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  • 1
    Publication Date: 2023-01-13
    Description: Coseismic surface faulting associated to the 6 April 2009, Mw 6.1 L'Aquila earthquake from the joint analysis of the Istituto Nazionale di Geofisica e Vulcanologia (INGV) and of the Istituto Superiore per la Protezione e la Ricerca Ambientale (ISPRA) field observations. The primary surface faulting reaches a total length of ca. 6 km and shows a ca. 3 km-long zone of continuous and consistently oriented surface ruptures in proximity of the village of Paganica, along a prominent NW-SE oriented, SW dipping normal fault. The deformation occurred in a ca. 500 m-wide zone. Secondary surface ruptures (antithetic and sympathetic) occurred along nearby faults. INGV - ISPRA joint database - 2009 L'Aquila earthquake surface rupture - Observation points: this file contains the tectonic ruptures observation points containing information about the typology, the geometrical characteristics, and a brief description of the observed feature. Credits: Blumetti et al., Report ISPRA 2009; Emergeo W.G., Terranova 2010 doi:10.1111/j.1365-3121.2009.00915.x; Cinti et al., JGR 2011 doi:10.1029/2010JB007988; Vittori et al., BSSA 2011 doi:10.1785/0120100140. INGV - ISPRA joint database - 2009 L'Aquila earthquake surface rupture - Surface faulting trace: this file displays as a line coverage the primary surface faulting associated to the 6 April 2009, Mw 6.1 L'Aquila earthquake. It is composed of multiple discrete rupture traces (mainly SW-facing free-faces and open cracks) with individual length ranging from 3 m to ca. 200 m. The traces are built based on the observation point layer, and contain information about the typology, the geometrical characteristics and the affected lithology (for this latter field attribute see Pucci et al., JoM 2015 doi:10.1080/17445647.2014.927128). INGV - ISPRA joint database - 2009 L'Aquila earthquake surface rupture - Secondary surface rupture trace: this file displays as a line coverage some of the secondary ruptures (antithetic and sympathetic) occurred along faults within the epicentral area.
    Keywords: Area/locality; Category; Description; Description 2 (continued); Dip; Direction; Identification; Italy; LAquila; LATITUDE; Length; LONGITUDE; Opening; Provenance/source; Typology; Vertical offset
    Type: Dataset
    Format: text/tab-separated-values, 2566 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-04-20
    Description: This dataset gathers all the published existing information on the coseismic surface ruptures produced by the Mw 6.9 earthquake that struck the Irpinia region (southern Italy) on the 23rd November 1980. The dataset is the sum of the observations made by several authors over the years (e.g., Carmignani et al., 1981, Westaway and Jackson, 1984, Pantosti and Valensise, 1990, Blumetti et al., 2002). The data were collected during field surveys carried out from right after the event till 2021 and were integrated by aerial photo interpretation. The most recent surveys by the authors of this database were focused on the evaluation, repositioning through GNSS handheld devices, and validation in the field of the observation points to overcome unprecise manual positioning of pre-GNSS times. The observations are organized in a database of 175 homogenous georeferenced points and 49 georeferenced lines (coseismic ruptures). The points data are available in .xlsx meanwhile the lines are available in .shp format. Each point is described by the following parameters, when available: Observation type, Latitude, Longitude, Elevation, Throw, Strike, Dip, References, Ranking, Comment, and Bibliography. The ranking assigned to each coseismic feature is based, with integrations, on Baize et al. 2021. Each feature is attributed to two ranking values, one referring to the compilers of this database and the other to the original author's interpretation. The scores are 1 to 4: 1) principal faulting; 2) simple distributed faulting; 3) sympathetic faulting; 4) ground shaking or shaking/gravity-induced slip (category assigned in this work). The lines are described by Type of observation, Uncertainty, Strike, Downthrow Side, Ranking, Comment, and Bibliography. The ranking values are the same as above. The downthrow side value for each line is the mode of the observation points located on the line itself. As a consequence of the different ages and origins of the data, including the variable scaling of the surveys, we have built the dataset at different scales; we suggest looking at the project at the scale spanning from 1:5.000 to 1:10.000.
