Tracking Episodes of Seismicity and Gas Transport in Campi Flegrei Caldera Through Seismic, Geophysical, and Geochemical Measurements

被引:23
作者
Giudicepietro, Flora [1 ]
Chiodini, Giovanni [2 ]
Avino, Rosario [1 ]
Brandi, Giuseppe [1 ]
Caliro, Stefano [1 ]
De Cesare, Walter [1 ]
Galluzzo, Danilo [1 ]
Esposito, Antonietta [1 ]
La Rocca, Adriano [1 ]
Lo Bascio, Domenico [1 ]
Obrizzo, Francesco [1 ]
Pinto, Salvatore [1 ]
Ricci, Tullio [3 ]
Ricciolino, Patrizia [1 ]
Siniscalchi, Agata [4 ]
Tramelli, Anna [1 ]
Vandemeulebrouck, Jean [5 ]
Macedonio, Giovanni [1 ]
机构
[1] Osserv Vesuviano, Ist Nazl Geofis & Vulcanol, Naples, Italy
[2] Ist Nazl Geofis & Vulcanol, Bologna, Italy
[3] Ist Nazl Geofis & Vulcanol, Rome, Italy
[4] Univ Bari ALDO MORO, Dipartimento Sci Terra & Geoambientali, Bari, Italy
[5] Univ Grenoble Alpes, Univ Savoie Mt Blanc, ISTerre, IFSTTAR,IRD,CNRS, Grenoble, France
关键词
Earthquakes;
D O I
10.1785/0220200223
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This article presents findings from two episodes of seismicity and gas emission that occurred on 7 October 2015 and 6 December 2019 in Campi Flegrei caldera. This caldera has been affected by long-term unrest since 2004. The 6 December 2019 episode, consisting of a swarm of 38 earthquakes (maximum duration magnitude 3.1, the largest between 1984 and March 2020), occurred at the end of a one month period characterized by an increase in the ground uplift rate from 0.19 +/- 0.01 to 0.72 +/- 0.05 mm/day. A sudden increase in the fumarolic tremor amplitude, which is a proxy of gas emission related parameters recorded at Solfatara?Pisciarelli hydrothermal area (e.g., CO2 air concentration), was observed during the seismicity episode. The uplift rate decreased immediately after the swarm (0.10 +/- 0.01 mm/day), whereas the fumarolic tremor amplitude remained higher than that observed prior to the swarm. Through analyzing the time series of uplift recorded in Pozzuoli (central area of the caldera) from differential measurements on tide gauges, we were able to identify the 2015 episode. This episode was characterized by increasing uplift rates that culminated in a seismic swarm of 33 earthquakes on 7 October, which was followed by decreasing uplift rates. We computed double-difference locations of earthquakes from the two swarms and found that they located along a conduit-like path, coinciding with a high-resistivity contrast zone, previously identified by audiomagnetotelluric measurements. The focal mechanisms of the major earthquakes of both swarms indicate fault planes radial with respect to the maximum uplift area. These phenomena can be interpreted as episodes of the volcanic and (or) hydrothermal system pressurization that culminate in an injection of fluids along the conduit-like path, which behaves as a valve that allows fluid discharge and the temporary depressurization of the source region.
引用
收藏
页码:965 / 975
页数:11
相关论文
共 39 条
  • [1] An overview of recent (1988 to 2014) caldera unrest: Knowledge and perspectives
    Acocella, V.
    Di Lorenzo, R.
    Newhall, C.
    Scandone, R.
    [J]. REVIEWS OF GEOPHYSICS, 2015, 53 (03) : 896 - 955
  • [2] New ground-based lidar enables volcanic CO2 flux measurements
    Aiuppa, Alessandro
    Fiorani, Luca
    Santoro, Simone
    Parracino, Stefano
    Nuvoli, Marcello
    Chiodini, Giovanni
    Minopoli, Carmine
    Tamburello, Giancarlo
    [J]. SCIENTIFIC REPORTS, 2015, 5
  • [3] Monitoring diffuse volcanic degassing during volcanic unrests: the case of Campi Flegrei (Italy)
    Cardellini, C.
    Chiodini, G.
    Frondini, F.
    Avino, R.
    Bagnato, E.
    Caliro, S.
    Lelli, M.
    Rosiello, A.
    [J]. SCIENTIFIC REPORTS, 2017, 7
  • [4] Clues on the origin of post-2000 earthquakes at Campi Flegrei caldera (Italy)
    Chiodini, G.
    Selva, J.
    Del Pezzo, E.
    Marsan, D.
    De Siena, L.
    D'Auria, L.
    Bianco, F.
    Caliro, S.
    De Martino, P.
    Ricciolino, P.
    Petrillo, Z.
    [J]. SCIENTIFIC REPORTS, 2017, 7
  • [5] Fumarolic tremor and geochemical signals during a volcanic unrest
    Chiodini, Giovanni
    Giudicepietro, F.
    Vandemeulebrouck, J.
    Aiuppa, A.
    Caliro, S.
    De Cesare, W.
    Tamburello, G.
    Avino, R.
    Orazi, M.
    D'Auria, L.
    [J]. GEOLOGY, 2017, 45 (12) : 1131 - 1134
  • [6] Magmas near the critical degassing pressure drive volcanic unrest towards a critical state
    Chiodini, Giovanni
    Paonita, Antonio
    Aiuppa, Alessandro
    Costa, Antonio
    Caliro, Stefano
    De Martino, Prospero
    Acocella, Valerio
    Vandemeulebrouck, Jean
    [J]. NATURE COMMUNICATIONS, 2016, 7
  • [7] Evidence of thermal-driven processes triggering the 2005-2014 unrest at Campi Flegrei caldera
    Chiodini, Giovanni
    Vandemeulebrouck, Jean
    Caliro, Stefano
    D'Auria, Luca
    De Martino, Prospero
    Mangiacapra, Annarita
    Petrillo, Zaccaria
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 2015, 414 : 58 - 67
  • [8] Early signals of new volcanic unrest at Campi Flegrei caldera? Insights from geochemical data and physical simulations
    Chiodini, Giovanni
    Caliro, S.
    De Martino, P.
    Avino, R.
    Gherardi, F.
    [J]. GEOLOGY, 2012, 40 (10) : 943 - 946
  • [9] Temperature and pressure gas geoindicators at the Solfatara fumaroles (Campi Flegrei)
    Chiodini, Giovanni
    Avino, Rosario
    Caliro, Stefano
    Minopoli, Carmine
    [J]. ANNALS OF GEOPHYSICS, 2011, 54 (02) : 151 - 160
  • [10] Repeated fluid-transfer episodes as a mechanism for the recent dynamics of Campi Flegrei caldera (1989-2010)
    D'Auria, L.
    Giudicepietro, F.
    Aquino, I.
    Borriello, G.
    Del Gaudio, C.
    Lo Bascio, D.
    Martini, M.
    Ricciardi, G. P.
    Ricciolino, P.
    Ricco, C.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2011, 116