Options
Noise-based seismic monitoring of the Campi Flegrei caldera
Language
English
Obiettivo Specifico
4V. Dinamica dei processi pre-eruttivi
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Title of the book
Issue/vol(year)
/44 (2017)
Pages (printed)
2237–2244
Issued date
March 6, 2017
Subjects
Abstract
The Campi Flegrei caldera is one of the highest risk volcanic fields worldwide, because
of its eruptive history and the large population hosted within the caldera. It experiences bradiseismic crises: sudden uplift with low energetic seismic swarm occurrences. No seismicity is recorded out of these deformation rate changes. Therefore, a continuous seismic monitoring of the caldera is possible only
by means of the ambient seismic noise. We apply a noise-based seismic monitoring technique to
the cross correlations of 5 year recordings at the mobile seismic network. The resulting relative velocity variations are compared to the temporal behavior of the geophysical and geochemical observations routinely sampled at Campi Flegrei. We discriminate between two kinds of crustal stress field variations acting at different timescales. They are related to a possible magmatic intrusion and to the gradual heating of the hydrothermal system, respectively. This study sets up the basis for future volcano monitoring strategies.
of its eruptive history and the large population hosted within the caldera. It experiences bradiseismic crises: sudden uplift with low energetic seismic swarm occurrences. No seismicity is recorded out of these deformation rate changes. Therefore, a continuous seismic monitoring of the caldera is possible only
by means of the ambient seismic noise. We apply a noise-based seismic monitoring technique to
the cross correlations of 5 year recordings at the mobile seismic network. The resulting relative velocity variations are compared to the temporal behavior of the geophysical and geochemical observations routinely sampled at Campi Flegrei. We discriminate between two kinds of crustal stress field variations acting at different timescales. They are related to a possible magmatic intrusion and to the gradual heating of the hydrothermal system, respectively. This study sets up the basis for future volcano monitoring strategies.
References
Amoruso, A., L. Crescentini, I. Sabbetta, P. De Martino, U. Obrizzo, and U. Tammaro (2014), Clues to the cause of the 2011–2013 Campi Flegrei caldera unrest, Italy, from continuous GPS data, Geophys. Res. Lett., 41, 3081–3088, doi:10.1002/2014GL059539.
Aster, R., R. P. Meyer, G. De Natale, A. Zollo, M. Martini, E. Del Pezzo, R. Scarpa, and G. Iannaccone (1992), Seismic investigation of Campi Flegrei caldera, in Volcanic Seismology, Proc. Volcanol. Series III, Springer, New York.
Bianco, F., and L. Zaccarelli (2009), A reappraisal of shear wave splitting parameters from Italian active volcanic areas through a semiautomatic algorithm, J. Seismol., 13, 253–266, doi:10.1007/s10950-008-9125-z.
Brenguier, F., N. M. Shapiro, M. Campillo, V. Ferrazzini, Z. Duputel, O. Coutant, and A. Nercessian (2008), Towards forecasting volcanic eruptions using seismic noise, Nat. Geosci., 1, 126–130.
Brenguier, F., M. Campillo, T. Takeda, Y. Aoki, N. M. Shapiro, X. Briand, K. Emoto, and H. Miyake (2014), Mapping pressurized volcanic fluids from induced crustal seismic velocity drops, Science, 345, 80–82.
Campillo, M. (2006), Phase and correlation in random seismic fields and the reconstruction of the Green function, Pure Appl. Geophys., 163, 475–502.
Chiodini, G., S. Caliro, P. De Martino, R. Avino, and F. Gherardi (2012), Early signals of new volcanic unrest at Campi Flegrei caldera? Insights from geochemical data and physical simulations, Geology, 40, 943–946, doi:10.1130/G33251.1.
Chiodini, G., J. Vandemeulebrouck, S. Caliro, L. D’Auria, P. De Martino, A. Mangiacapra, and Z. Petrillo (2015), Evidence of thermal-driven processes triggering the 2005–2014 unrest at Campi Flegrei caldera, Earth Planet. Sci. Lett., 414, 58–67.
