Low frequency seismic source investigation in volcanic environment: the Mt. Vesuvius atypical case
Simona Petrosino
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli –
Osservatorio Vesuviano, Naples, Italy
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli –
Osservatorio Vesuviano, Naples, Italy
Related authors
Paola Cusano, Enza De Lauro, Antonietta Esposito, Mariarosaria Falanga, Danilo Galluzzo, and Simona Petrosino
Adv. Geosci., 52, 153–158, https://doi.org/10.5194/adgeo-52-153-2021, https://doi.org/10.5194/adgeo-52-153-2021, 2021
Lucia Nardone, Roberta Esposito, Danilo Galluzzo, Simona Petrosino, Paola Cusano, Mario La Rocca, Mauro Antonio Di Vito, and Francesca Bianco
Adv. Geosci., 52, 75–85, https://doi.org/10.5194/adgeo-52-75-2020, https://doi.org/10.5194/adgeo-52-75-2020, 2020
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We studied the subsoil structure of the Campi Flegrei area using both spectral ratios and array techniques (f-k and MSPAC) applied to seismic noise recorded by three different array. By means of joint inversion of dispersion curve and spectral ratio we obtained a Vs model, that is in a good agreement with the stratigraphic information available in the area. In areas such as Campi Flegrei the definition of the velocity model is a crucial issue to characterize the physical parameters of the medium
Teresa Caputo, Paola Cusano, Simona Petrosino, Fabio Sansivero, and Giuseppe Vilardo
Adv. Geosci., 52, 55–65, https://doi.org/10.5194/adgeo-52-55-2020, https://doi.org/10.5194/adgeo-52-55-2020, 2020
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The Solfatara volcano (Italy), is monitored by a thermal infrared camera ground network handled by INGV. The dataset processed in this work consists of daily maximum temperatures time-series from 25 April 2014 to 31 May 2019. After a pre-processing, PSD's were calculated, filtering in [15–120] day band, to check if characteristic periodicities exist. Most of the periodicities are ascribable to ambient factors, while 18.16 and 88.71 days have a possible endogenous origin.
Paola Cusano, Simona Petrosino, Enza De Lauro, Salvatore De Martino, and Mariarosaria Falanga
Adv. Geosci., 52, 19–28, https://doi.org/10.5194/adgeo-52-19-2020, https://doi.org/10.5194/adgeo-52-19-2020, 2020
Simona Petrosino, Ciro Ricco, Enza De Lauro, Ida Aquino, and Mariarosaria Falanga
Adv. Geosci., 52, 9–17, https://doi.org/10.5194/adgeo-52-9-2020, https://doi.org/10.5194/adgeo-52-9-2020, 2020
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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.
The results indicate that the tidal tilting is mainly controlled by the local stress field distribution and rheology; in addition, seasonal exogenous factors like rainfalls play a role in modulating the ground deformation.
Mariarosaria Falanga, Enza De Lauro, Simona Petrosino, and Salvatore De Martino
Adv. Geosci., 52, 1–8, https://doi.org/10.5194/adgeo-52-1-2019, https://doi.org/10.5194/adgeo-52-1-2019, 2019
Short summary
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We study oscillations recorded at Stromboli and Campi Flegrei by different sensors. Seismicity and deformation are investigated on several time scales in order to identify the basic elements of their interaction, whose understanding should provide new insights on the predictive models. At Stromboli, a departure from the equilibrium state is marked by solid tide variations in a certain frequency band. At Campi Flegrei diurnal to annual solid tides modulate an increase of volcanic activity.
