ITACA (ITalian ACcelerometric Archive): a Web Portal for the Dissemination of the Italian Strong Motion Data

The Italian strong-motion database contains 2182 three component waveforms generated by 1004 earthquakes with a maximum magnitude of 6.9 (1980 Irpinia earthquake) covering the period range from 1972 to 2004. The database is devoted to serving the seismological and engineering communities. The database can be accessed on-line at the site http://itaca.mi.ingv.it, where a wide range of search tools enables the user to interactively search events, recording stations and retrieve waveforms with particular characteristics, whose parameters can be specified, as needed, through a graphical user interface. A range of display options allows users to view data in different contexts, extract and download time series and spectral data. The database was created during a joint project between Istituto Nazionale di Geofisica e Vulcanologia (INGV, Italian institute for geophysics and vulcanology) and Dipartimento della Protezione Civile (DPC, Italian civil protection). The aim of the project was the collection, homogenization and distribution of data acquired over the time period 1972-2004 in Italy by different Italian institutions, namely Ente Nazionale per l’Energia Elettrica (ENEL, Italian electricity company), Ente per le Nuove tecnologie, l’Energia e l’Ambiente (ENEA, Italian energy and environment organization) and DPC. The project had multiple purposes, such as permanent strong motion monitoring and temporary monitoring during seismic sequences or before permanent installation. This database brings up to date the ENEA strong motion data collection which ended in 1993 and the European database where the most recent Italian data pertain to the Umbria-Marche sequence of 1997-1998 (Ambraseys at al., 2002). In addition effort was spent reviewing strong motion metadata and data processing to increase data quality and reliability. This article describes the steps that led to the completion of the project and provides an overview of the search capabilities available at the database interface website

Geometry and evolution of a fault-controlled Quaternary basin by means of TDEM and single-station ambient vibration surveys: The example of the 2009 L'Aquila earthquake area, central Italy

We applied a joint survey approach integrating time domain electromagnetic soundings and single-station ambient vibration surveys in the Middle Aterno Valley (MAV), an intermontane basin in central Italy and the locus of the 2009 L’Aquila earthquake. By imaging the buried interface between the infilling deposits and the top of the pre-Quaternary bedrock, we reveal the 3-D basin geometry and gain insights into the long-term basin evolution. We reconstruct a complex subsurface architecture, characterized by three main depocenters separated by thresholds. Basin infill thickness varies from ~200–300m in the north to more than 450m to the southeast. Our subsurface model indicates a strong structural control on the architecture of the basin and highlights that the MAV experienced considerable modifications in its configuration over time. The buried shape of the MAV suggests a recent and still ongoing predominant tectonic control by the NW-SE trending Paganica-San Demetrio Fault System (PSDFS), which crosscuts older ~ENE and NNE trending extensional faults. Furthermore, we postulate that the present-day arrangement of the PSDFS is the result of the linkage of two previously isolated fault segments. We provide constraints on the location of the southeastern boundary of the PSDFS, defining an overall ~19 km long fault system characterized by a considerable seismogenetic potential and a maximum expected magnitude larger than M6.5. This study emphasizes the benefit of combining two easily deployable geophysical methods for reconstructing the 3-D geometry of a tectonically controlled basin. Our joint approach provided us with a consistent match between these two independent estimations of the basin substratum depth within 15%.Published2236–22597T. Struttura della Terra e geodinamica2TR. Ricostruzione e modellazione della struttura crostaleJCR Journa

The 2016–2017 earthquake sequence in Central Italy: macroseismic survey and damage scenario through the EMS-98 intensity assessment

In this paper we describe the macroseismic effects produced by the long and destructive seismic sequence that hit Central Italy from 24 August 2016 to January 2017. Starting from the procedure adopted in the complex field survey, we discuss the characteristics of the building stock and its classification in terms of EMS-98 as well as the issues associated with the intensity assessment due to the evolution of damage caused by multiple shocks. As a result, macroseismic intensity for about 300 localities has been determined; however, most of the intensities assessed for the earthquakes following the first strong shock on 24 August 2016, represent the cumulative effect of damage during the sequence. The earthquake parameters computed from the macroseismic datasets are compared with the instrumental determinations in order to highlight critical issues related to the assessment of macroseismic parameters of strong earthquakes during a seismic sequence. The results also provide indications on how location and magnitude computation can be strongly biased when dealing with historical seismic sequences.Presidenza del Consiglio dei Ministri - Dipartimento della Protezione Civile (DPC)Published2407–24314T. Sismicità dell'Italia1SR TERREMOTI - Sorveglianza Sismica e Allerta Tsunami2SR TERREMOTI - Gestione delle emergenze sismiche e da maremoto5SR TERREMOTI - Convenzioni derivanti dall'Accordo Quadro decennale INGV-DPCJCR Journa

ITACA (ITalian ACcelerometric Archive): un sito web per la disseminazione dei dati accelerometrici italiani

La creazione del data base dei dati accelerometrici italiani è un’iniziativa nata nell’ambito della convenzione tra il Dipartimento della Protezione Civile e l’Istituto Nazionale di Geofisica e Vulcanologia nel biennio 2004-2006 (progetto di interesse sismologico S6 denominato Data base dei dati accelerometrici italiani relativi al periodo 1972-2004), in risposta alla crescente richiesta da parte della comunità scientifica di dati strong motion per diverse applicazioni (leggi di attenuazione, verifica di scenari di scuotimento e mappe di pericolosità, shake maps, ecc.). Scopo del progetto è stata la raccolta e l’omogeneizzazione delle forme d’onda acquisite nel corso degli anni dall’Ente Nazionale per l’Energia Elettrica (ENEL), dall’Ente per le Nuove tecnologie, l’Energia e l’Ambiente (ENEA) e dal Dipartimento della Protezione Civile. In aggiunta, le registrazioni sono state qualificate attraverso l’inserimento di metadati relativi agli eventi, ai siti di registrazione e agli strumenti. Un notevole sforzo è stato compiuto per garantire la disseminazione dei dati attraverso un portale web e una serie di strumenti per la consultazione interattiva della banca dati.PublishedRoma5.2. TTC - Banche dati di sismologia strumentaleope

Indagini Geofisiche

Nell'ambito del progetto per la Microzonazione sismica dell'area aquilana, coordinata dal DPC, il Gruppo di Lavoro ha condotto le indagini di MS nella Conca di Roio.Published336-3854T. Sismologia, geofisica e geologia per l'ingegneria sismic

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

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 km 2. 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

Numerical modelling of local seismic response in alluvial valleys filled by heterogeneous deposits for seismic microzonation studies in Northern Latium (Italy)

After the 2016–2017 seismic sequence in Central Apennines, seismic microzonation studies were planned in the framework of the Ordinance 24 of the 12 th of May 2017 (OPCM 24/2017) issued by the Italian Presidency of the Council of Ministers. Numerical simulations aiming at estimating seismic amplification factors of uniform microzones located in several municipalities of the Latium Region were carried out in order to provide quantitative elements for reconstruction. The investigated areas include alluvial valleys of variable shapes filled by heterogeneous deposits. The obtained results demonstrate that the heterogeneities of the alluvial deposits are responsible for variations in the seismic response; therefore, they cannot be neglected in estimating the local seismic response of the sites. The two case studies of Fonte del Campo and Posta were selected among the studied municipalities for illustrating the main findings