Chiodini, G., A. Paonita, A. Aiuppa, A. Costa, S. Caliro, P. De Martino, V. Acocella, and J. Vandemeulebrouck (2016), Magmas near the critical degassing pressure drive volcanic unrest towards a critical state, Nat. Commun., 7, 13712, doi:10.1038/ncomms13712.
D’Auria, L., et al. (2015), Magma injection beneath the urban area of Naples: A new mechanism for the 2012–2013 volcanic unrest at Campi Flegrei caldera, Sci. Rep., 5, 13100, doi:10.1038/srep13100.
Derode, A., E. Larose, M. Tanter, J. de Rosny, A. Tourin, M. Campillo, and M. Fink (2003), Recovering the Greens function from field—Field correlations in an open scattering medium (L), J. Acoust. Soc. Am., 113, 2973–2976.
De Martino, P., U. Tammaro, and F. Obrizzo (2014), GPS time series at Campi Flegrei caldera (2000–2013), Ann. Geophys., 57(2), S0213, doi:10.4401/ag-6431.
De Siena, L., E. Del Pezzo, and F. Bianco (2011), A scattering image of Campi Flegrei from the autocorrelation functions of velocity tomograms, Geophys. J. Int., 184, 1304–1310, doi:10.1111/j.1365-246X.2010.04911.x.Di Luccio, F., N. A. Pino, A. Piscini, and G. Ventura (2015), Significance of the 1982–2014 Campi Flegrei seismicity: Preexisting structures, hydrothermal processes, and hazard assessment, Geophys. Res. Lett., 42, 7498–7506, doi:10.1002/2015GL064962.
Froment, B., M. Campillo, P. Roux, P. Gouédard, A. Verdel, and R. L. Weaver (2010), Estimation of the effects of nonisotropically distributed energy on the apparent arrival time in correlations, Geophysics, 75(5), SA85–SA93.
Hadziioannou, C., E. Larose, O. Coutant, P. Roux, and M. Campillo (2009), Stability of monitoring weak changes in multiply scattering media with ambient noise correlation: Laboratory experiments, J. Acoust. Soc. Am., 125(6), 3688–3695.
Hillers, G., M. Campillo, and K.-F. Ma (2014), Seismic velocity variations at TCDP are controlled by MJO driven precipitation pattern and high fluid discharge properties, Earth Planet. Sci. Lett., 391, 121–127.
Istituto Nazionale di Geofiscia e Vulcanologia (INGV), Osservatorio Vesuviano, and sezione di Napoli (2015). [Available at http://www.ov.ingv.it/ov/bollettini-campi-flegrei/.]
Landès, M., F. Hubans, N. M. Shapiro, A. Paul, and M. Campillo (2010), Origin of deep ocean microseisms by using teleseismic body waves, J. Geophys. Res., 115, B05302, doi:10.1029/2009JB006918.
Lesage, P., G. Reyes-Davila, and R. Arambula-Mendoza (2014), Large tectonic earthquakes induce sharp temporary decreases in seismic velocity in volcan de Colima, Mexico, J. Geophys. Res., 119, 4360–4376, doi:10.1002/2013JB010884.
Lobkis, O. I., and R. L. Weaver (2001), On the emergence of the Greens function in the correlations of a diffuse field, J. Acoust. Soc. Am., 110, 3011 – 3017.
Maeda, T., K. Obara, and Y. Yukutake (2010), Seismic velocity decrease and recovery related to earthquake swarms in a geothermal area, Earth Planets Space, 62(9), 685–691.
Margerin, L., M. Campillo, B. A. Van Tiggelen, and R. Hennino (2009), Energy partition of seismic coda waves in layered media: Theory and application to Pinyon Flats Observatory, Geophys. J. Int., 177(2), 571–585.
Orsi, G., M. A. Di Vito, J. Selva, and W. Marzocchi (2009), Long-term forecast of eruption style and size at Campi Flegrei, Earth Planet. Sci. Lett., 287, 265–276.
Paul, A., M. Campillo, L. Margerin, E. Larose, and A. Derode (2005), Empirical synthesis of time-asymmetrical Green functions from the correlation of coda waves, J. Geophys. Res., 110, B08302, doi:10.1029/2004JB003521.
