Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5890| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Finizola, A.; Laboratoire GéoSciences Réunion, Université de La Réunion | en |
| dc.contributor.authorall | Aubert, M.; Laboratoire Magmas et Volcans, Clermont-Université | en |
| dc.contributor.authorall | Revil, A.; LGIT, UMR 5559, CNRS, Equipe Volcan, Université de Savoie | en |
| dc.contributor.authorall | Schütze, C.; Department of Geophysics and Geology, Universität Leipzig | en |
| dc.contributor.authorall | Sortino, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
| dc.date.accessioned | 2010-02-04T09:20:45Z | en |
| dc.date.available | 2010-02-04T09:20:45Z | en |
| dc.date.issued | 2009-04-17 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/5890 | en |
| dc.description.abstract | assess the stability of the flanks of this volcanic edifice during such a crisis. To provide a response to this question, we analyzed a detailed fluid flow mapping plus the reiteration of a profile located in the vicinity of the active vents using the self-potential method, temperature data, soil-gas (CO2) measurements, and electric resistivity tomography. Coupling the interpretation of these methods that are sensitive to the flow of gas and water in the ground indicates the position of areas of mechanical weakness. In addition, they can be used to monitor the change in the discharge of fluids associated with these features before and during the 2002–2003 eruptive crisis. Our results emphasize the importance of old structural boundaries, such as the Large Fossa crater, in the development of the new set of fractures observed during the 2002–2003 eruptive crisis. Between October 2002 and January 2003, the use of CO2 soil-gas technique evidenced an increase in the discharge of CO2 outside the Large Fossa crater boundaries, along the failure boundary of the southern Sciara del Fuoco area. Self-potential and temperature measurements made before the 2002–2003 eruptive crisis reveal significant changes along the main structural boundaries of the Fossa area. The development of these anomalies is interpreted as an increase of the permeability of the structure from May 2000 to May 2002. Between January 2003 and March 2003 the reiteration of self-potential, temperature, and CO2 measurements shows an increase of fluid discharge along weakness planes located inside the Large Fossa crater boundary. They evidence no change outside this structural boundary. The importance of the Large Fossa crater boundary in controlling the deformation and fluid flow from January to March 2003 has been attested by the development of the fractures inside the Large Fossa crater boundary, and also with a network of electrooptical distance measurement stations located inside and outside this ancient crater. This multidisciplinary approach to fluid flow assessment before and during an eruptive crisis is complementary to geodetic measurements of the deformation of the edifice. It demonstrates for the first time the powerful potential of combining electrical resistivity tomography, self-potential, temperature, and soil CO2 measurements in assessing the position of the planes of mechanical weakness in a volcanic edifice. | en |
| dc.language.iso | English | en |
| dc.relation.ispartof | Journal of Volcanology and Geothermal Research | en |
| dc.relation.ispartofseries | /183 (2009) | en |
| dc.subject | Selp potencial | en |
| dc.subject | degassing | en |
| dc.title | Importance of structural history in the summit area of Stromboli during the 2002–2003 eruptive crisis inferred from temperature, soil CO2, self-potential, and electrical resistivity tomography | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.description.pagenumber | 213–227 | en |
| dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks | en |
| dc.identifier.doi | 10.1016/j.jvolgeores.2009.04.002 | en |
| dc.relation.references | Acocella, V., Funiciello, R., Marotta, E., Orsi, G., de Vita, S., 2004. The role of extensional structures on experimental calderas and resurgence. J. Volcanol. Geotherm. Res.129 (1–3), 199–217. doi:10.1016/S0377-0273(03)00240-3. Aizawa, K., Uyeshima, M., Nogami, K., 2008. Zeta potential estimation of volcanic rocks on 11 island arc-type volcanoes in Japan: implication for the generation of local selfpotential anomalies. J. Geophys. Res. 113, B02201. doi:10.1029/2007JB005058. Apuani, T., Corazzato, C., Cancelli, A., Tibaldi, A., 2005a. Stability of a collapsing volcano (Stromboli, Italy): limit equilibrium analysis and numerical modelling. J. Volcanol. Geotherm. Res. 144 (1–4), 191–210. doi:10.1016/j.jvolgeores.2004.11.028. Apuani, T., Corazzato, C., Cancelli, A., Tibaldi, A., 2005b. Physical and mechanical properties of rock masses at Stromboli: a dataset for volcano instability evaluation. Bull. Eng. Geol. Environ. 64 (4), 419–431. doi:10.1007/s10064005-0007-0. Aubert, M., 1999. Practical evaluation of steady heat discharge from dormant active volcanoes: case study of Vulcarolo fissure (Mount Etna, Italy). J. Volcanol. Geotherm. Res. 92, 413–429. Aubert, M., Kieffer, G., 1984. Evolution d'une intrusion magmatique dans le flanc sud de l'Etna entre juin 1982 et juin 1983. Résultats de potentiel spontané (PS) et essai d'interprétation de l'éruption de 1983. C. R. Acad. Sci. Paris t.296, 379–382 Série II-8. Aubert, M., Lima, E., 1986. Hydrothermal activity detected by self-potential measurements (SP) at the N–S volcanic axis between the volcanoes “Nevado de Colima” and “Fuego de Colima”, Mexico. Geophys. J. Int. 25–4, 575–586. Aubert,M., Baubron, J.C.,1988. Identification of a hidden thermal fissure in a volcanic terrain using a combination of hydrothermal convection indicators and soil-atmosphere analysis. J. Volcanol. Geotherm. Res. 35, 217–225. Aubert, M., Auby, R., Bourley, F., Bourley, Y., 1984. Contribution à la surveillance de l'activité de l'Etna à partir de l'étude des zones fumeroliennes. Bull. Volcanol. 47, 1039–1050. Baldi, P., Fabris, M., Marsella, M., Monticelli, R., 2005. Monitoring the morphological evolution of the Sciara del Fuoco during the 2002–2003 Stromboli eruption using multi-temporal photogrammetry. J. Photogram. Rem. Sens. 59 (4), 199–211. doi:10.1016/j.isprsjprs.2005.02.004. Ballestracci, R., 1982. Self-potential survey near the craters of Stromboli volcano (Italy). Inference for internal structure and eruption mechanism. Bull. Volcanol. 45, 349–365. Barberi, F., Rosi, M., Sodi, A., 1993. Volcanic hazard assessment at Stromboli based on review of historical data. Acta Vulcanol. 3, 173–187. Bertagnini, A., Landi, P., 1996. The Secche di Lazzaro pyroclastics of Stromboli volcano: a phreatomagmatic eruption related to the Sciara del Fuoco sector collapse. Bull. Volcanol. 58, 239–245. Bolève, A., Revil, A., Janod, F., Mattiuzzo, J.L., Jardani, A., 2007. Forward modeling and validation of a new formulation to compute self-potential signals associated with ground water flow. Hydrol. Earth Syst. Sci. 11 (5), 1661–1671. Bonaccorso, A., Calvari, S., Garfì, G., Lodato, L., Patanè, D., 2003. Dynamics of the December 2002 flank failure and tsunami at Stromboli volcano inferred by volcanological and geophysical observations. Geophys. Res. Lett. 30 (18), 1941. doi:10.1029/2003GL017702. Bullard, F.M., 1954. Activity of Stromboli in June and December 1952. Bull. Volcanol. 