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  • 1
    Publication Date: 2017-04-04
    Description: A ML=4.9 earthquake occurred in the Sannio-Matese area at 18:08 on December 29 2013. The epicenter was located in the “Monti del Matese seismic district”. The epicentral area lies between the small towns of San Gregorio Matese, Cusano Mutri, Gioia Sannitica, Piedimonte Matese, San Potito Sannita in the Caserta province in an area with an high seismic Hazard. The area was struck by large and destructive earthquakes in the past (1456, 1688, 1702, 1732, 1805,1962) with maximum magnitude up to 7.2. Past and recent seismicity of the area is generally characterized by both single events and low energy seismic sequences (1885, 1903, 1905, 1990, 1992, 1997). The last sequence occurred on 1997 with the largest event (MD = 4.1, 19 March) occurred at the border between the Benevento and Campobasso provinces followed by an intense activity ended only in September of the same year. The epicentral distribution of the 1997 low energy (M ≤ 4.0) seismic sequence is mainly NE-SW oriented suggesting the activation of anti-Apennine faults. The December 29 2013 seismic event, is located very close to the 1688 earthquake area. Still open debate is the association of the main event of the sequence and its aftershocks with the seismogenic structures present in the area. The SAGNET (Southern Apennine Geodetic NETwork) is the Non-permanent GPS network covering the area between the Matese Mounts and the Mainarde–Meta Mountains and consists of 40 3D GPS vertices. GPS dataset consists of data recorded at non-permanent stations in the time spam 2002-2014 and at the Continuous GPS stations (CGPS) of the RING network (managed of INGV) located in the central and southern Apennines regions. We have calculated the GPS velocity field with permanent and non-permanent stations (with time series of at least 3 surveys). The horizontal velocity field, expressed with respect to a fixed Eurasian plate, shows a good coherence between the velocities field estimated from the SAGNET and CGPS. In this paper we have evaluated the strain rate in the Sannio-Matese area. Before the earthquake, GPS data analysis showed a decrease in the velocity in the southern sector of Matese Massif (where the December 29 2013 earthquake epicenter will be localized) with respect to the surrounding areas which is also evident from the lower values of the strain rate ranging between 15÷20 *10-9 yr-1. Lower GPS Strain rate has been recognized at the end of seismic cycle and appear as a useful tool to point out hazardous seismic areas as already highlighted in the 2009 L'Aquila and in the 2012 Emilia earthquakes.
    Description: OGS - ENI - Dip. Scienze della Terra "Ardito Desio"
    Description: Published
    Description: Milano
    Description: 3T. Pericolosità sismica e contributo alla definizione del rischio
    Description: open
    Keywords: Sannio-Matese, GPS, deformation field, Strain Rate ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Oral presentation
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  • 2
    Publication Date: 2020-02-24
    Description: This work shows the experience acquired by the INGV-Osservatorio Vesuviano GPS Team to study the displacement field at Ischia island. After the last GPS survey, carried out in June 2010, we decided to reorganize and to reprocess the GPS data. The results were integrated with those of the three permanent GPS stations operating on the island. Data quality and repeatability have been evaluated. In order to define the GPS velocity field, we combined multi-year solutions in the period from 1998 to 2010.We defined a local reference system and analyzed the time series for a realistic error estimate. After a description of recent volcanic history and dynamics of Ischia, we describe the data-set, data processing strategy, and finally, some considerations on the achieved results are exposed.
    Description: Published
    Description: 1-61
    Description: 1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive
    Description: N/A or not JCR
    Description: open
    Keywords: GPS, Ischia Island, velocity field ; 04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2017-04-04
    Description: The Matese carbonatic massive occupies the northernmost part of the campanian Apennine while Sannio mounts, located to the East of massive, consists primarily of quaternary deposits and represent the area of Apennine chain degrading to East towards the Bradanica foredeep. The area was affected in historical time by several destructive earthquakes. The first ground deformation studies in this area started from 1990-2000 with the definition of geodetic networks, covering all or part of the massive Matese, with the aim of evaluating seismogenic sources responsible for the seismicity of the area. In 2002, a careful inspection of the existing GPS benchmarks was carried out; those which had a good state of preservation and a good level of reliability were included into a new geodetic Matese network, consisting of 38 3D benchmarks. Several surveys were conducted in 2000, 2002 and 2004,with the aim of defining the strain field, defined by plano-altimetric components. In 2005, an intensive work of gathering and validating available data started, integrating data collected by previous surveys with those collected during the new survey carried out in 2006. This work describes in detail the various stages of implementing the final network S.A.G.NET, whose geometry was also bound to the distribution of the known seismogenic sources present in the area. We also show the first results obtained from data collected from2000 to 2006 and the resulting kinematic model for this area.