Piccinini, D., L. Zaccarelli, M. Pastori, L. Margheriti, F. P. Lucente, P. De Gori, L. Faenza, and G. Soldati (2015), Seismic measurements to reveal short-term variations in the elastic properties of the Earth crust, Boll. di Geofis. Teorica e Appl., 56(2), 257–274, doi:10.4430/bgta0140. Poupinet, G., W. L. Ellsworth, and J. Frechet (1984), Monitoring velocity variations in the crust using earthquake doublets: An application to
the Calaveras fault, California, J. Geophys. Res., 89, 5719–5731.
Richter, T., C. Sens-Schönfelder, R. Kind, and G. Ash (2014), Comprehensive observation and modeling of earthquake and
tenperature-related seismic velocity changes in northern Chile with passive image interferometry, J. Geophys. Res. Solid Earth, 119,
4747–4765, doi:10.1002/2013JB010695.
Saccorotti, G., F. Bianco, M. Castellano, and E. Del Pezzo (2001), The July–August 2000 seismic swarms at Campi Flegrei volcanic complex,
Italy, Geophys. Res. Lett., 28, 2525–2528.
Sens-Schönfelder, C., and U. Wegler (2006), Passive image interferometry and seasonal variations of seismic velocities at Merapi Volcano,
Indonesia, Geophys. Res. Lett., 33, L21302, doi:10.1029/2006GL027797.
Stehly, L., M. Campillo, and N. M. Shapiro (2006), A study of the seismic noise from its long-range correlation properties, J. Geophys. Res.,
111(B10306), doi:10.1029/2005JB004237.
Trasatti, E., M. Polcari, M. Bonafede, and S. Stramondo (2015), Geodetic constraints to the source mechanism of the 2011–2013 unrest at
Campi Flegrei (Italy) caldera, Geophys. Res. Lett., 42, 3847–3854, doi:10.1002/2015GL063621.
Ueno, T., T. Saito, K. Shiomi, B. Enescu, H. Hirose, and K. Obara (2012), Fractional seismic velocity change related to magma intrusions during
earthquake swarms in the eastern Izu peninsula, central Japan, J. Geophys. Res., 117, B12305, doi:10.1029/2012JB009580.
VanDecar, J. C., and R. S. Crosson (1990), Determination of teleseismic relative phase arrival times using multi-channel cross-correlation and
least squares, Bull. Seismol. Soc. Am., 80, 150–169.
Zaccarelli, L., N. M. Shapiro, L. Faenza, G. Soldati, and A. Michelini (2011), Variations of the elastic properties during the 2009 L’Aquila
earthquake inferred from cross-correlations of ambient seismic noise, Geophys. Res. Lett., 38, L24304, doi:10.1029/2011GL049750. Zatsepin, S. V., and S. Crampin (1997), Modeling the compliance of crustal rock—I. Response of shear-wave splitting to differential stress,
Geophys. J. Int., 129, 477–494.
Aster, R., R. P. Meyer, G. De Natale, A. Zollo, M. Martini, E. Del Pezzo, R. Scarpa, and G. Iannaccone (1992), Seismic investigation of Campi Flegrei caldera, in Volcanic Seismology, Proc. Volcanol. Series III, Springer, New York.
Bianco, F., and L. Zaccarelli (2009), A reappraisal of shear wave splitting parameters from Italian active volcanic areas through a semiautomatic algorithm, J. Seismol., 13, 253–266, doi:10.1007/s10950-008-9125-z.
Brenguier, F., N. M. Shapiro, M. Campillo, V. Ferrazzini, Z. Duputel, O. Coutant, and A. Nercessian (2008), Towards forecasting volcanic eruptions using seismic noise, Nat. Geosci., 1, 126–130.
Brenguier, F., M. Campillo, T. Takeda, Y. Aoki, N. M. Shapiro, X. Briand, K. Emoto, and H. Miyake (2014), Mapping pressurized volcanic fluids from induced crustal seismic velocity drops, Science, 345, 80–82.
Campillo, M. (2006), Phase and correlation in random seismic fields and the reconstruction of the Green function, Pure Appl. Geophys., 163, 475–502.
