The Correlation Between Historical and Instrumental Seismicity in the Sansepolcro Basin, Northern Apennines, Italy

The area investigated, the Sansepolcro basin, is characterized by the presence of important earthquakes in the past with estimated intensity even larger than IX MCS (the 1352 Monterchi earthquake, the 1389 Boccaserriola, the 1458 Citta’ di Castello, the 1781 Cagliese and the 1917 Monterchi-Citerna earthquakes, CPTI Working Group, 2004) and by a surprisingly scarce instrumental seismicity compared to the adjacent areas struck by high seismicity (Castello et al., 2005; Ciaccio et al., 2006). The area north of Sansepolcro has been struck in recent years by four minor sequences, occurred between 1987 and 2001 with magnitude ranging from Ml3.0 to Mw4.7. In this work we analyse the most important earthquakes of the 20th century occurred in the Altotiberina Valley in 1917, 1918, 1919 and 1948; in particular instrumental relocation, focal mechanisms and Ms and Mw magnitude estimation are re-evaluated. The relocation of these earthquakes is particularly critical and is an important issue. An instrumental and precise location is critical for the complexity of the problems associated with the study of seismograms prior to the first half of the twentieth century and is relevant because in the surrounding regions higher seismicity is observed. Regarding this peculiarity of the area, it’s very important to detect the location of the historical earthquakes: in particular, the 1917 event is often associated to the possibility that the regional low angle Altotiberina Fault (Barchi et al., 1998) is able or not to nucleate large- or moderate-magnitude events, being historically located close to its surface (Boncio and Lavecchia, 2000)

Un anno di Comitato Unico di Garanzia: riflessioni all'INGV

L’Istituto Nazionale di Geofisica e Vulcanologia - INGV ha istituito il Comitato Unico di Garanzia per le pari opportunità, la valorizzazione del benessere di chi lavora e contro le discriminazioni – CUG nel luglio 2011, ai sensi della L.183/2010. Il CUG ha assunto, estendendoli, i compiti del precedente Comitato Pari Opportunità, ossia, come da delibera CD n.4.3.2.11 del 28/6/2011: • focalizzare i problemi relativi alle pari opportunità; • contribuire a migliorare la qualità della vita negli ambienti di lavoro e a valorizzare le risorse umane; • verificare gli equilibri tra i sessi nelle posizioni funzionali a parità di requisiti professionali; • formulare proposte per: la gestione flessibile delle risorse umane e le attività di formazione professionale; è inoltre chiamato a perseguire gli obiettivi della direttiva dei dipartimenti della Funzione Pubblica e per le Pari Opportunità del 4 marzo 2011, per esercitare compiti propositivi, consultivi e di verifica. I compiti affidati dall’Amministrazione da un lato e le sollecitazioni ricevute dal personale dall’altro hanno portato ad una serie di azioni, tra le principali: • la redazione di un Codice per la tutela della dignità delle persone e per la prevenzione delle molestie sessuali e morali dell’INGV, l’individuazione della Consigliera di Fiducia e l’avvio di un ciclo di seminari sull’argomento, nell’ambito della prevenzione delle discriminazioni; • una lettura di genere delle bozze dei nuovi regolamenti dell’ente, con proposte di modifiche ispirate alla Carta Europea dei Ricercatori – CdR (e.g. principi di Non discriminazione, Equilibrio di genere) e alla normativa in tema di pari opportunità e tutela della maternità, parte delle quali recepite nel Regolamento del Personale e nel Disciplinare in materia di orario di servizio; un’azione, questa, legata all’adesione in via sperimentale alla Human Resources Strategy for Researchers, iniziativa della Comunità Europea per l’effettiva implementazione della CdR; • nell’ambito del processo di valutazione della ricerca dell’ANVUR, l’evidenziazione di alcune criticità presenti nel bando, in relazione alla valutazione della maternità, risultate in una interrogazione parlamentare e in una lettera aperta, grazie al contributo dell’Associazione Donne e Scienza e dei CUG dell’INFN e del CNR. Le esperienze fatte confermano l’opportunità di dare voce a tutte le donne dell’Istituto e di fare rete tra i Comitati degli enti di ricerca.UnpublishedCertosa di Pontignano (Siena), Italyope

