the expected SLR in the coming decades on the coasts and islands of the lagoon due to global warming. From the analysis of geodetic data and climatic projections for the Shared Socioeconomic Pathways (SSP1-2.6; SSP3-7.0 and SSP5-8.5) released in the Sixth Assessment Report (AR6) of the Intergovernmental Panel on Climate Change (IPCC), we estimated the rates of LS, the projected local relative sea level rise (RSLR), and the expected extent of flooded surfaces for 11 selected areas of the Venice Lagoon for the years 2050, 2100, and 2150 AD. Vertical Land Movements (VLM) were obtained from the integrated analysis of Global Navigation Satellite System (GNSS) and Interferometry Synthetic Aperture Radar (InSAR) data in the time spans of 1996–2023 and 2017–2023, respectively. The spatial distribution of VLM at 1–3 mm/yr, with maximum values up to 7 mm/yr, is driving the observed variable trend in the RSLR across the lagoon, as also shown by the analysis of the tide gauge data. This is leading to different expected flooding scenarios in the emerging sectors of the investigated area. Scenarios were projected on accurate high-resolution Digital Surface Models (DSMs) derived from LiDAR data. By 2150, over 112 km2 is at risk of flooding for the SSP1-2.6 low-emission scenario, with critical values of 139 km2 for the SSP5-8.5 high-emission scenario. In the case of extreme events of high water levels caused by the joint effects of astronomical tides, seiches, and atmospheric forcing, the RSLR in 2150 may temporarily increase up to 3.47 m above the reference level of the Punta della Salute tide gauge station. This results in up to 65% of land flooding. This extreme scenario poses the question of the future durability and effectiveness of the MoSE (Modulo Sperimentale Elettromeccanico), an artificial barrier that protects the lagoon from high tides, SLR, flooding, and storm surges up to 3 m, which could be submerged by the sea around 2100 AD as a consequence of global warming. Finally, the expected scenarios highlight the need for the local communities to improve the flood resiliency plans to mitigate the consequences of the expected RSLR by 2150 in the UNESCO site of Venice and the unique environmental area of its lagoon.
Relative Sea Level Rise Projections Up to 2150 Along the Italian Coasts From Geodesy, High Resolution Topography and Climatic Projections Marco Anzidei, Daniele Trippanera, Alessandro Bosman, Carlo Alberto Brunori, Tommaso Alberti, Antonio Vecchio, Enrico Serpelloni, Cristiano Tolomei, Francesca Iacono, Marina Bisson Proceedings of the International Conference on Electromagnetics in Advanced Applications Iceaa, 2025 Sea level change along the coast is caused by vertical land movements (VLM), changes in the ocean volume and additional factors. Space based observations from Synthetic Aperture Radar (SAR) satellites, combined with ground observations from GNSS data, are crucial to estimate the current rates of VLM and, in combination with climatic data, relative sea level rise projections (RSLR) along the coasts. Here we focus on the Mediterranean basin and especially on the Italian coasts, which are affected by spatially variable VLM, to estimate the RSLR projections and flooding scenarios up to 2150 AD. For the Italian region, we estimated the current and expected RSLR trend at <tex xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">$\mathbf{2 0 3 0}-\mathbf{2 0 5 0}-\mathbf{2 1 0 0}$</tex> and <tex xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">$\mathbf{2 1 5 0}$</tex> for <tex xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">$\mathbf{3 9}$</tex> main coastal plains which are yet exposed to coastal hazard. Geodetic data consist in about 27 years of continuous GNSS observations at selected stations located within 5 km from the coast and InSAR data from the Copernicus European Ground Motion Service (https://egms.land.copernicus.eu/). The latter were integrated with additional InSAR data sets to extend to past years the data time series at specific sites, such as for the Venice lagoon. Finally, we provide revised sea level rise projections for the selected coastal plains of the Italian region by including VLM in the analysis. Scenarios are based on the IPCC-AR6 Report for different Shared Socio-economic Pathways (SSP) and global warming levels (www.ipcc.ch). In the analysis, we also considered the SL data recorded at the operational tidal networks managed by the PSMSL (https://psmsl.org) and ISPRA (https://www.mareografico.it/). Our analysis show that IPCC often underestimate the projected SLR since the current VLM rates are neglected or not adequately considered. Finally, detailed maps of the expected flooding scenarios for 39 Italian coastal plains projected on high resolution DEM obtained by the analysis of LiDAR data or low elevated aerial photogrammetry surveys by UAVs, are provided. In addition, more 65 exposed coastal zones in the Mediterranean were identified through a geoprocessing analysis, highlighting about <tex xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">$10,000\ \text{km}^{2}$</tex> of the Italian coasts yet exposed to multiple hazard and about <tex xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">$38,500\ \text{km}^{2}$</tex> in the Mediterranean. Based on these scenarios, adaptation measures to face the ongoing RSLR, are required.