Paola Cusano, Enza De Lauro, Antonietta Esposito, Mariarosaria Falanga, Danilo Galluzzo, and Simona Petrosino
Adv. Geosci., 52, 153–158, https://doi.org/10.5194/adgeo-52-153-2021, https://doi.org/10.5194/adgeo-52-153-2021, 2021
Lucia Nardone, Roberta Esposito, Danilo Galluzzo, Simona Petrosino, Paola Cusano, Mario La Rocca, Mauro Antonio Di Vito, and Francesca Bianco
Adv. Geosci., 52, 75–85, https://doi.org/10.5194/adgeo-52-75-2020, https://doi.org/10.5194/adgeo-52-75-2020, 2020
Short summary
Short summary
We studied the subsoil structure of the Campi Flegrei area using both spectral ratios and array techniques (f-k and MSPAC) applied to seismic noise recorded by three different array. By means of joint inversion of dispersion curve and spectral ratio we obtained a Vs model, that is in a good agreement with the stratigraphic information available in the area. In areas such as Campi Flegrei the definition of the velocity model is a crucial issue to characterize the physical parameters of the medium
Teresa Caputo, Paola Cusano, Simona Petrosino, Fabio Sansivero, and Giuseppe Vilardo
Adv. Geosci., 52, 55–65, https://doi.org/10.5194/adgeo-52-55-2020, https://doi.org/10.5194/adgeo-52-55-2020, 2020
Short summary
Short summary
The Solfatara volcano (Italy), is monitored by a thermal infrared camera ground network handled by INGV. The dataset processed in this work consists of daily maximum temperatures time-series from 25 April 2014 to 31 May 2019. After a pre-processing, PSD's were calculated, filtering in [15–120] day band, to check if characteristic periodicities exist. Most of the periodicities are ascribable to ambient factors, while 18.16 and 88.71 days have a possible endogenous origin.
Paola Cusano, Simona Petrosino, Enza De Lauro, Salvatore De Martino, and Mariarosaria Falanga
Adv. Geosci., 52, 19–28, https://doi.org/10.5194/adgeo-52-19-2020, https://doi.org/10.5194/adgeo-52-19-2020, 2020
Simona Petrosino, Ciro Ricco, Enza De Lauro, Ida Aquino, and Mariarosaria Falanga
Adv. Geosci., 52, 9–17, https://doi.org/10.5194/adgeo-52-9-2020, https://doi.org/10.5194/adgeo-52-9-2020, 2020
Short summary
Short summary
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.
The results indicate that the tidal tilting is mainly controlled by the local stress field distribution and rheology; in addition, seasonal exogenous factors like rainfalls play a role in modulating the ground deformation.
Mariarosaria Falanga, Enza De Lauro, Simona Petrosino, and Salvatore De Martino
Adv. Geosci., 52, 1–8, https://doi.org/10.5194/adgeo-52-1-2019, https://doi.org/10.5194/adgeo-52-1-2019, 2019
Short summary
Short summary
We study oscillations recorded at Stromboli and Campi Flegrei by different sensors. Seismicity and deformation are investigated on several time scales in order to identify the basic elements of their interaction, whose understanding should provide new insights on the predictive models. At Stromboli, a departure from the equilibrium state is marked by solid tide variations in a certain frequency band. At Campi Flegrei diurnal to annual solid tides modulate an increase of volcanic activity.
Cited articles
Abercrombie, R. E.: Earthquake source scaling relationships from -1 to 5ML
using seismograms recorded at 2.5-km depth, J. Geophys. Res., 100,
24015–24036, https://doi.org/10.1029/95JB02397, 1995.
Auger, E., Gasparini, P., Virieux, J., and Zollo, A.: Seismic evidence of an
extended magmatic sill under Mt. Vesuvius, Science, 294, 1510–1512,
https://doi.org/10.1126/science.1064893, 2001.
Bianco, F., Castellano, M., Milano, G., Ventura, G., and Vilardo, G.: The
Somma–Vesuvius stress field induced by regional tectonics: evidences from
seismological and mesostructural data, J. Volcanol. Geoth. Res., 82,
199–218, 1998.
Bianco, F., Cusano, P., Petrosino, S., Castellano, M., Buonocunto, C.,
Capello, M., and Del Pezzo, E.: Small-aperture array for seismic monitoring
of Mt. Vesuvius, Seismol. Res. Lett., 76, 344–355,
https://doi.org/10.1785/gssrl.76.3.344, 2005.
Bean, C., Lokmer, I., and O'Brien, G.: Influence of near-surface volcanic
structure on long-period seismic signals and on moment tensor inversions:
Simulated examples from Mount Etna, J. Geophys. Res., 113, B08308,
https://doi.org/10.1029/2007JB005468, 2008.