    Keywords: Irpinia; SEIS; Seismic
    Type: Dataset
    Format: application/zip, 69.2 kBytes
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Villani, Fabio; Pucci, Stefano; Azzaro, Raffaele; Civico, Riccardo; Cinti, Francesca Romana; Pizzimenti, Luca; Tarabusi, Gabriele; Branca, Stefano; Brunori, Carlo Alberto; Caciagli, Marco; Cantarero, Massimo; Cucci, Luigi; D'Amico, Salvatore; De Beni, Emanuela; De Martini, Paolo Marco; Mariucci, Maria Teresa; Messina, A; Montone, Paola; Nappi, Rosa; Nave, Rosella; Pantosti, Daniela; Ricci, Tullio; Sapia, Vincenzo; Smedile, Alessandra; Vallone, Roberto; Venuti, Alessandra (2020): Surface ruptures database related to the 26 December 2018, MW 4.9 Mt. Etna earthquake, southern Italy. Scientific Data, 7(1), 42, https://doi.org/10.1038/s41597-020-0383-0
    Publication Date: 2024-06-22
    Description: We provide a database of the coseismic surface ruptures produced by the 26 December 2018 Mw 4.9 earthquake that struck the eastern flank of Mt. Etna (southern Italy), the largest active volcano in Europe. Despite its small size, this shallow earthquake caused an impressive system of coseismic surface ruptures extending about 8.5 km, along the trace of the NNW-trending active Fiandaca Fault. We performed detailed field surveys were performed in the epicentral region to describe the ruptures geometry and kinematics. These exhibit a dominant right-oblique sense of slip with coseismic displacement peaks of 0.35 m. The Fiandaca Fault is part of a complex active faults system affecting the eastern flank of Mt. Etna. Its seismic history indicates a prominent surface-faulting potential, so our study is essential for unravelling the seismotectonics of shallow earthquakes in volcanic settings, and contributes updating empirical scaling laws relating moderate-sized earthquakes and surface faulting. The collected observations have been parsed and organized in a concise database consisting of 874 homogeneous georeferenced records. The main features describing the coseismic ruptures are the following: ID, time of sample collection, location (latitude, longitude, elevation), type of rupture, type of affected substratum, attitude (dip angle, dip direction, strike), surface offset (opening, throw, strike slip, net slip), kinematics, slip vector attitude, width of the deformation zone.
    Keywords: Angle; Compass; DATE/TIME; Direction; earthquake; ELEVATION; Etna; ETNA; Fiandaca fault; Kinematics; LATITUDE; Length; LONGITUDE; Mount Etna, Sicily, Italia; Observation; Offset; Opening; ORDINAL NUMBER; Plunge; rupture; Strike; Strike-slip; Substratum; surface faulting; Throw; Trend; volcano; Width
    Type: Dataset
    Format: text/tab-separated-values, 6893 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2020-12-15
    Description: Fault displacement hazard assessment is based on empirical relationships that are established using historic earthquake fault ruptures. These relationships evaluate the likelihood of coseismic surface slip considering on-fault and off-fault ruptures, for given earthquake magnitude and distance to fault. Moreover, they allow predicting the amount of fault slip at and close to the active fault of concern. Applications of this approach include land use planning, structural design of infrastructure, and critical facilities located on or close to an active fault. To date, the current equations are based on sparsely populated datasets, including a limited number of pre-2000 events. In 2015, an international effort started to constitute a worldwide and unified fault displacement database (SUrface Ruptures due to Earthquakes [SURE]) to improve further hazard estimations. After two workshops, it was decided to unify the existing datasets (field-based slip measurements) to incorporate recent and future cases, and to include new parameters relevant to properly describe the rupture. This contribution presents the status of the SURE database and delineates some perspectives to improve the surface-faulting assessment. Original data have been compiled and adapted to the structure. The database encompasses 45 earthquakes from magnitude 5–7.9, with more than 15,000 coseismic surface deformation observations (including slip measurements) and 56,000 of rupture segments. Twenty earthquake cases are from Japan, 15 from United States, two from Mexico, Italy, and New Zealand, one from Kyrgystan, Ecuador, Turkey, and Argentina. Twenty-four earthquakes are strike-slip faulting events, 11 are normal or normal oblique, and 10 are reverse faulting.
    Description: Published
    Description: 499–520
    Description: 6T. Studi di pericolosità sismica e da maremoto
    Description: JCR Journal
    Keywords: surface rupture ; fault displacement hazard ; 04.04. Geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 5
    Publication Date: 2021-06-07
    Description: In order to geometrically characterize the liquefaction features observed in the epicentral sector of the 2012 Emilia seismic sequence and to evaluate the potential for recording palaeoseismic features of the area, we performed two electric resistivity tomographic sections and 4 shallow corings, coupled with 14C datings and archaeological age estimates in selected sites. Preliminary results show that there is a good agreement between ERT sections and core-logs; moreover a major role in determining the scalar relationships of the liquefaction features is played by the local geomorphological and topographic setting. The high sedimentation rates obtained through core datings (4 – 20 mm/yr) suggest that the described methodological approach can cover time windows of only a few centuries, thus hardly encompassing, in this tectonic setting, a significant period for paleoseismological purposes.