The NE-SW Sibari fault zone: A seismic hazard source in Ionian Northern Calabria (Italy) F.R. Cinti, L. Alfonsi, L. Cucci, D. Pantosti, C. Pauselli, M. Ercoli, C.A. Brunori, G. Cianflone, R. Dominici Tectonophysics, 2024 A multidisciplinary approach including archaeological, geophysical, and geological/geomorphological surveys provided pieces of evidence that allowed us to identify the Sibari fault zone (SFZ) in Northern Calabria (Italy). The SFZ runs in a ~ NE-SW direction for a length of ~18 km from the Ionian coastline to Terranova da Sibari and has an oblique normal-dextral kinematics. The envelope of the SFZ is derived from several direct and indirect evidence resulting in subparallel and locally en-echelon fault traces over a maximum 500 m-wide band, running at different elevations across hills and flat lands. The SFZ was active since at least the Middle-Upper Pleistocene, producing faulting of alluvial deposits, marine terraces, drainage incisions, and the archaeological structures of Sybaris. Given the fault length and assuming a seismogenic behavior, the SFZ is a primary earthquake source possibly producing moderate to large earthquakes (M ≥ 6). We calculated the average slip rates along the SFZ based on the ages and on the accumulated displacements of offset streams and marine terraces. The estimates are of 0.05–0.18 mm/yr and 0.41–0.70 mm/yr for vertical and dextral slip, respectively. Based on both the measured (min. 30 cm) and the expected value (av. 40 cm) of lateral slip per event, we infer an average recurrence for surface faulting events on the SFZ of about 700–1000 yrs. The most recent surface faulting earthquake occurred on the fault is dated 1300–1100 yrs. ago, highlighting that the elapsed time approaches the estimated average recurrence. Considering these findings, the newly recognized SFZ should be included among the faults that contain a potential seismic hazard in this poorly known portion of the Ionian sector of northern Calabria.
High-resolution geophysical investigations in the central Apennines seismic belt (Italy): Results from the Campo Felice tectonic basin F. Villani, S. Maraio, L. Improta, V. Sapia, G. Di Giulio, P. Baccheschi, M. Pischiutta, M. Vassallo, V. Materni, P.P. Bruno, C.A. Brunori, R. Civico, A. D'Alessandro, C. Felicetta, S. Lovati, T. Ricci, S. Scudero, P.M. De Martini Tectonophysics, 2024 The Campo Felice basin, in the central Apennines seismic belt (Italy), developed in the hangingwall of a 30 km-long system of NW-trending normal faults with Holocene paleoseismic activity and potential sources of M6–7 earthquakes. We provide the first subsurface images of a key portion of the basin bounded by the Mt. Cefalone fault along two intersecting profiles trending NNE-SSW (CF-Dip, 1195 m-long) and WNW-ESE (CF-Strike, 1315-m long). We combined high-resolution depth-migrated reflection sections with P-wave velocity and electrical resistivity tomography models. CF-Dip profile displays a wedge-like syn-tectonic sedimentary sequence of alluvial and glacial deposits with Vp ~ 2500–3000 m/s and resistivity > 500 Ωm in the hangingwall of Mt. Cefalone fault, overlying a high-Vp (>4000 m/s) limestone bedrock ~ 300 m deep. The whole sequence displays reflectors truncated by the Mt. Cefalone fault zone and subsidiary antithetic faults. CF-Strike profile, tied to three 80–110 m-deep boreholes, shows a thick fluvio-lacustrine sequence with low-Vp (<2000 m/s) and low resistivity (<100 Ωm), and a bedrock that deepens to the southeast (>450 m). Single-station ambient noise measurements display Horizontal to Vertical Spectral Ratios with peaks at ~1 Hz, decreasing to ~0.8 Hz to the southeast in agreement with the bedrock deepening indicated by seismic profiling. According to our results, the Campo Felice basin is a deep asymmetric half-graben controlled by faulting whose activity likely started before the Middle Pleistocene. Our minimum displacement estimate accrued in the past 0.5 Ma by the Mt. Cefalone fault is in the range of ~100–250 m.
