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  • 2
    Publication Date: 2021-05-12
    Description: An accelerating process of ground deformation that began 10 years ago is currently affecting the Campi Flegrei caldera. The deformation pattern is here explained with the overlapping of two processes: short time pulses that are caused by injection of magmatic fluids into the hydrothermal system; and a long time process of heating of the rock. The short pulses are highlighted by comparison of the residuals of ground deformation (fitted with an accelerating polynomial function) with the fumarolic CO2/CH4 and He/CH4 ratios (which are good geochemical indicators of the arrival of magmatic gases). The two independent datasets show the same sequence of five peaks, with a delay of ∼200 days of the geochemical signal with respect to the geodetic signal. The heating of the hydrothermal system, which parallels the long-period accelerating curve, is inferred by temperature–pressure gas geoindicators. Referring to a recent interpretation that relates variations in the fumarolic inert gas species to open system magma degassing, we infer that the heating is caused by enrichment in water of the magmatic fluids and by an increment in their flux. Heating of the rock caused by magmatic fluids can be a central factor in triggering unrest at calderas.
    Description: Published
    Description: 58-67
    Description: 2V. Dinamiche di unrest e scenari pre-eruttivi
    Description: JCR Journal
    Description: restricted
    Keywords: Campi Flegrei Caldera ; hydrothermal system ; ground deformation ; magmatic fluids ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2017-04-04
    Description: This study shows how the GPS technique can be utilized for seafloor displacement measurements and improved the survey control infrastructure in Campi Flegrei caldera, two thirds of which is submerged under the sea. In the Gulf of Pozzuoli, about 2.5 km from the coast where the sea depth is 97 m, a continuous GPS station (CFB1) has been installed since the end of 2011 on the top of a elastic-beacon buoy, rigidly connected by a steel cable to the ballast on the sea bottom. We investigate the use of GPS data to estimate the vertical displacement of the seafloor under the buoy. The GPS data were processed in kinematic mode and the vertical component of the measure- ments was corrected for the errors due to the horizontal motion of the buoy induced by wind and sea currents. We report here the results for approximately 17 months of continuous GPS data acquisition, and we show, for the first time, a measure of vertical displacement of the seabed in the Gulf of Pozzuoli. From January 2012 to May 2013, the seafloor uplifted by about 3–4 cm. The similarity of the pattern of the CFB1 time-series compared to the permanent GPS stations of the NeVoCGPS network located onshore is remarkable, evaluation of the Pearson's correlation coefficient between these stations and CFB1 indicates that the stations are measuring the same phe- nomenon. This result is important, because all models of evolution of bradyseism in the Campi Flegrei caldera are based on the interpretation of measures only on the emerged part of the caldera, without use of any measures to date in the Gulf of Pozzuoli. The methodology shown in this paper is reliable over time and economical, compared to other systems of measurement of marine geodesy. The major limitation is the depth of the sea, confining this technique to the shallow water, up to 100 m depth. However, a large part of the submerged Campi Flegrei caldera is shallower than 100 m, so geodetic monitoring by means of GPS buoys at several sites in the Gulf of Pozzuoli would allow to extend interpretative models to the entire caldera, submerged and emerged.
    Description: Published
    Description: 145-151
    Description: 5V. Sorveglianza vulcanica ed emergenze
    Description: JCR Journal
    Description: reserved
    Keywords: Seafloor displacement, Campi Flegrei caldera, monitoring GPS, Buoy ; 05. General::05.04. Instrumentation and techniques of general interest::05.04.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2020-02-24
    Description: Results of observations of the Mt. Vesuvius caldera, carried out by means of terrestrial laser scanning (TLS) in May 2005, October 2006 and June 2009, are reported here. In each survey the whole crater was acquired with 17/20 scans from 6 different viewpoints and the corresponding digital surface models were generated and registered into the UTM-WGS84 reference frame. In this way, a comparison between the multitemporal models leads to an evaluation of the occurred changes. The deformation maps, i.e. the contouring plots of the differences between the models along the direction of maximum variations, showed a progressive mass loss due to rock-falls from the NE vertical crater wall whose area was about View the MathML source. The TLS data also showed the accumulation at the bottom. The volume loss which occurred from 2005 to 2009, was computed by subtraction of volumes defined with respect to reference planes parallel to the caldera walls and was estimated to be View the MathML source. The volume uncertainties due to registration errors, subsampling noise effects, and effects due to choice of the reference plane, were also estimated. Some results were also interpreted on the basis of micro-seismic and meteorological data in order to plan a monitoring technique where seismic signals related to rock-fall and/or signals of intense rainfalls are used as alarms for fast TLS surveys able to characterize the corresponding changes of the caldera walls. The proposed methodology, in particular the simple but effective approach used in the estimation of volume uncertainties, can be applied to each rock slope instability phenomenon, regardless of the particular environment.
    Description: Published
    Description: 327–336
    Description: JCR Journal
    Description: restricted
    Keywords: Terrestrial laser scanning ; 04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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