Task 1 - Scenari di scuotimento - Deliverable D0: Tecniche di simulazione

Progetto INGV-DPC S3 “Scenari di scuotimento in aree di interesse prioritario e/o strategico”Published4.1. Metodologie sismologiche per l'ingegneria sismicaope

Analysis of the ionospheric scintillations during 20-21 January 2016 from SANAE by means of the DemoGRAPE scintillation receivers

This paper presents ionospheric scintillation data recorded at SANAE in Antarctica during a moderate geomagnetic storm on 20-21 January 2016 which gives evidence of the advantages of the new generation of instrumentation for monitoring ionospheric scintillation. The data was collected as part of the DemoGRAPE project aimed at the demonstration of cutting edge technology for the empirical assessment of the ionospheric delay and ionospheric scintillations in the polar regions which affect the accuracy of satellite navigation

2D seismic tomography of Somma-Vesuvius: Description of the experiment and preliminary results

A multidisciplinary project for the investigation of Mt. Vesuvius structure was started in 1993. The core of the project is represented by a high resolution seismic tomography study by using controlled and natural sources. The main research objective is to investigate the feeding system of the volcano and to retrieve details of the upper crustal structure in the area. A first 2D active seismic experiment was performed in May 1994, with the aim of studing the feasibility of using tomographic techniques for exploring the volcano interiors. Particularly, this experiment was designed to obtain information on the optimal sources-receivers configuration and on the depth extension of the volume sampled by shot-generated seismic waves. 66 three-component seismic stations and 16 single-component analogue instruments were installed by several Italian and French groups to record signals generated by three on-land, underground explosions. Sources and geophones were deployed along a 30-km NW-SE profile passing through the volcano crater. Receivers were placed at an average spacing of 250 m in the middle of the recording line and at 500 m outside. The arrival time data base was complemented by first P and S readings of microearthquakes which occurred in the recent past within the volcano. The first arrival data set was preliminarily used to determine the shallow structure of the volcano by applying Thurber's (1983) tomographic inversion technique. This analysis shows evidence for a high-velocity body which extends vertically from about 400 m below the crater down to at least 3000 m and for a shallow 300-500 m thick low-velocity cover which borders the edifice. Data from the distant shot show evidence for arrivals of deep reflected/converted phases and provide information on the deeper structure under the volcano. The results from the interpretation of 2D data are used for planning a 3D tomographic survey which will be carried out in 1996

An upper bound on the rate of strain in the Central Apennines, Italy, from triangulation measurements between 1869 and 1963

Italy is covered by a first-order triangulation network that was established between 1869 and 1908 and re-measured in patches between 1936 and 1963. We analyse the measurements made in the central part of Italy to form an estimate of the rate of strain in the Central Apennines. We conclude that the rate of strain in this region is too small to detect from the repeated triangulation measurement. This result places an upper bound of about 10(exp-7)/yr on the strain rate of the Central Apennines, and implies that the maximum rate of extension across the region is no higher than about 3 mm/yr

An upper bound on the rate of strain in the Central Apennines, Italy, from triangulation measurements between 1869 and 1963

Italy is covered by a first-order triangulation network that was established between 1869 and 1908 and re-measured in patches between 1936 and 1963. We analyse the measurements made in the central part of Italy to form an estimate of the rate of strain in the Central Apennines. We conclude that the rate of strain in this region is too small to detect from the repeated triangulation measurements. This result places an upper bound of about 10-7/yr on the strain rate of the Central Apennines, and implies that the maximum rate of extension across the region is no higher than about 3 mm/yr