High-Resolution Seismic Imaging of Active Faults and Tectonic Basins in the Central Apennines Seismic Belt (Italy) S. Maraio, L. Improta, F. Villani, P.M. De Martini, V. Sapia, P.P. Bruno, and 6th Asia Pacific Meeting on Near Surface Geoscience and Engineering Smart Technologies Kind to the Planet, 2024 Summary The Central Apennines in Italy exhibit geological complexity due to polyphase tectonic activity. As a well-known example of a Tertiary fold-and-thrust belt in the active Mediterranean region, the Apennines underwent post-orogenic extensional tectonics from late Pliocene to the present. This prolonged extensional activity shaped the landscape, forming extensional basins related to normal fault activity. These basins are important archives for understanding the region’s tectonic evolution, crucial for assessing earthquake hazards in an area prone to M6-7 earthquakes. Geophysical imaging, particularly high resolution seismic reflection profiling, plays a key role in understanding subsurface structures. Combining reflection and refraction seismic methods proves advantageous for shallow imaging of complex structures like tectonic basin, since tomographic velocity models aid lithological classification and interpretation of seismic images. This contribution presents two case studies using high-resolution seismic imaging in the Campo Felice and Fucino basins, focusing on basin architecture, fault geometries, sedimentary infill, and evolution. The study aims to highlight differences in results quality between basins with distinct geological settings, emphasizing the imaging of active faults. The presented seismic sections offer insights into the subsurface structures of Mt. Cefalone, San Benedetto, and Trasacco faults.
Spatiotemporal Evolution of Ground Subsidence and Extensional Basin Bedrock Organization: An Application of Multitemporal Multi-Satellite SAR Interferometry Carlo Alberto Brunori, Federica Murgia Geosciences Switzerland, 2023 Since the early 1990s, the European (ESA) and Italian (ASI) space agencies have managed and distributed a huge amount of satellite-recorded SAR data to the research community and private industries. Moreover, the availability of advanced cloud computing services implementing different multi-temporal SAR interferometry techniques allows the generation of deformation time series from massive SAR images. We exploit the information provided by a large PS dataset to determine the temporal trend of ground deformation and the relative deformation rate with millimetric accuracy to analyze the spatial and temporal distribution of land subsidence induced by water pumping from a deep confined aquifer in the Northern Valle Umbra Basin (Central Italy), exploiting 24 years of Permanent Scatterers—interferometric SAR data archives. The SAR images were acquired between 1992 and 2016 by satellites ERS1/2 and ENVISAT, the Sentinel 1 ESA missions and the COSMO-SkyMed ASI mission. We observed ground velocities and deformation geometries between 1992 and 2016, with displacements of more than 70 cm and velocities of up to 55 mm/yr. The results suggest that the shape and position of the surface ground displacement are controlled by the fault activity hidden under the valley deposits.
Mapping and chronological classification of marine terraces along the southern side of the Sibari Plain (northern Calabria, Italy) by means of digital and analogue tools Laura Alfonsi, Carlo Alberto Brunori, Luigi Cucci Journal of Maps, 2023 We study the marine terraces of the southern side of the Sibari Plain in Northern Calabria (Italy) through the use of traditional and quantitative analyses of the Digital Terrain Model (DTM). The main aim of the present work consists in the extensive use of GIS tools that were never used before in the area, and in checking the applicability of this procedure. The terraced surfaces identified using photo interpretation and those recognized semi-automatically through the GIS tools were compared to finally produce a consensus map. In the final map, we identified 272 terraced surfaces and 62 morphological features associated with inner margins (i.e. paleoshorelines). The main map shows a well-developed flight of seven orders of marine terraces with elevation ranging from 45 to 360 m asl and age ranging from Marine Isotope Stage (MIS) 5a to 11.
