Inner structure of La Fossa di Vulcano ( Vulcano Island, southern Tyrrhenian Sea, Italy) revealed by high-resolution electric resistivity tomography coupled with self-potential, temperature, and CO2 diffuse degassing measurements (Articolo in rivista)

Type
Label
  • Inner structure of La Fossa di Vulcano ( Vulcano Island, southern Tyrrhenian Sea, Italy) revealed by high-resolution electric resistivity tomography coupled with self-potential, temperature, and CO2 diffuse degassing measurements (Articolo in rivista) (literal)
Anno
  • 2008-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1029/2007JB005394 (literal)
Alternative label
  • Revil A; Finizola A ; Piscitelli S; Rizzo E ; Ricci T; Crespy A; Angeletti B; Balasco M; Cabusson SB; Bennati L; Bolève A; Byrdina S; Carzaniga N; Di Gangi F; Morin J; Perrone A; Rossi M; Roulleau E; Suski B (2008)
    Inner structure of La Fossa di Vulcano ( Vulcano Island, southern Tyrrhenian Sea, Italy) revealed by high-resolution electric resistivity tomography coupled with self-potential, temperature, and CO2 diffuse degassing measurements
    in Journal of geophysical research
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Revil A; Finizola A ; Piscitelli S; Rizzo E ; Ricci T; Crespy A; Angeletti B; Balasco M; Cabusson SB; Bennati L; Bolève A; Byrdina S; Carzaniga N; Di Gangi F; Morin J; Perrone A; Rossi M; Roulleau E; Suski B (literal)
Pagina inizio
  • B07207 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 113 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 21 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • B7 (literal)
Note
  • Scopu (literal)
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Department of Geophysics, Colorado School of Mines, Golden, Colorado, USA. Université Aix Marseille III, CNRS, Aix en Provence, France. UMR5559, Equipe Volcan, University of Savoie, INSU, LGIT, CNRS, Bourget du Lac, France. Istituto Nazionale di Geofisica e Vulcanologia, Palermo, Italy. Laboratoire Ge´oSciences Re´union, UMR7154, UR, IPGP, La Re´union, France. Laboratory of Geophysics, IMAA, CNR, Tito Scalo, Italy. INGV, Universita` Roma Tre, Rome, Italy. Universite Aix Marseille III, CNRS, Aix en Provence, France Laboratoire Magma et Volcan, Universite´ Blaise Pascal, UMR6524, IRD, CNRS, Clermont-Ferrand, France. Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana, USA. Savoie Technolac, Sobesol, Le Bourget du Lac, France. IPGP, CNRS, Paris, France. Department of Geology and Geosciences, Universita` Milano-Bicocca, Milan, Italy. Pantheon-Sorbonne, Universite´ Paris 1, Paris, France. GEOTOP-UQAM-McGill, Montreal, Quebec, Canada. Institut de Geophysique, Colle`ge Prope´deutique, Universite´ de Lausanne, Lausanne, Switzerland (literal)
Titolo
  • Inner structure of La Fossa di Vulcano ( Vulcano Island, southern Tyrrhenian Sea, Italy) revealed by high-resolution electric resistivity tomography coupled with self-potential, temperature, and CO2 diffuse degassing measurements (literal)
Abstract
  • La Fossa cone is an active stratovolcano located on Vulcano Island in the Aeolian Archipelago (southern Italy). Its activity is characterized by explosive phreatic and phreatomagmatic eruptions producing wet and dry pyroclastic surges, pumice fall deposits, and highly viscous lava flows. Nine 2-D electrical resistivity tomograms (ERTs; electrode spacing 20 m, with a depth of investigation > 200 m) were obtained to image the edifice. In addition, we also measured the self-potential, the CO2 flux from the soil, and the temperature along these profiles at the same locations. These data provide complementary information to interpret the ERT profiles. The ERT profiles allow us to identify the main structural boundaries (and their associated fluid circulations) defining the shallow architecture of the Fossa cone. The hydrothermal system is identified by very low values of the electrical resistivity (< 20 Omega m). Its lateral extension is clearly limited by the crater boundaries, which are relatively resistive (>400 Omega m). Inside the crater it is possible to follow the plumbing system of the main fumarolic areas. On the flank of the edifice a thick layer of tuff is also marked by very low resistivity values (in the range 1-20 Omega m) because of its composition in clays and zeolites. The ashes and pyroclastic materials ejected during the nineteenth-century eruptions and partially covering the flank of the volcano correspond to relatively resistive materials (several hundreds to several thousands Omega m). We carried out laboratory measurements of the electrical resistivity and the streaming potential coupling coefficient of the main materials forming the volcanic edifice. A 2-D simulation of the groundwater flow is performed over the edifice using a commercial finite element code. Input parameters are the topography, the ERT cross section, and the value of the measured streaming current coupling coefficient. From this simulation we computed the self-potential field, and we found good agreement with the measured self-potential data by adjusting the boundary conditions for the flux of water. Inverse modeling shows that self-potential data can be used to determine the pattern of groundwater flow and potentially to assess water budget at the scale of the volcanic edifice. (literal)
Prodotto di
Autore CNR
Insieme di parole chiave

Incoming links:


Autore CNR di
Prodotto
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi
Insieme di parole chiave di
data.CNR.it