    Description: Published
    Description: 3.2. Tettonica attiva
    Description: N/A or not JCR
    Description: open
    Keywords: GPS, Matese, SAGNet ; 04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2017-04-04
    Description: The Neapolitan volcanic area,located around the ciry of Naples in the Southern patt of the Campanran plain, is one of the most relevant active volcanic areas, chanctenzed by a hrgh risk, due to the dense urbantzatton and to presence of three active volcanoes (Campi Flegrei caldera, Somma-Vesuvio and Ischià Ishnd). Campi Flegrei caldera, placed west of Naples, is a well known example of peculiar ground deforàations (bradyseism), chanctenzed by period of intense uplift, nor necessarily culminating in an eruptive phase (the last eruption occurred in 1538), followed by a subsidence phase. Recently, during the 1970-1972 and 1,982-1984,t he caldera has been affected by two intense episode of intense uplift (sine eruption). In 1985 a subsidence phase started (with some episodic small and fast uplifts superimposed) and terminated at end of 2004. Somma-Vesuvio, at east of Naples, is a quiescent volcano (the last eruption occurred in 1944) and is charactenzed by a low level of ground deformatio.r, .*..p. small and limited subsidence are s, located near craLter area and around the volcanic edifice. Ischia island, at S\ù7 of Naples, has been characterrzed rn the past times by a both explosive and effusive volcanic activity (the last eruption occurred in 1302). Successively the ground deformation activity has been charactenzed by a meaningful subsidence in the S and NW sectors of the island. Ground deformation is usualy ónnected with pressure changes of magma reservoirs or with intrusive events. So, monitoring and analysis of ground deformations are important tools in order to understanding the geometry, dynamics and evolution of thr source. The NeVoCGPS QNeapolitan Volcanic Continuous GPS) network consists of 25 stations (Fig. 1), managed by remote control. The data are automatically downloaded and proceised daily by the Ultra rapid IGS products. \ù7hen the IGS final orbits and Earth rotation parameters (trRPt become avallable the data are reprocessed and weekly solutionr àr. obtained, also. The data processing is performed by the Bernese Processing Engine (BPE) of the Bernese GPS software v. 5.0 in double difference mode. The èlevaiion cut-off is set at 1'5o and the IGS absolute phase centre variations (APCVO for the satellite and receiver antennas are applied. To minimize the tectonic movements contribution, the GPS position time series are estimated relative to the stable station ENAV located outside the volcanTc area. The NeVoCGPS datahave been always very useful for ground deformadon study, pointing out also small intensity phenome na, that usually are not discriminated by discontinuous measures.
    Description: Published
    Description: Nicolosi (Catania)
    Description: 1.1. TTC - Monitoraggio sismico del territorio nazionale
    Description: 1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive
    Description: 1.9. Rete GPS nazionale
    Description: open
    Keywords: GPS permanenti per il monitoraggio ; NeVoCGPS ; Campanian plain ; ground movements activity ; intense uplift ; Campi Flegrei caldera, Somma-Vesuvio and Ischià Ishnd ; 04. Solid Earth::04.03. Geodesy::04.03.99. General or miscellaneous ; 04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring ; 04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 5
    Publication Date: 2017-04-04
    Description: Osservatorio Vesuviano, department of Istituto Nazionale di Geofisica e Vulcanologia, installed a permanent GPS network (NeVoCGPS), constituted of 25 stations, in Neapolitan volcanic area, where three active volcanoes (Somma-Vesuvius, Campi Flegrei caldera and Ischia Island) rise, each characterized by a peculiar type of ground movements activity. The Somma-Vesuvius system exhibits now a low level of ground deformation; the Campi Flegrei, caracterized from over 2000 years by slow up and down vertical movements (bradyseism), at present is in a very slow uplift phase; Ischia, finally, shows subsidence in the specific areas (Southern and North-West sectors of the island). The presence of these volcanoes and the dense urbanization of the area make the ground deformation monitoring a crucial point for risk mitigation and modelling aims. The 3D ground displacements are calculated using CGPS data, acquired with a 30s rate and with the daily and weekly vertexes position estimate. All the stations are managed by remote control and the data are automatically downloaded and processed using Bernese software package. The entire chain of acquisition, processing and data analysis is accurately described and some results obtained in the last years are shown.