Surface ruptures database related to the 26 December 2018, MW 4.9 Mt. Etna earthquake, southern Italy F. Villani, S. Pucci, R. Azzaro, R. Civico, F. R. Cinti, L. Pizzimenti, G. Tarabusi, S. Branca, C. A. Brunori, M. Caciagli, M. Cantarero, L. Cucci, S. D’Amico, E. De Beni, P. M. De Martini, M. T. Mariucci, A. Messina, P. Montone, R. Nappi, R. Nave, D. Pantosti, T. Ricci, V. Sapia, A. Smedile, R. Vallone, A. Venuti Scientific Data, 2020
Correction: A database of the coseismic effects following the 30 October 2016 Norcia earthquake in central Italy (Scientific Data, (2018) 5, 10.1038/sdata.2018.49) Fabio Villani, Riccardo Civico, Stefano Pucci, Luca Pizzimenti, Rosa Nappi, Paolo Marco De Martini, Fabio Villani, Riccardo Civico, Stefano Pucci, Luca Pizzimenti, Rosa Nappi, Paolo Marco De Martini, F. Agosta, G. Alessio, L. Alfonsi, M. Amanti, S. Amoroso, D. Aringoli, E. Auciello, R. Azzaro, S. Baize, S. Bello, L. Benedetti, A. Bertagnini, G. Binda, M. Bisson, A. M. Blumetti, L. Bonadeo, P. Boncio, P. Bornemann, S. Branca, T. Braun, F. Brozzetti, C. A. Brunori, P. Burrato, M. Caciagli, C. Campobasso, M. Carafa, F. R. Cinti, D. Cirillo, V. Comerci, L. Cucci, R. De Ritis, G. Deiana, P. Del Carlo, L. Del Rio, A. Delorme, P. Di Manna, D. Di Naccio, L. Falconi, E. Falcucci, P. Farabollini, J. P. Faure Walker, F. Ferrarini, M. F. Ferrario, M. Ferry, N. Feuillet, J. Fleury, U. Fracassi, C. Frigerio, F. Galluzzo, R. Gambillara, G. Gaudiosi, H. Goodall, S. Gori, L. C. Gregory, L. Guerrieri, S. Hailemikael, J. Hollingsworth, F. Iezzi, C. Invernizzi, D. Jablonská, E. Jacques, H. Jomard, V. Kastelic, Y. Klinger, G. Lavecchia, F. Leclerc, F. Liberi, A. Lisi, F. Livio, L. Lo Sardo, J. P. Malet, M. T. Mariucci, M. Materazzi, L. Maubant, F. Mazzarini, K. J. W. McCaffrey, A. M. Michetti, Z. K. Mildon, P. Montone, M. Moro, R. Nave, M. Odin, B. Pace, S. Paggi, N. Pagliuca, G. Pambianchi, D. Pantosti, A. Patera, E. Pérouse, G. Pezzo, L. Piccardi, P. P. Pierantoni, M. Pignone, S. Pinzi, E. Pistolesi, J. Point, L. Pousse, A. Pozzi, M. Proposito, C. Puglisi, I. Puliti, T. Ricci, L. Ripamonti, M. Rizza, G. P. Roberts, M. Roncoroni, V. Sapia, M. Saroli, A. Sciarra, O. Scotti, G. Skupinski, A. Smedile, Anne Socquet, G. Tarabusi, S. Tarquini, S. Terrana, J. Tesson, E. Tondi, A. Valentini, R. Vallone, J. Van der Woerd, P. Vannoli, A. Venuti, E. Vittori, T. Volatili, L. N. J. Wedmore, M. Wilkinson, M. Zambrano, and Scientific Data, 2019
Surface ruptures following the 26 December 2018, Mw 4.9, Mt. Etna earthquake, Sicily (Italy): EMERGEO Working Group (Etna 2018) Riccardo Civico, Stefano Pucci, Rosa Nappi, Raffaele Azzaro, Fabio Villani, Daniela Pantosti, Francesca R. Cinti, Luca Pizzimenti, Stefano Branca, Carlo Alberto Brunori, Marco Caciagli, Massimo Cantarero, Luigi Cucci, Salvatore D’Amico, Emanuela De Beni, Paolo Marco De Martini, Maria Teresa Mariucci, Paola Montone, Rosella Nave, Tullio Ricci, Vincenzo Sapia, Alessandra Smedile, Gabriele Tarabusi, Roberto Vallone, Alessandra Venuti Journal of Maps, 2019
A database of the coseismic effects following the 30 October 2016 Norcia earthquake in Central Italy Fabio Villani, Riccardo Civico, Stefano Pucci, Luca Pizzimenti, Rosa Nappi, Paolo Marco De Martini, Fabio Villani, Riccardo Civico, Stefano Pucci, Luca Pizzimenti, Rosa Nappi, Paolo Marco De Martini, F. Agosta, G. Alessio, L. Alfonsi, M. Amanti, S. Amoroso, D. Aringoli, E. Auciello, R. Azzaro, S. Baize, S. Bello, L. Benedetti, A. Bertagnini, G. Binda, M. Bisson, A.M. Blumetti, L. Bonadeo, P. Boncio, P. Bornemann, S. Branca, T. Braun, F. Brozzetti, C.A. Brunori, P. Burrato, M. Caciagli, C. Campobasso, M. Carafa, F.R. Cinti, D. Cirillo, V. Comerci, L. Cucci, R. De