Bean, C. J., De Barros, L., Lokmer, I., Métaxian, J. P., O'Brien, G.,
and Murphy, S.: Long-period seismicity in the shallow volcanic edifice
formed from slow-rupture earthquakes, Nat. Geosci., 7, 71–75,
https://doi.org/10.1038/ngeo2027, 2014.
Caliro, S., Chiodini, G., Avino, R., Minopoli, C., and Bocchino, B.: Long
time-series of chemical and isotopic compositions of Vesuvius fumaroles:
evidence for deep and shallow processes, Ann. Geophys, 54, 137–149, https://doi.org/10.4401/ag-5034, 2011.
Capuano, P., De Lauro, E., De Martino, S., and Falanga, M.: Detailed
investigation of long-period activity at Campi Flegrei by convolutive
independent component analysis, Phys. Earth Planet. In., 253, 48–57,
https://doi.org/10.1016/j.pepi.2016.02.003, 2016.
Capuano, P., De Lauro, E., De Martino, S., Falanga, M., and Petrosino, S.:
Convolutive independent component analysis for processing massive datasets:
a case study at Campi Flegrei (Italy), Nat. Hazards, 86, 417–429, https://doi.org/10.1007/s11069-016-2545-0, 2017.
Chouet, B. A. and Matoza, R. S.: A multi-decadal view of seismic methods
for detecting precursors of magma movement and eruption, J. Volcanol.
Geoth. Res., 252, 108–175,
https://doi.org/10.1016/j.jvolgeores.2012.11.013, 2013.
Coté, D. M., Belachew, M., Quillen, A. C., Ebinger, C. J., Keir, D.,
Ayele, A., and Wright, T.: Low-frequency hybrid earthquakes near a magma
chamber in Afar: quantifying path effects, B. Seismol. Soc. Am., 100,
1892–1903, https://doi.org/10.1785/0120090111, 2010.
Cusano, P., Petrosino, S., Bianco, F., and Del Pezzo, E.: The first Long
Period earthquake detected in the background seismicity at Mt. Vesuvius,
Ann. Geophys., 56, S0440, https://doi.org/10.4401/ag-6447.S0440, 2013a.
Cusano, P., Petrosino, S., Madonia, P., and Federico, C.: Seismic activity and
thermal regime of low temperature fumaroles at Mt. Vesuvius in 2004-2011:
distinguishing among seismic, volcanic and hydrological signals, Ann.
Geophys., 56, S0441, https://doi.org/10.4401/ag-6446, 2013b.
Cusano, P., Petrosino, S., De Lauro, E., and Falanga, M.: The whisper of the
hydrothermal seismic noise at Ischia Island, J. Volcanol. Geoth. Res., 389,
106693, https://doi.org/10.1016/j.jvolgeores.2019.106693, 2020.
D'Auria, L., Massa, B., and De Matteo, A.: The stress field beneath a
quiescent stratovolcano: The case of Mount Vesuvius, J. Geophys. Res.-Sol.
Ea., 119, 1181–1199, https://doi.org/10.1002/2013JB010792, 2014.
De Lauro, E., De Martino, S., Del Pezzo, E., Falanga, M., Palo, M., and
Scarpa, R.: Model for high-frequency Strombolian tremor inferred by
wavefield decomposition and reconstruction of asymptotic dynamics, J.
Geophys. Res.-Sol. Ea., 113, B02302, https://doi.org/10.1029/2006JB004838, 2008.
De Lauro, E., Falanga, M., and Petrosino, S.: Study on the long period
source mechanism at Campi Flegrei (Italy) by a multiparametric analysis,
Phys. Earth Planet. In., 206–207, 16–30,
https://doi.org/10.1016/j.pepi.2012.06.006, 2012.
De Lauro, E., Petrosino, S., Ricco, C., Aquino, I., and Falanga, M.: Medium
and long period ground oscillatory pattern inferred by borehole tiltmetric
data: New perspectives for the Campi Flegrei caldera crustal dynamics, Earth
Planet. Sc. Lett., 504, 21–29, https://doi.org/10.1016/j.epsl.2018.09.039, 2018.