Chiodini, G., S. Caliro, P. De Martino, R. Avino, and F. Gherardi (2012), Early signals of new volcanic unrest at Campi Flegrei caldera? Insights from geochemical data and physical simulations, Geology, 40, 943–946, doi:10.1130/G33251.1.
Chiodini, G., J. Vandemeulebrouck, S. Caliro, L. D’Auria, P. De Martino, A. Mangiacapra, and Z. Petrillo (2015), Evidence of thermal-driven processes triggering the 2005–2014 unrest at Campi Flegrei caldera, Earth Planet. Sci. Lett., 414, 58–67.
Chiodini, G., A. Paonita, A. Aiuppa, A. Costa, S. Caliro, P. De Martino, V. Acocella, and J. Vandemeulebrouck (2016), Magmas near the critical degassing pressure drive volcanic unrest towards a critical state, Nat. Commun., 7, 13712, doi:10.1038/ncomms13712.
D’Auria, L., et al. (2015), Magma injection beneath the urban area of Naples: A new mechanism for the 2012–2013 volcanic unrest at Campi Flegrei caldera, Sci. Rep., 5, 13100, doi:10.1038/srep13100.
Derode, A., E. Larose, M. Tanter, J. de Rosny, A. Tourin, M. Campillo, and M. Fink (2003), Recovering the Greens function from field—Field correlations in an open scattering medium (L), J. Acoust. Soc. Am., 113, 2973–2976.
De Martino, P., U. Tammaro, and F. Obrizzo (2014), GPS time series at Campi Flegrei caldera (2000–2013), Ann. Geophys., 57(2), S0213, doi:10.4401/ag-6431.
De Siena, L., E. Del Pezzo, and F. Bianco (2011), A scattering image of Campi Flegrei from the autocorrelation functions of velocity tomograms, Geophys. J. Int., 184, 1304–1310, doi:10.1111/j.1365-246X.2010.04911.x.Di Luccio, F., N. A. Pino, A. Piscini, and G. Ventura (2015), Significance of the 1982–2014 Campi Flegrei seismicity: Preexisting structures, hydrothermal processes, and hazard assessment, Geophys. Res. Lett., 42, 7498–7506, doi:10.1002/2015GL064962.
Froment, B., M. Campillo, P. Roux, P. Gouédard, A. Verdel, and R. L. Weaver (2010), Estimation of the effects of nonisotropically distributed energy on the apparent arrival time in correlations, Geophysics, 75(5), SA85–SA93.
Hadziioannou, C., E. Larose, O. Coutant, P. Roux, and M. Campillo (2009), Stability of monitoring weak changes in multiply scattering media with ambient noise correlation: Laboratory experiments, J. Acoust. Soc. Am., 125(6), 3688–3695.
Hillers, G., M. Campillo, and K.-F. Ma (2014), Seismic velocity variations at TCDP are controlled by MJO driven precipitation pattern and high fluid discharge properties, Earth Planet. Sci. Lett., 391, 121–127.
Istituto Nazionale di Geofiscia e Vulcanologia (INGV), Osservatorio Vesuviano, and sezione di Napoli (2015). [Available at http://www.ov.ingv.it/ov/bollettini-campi-flegrei/.]
Landès, M., F. Hubans, N. M. Shapiro, A. Paul, and M. Campillo (2010), Origin of deep ocean microseisms by using teleseismic body waves, J. Geophys. Res., 115, B05302, doi:10.1029/2009JB006918.
Lesage, P., G. Reyes-Davila, and R. Arambula-Mendoza (2014), Large tectonic earthquakes induce sharp temporary decreases in seismic velocity in volcan de Colima, Mexico, J. Geophys. Res., 119, 4360–4376, doi:10.1002/2013JB010884.
Lobkis, O. I., and R. L. Weaver (2001), On the emergence of the Greens function in the correlations of a diffuse field, J. Acoust. Soc. Am., 110, 3011 – 3017.
Maeda, T., K. Obara, and Y. Yukutake (2010), Seismic velocity decrease and recovery related to earthquake swarms in a geothermal area, Earth Planets Space, 62(9), 685–691.
