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  • 1
    Publication Date: 2017-04-03
    Description: Questo lavoro è contenuto nel terzo volume di una serie che la Regione Marche pubblica al fine di divulgare i risultati di attività di ricerca svolte nel settore della valutazione del rischio sismico. Le attività descritte in questo volume riguardano la definizione di scenari di intensità macrosismica per la fascia costiera marchigiana. In particolare il lavoro sintetizza i risultati conseguiti da un gruppo di ricercatori afferenti all’Istituto Nazionale di Geofisica e Vulcanologia, all’Università di Perugia e all’Università di Pavia. Si tratta di un lavoro molto articolato e dotato di ampio supporto iconografico che si articola su sette paragrafi, ognuno corrispondente ad una linea di attività indipendente. Il paragrafo conclusivo, che sintetizza tutte le conoscenze disponibili sulle sorgenti sismogenetiche delle Marche, rappresenta anche una sintesi ideale dei contributi individuali forniti nei paragrafi precedenti. Per ogni linea di ricerca vengono presentate una sintetica ma esauriente descrizione e numerose immagini significative. Si rimarca come questo capitolo descriva con dettaglio sia le attività svolte (i risultati conseguiti e la loro parametrizzazione) sia l’uso di una banca dati GIS appositamente realizzata. I risultati delle ricerche descritte in questo capitolo rappresentano una estensione fortemente mirata delle ricerche sulla sismogenesi che il gruppo di ricerca dell’INGV svolge sistematicamente. Il denominatore comune di queste ricerche è lo studio sulle sorgenti sismogenetiche italiane e il loro baricentro è il Database of Individual Seismogenic Sources (DISS), Versione 3.0.4 [DISS Working Group, 2007; disponibile anche su Internet all’indirizzo: http://www.ingv.it/DISS].
    Description: Published
    Description: 3-70
    Description: 3.2. Tettonica attiva
    Description: open
    Keywords: seismogenic source ; Blind thrust fault ; Marche region ; 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 2
    Publication Date: 2017-04-03
    Description: The April 3, 1998 Mw=5.1 Gualdo Tadino earthquake (central Italy) was the last significant event in the 6-month-long Umbria–Marche seismic crisis. This event and its aftershocks occurred in an area where active faulting produces no striking geological and geomorphological effects. In this study, we investigated the ruptured fault using detailed seismological data and a re-processed and re-interpreted seismic reflection profile. Aftershock location and focal mechanisms were used to constrain the geometry and kinematics of the ruptured fault and a comparison was made with the subsurface image provided by the seismic profile. We found that the 1998 Gualdo Tadino earthquake occurred on a WSW-dipping, normal fault, with a length of about 8 km and a relatively gentle dip (308–408), confined between 3.5 and 7 km in depth. Kinematics of the mainshock and aftershocks revealed a NE-trending extension, in agreement with the regional stress field active in the Northern Apennines belt. The Mw = 5.1 earthquake originated above the top of the basement and ruptured within the sedimentary cover, which consists of an evaporites–carbonates multilayer. We hypothesised that the active fault does not reach the surface (blind normal fault). D 2005 Elsevier B.V. All rights reserved.
    Description: Published
    Description: 233-247
    Description: 3.2. Tettonica attiva
    Description: JCR Journal
    Description: reserved
    Keywords: Aftershocks; Seismicity; Blind normal fault; Seismic reflection profile; Focal mechanisms; Umbria–Marche Apennines ; 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2024-02-01
    Description: We present a reconstruction of the central Marche thrust system in the central-northern Adriatic domain aimed at constraining the geometry of the active faults deemed to be potential sources of moderate to large earthquakes in this region and at evaluating their long-term slip rates. This system of contractional structures is associated with fault-propagation folds outcropping along the coast or buried in the offshore that have been active at least since about 3Myr. The ongoing deformation of the coastal and offshore Marche thrust system is associated with moderate historical and instrumental seismicity and recorded in sedimentary and geomorphic features. In this study, we use subsurface data coming from both published and original sources. These comprise cross-sections, seismic lines, subsurface maps and borehole data to constrain geometrically coherent local 3D geological models, with particular focus on the Pliocene and Pleistocene units. Two sections crossing five main faults and correlative anticlines are extracted to calculate slip rates on the driving thrust faults. Our slip rate calculation procedure includes a) the assessment of the onset time which is based on the sedimentary and structural architecture, b) the decompaction of clastic units where necessary, and c) the restoration of the slip on the fault planes. The assessment of the differential compaction history of clastic rocks eliminates the effects of compaction-induced subsidence which determine unwanted overestimation of slip rates. To restore the displacement along the analyzed structures, we use two different methods on the basis of the deformation style: the fault parallel flow algorithm for faulted horizons and the trishear algorithm for fault-propagation folds. The time of fault onset ranges between 5.3-2.2 Myr; overall the average slip rates of the various thrusts are in the range of 0.26-1.35 mm/yr.
    Description: Published
    Description: 122-134
    Description: 3.2. Tettonica attiva
    Description: 4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionale
    Description: JCR Journal
    Description: open
    Keywords: slip rate ; 3D geological model ; structural restoration ; seismogenic source ; thrust tectonics ; northern Apennines ; Adriatic Sea ; 04. Solid Earth::04.04. Geology::04.04.04. Marine geology ; 04. Solid Earth::04.04. Geology::04.04.09. Structural geology ; 04. Solid Earth::04.07. Tectonophysics::04.07.04. Plate boundaries, motion, and tectonics ; 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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