15, 91–98. Calvari, S., Spampinato, L., Lodato, L., Harris, A.J.L., Patrick, M.R., Dehn, J., Burton, M.R., Andronico, D., 2005. Chronology and complex volcanic processes during the 2002– 2003 flank eruption at Stromboli volcano (Italy) reconstructed from direct observations and surveys with a handheld thermal camera. J. Geophys. Res. 110, B02201. doi:10.1029/2004JB003129. Calvari, S., Spampinato, L., Lodato, L., 2006. The 5 April 2003 vulcanian paroxysmal explosion at Stromboli volcano (Italy) from field observations and thermal data. J. Volcanol. Geotherm. Res. 149, 160–175. doi:10.1016/j.jvolgeores.2005.06.006. Carapezza, M.L., Federico, C., 2000. The contribution of fluid geochemistry to the volcano monitoring of Stromboli. J. Volcanol. Geotherm. Res. 95, 227–245. Chiocci, F.L., Romagnoli, C., Tommasi, P., Bosman, A., 2008. The Stromboli 2002 tsunamigenic submarine slide: characteristics and possible failure mechanisms. J. Geophys. Res. 113, B10102. doi:10.1029/2007JB005172. Chiodini, G., Granieri, D., Avino, R., Caliro, S., Costa, A.,Werner, C., 2005. Carbon dioxide diffuse degassing and estimation of heat release from volcanic and hydrothermal systems. J. Geophys. Res. 110, B08204. doi:10.1029/2004JB003542. Crespy, A., Bolève, A., Revil, A., 2007. Influence of the Dukhin and Reynolds numbers on the apparent zeta potential of granular media. J. Colloid Interface Sci. 305, 188–194. Etiope, G., Beneduce, P., Calcara, M., Favali, P., Frugoni, F., Schiattarella, M., Smriglio, G., 1999. Structural pattern and CO2–CH4 degassing of Ustica Island, Southern Tyrrhenian basin. J. Volcanol. Geotherm. Res. 88, 291–304. Finizola, A., Sortino, F., Lénat, J.F., Valenza, M., 2002. Fluid circulation at Stromboli volcano, (Aeolian Island, Italy) from self-potential and CO2 surveys. J. Volcanol. Geotherm. Res. 116 (1–2), 1–18. Finizola, A., Sortino, F., Lénat, J.F., Aubert, M., Ripepe, M., Valenza, M., 2003. The summit hydrothermal system of Stromboli: new insights from self-potential, temperature, CO2 and fumarolic fluids measurements, with structural and monitoring implications. Bull. Volcanol. 65, 486–504. doi:10.1007/s00445-003-0276-2. Finizola, A., Lénat, J.F.,Macedo, O., Ramos, D., Thouret, J.C., Sortino, F., 2004. Fluid circulation and structural discontinuities inside Misti volcano (Peru) inferred from self-potential measurements. J. Volcanol. Geotherm. Res.135, 343–360. doi:10.1016/j.jvolgeores.2004. 03.009. Finizola, A., Revil, A., Rizzo, E., Piscitelli, S., Ricci, T., Morin, J., Angeletti, B., Mocochain, L., Sortino, F., 2006. Hydrogeological insights at Stromboli volcano (Italy) from geoelectrical, temperature, and CO2 soil degassing investigations. Geophys. Res. Lett. 33, L17304. doi:10.1029/2006GL026842. Guichet, X., Jouniaux, L., Catel, N., 2006. Modification of streaming potential by precipitation of calcite in a sand-water system: laboratory measurements pH range from 4 to 12. Geophys. J. Int. 166, 445–460. doi:10.1111/j.1365-246X.2006.02922.x. Hase, H., Ishido, T., Takakura, S., Hashimoto, T., Sato, K., Tanaka, Y., 2003. ζ potential measurement of volcanic rocks from Aso caldera. Geophys. Res. Lett. 30 (23), 2210. doi:10.1029/2003GL018694. Hornig-Kjarsgaard, I., Keller, J., Koberski, U., Stadlbauer, E., Francalanci, L., Lenhart, R., 1993. Geology, stratigraphy and volcanological evolution of the island of Stromboli, Aeolian Arc, Italy. Acta Vulcanol. 3, 21–68. Ishido, T., 2004. Electrokinetic mechanism for the “W”-shaped self-potential profile on volcanoes. Geophys. Res. Lett. 31, L15616. doi:10.1029/2004GL020409. Lénat, J.F., Robineau, B., Durand, S., Bachélery, P., 1998. Etude de la zone sommitale du volcan Karthala (Grande Comore) par polarisation spontanée. C. R. Acad. Sci. 327, 781–788. Lewicki, J.L., Connor, C., St-Amand, K., Stix, J., Spinner, W., 2003. Self-potential, soil CO2 flux, and temperature on Masaya volcano, Nicaragua. Geophys. Res. Lett. 30 (15), 1–4. doi:10.1029/2003GL017731 1817. Linde, N., Jougnot, D., Revil, A., Matthaï, S.K., Arora, T., Renard, D., Doussan, C., 