Margerin, L., M. Campillo, B. A. Van Tiggelen, and R. Hennino (2009), Energy partition of seismic coda waves in layered media: Theory and application to Pinyon Flats Observatory, Geophys. J. Int., 177(2), 571–585.
Orsi, G., M. A. Di Vito, J. Selva, and W. Marzocchi (2009), Long-term forecast of eruption style and size at Campi Flegrei, Earth Planet. Sci. Lett., 287, 265–276.
Paul, A., M. Campillo, L. Margerin, E. Larose, and A. Derode (2005), Empirical synthesis of time-asymmetrical Green functions from the correlation of coda waves, J. Geophys. Res., 110, B08302, doi:10.1029/2004JB003521.
Piccinini, D., L. Zaccarelli, M. Pastori, L. Margheriti, F. P. Lucente, P. De Gori, L. Faenza, and G. Soldati (2015), Seismic measurements to reveal short-term variations in the elastic properties of the Earth crust, Boll. di Geofis. Teorica e Appl., 56(2), 257–274, doi:10.4430/bgta0140. Poupinet, G., W. L. Ellsworth, and J. Frechet (1984), Monitoring velocity variations in the crust using earthquake doublets: An application to
the Calaveras fault, California, J. Geophys. Res., 89, 5719–5731.
Richter, T., C. Sens-Schönfelder, R. Kind, and G. Ash (2014), Comprehensive observation and modeling of earthquake and
tenperature-related seismic velocity changes in northern Chile with passive image interferometry, J. Geophys. Res. Solid Earth, 119,
4747–4765, doi:10.1002/2013JB010695.
Saccorotti, G., F. Bianco, M. Castellano, and E. Del Pezzo (2001), The July–August 2000 seismic swarms at Campi Flegrei volcanic complex,
Italy, Geophys. Res. Lett., 28, 2525–2528.
Sens-Schönfelder, C., and U. Wegler (2006), Passive image interferometry and seasonal variations of seismic velocities at Merapi Volcano,
Indonesia, Geophys. Res. Lett., 33, L21302, doi:10.1029/2006GL027797.
Stehly, L., M. Campillo, and N. M. Shapiro (2006), A study of the seismic noise from its long-range correlation properties, J. Geophys. Res.,
111(B10306), doi:10.1029/2005JB004237.
Trasatti, E., M. Polcari, M. Bonafede, and S. Stramondo (2015), Geodetic constraints to the source mechanism of the 2011–2013 unrest at
Campi Flegrei (Italy) caldera, Geophys. Res. Lett., 42, 3847–3854, doi:10.1002/2015GL063621.
Ueno, T., T. Saito, K. Shiomi, B. Enescu, H. Hirose, and K. Obara (2012), Fractional seismic velocity change related to magma intrusions during
earthquake swarms in the eastern Izu peninsula, central Japan, J. Geophys. Res., 117, B12305, doi:10.1029/2012JB009580.
VanDecar, J. C., and R. S. Crosson (1990), Determination of teleseismic relative phase arrival times using multi-channel cross-correlation and
least squares, Bull. Seismol. Soc. Am., 80, 150–169.
Zaccarelli, L., N. M. Shapiro, L. Faenza, G. Soldati, and A. Michelini (2011), Variations of the elastic properties during the 2009 L’Aquila
earthquake inferred from cross-correlations of ambient seismic noise, Geophys. Res. Lett., 38, L24304, doi:10.1029/2011GL049750. Zatsepin, S. V., and S. Crampin (1997), Modeling the compliance of crustal rock—I. Response of shear-wave splitting to differential stress,
Geophys. J. Int., 129, 477–494.
Type
article
File(s)
Loading...
Name
2017GRL_Zaccarelli-Bianco.pdf
Description
article
Size
1.49 MB
Format
Adobe PDF
Checksum (MD5)
31b427c1abf98dbb87c47fbea8042fc0
Loading...
Name
2017GRL_Zaccarelli-Bianco_SI.pdf
Description
supplementary information
Size
884.56 KB
Format
Adobe PDF
Checksum (MD5)
65dfaf00b2ae5feae0636669dd06ecc3