Del Pezzo, E. and Bianco, F.: Inside Mt. Vesuvius: a new method to look at
the seismic (velocity and attenuation) tomographic imaging, Ann. Geophys,
56, S0443, https://doi.org/10.4401/ag-6449, 2013.
Del Pezzo, E., Chiodini, G., Caliro, S., Bianco, F., and Avino, R.: New
insights into Mt. Vesuvius hydrothermal system and its dynamic based on a
critical review of seismic tomography and geochemical features, Ann.
Geophys., 56, S0444, https://doi.org/10.4401/ag-6450, 2013.
Eyre, T. S., Bean, C. J., De Barros, L., Martini, F., Lokmer, I., Mora, M.
M.,. Pacheco, J. F., and Soto, G. J.: A brittle failure model for
long-period seismic events recorded at Turrialba Volcano, Costa Rica, J.
Geophys. Res., 120, 1452–1472, https://doi.org/10.1002/2014JB011108,
2015.
Federico, C., Madonia, P., Cusano, P., and Petrosino, S.: Groundwater
geochemistry of the Mt. Vesuvius area: implications for volcano surveillance
and relationship with hydrological and seismic signals, Ann. Geophys.,
56, S0447, https://doi.org/10.4401/ag-6453, 2013.
Galluzzo, D., Del Pezzo, E., La Rocca, M., and Petrosino, S.: Peak ground
acceleration produced by local earthquakes in volcanic areas of Campi
Flegrei and Mt. Vesuvius, Ann. Geophys., 47, 1377–1389, https://doi.org/10.4401/ag-4401, 2004.
Greenfield, T., Keir, D., Kendall, J. M., and Ayele, A.: Low-frequency
earthquakes beneath Tullu Moye volcano, Ethiopia, reveal fluid pulses from
shallow magma chamber, Earth Planet. Sc.
Lett., 526, 115782, https://doi.org/10.1016/j.epsl.2019.115782, 2019.
Harrington, R. M. and Benson, P. M.:. Analysis of laboratory simulations of
volcanic hybrid earthquakes using empirical Green's functions, J. Geophys.
Res., 116, B11303, https://doi.org/10.1029/2011JB008373, 2011.
Harrington, R. M. and Brodsky, E. E.: Volcanic hybrid earthquakes that are
brittle-failure events, Geophys. Res. Lett., 34, L06308,
https://doi.org/10.1029/2006GL028714, 2007.
Harrington, R. M., Kwiatek, G., and Moran, S. C.: Self-similar rupture
implied by scaling properties of volcanic earthquakes occurring during the
2004–2008 eruption of Mount St. Helens, Washington, J. Geophys. Res.,
120, 4966–4982, https://doi.org/10.1002/2014JB011744, 2015.
Horton, S., Norris, R. D., and Moran, S.: Broadband characteristics of
earthquakes recorded during a dome-building eruption at Mount St. Helens,
Washington, between October 2004 and May 2005, in: A Volcano Rekindled: The
Renewed Eruption of Mount St. Helens, 2004–2006, 97–110, U.S. Geological
Survey Professional Paper 1750, 2008.
Julian, B. R.: Volcanic tremor: nonlinear excitation by fluid flow, J.
Geophys. Res., 99, 11859–11877, https://doi.org/10.1029/93JB03129,
1994.
La Rocca, M. and Galluzzo, D.: Seismic monitoring of Campi Flegrei and Mt.
Vesuvius by stand alone instruments, Ann. Geophys., 58, S0544,
https://doi.org/10.4401/ag-6748, 2015.
La Rocca, M. and Galluzzo, D.: Volcanic tremor at Mt Vesuvius associated
with low frequency shear failures, Earth Planet. Sc. Lett., 442, 32–38,
https://doi.org/10.1016/j.epsl.2016.02.048, 2016.
Lomax, A., Virieux, J., Volant, P., and Berge, C.: Probabilistic earthquake
location in 3D and layered models: Introduction of a
Metropolis-Gibbs method and comparison with linear locations, in: Advances in
Seismic Event Location, edited by: Thurber, C. H. and Rabinowitz, N., 101–134,
Kluwer, 2000.