2007. Streaming current generation in two-phase flowconditions. Geophys. Res. Lett. 34 (3), L03306. doi:10.1029/2006GL028878. Lorne, B., Perrier, F., Avouac, J.P.,1999a. Streaming potential measurements,1, properties of the electrical double layer from crushed rock samples. J. Geophys. Res. 104, 17,857–17,877. Lorne, B., Perrier, F., Avouac, J.P., 1999b. Streaming potential measurements, 2, relationship between electrical and hydraulic flow patterns from rock samples during deformation. J. Geophys. Res. 104, 17,879–17,896. Malengreau, B., Lénat, J.F., Bonneville, A., 1994. Cartographie et surveillance temporelle des anomalies de Polarisation Spontanée (PS) sur le Piton de la Fournaise. Bull. Soc. Geol. Fr. 165, 221–232. Maramai, A., Graziani, L., Alessio, G., Burrato, P., Colini, L., Cucci, L., Nappi, R., Nardi, A., Vilardo, G., 2005. Near-and far-field survey report of the 30 December 2002 Stromboli (Southern Italy) tsunami. Mar. Geol. 215 (1–2), 93–106. doi:10.1016/j. margeo.2004.11.009. Matsushima, N., Michiwaki, M., Okazaki, N., Ichikawa, N., Takagi, A., Nishida, Y., Mori, H.Y., 1990. Self-potential study in volcanic areas—Usu,Hokkaido Komaga-take and Me-akan. J. Fac. Sci. Hokkaido Univ. Ser VII 8, 465–477. Mercalli, G., 1881. Natura delle eruzioni dello Stromboli ed in generale dell'attività sismo-vulcanica delle Isole Eolie. Atti Soc. It. Sc. Nat. 24, 105–134. Merle, O., Lénat, J.F., 2003. Hybrid collapse mechanism at Piton de la Fournaise volcano, Reunion Island, Indian Ocean. J. Geophys. Res.108 (B3), 2166. doi:10.1029/2002JB002014. Merle, O., Vidal, N., Van Wyk de Vries, B., 2001. Experiments on vertical basement fault reactivation below volcanoes. J. Geophys. Res. 106, 2153–2162. Neri, M., Lanzafame, G., 2008. Structural features of the 2007 Stromboli eruption. J. Volcanol. Geotherm. Res. doi:10.1016/j.jvolgeores.2008.07.021. Nishida, Y., Tomiya, H., 1987. Self-potential studies in volcanic areas — Usu volcano. J. Fac. Sci. Hakkaiodo Univ. Ser VII. 8, 173–190. Porreca, M., Giordano, G., Mattei, M., Musacchio, P., 2006. Evidence of two Holocene phreatomagmatic eruptions at Stromboli volcano (Aeolian Islands) from paleomagnetic data. Geophys. Res. Lett. 33, L21316. doi:10.1029/2006GL027575. Puglisi, G., Bonaccorso, A., Mattia, M., Aloisi, M., Bonforte, A., Campisi, O., Cantarero, M., Falzone, G., Puglisi, B., Rossi, M., 2005. New integrated geodetic monitoring system at Stromboli volcano (Italy). Eng. Geol. 79 (1–2), 13–31. Revil, A., Pezard, P.A., Glover, P.W.J., 1999a. Streaming potential in porous media. 1. Theory of the zeta potential. J. Geophys. Res. 104, 20,021–20,031. Revil, A., Schwaeger, H., Cathles, L.M., Manhardt, P.D., 1999b. Streaming potential in porous media. 2. Theory and application to geothermal systems. J. Geophys. Res. 104, 20,033–20,048. Revil, A., Leroy, P., 2001. Hydroelectric coupling in a clayey material. Geophys. Res. Lett. 28, 1643–1646. Revil, A., Linde, N., 2006. Chemico-electromechanical coupling in microporous media. J. Colloid Interface Sci. 302, 682–694. doi:10.1016/j.jcis.2006.06.051. Revil, A., Naudet, V., Nouzaret, J., Pessel, M., 2003a. Principles of electrography applied to self-potential electrokinetic sources and hydrogeological applications. Water Resour. Res. 39 (5), 1114. doi:10.1029/2001WR000916. Revil, A., Saracco, G., Labazuy, P., 2003b. The volcano-electric effect. J. Geophys. Res. 108 (B5), 2251. doi:10.1029/2002JB001835. Revil, A., Finizola, A., Sortino, F., Ripepe, M., 2004. Geophysical investigations at Stromboli volcano, Italy: implications for ground water flow and paroxysmal activity. Geophys. J. Int. 157, 426–440. doi:10.1111/j.1365-246X.2004.02181.x. Revil, A., Linde, N., Cerepi, A., Jougnot, D., Matthäi, S., Finsterle, S., 2007. Electrokinetic coupling in unsaturated porous media. J. Colloid Interface Sci. 313 (1), 315–327. doi:10.1016/j.jcis.2007.03.037. Rittmann, A., 1931. Der Ausbruch des Stromboli am 11 September 1930. Zeits. Vulkanol. 