    Description: Published
    Description: held 19-24 April, 2009 in Vienna, Austria http://meetings.copernicus.org/egu2009
    Description: 1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive
    Description: 1.9. Rete GPS nazionale
    Description: open
    Keywords: permanent GPS network ; NeVoCGPS ; Somma-Vesuvius, Campi Flegrei caldera and Ischia Island ; ground movements activity ; 04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring ; 05. General::05.09. Miscellaneous::05.09.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 6
    Publication Date: 2017-04-04
    Description: L’Osservatorio Vesuviano, Sezione di Napoli dell’Istituto Nazionale di Geofisica e Vulcanologia, gestisce il sistema di monitoraggio per la sorveglianza delle aree vulcaniche del Somma Vesuvio, dei Campi Flegrei e dell’isola d’Ischia. Tale sistema comprende reti geofisiche e geochimiche: quelle geofisiche controllano l’attività sismica, le deformazioni del suolo e le variazioni del campo gravimetrico, mentre quelle geochimiche misurano la composizione chimica dei gas emessi dalle fumarole e di quelli disciolti nelle acque di falda. Per quanto concerne l’isola d’Ischia, il controllo delle deformazioni del suolo viene effettuato utilizzando tecniche classiche (livellazioni di precisione, gravimetria, mareometria) e metodi satellitari (GPS, SAR). In particolare, sull’isola sono state installate una rete di livellazione, una rete gravimetrica, un mareografo e una rete GPS. Nel corso del primo semestre del 2010, sull’isola d’Ischia sono state effettuate una campagna gravimetrica, una di livellazione ed una di misure GPS. Oggetto di questo rapporto è la descrizione dell’attività svolta durante la campagna di misure GPS realizzata dal 28 maggio (DoY 148) al 11 giugno (DoY 162) 2010.
    Description: Istituto Nazionale di Geofisica e Vulcanologia
    Description: Published
    Description: 1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive
    Description: open
    Keywords: misure GPS ; Ischia ; 04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: report
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  • 7
    Publication Date: 2017-04-04
    Description: The Neapolitan volcanic area is located in the southern part of the Campanian plain and includes three active volcanoes (Vesuvius, Campi Flegrei Caldera and Ischia Island). This area shows different dynamical behaviours. Campi Flegrei caldera represents one well known and peculiar example of ground deformations (bradyseism), with periods of intense uplift during the 1969-72 and 1982-84, followed by subsidence phase with some episodic mini-uplifts superimposed. Contrary, Vesuvius is a substantially stable volcano, with small and localized subsidence mainly in the crater zone. Ischia Island has been characterized by subsidence in the S and NW sectors of the island. The presence of these three volcanoes in a dense populated area, makes ground deformation detection a crucial point in the risk mitigation. Ground deformation is an important volcanic precursor, because linked to magma overpressure and migration, thus, continuous monitoring and modelling is one of the main instruments to attempt for a short time forecast of eruptive activity. Since several years, the INGV – Osservatorio Vesuviano installed a permanent GPS network (NeVoCGPS), constituted of 27 stations, in the Neapolitan volcanic area with a configuration that guarantees a continuous and fast 3D information about the dynamics of the area. All the GPS stations are managed by remote control, the data are daily downloaded automatically. After an automatic quality control procedure, the data processing is performed by the Bernese Processing Engine (BPE) of the Bernese GPS software v. 5.0. In this work, the entire chain of data acquisition and processing is described and some results obtained in last years are presented.
    Description: INGV,Sezione di Napoli,Osservatorio Vesuviano
    Description: Published
    Description: Puerto de la Cruz, Tenerife (Canary Islands, Spain)
    Description: open
    Keywords: GPS Monitoring ; Vesuvio ; Campi Flegrei Caldera ; Ischia Island ; 04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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  • 8
    Publication Date: 2022-05-26
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Microbiology 4 (2013): 189, doi:10.3389/fmicb.2013.00189.
    Description: The vast marine deep biosphere consists of microbial habitats within sediment, pore waters, upper basaltic crust and the fluids that circulate throughout it. A wide range of temperature, pressure, pH, and electron donor and acceptor conditions exists—all of which can combine to affect carbon and nutrient cycling and result in gradients on spatial scales ranging from millimeters to kilometers. Diverse and mostly uncharacterized microorganisms live in these habitats, and potentially play a role in mediating global scale biogeochemical processes. Quantifying the rates at which microbial activity in the subsurface occurs is a challenging endeavor, yet developing an understanding of these rates is essential to determine the impact of subsurface life on Earth's global biogeochemical cycles, and for understanding how microorganisms in these “extreme” environments survive (or even thrive). Here, we synthesize recent advances and discoveries pertaining to microbial activity in the marine deep subsurface, and we highlight topics about which there is still little understanding and suggest potential paths forward to address them. This publication is the result of a workshop held in August 2012 by the NSF-funded Center for Dark Energy Biosphere Investigations (C-DEBI) “theme team” on microbial activity (www.darkenergybiosphere.org).
    Description: Funding for the meeting was provided by C-DEBI, a US National Science Foundation (NSF)-funded Science and Technology Center (OCE-0939564). Funding for this publication was provided, in part, by NSF (OCE-1233226 to BNO).
    Keywords: Deep biosphere ; IODP ; Biogeochemistry ; Sediment ; Oceanic crust ; C-DEBI ; Subsurface microbiology
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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