    Description: Published
    Description: 206-209
    Description: 2T. Deformazione crostale attiva
    Description: N/A or not JCR
    Keywords: liquefaction ; earthquake ; 04.04. Geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2017-04-04
    Description: The occurrence of the Mw 6.3, April 6, 2009 earthquake has highlighted how critical is the knowledge of the location and of the characteristics of the active faults in a seismic region. This is true not only as a contribution to the seismic hazard assessment but also for the local planning of residential areas, plants and infrastructures. The 2009 earthquake occurred on the Paganica normal fault (PF hereinafter) and produced 3 km-long, maximum 0.1 m-high surface rupture along its central section, and secondary slip along nearby tectonic structures. The PF consists of a prominent morphologic scarp formed by the tectonic juxtaposition of Pliocene-middle Pleistocene and late Pleistocene alluvial deposits, and by lower scarps in late Pleistocene-Holocene deposits. The fault, NW-SE striking and SW dipping, runs for a total length of about 20 km along the NE side of the Aterno River valley, a graben-type basin bounded by marked antithetic faults. The limited extent and the small throw of the 2009 surface ruptures, when compared to the size of the Paganica long-term fault scarp, suggest that the PF probably experienced larger Magnitude earthquakes than the 2009 seismic event. Thus, although the April 6, 2009 earthquake and associated surface faulting caused loss of lives and major damage, we believe that this event does not fully characterize the seismic hazard of the area. Therefore, a campaign of paleoseismological investigations is underway with the aim of defining the Max Magnitude, the average rate of displacement and the frequency of seismic events on the PF and on the nearby faults. An amazing “coseismic” trench, caved by the overpressure produced by the broken pipe of an aqueduct, provided the exposure of a 30-m wide fault zone of the PF. We show the preliminary results from the analysis of this site, as well as from other sites along the PF. In addition, we also present preliminary paleoseismological data from the antithetic Fossa fault. A major finding at this early stage of our field campaign is the recognition of large displacements (0.5 to 1 m) associated to individual events affecting deposits of Holocene age based on radiocarbon dating and pottery content.
    Description: Published
    Description: 2009 AGU Fall Meeting 14–18 December Moscone Convention Center Howard Street, Between Third & Fifth Sts. San Francisco, California, USA
    Description: 3.2. Tettonica attiva
    Description: open
    Keywords: paleoseismology ; 6 April 2009 L'Aquila earthquake ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Oral presentation
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  • 7
    Publication Date: 2020-02-11
    Description: We provide a database of the surface ruptures produced by the 26 December 2018 Mw 4.9 earthquake that struck the eastern flank of Mt. Etna volcano in Sicily (southern Italy). Despite its relatively small magnitude, this shallow earthquake caused about 8 km of surface faulting, along the trace of the NNW-trending active Fiandaca Fault. Detailed field surveys have been performed in the epicentral area to map the ruptures and to characterize their kinematics. The surface ruptures show a dominant right-oblique sense of displacement with an average slip of about 0.09 m and a maximum value of 0.35 m. We have parsed and organized all observations in a concise database, with 932 homogeneous georeferenced records. The Fiandaca Fault is part of the complex active Timpe faults system affecting the eastern flank of Etna, and its seismic history indicates a prominent surface-faulting potential. Therefore, this database is essential for unravelling the seismotectonics of shallow earthquakes in volcanic areas, and contributes updating empirical scaling regressions that relate magnitude and extent of surface faulting.
    Description: Published
    Description: id 42
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Keywords: Surface faulting ; Coseismic effects ; 04.04. Geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2019-04-01
    Description: Rapid and permanent granulometric changes within the clastic sedimentary deposits of the Tiber River are directly linked to changes in sediment transport capacity and give insight on climate fluctuations and related sea-level oscillations during Late Pleistocene–Holocene times. In this work, we investigate the stratigraphic features of the sedimentary fill of the Tiber River channel as far as 30 km from the coast, and of one tributary, the Grottaperfetta stream. Through direct observation and core sampling of ten, 30 to 80 m deep boreholes, and the analysis of a large number of stratigraphic log data, we reconstruct a series of transverse sections and correlate them along a longitudinal profile of the Tiber River course. We provide geochronologic constraints to the deposition of distinct lithostratigraphic units by means of 8 newly acquired 14C ages and 21 previously reported ages of intercalated peat layers and wood fragments. Moreover, we review and select 28 radiocarbon ages fromliterature on the deposits of the Tiber River in the coastal plain, in order to reconstruct the aggradational history throughout the distal portion of the basin. Finally, we provide curves of sediment aggradation vs. time during the last 19,000 yr for the different investigated portions of the Tiber River course. We compare them to sea-level curves from the literature. To perform this comparison, we use a rigorous geotechnical approach to estimate the subsidence due to sediment compaction, andwe apply a correction to the Present-day elevation of the dated samples of organic material interbedded with the sedimentary deposits. Two significant sedimentary events at around 13,800 yr BP and 7500 yr BP, marked by sharp stratigraphic and granulometric changes, are recognized and correlate to important variations in the rate of sea-level rise. Moreover, we show evidence of an erosional event coupled to a reversal of the granulometry (increase in gain size of sediments) affecting the whole investigated tract of the Tiber River channel between 5500 and 3500 yr BP and discuss its possible causes. In particular, we discuss whether besides the change in capacity of transport due to a climatic change, also a drop in sea level, in the order of 2–3 meters, may have occurred in this time span, either in response to an increase in global ice volume, glacial isostatic adjustment, or local tectonic uplift.
