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  • PANGAEA  (3)
  • CNR - INGV  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Villani, Fabio; Civico, Riccardo; Pizzimenti, Luca; Pucci, Stefano; De Martini, Paolo Marco; Nappi, Rosa; Open EMERGEO Working Group (2018): A database of the coseismic effects following the 30 October 2016 Norcia earthquake in Central Italy. Scientific Data, 5, 180049, https://doi.org/10.1038/sdata.2018.49
    Publikationsdatum: 2023-07-10
    Beschreibung: We provide a database that embodies more than 7000 punctual observations of the coseismic surface geological effects following the 30 October 2016 Mw 6.5 earthquake that hit central Italy. This earthquake caused widespread surface ruptures over a 〉400 km2-wide mountainous area. The Open EMERGEO Working Group, originated by the collaboration of several European geological survey teams coordinated by the Istituto Nazionale di Geofisica e Vulcanologia, involved about 130 researchers to perform detailed geological field surveys in the epicentral region. These observations mostly include accurate description of the geometry and kinematics of ground breaks caused by primary surface faulting, and subordinately by landslides due to shaking. The database consists of georeferenced records containing both numeric and string fields in the form of a suitable .txt file.
    Schlagwort(e): Angle; Central_Italy_earthquake; DATE/TIME; Direction; ELEVATION; Europe, Italy; Group; LAND; LATITUDE; Length; LONGITUDE; Observation; Offset; Opening; ORDINAL NUMBER; Plunge; Rake; Rock type; Sampling/measurement on land; Strike; Throw; Trend
    Materialart: Dataset
    Format: text/tab-separated-values, 51320 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 2
    Publikationsdatum: 2024-06-22
    Beschreibung: We provide a database of the coseismic surface ruptures produced by the 21 August 2017 Md 4.0 earthquake that struck the Casamicciola Terme village in the north of Ischia volcanic island (Italy). Despite its small size, the earthquake caused two fatalities and heavy damages in a restricted area of a few square kilometers. The shallow hypocentral depth of the earthquake caused a significant coseismic surface faulting, testified by a main alignment of ruptures mapped for a 2 km end-to-end length along the Casamicciola E-W trending normal fault system, bounding the northern slope of Mt. Epomeo. Casamicciola Terme has been recurrently destroyed in the last centuries by similar volcano-tectonic earthquakes (1762, 1767, 1796, 1828, 1881, and 1883). After the catastrophic 1883 Casamicciola event (2343 casualties), this is the first heavy damaging earthquake at Ischia that provides, for the first time, the opportunity of integrating historical seismicity, macroseismic observations, instrumental information, and detailed mapping of coseismic geological effects. We performed a detailed field surveys in the epicentral region of the 21 August earthquake to describe the ruptures geometry and kinematics of the seismogenetic fault responsible of the earthquake with the aim of contributing to the seismic hazard evaluation and land use planning in the Ischia island, one of the most crowded touristic destinations worldwide. Summarizing our study of ground effects for the 21 August 2017 earthquake is important for improving knowledge on surface earthquake in the volcanic area and contributing to complete the gap of empirical scaling relating to the surface-faulting mechanism due to small-size or moderate earthquakes in volcano-tectonic framework. The collected field observations result in a dataset of 88 georeferenced records describing coseismic ruptures/fractures by features as ID number, 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.
    Schlagwort(e): Casamicciola_Terme_coseismic_ruptures; Casamicciola fault; coseismic rupture; DATE/TIME; Direction; earthquake; ELEVATION; Ischia, Italy; Ischia island; Kinematics; LATITUDE; Length; LONGITUDE; Observation; Opening; ORDINAL NUMBER; Strike; Substrate type; Throw; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; volcano-tectonic
    Materialart: Dataset
    Format: text/tab-separated-values, 775 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 3
    facet.materialart.
    Unbekannt
    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
    Publikationsdatum: 2024-06-22
    Beschreibung: 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.
    Schlagwort(e): 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
    Materialart: Dataset
    Format: text/tab-separated-values, 6893 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 4
    Publikationsdatum: 2021-03-12
    Beschreibung: A quasi quaranta anni dal sisma che sconvolse la Campania e la Basilicata il 23 novembre 1980, è possibile fare una sintesi delle modalità di ricostruzione dei paesi distrutti o gravemente danneggiati. In questo studio si evidenzia come gli effetti ambientali abbiano condizionato le scelte ricostruttive, sia in situ, sia lontano dal nucleo originario e come la popolazione ha percepito lo sviluppo urbanistico ai fini della mitigazione del rischio sismico. Il terremoto dell'Irpinia e della Basilicata può essere considerato attualmente il più forte sisma registrato in Italia negli ultimi 100 anni, fu caratterizzato da una intensità epicentrale I0=X MCS, I0=X ESI e magnitudo ML=6.9. Il sisma causò circa 3000 vittime e danni in 800 paesi ubicati soprattutto a ridosso dell'Appennino meridionale. Castelnuovo di Conza, Conza della Campania, Lioni, Santomenna, Sant'Angelo dei Lombardi, Caposele, Calabritto, San Mango sul Calore, San Michele di Serino, Pescopagano, Guardia dei Lombardi, Laviano, Sant'Andrea di Conza, Senerchia e Teora, furono quasi completamente distrutti. Numerosi e devastanti furono gli effetti sull'ambiente naturale quali fenomeni di fagliazione superficiale ma anche e soprattutto fenomeni franosi, fratture nel suolo, variazioni idrologiche e fenomeni di liquefazione. Il grave livello di danneggiamento e gli estesi fenomeni di dissesto idrogeologico, hanno in molti casi condizionato la ricostruzione, talvolta sconvolgendo l'assetto degli originari insediamenti abitativi. In quest'ottica sono stati eseguiti studi di dettaglio per alcuni dei paesi più gravemente colpiti dal terremoto: Conza della Campania, San Mango sul Calore, Calitri, San Michele di Serino e Romagnano al Monte. Di questi, Conza della Campania e Romagnano al Monte, sono stati delocalizzati e ricostruiti completamente ex-novo, non senza conseguenze socio-economiche per la popolazione, mentre San Mango sul Calore, Calitri e San Michele di Serino, hanno cercato di recuperare il patrimonio edilizio esistente e di ricostruire con prevalenza di strutture in cemento armato rispettando l'originale assetto urbano.
    Beschreibung: Published
    Beschreibung: NAPLES
    Beschreibung: 6T. Studi di pericolosità sismica e da maremoto
    Schlagwort(e): terremoto irpino ; 23 novembre 1980 ; paesi distrutti ; modalità di ricostruzione
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: Conference paper
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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