Ritis, G. Deiana, P. Del Carlo, L. Del Rio, A. Delorme, P. Di Manna, D. Di Naccio, L. Falconi, E. Falcucci, P. Farabollini, J.P. Faure Walker, F. Ferrarini, M.F. Ferrario, M. Ferry, N. Feuillet, J. Fleury, U. Fracassi, C. Frigerio, F. Galluzzo, R. Gambillara, G. Gaudiosi, H. Goodall, S. Gori, L.C. Gregory, L. Guerrieri, S. Hailemikael, J. Hollingsworth, F. Iezzi, C. Invernizzi, D. Jablonská, E. Jacques, H. Jomard, V. Kastelic, Y. Klinger, G. Lavecchia, F. Leclerc, F. Liberi, A. Lisi, F. Livio, L. Lo Sardo, J.P. Malet, M.T. Mariucci, M. Materazzi, L. Maubant, F. Mazzarini, K.J.W. McCaffrey, A.M. Michetti, Z.K. Mildon, P. Montone, M. Moro, R. Nave, M. Odin, B. Pace, S. Paggi, N. Pagliuca, G. Pambianchi, D. Pantosti, A. Patera, E. Pérouse, G. Pezzo, L. Piccardi, P.P. Pierantoni, M. Pignone, S. Pinzi, E. Pistolesi, J. Point, L. Pousse, A. Pozzi, M. Proposito, C. Puglisi, I. Puliti, T. Ricci, L. Ripamonti, M. Rizza, G.P. Roberts, M. Roncoroni, V. Sapia, M. Saroli, A. Sciarra, O. Scotti, G. Skupinski, A. Smedile, Anne Socquet, G. Tarabusi, S. Tarquini, S. Terrana, J. Tesson, E. Tondi, A. Valentini, R. Vallone, J. Van der Woerd, P. Vannoli, A. Venuti, E. Vittori, T. Volatili, L.N.J. Wedmore, M. Wilkinson, M. Zambrano, and Scientific Data, 2018
Coseismic ruptures of the 24 August 2016, Mw 6.0 Amatrice earthquake (central Italy) S. Pucci, P. M. De Martini, R. Civico, F. Villani, R. Nappi, T. Ricci, R. Azzaro, C. A. Brunori, M. Caciagli, F. R. Cinti, V. Sapia, R. De Ritis, F. Mazzarini, S. Tarquini, G. Gaudiosi, R. Nave, G. Alessio, A. Smedile, L. Alfonsi, L. Cucci, D. Pantosti Geophysical Research Letters, 2017
Coseismic effects of the 2016 Amatrice seismic sequence: First geological results EMERGEO W.G. :, S. Pucci, P.M. De Martini, R. Civico, R. Nappi, T. Ricci, F. Villani, C.A. Brunori, M. Caciagli, V. Sapia, F.R. Cinti, M. Moro, D. Di Naccio, S. Gori, E. Falcucci, R. Vallone, F. Mazzarini, S. Tarquini, P. Del Carlo, V. Kastelic, M. Carafa, R. De Ritis, G. Gaudiosi, R. Nave, G. Alessio, P. Burrato, A. Smedile, L. Alfonsi, P. Vannoli, M. Pignone, S. Pinzi, U. Fracassi, L. Pizzimenti, M.T. Mariucci, N. Pagliuca, A. Sciarra, R. Carluccio, I. Nicolosi, M. Chiappini, F. D’Ajello Caracciolo, G. Pezzo, A. Patera, R. Azzaro, D. Pantosti, P. Montone, M. Saroli, L. Lo Sardo, M. Lancia Annals of Geophysics, 2016
The liquefaction features in the area of the May-June 2012 Emilia seismic sequence: An investigation approach coupling Electric Resistivity Tomography (ERT) with coring Rendiconti Online Societa Geologica Italiana, 2013
The March 11th, 2011, M 9.0 earthquake offshore Honshu island (Japan): A synthesis of the Tohoku-Oki INGV Team research activities Quaderni Di Geofisica, 2013
G.I.S. methodology applied to proposals for geotourism in the area of Ascoli Piceno Province Rendiconti Online Societa Geologica Italiana, 2009
FieLd geological survey in the epicentral area of the Abrazzi (central Italy) seismic sequence of April 6th, 2009 Quaderni Di Geofisica, 2009
The sigris project: A remote sensing system for seismic risk management Marco Chini, Christian Bignami, Simone Atzori, Carlo Alberto Brunori, Christodoulos Kyriakopoulos, Marco Moro, Stefano Salvi, Salvatore Stramondo, Cristiano Tolomei, Elisa Trasatti, Simona Zoffoli International Geoscience and Remote Sensing Symposium IGARSS, 2008
Towards a geological information system: The CARGeo system and the regione lombardia geological database Rendiconti Della Societa Geologica Italiana, 2007