Madonia, P., Federico, C., Cusano, P., Petrosino, S., Aiuppa, A., and
Gurrieri, S.: Crustal dynamics of Mount Vesuvius from 1998 to 2005: Effects
on seismicity and fluid circulation, J. Geophys. Res., 113, B05206,
https://doi.org/10.1029/2007JB005210, 2008.
McNutt, S. R.: Volcanic seismology, Annu. Rev. Earth Pl. Sc., 32,
461–491, 2005.
Montalbetti, J. F. and Kanasewich, E. R.: Enhancement of teleseismic body
phases with a polarization filter, Geophys. J. Int., 21, 119–129,
https://doi.org/10.1111/j.1365-246X.1970.tb01771.x, 1970.
Neuberg, J., Luckett, R., Baptie, B., and Olsen, K.: Models of tremor and
low-frequency earthquake swarms on Montserrat, J. Volcanol. Geoth. Res.,
101, 83–104, https://doi.org/10.1016/S0377-0273(00)00169-4, 2000.
Orazi, M., D'Auria, L., Tramelli, A., Buonocunto, C., Capello, M., Caputo, A., De Cesare, W., Giudicepietro, F., Martini, M., Peluso, R., and Scarpato, G.: The seismic monitoring network of Mt. Vesuvius, Ann. Geophys., 56, S0450, https://doi.org/10.4401/ag-6456, 2013.
Peng, Z. and Gomberg, J.: An integrated perspective of the continuum
between earthquakes and slow-slip phenomena, Nat. Geosci., 3,
599–607, https://doi.org/10.1038/ngeo940, 2010.
Petrosino, S., Cusano, P., and Madonia, P.: Tidal and hydrological
periodicities of seismicity reveal new risk scenarios at Campi Flegrei
caldera, Sci. Rep., 8, 13808, https://doi.org/10.1038/s41598-018-31760-4, 2018.
Piochi, M., Bruno, P. P., and De Astis, G.: Relative roles of rifting
tectonics and magma ascent processes: Inferences from geophysical,
structural, volcanological, and geochemical data for the Neapolitan volcanic
region (southern Italy), Geochem. Geophy. Geosy., 6, Q07005,
https://doi.org/10.1029/2004GC000885, 2005.
Saccorotti, G., Ventura, G., and Vilardo, G.: Seismic swarms related to
diffusive processes: The case of Somma-Vesuvius volcano, Italy, Geophysics,
67, 199–203, https://doi.org/10.1190/1.1451551, 2002.
Ricco, C., Petrosino, S., Aquino, I., Del Gaudio, C., and Falanga, M.: Some
Investigations on a Possible Relationship between Ground Deformation and
Seismic Activity at Campi Flegrei and Ischia Volcanic Areas (Southern
Italy), Geosciences, 9, 222, https://doi.org/10.3390/geosciences9050222, 2019.
Soosalu, H., Key, J., White, R. S., Knox, C., Einarsson, P., and
Jakobsdóttir, S. S: Lower-crustal earthquakes caused by magma movement
beneath Askja volcano on the north Iceland rift, B. Volcanol., 72, 55–62,
https://doi.org/10.1007/s00445-009-0297-3, 2010.
Tepp, G., Ebinger, C. J., and Yun, S. H.: Spectral analysis of dike-induced
earthquakes in Afar, Ethiopia, J. Geophys. Res., 121, 2560–2574, https://doi.org/10.1002/2015JB012658, 2016.
Wessel, P. and Smith, W. H. F.: New, improved version of the generic mapping tools released, EOS Trans AGU, 79, p. 579, 1998.
Short summary
We present a detailed analysis of the atypical low frequency seismicity occurred at Mt. Vesuvius in 2003-2018. The different decay patterns of the spectra, the existence of families as well as single events, the wide seismogenic volume, indicate that these events are caused by distinct source mechanisms: slow brittle failure in dry rocks and resonance of fluid-filled cracks. On these basis, we classified the earthquakes as Low Frequency (LF) and Long Period (LP).
We present a detailed analysis of the atypical low frequency seismicity occurred at Mt. Vesuvius...