0000000000343986

AUTHOR

Simona Petrosino

0000-0002-5042-0244

showing 4 related works from this author

Interaction between seismicity and deformation on different time scales in volcanic areas: Campi Flegrei and Stromboli

2019

We study oscillations recorded at Stromboli and Campi Flegrei by different sensors: seismometers, strainmeters and tiltmeters. We examine both the high-frequency (>0.5 Hz) portion of the spectrum and very long period signals up to tidal scales. In this context, seismicity and deformation are investigated on different time scales (from minutes to days/years) in order to identify the basic elements of their interaction, whose understanding should provide new insights on the predictive models. In this work, the strict relation of tides and volcanic processes is shown. At Stromboli, indeed the transition from the stationary phase to the non-stationary phase seems to have a tidal precu…

Seismometer010504 meteorology & atmospheric scienceslcsh:Dynamic and structural geologyanalysisfrequency analysisTiltmeterContext (language use)VolcanismInduced seismicity010502 geochemistry & geophysicsdiurnal variation01 natural sciencesvolcanic eruptionvolcanologylcsh:QE500-639.5lcsh:Science0105 earth and related environmental sciencesgeographyvolcanismgeography.geographical_feature_categoryVulcanian eruptionlcsh:QE1-996.5deformationGeneral MedicineVolcanologydeformation; diurnal variation; frequency analysis; numerical model; seismicity; time series; analysis; volcanic eruption; volcanism;volcanologylcsh:GeologyVolcanolcsh:Qseismicitytime seriesnumerical modelGeologySeismology
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Characterization of the seismic dynamical state through joint analysis of earthquakes and seismic noise: the example of Ischia Volcanic Island (Italy)

2020

This work is devoted to the study of both earthquakes and background seismic noise at Ischia Island (Italy) recorded pre and post the Md 4.0 earthquake occurred on 21 August 2017 (18:57 UTC). We compare and characterize noise and earthquakes in terms of Independent Component Analysis, energy and polarization properties. The earthquakes' waveforms and the background noise are decomposed into a few independent components with two main common signals peaked around 1–2 and 3–4 Hz, respectively. A slight increase of the energy of the background seismic noise is observed comparing samples recorded in 2016 and 2017, whereas no variations are detected in 2017 pre and post the main ear…

lcsh:Dynamic and structural geology010504 meteorology & atmospheric sciencesVolcanic islandlcsh:QE1-996.5General MedicineJoint analysisSeismic noise01 natural sciencesIndependent component analysislcsh:GeologyAzimuthBackground noiselcsh:QE500-639.5lcsh:Qlcsh:SciencePre and postGeologyNoise (radio)Seismology0105 earth and related environmental sciencesAdvances in Geosciences
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Crustal dynamics of Mount Vesuvius from 1998 to 2005: Effects on seismicity and fluid circulation

2008

[1] This paper presents the results of hydrogeochemical and seismological studies carried out at Mount Vesuvius during the period June 1998 to December 2005. Hydrogeochemical data show the occurrence of slowly varying long-term variations in the total dissolved salts and bicarbonate contents of the groundwaters, accompanied by a general decline in water temperatures. The temporal distributions of air temperature and rainfall in the Vesuvius area suggest that these variations do not depend on changes in the hydrological regime. The changes in the geochemical parameters are accompanied by slight variations in both the seismicity rate and energy release. A further relationship between seismic …

Atmospheric ScienceSoil Sciencehydrogeochemistry vesuviusAquiferAquatic ScienceInduced seismicityOceanographyGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyPaleontologyForestryAtmospheric temperatureStress fieldGeophysicsVolcanoShear (geology)Space and Planetary ScienceSedimentary rockGroundwaterGeologySeismologyJournal of Geophysical Research
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Time evolution of medium and long-period ground tilting at Campi Flegrei caldera

2020

Abstract. We analyse tiltmeter time series recorded from April 2015 to March 2019 at three borehole instruments installed at Campi Flegrei caldera (Italy). We evaluate the crustal response in terms of ground tilting to external excitations of medium/long-period tidal constituents by applying a polarization analysis. The azimuths of the tilt vectors show well-defined polarization directions and the ground tilting planes oscillate with the periodicity of the corresponding tidal constituents. For two of the three tiltmeters, the average ground oscillation pattern related to the monthly Mm and fortnightly Mf constituents show seasonal variations, which can be ascribed to rainfall-induced tiltin…

lcsh:Dynamic and structural geology010504 meteorology & atmospheric sciencesOscillationlcsh:QE1-996.5BoreholeTiltmeterGeneral MedicineGeodesyPolarization (waves)01 natural sciencesPhysics::Geophysicslcsh:GeologyAzimuthStress fieldThermoelastic dampinglcsh:QE500-639.5Calderalcsh:Qlcsh:ScienceGeology0105 earth and related environmental sciencesAdvances in Geosciences
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