14, 47–77. Roche, O., Druitt, T.H., Merle, O., 2000. Experimental study of caldera formation. J. Geophys. Res., B, Solid Earth Planets 105 (1), 395–416. Rosi, M., Bertagnini, A., Landi, P., 2000. Onset of the persistent activity at Stromboli volcano (Italy). Bull. Volcanol. 62, 294–300. Tibaldi, A., 2001. Multiple sector collapse at Stromboli volcano, Italy: how they work. Bull. Volcanol. 63, 112–125. Tibaldi, A., Corazzato, C., Apuani, T., Cancelli, A., 2003. Deformation at Stromboli volcano (Italy) revealed by rock mechanics and structural geology. Tectonophys 361, 187–204. doi:10.1016/S0040-1951(02)00589-9. Tinti, S., Pagnoni,G., Zaniboni, F., Bortolucci, E., 2003. Tsunami generation in Stromboli island and impact on the south-east Tyrrhenian coasts. Nat. Hazards Earth Syst. Sci. 3, 1–11. Tommasi, P., Baldi, P., Chiocci, F.L., Coltelli, M., Marsella, M., Pompilio, M., Romagnoli, C., 2005. The landslide sequence induced by the 2002 eruption at Stromboli volcano. In: Sassa, K., Fukuoka, H., Wang, F., Wang, G. (Eds.), Landslides Risk Analysis and Sustainable Disaster Management, pp. 251–258. doi:10.1007/3-540-28680-2_32. Van Wyk de Vries, B., Matela, R., 1998. Styles of volcano-induced deformation: numerical models of substratum flexure, spreading and extrusion. J. Volcanol. Geotherm. Res. 81, 1–18. Van Wyk de Vries, B., Kerle, N., Petley, D., 2000. Sector collapse forming at Casita Volcano, Nicaragua. Geology 28 (2), 167–170. Vidal, N., Merle, O., 2000. Reactivation of basement faults beneath volcanoes; a new model of flank collapse. J. Volcanol. Geotherm. Res. 99 (1–4), 9–26. Zablocki, C.J., 1976. Mapping thermal anomalies on an active volcano by the selfpotential method, Kilauea, Hawaii. Proceedings, 2nd U N Symposium of the development and use of geothermal resources San Francisco California, May 1975, pp. 1299–1309. Zlotnicki, J., Nishida, Y., 2003. Review on morphological insights of self-potential anomalies on volcanoes. Surv. Geophys. 24, 291–338. doi:10.1023/B:GEOP.0000004188.67923.ac | en |
| dc.description.obiettivoSpecifico | 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | reserved | en |
| dc.contributor.author | Finizola, A. | en |
| dc.contributor.author | Aubert, M. | en |
| dc.contributor.author | Revil, A. | en |
| dc.contributor.author | Schütze, C. | en |
| dc.contributor.author | Sortino, F. | en |
| dc.contributor.department | Laboratoire GéoSciences Réunion, Université de La Réunion | en |
| dc.contributor.department | Laboratoire Magmas et Volcans, Clermont-Université | en |
| dc.contributor.department | LGIT, UMR 5559, CNRS, Equipe Volcan, Université de Savoie | en |
| dc.contributor.department | Department of Geophysics and Geology, Universität Leipzig | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Laboratoire Magmas et Volcans, Clermont-Université | - |
| crisitem.author.dept | Centre National de la Recherche Scientifique, Université Paul Cézanne-Aix-Marseille III, CEREGE, Equipe Hydrogéophysique et Milieux Poreux, Aix-en-Provence, France. | - |
| crisitem.author.dept | Department of Geophysics and Geology, Universität Leipzig | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia | - |
| crisitem.author.orcid | 0000-0002-5083-7349 | - |
| crisitem.author.orcid | 0000-0002-2400-911X | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
Files in This Item:
| File | Description | Size | Format | Existing users please Login |
|---|---|---|---|---|
| Finizola et al.JVGR_20091.pdf | 2.06 MB | Adobe PDF |
WEB OF SCIENCETM
Citations
26
checked on Feb 10, 2021
Page view(s)
192
checked on Apr 13, 2024
Download(s)
26
checked on Apr 13, 2024