    Description: Published
    Description: 157–176
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Keywords: Tiber River ; Holocene climate ; Fluvio-deltaic sedimentation ; Post-glacial sea-level rise ; 04.04. Geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2018-03-12
    Description: Two underground cavities in the Northern Calabria region, the Romito and the San Paolo caves, have been selected for speleoseismic analysis in order to provide a timeframe for paleoearthquakes which have shocked the cave sites and the surrounding area. The caves are positioned in a seismogenically active region, which has been struck by medium to large earthquakes in historical and pre-historic times. Moreover, frequent instrumentally measured small to moderate seismicity occurs in the area (M 5.6). We document damaged carbonate cave deposits, including collapsed and broken stalactites, in-situ severed stalagmites and stalactites, and collapsed bedrock ceilings. Samples were sawed in order to expose breakages and contacts within the laminae. Sixteen laminae, eight pairs of pre and post event laminae, were drilled for dating by the UraniumeThorium disequilibrium technique. Three discrete events were defined by six of the speleoseismites to (I) 7.4e2.9 ka, (II) 9.7e8.2 ka, and (III) 28.4e27.4 ka. Two additional speleoseismites gave wide age brackets, but are confined to 65.7e18.6 ka, which overlaps with event III, but might represent additional events. The present speleoseismic work depicts a scenario of a minimum of three well-constrained strong shaking events in a time span of the past ~28 ky, yielding a maximum recurrence interval of ~9 ky. In 2012 the area was shaken by a Mw5.2 earthquake that apparently did not produced damage within the study cavities, suggesting that this size is a lower magnitude limit for producing permanent effects in the caves deposits. The speleoseismites we studied collected must have been generated by larger magnitude events, and/or with different epicenter locations. This study adds medium or large earthquake events, previously lacking, to the historic and instrumental record. This may contribute to reduction of gaps in the earthquake record and consequently a more reliable recurrence interval estimate for damaging earthquakes in the region.
    Description: Published
    Description: 176-184
    Description: 3T. Storia Sismica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2019-01-24
    Description: The setting of a flight of marine terraces along a 65-km-long section of the Ionian coast of northern Calabria is the result of the interaction between interglacial sea levels, regional uplift, and local fault-related elevation changes. Seven terraces with corresponding palaeoshoreline angles at elevations ranging from 12 m to similar to 420 m were recognised by aerial photo interpretation and field surveying. The terraces were correlated to the oxygen isotope stages 1, 5a, 5c, 5e, 7, 9, 15, which correspond to the 7, 81, 102, 124, 215, 330 and similar to 600 ka highstands of the palaeosea-level curve. The similar to 600-ka-long regional ascent of the terraces took place at an average uplift rate of 0.67 mm/yr; this value slightly but progressively increases southward along the coastline. The elevation of the strandlines is related to the activity of tectonic structures. Three cases were analysed, allowing us: (1) to recognise the height anomalies of the terraces on the Sibari plain as the result of cumulated coseismic deformation caused by the normal Castrovillari fault, and on this basis calculate a minimum slip rate and a mean recurrence time for a single event of deformation; (2) to exclude the presence of significant vertical deformations and consequently activity on the easternmost section of the normal Pollino fault; and (3) to hypothesise the presence of an hitherto unknown active fault responsible for the strong vertical displacements of the flight of terraces near the river Avena. Finally, we find the ratio of the rate of regional uplift to the average rates of local tectonic deformation to be 2 to 3: 1. (C) 1998 Elsevier Science B.V. All rights reserved.
    Description: Published
    Description: 67-83
    Description: 1T. Deformazione crostale attiva
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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