Volcanic tremor and local earthquakes at Copahue volcanic complex, Southern Andes, Argentina

In the present paper we describe the results of a seismic field survey carried out at Copahue Volcano, Southern Andes, Argentina, using a small-aperture, dense seismic antenna. Copahue Volcano is an active volcano that exhibited a few phreatic eruptions in the last 20 years. The aim of this experime...

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Autor principal: Ibáñez, J.M
Otros Autores: Del Pezzo, E., Bengoa, C., Caselli, A., Badi, G., Almendros, J.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 2008
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100 1 |a Ibáñez, J.M. 
245 1 0 |a Volcanic tremor and local earthquakes at Copahue volcanic complex, Southern Andes, Argentina 
260 |c 2008 
270 1 0 |m Ibáñez, J.M.; Instituto Andaluz de Geofísica, Universidad de Granada, Campus de Cartuja s/n, 18071 Granada, Spain; email: jibanez@ugr.es 
506 |2 openaire  |e Política editorial 
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504 |a Ibáñez, J.M., Del Pezzo, E., Almendros, J., La Rocca, M., Alguacil, G., Ortiz, R., García, A., Seismo volcanic signals at Deception Island volcano (Antarctica): wavefield analysis and source modeling (2000) J. Geophys. Res., 105 (6), pp. 13905-13931 
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504 |a La Rocca, M., Petrosino, S., Saccorotti, G., Simini, M., Ibáñez, J.M., Almendros, J., Del Pezzo, E., Location of the source and shallow velocity model deduced by the explosion quakes recorded by two seismic antennas at Stromboli volcano (2000) Phys. Chem. Earth, 25, pp. 731-736 
504 |a La Roca, M., Saccorotti, G., Del Pezzo, E., Ibáñez, J., Probabilistic source location of Explosion Quakes at Stromboli volcano estimated with double array data (2004) J. Vol. Geo. Res., 131, pp. 123-142 
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504 |a Martinez-Arevalo, C., Bianco, F., Ibáñez, J.M., Del Pezzo, E., Shallow seismic attenuation and shear waves splitting in the short period range of Deception Island volcano (Antarctica) (2003) J. Vol. Geo. Res., 128, pp. 89-113 
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504 |a Palo, M., Ibáñez, J.M., Cisneros, M., Bretón, M., Del Pezzo, E., Ocaña, E., Orozco-Rojas, J., submitted for publication. Analysis of the wavefield properties of volcanic explosions at Volcán de Colima, México: insights into the source mechanism. Geophys. J. Int; Pesce, A., Evolución volcano-tectónica del complejo efusivo Copahue-Caviahue y su modelo geotérmico preliminar (1989) Revista de la Asociación Geológica Argentina, 44, pp. 307-327 
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504 |a Varekamp, J., Ouimette, A., Hermán, S., Bermúdez, A., Delpino, D., Hydrothermal element fluxes from Copahue, Argentina: A "beehive" volcano in turmoil (2001) Geology, 29 (ll), pp. 1059-1062 
520 3 |a In the present paper we describe the results of a seismic field survey carried out at Copahue Volcano, Southern Andes, Argentina, using a small-aperture, dense seismic antenna. Copahue Volcano is an active volcano that exhibited a few phreatic eruptions in the last 20 years. The aim of this experiment was to record and classify the background seismic activity of this volcanic area, and locate the sources of local earthquakes and volcanic tremor. Data consist of several volcano-tectonic (VT) earthquakes, and many samples of back-ground seismic noise. We use both ordinary spectral, and multi-spectral techniques to measure the spectral content, and an array technique [Zero Lag Cross Correlation technique] to measure the back-azimuth and apparent slowness of the signals propagating across the array. We locate VT earthquakes using a procedure based on the estimate of slowness vector components and S-P time. VT events are located mainly along the border of the Caviahue caldera lake, positioned at the South-East of Copahue volcano, in a depth interval of 1-3 km below the surface. The background noise shows the presence of many transients with high correlation among the array stations in the frequency band centered at 2.5 Hz. These transients are superimposed to an uncorrelated background seismic signal. Array solutions for these transients show a predominant slowness vector pointing to the exploited geothermal field of "Las Maquinitas" and "Copahue Village", located about 6 km north of the array site. We interpret this coherent signal as a tremor generated by the activity of the geothermal field. © 2008 Elsevier B.V. All rights reserved.  |l eng 
536 |a Detalles de la financiación: Ministry of Education 
536 |a Detalles de la financiación: Division of Antarctic Sciences 
536 |a Detalles de la financiación: We are grateful to Dr. Philippe Lesage and Dr. Gilberto Saccorotti who provided very helpful comments that have improved the present manuscript. This work has been partially supported by the research projects VOLUME, UE, FP6-2004-Global-3-018471, SISVOLTEDEC CGL2005-05789-C03-02/ANT, FIRB — Italy's Ministry of Education for base research, and DPC-INGV (Italy's Civil Protection and INGV funds for volcano monitoring) V3_4 Project. Appendix A 
593 |a Instituto Andaluz de Geofísica, Universidad de Granada, Campus de Cartuja s/n, 18071 Granada, Spain 
593 |a Departamento de Física Teórica y del Cosmos, Área de Física de la Tierra, Universidad de Granada, Spain 
593 |a Istituto Nazionale di Geofisica e Vulcanologia, sezione di Napoli - Osservatorio Vesuviano, Via Diocleziano, 328, 80124 Napoli, Italy 
593 |a Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentina 
593 |a Facultad de Astronomía y Geofísica, Universidad Nacional de La Plata, Argentina 
690 1 0 |a SEISMIC ARRAY 
690 1 0 |a VOLCANIC SEISMICITY 
690 1 0 |a VOLCANIC TREMOR 
690 1 0 |a VOLCANO TECTONIC EARTHQUAKES 
690 1 0 |a ANTENNA ACCESSORIES 
690 1 0 |a CORRELATION METHODS 
690 1 0 |a EARTHQUAKES 
690 1 0 |a FREQUENCY BANDS 
690 1 0 |a GEOTHERMAL FIELDS 
690 1 0 |a GEOTHERMAL WELLS 
690 1 0 |a LANDFORMS 
690 1 0 |a MICROFLUIDICS 
690 1 0 |a SEISMOLOGY 
690 1 0 |a TRANSIENTS 
690 1 0 |a VECTORS 
690 1 0 |a (1 1 0) SURFACE 
690 1 0 |a ACTIVE VOLCANOES 
690 1 0 |a BACKGROUND NOISES 
690 1 0 |a COHERENT SIGNALING 
690 1 0 |a CROSS CORRELATION TECHNIQUE (CC) 
690 1 0 |a ELSEVIER (CO) 
690 1 0 |a LOCAL EARTHQUAKES 
690 1 0 |a MULTI-SPECTRAL (MS) 
690 1 0 |a PHREATIC 
690 1 0 |a SEISMIC ACTIVITIES 
690 1 0 |a SEISMIC FIELD 
690 1 0 |a SEISMIC NOISE 
690 1 0 |a SEISMIC SIGNALS 
690 1 0 |a SPECTRAL CONTENTS 
690 1 0 |a UNCORRELATED 
690 1 0 |a VECTOR COMPONENTS 
690 1 0 |a VOLCANIC COMPLEX 
690 1 0 |a VOLCANIC TREMORS 
690 1 0 |a VOLCANOTECTONIC (VT) EARTHQUAKES 
690 1 0 |a VOLCANOES 
690 1 0 |a BACKGROUND LEVEL 
690 1 0 |a EARTHQUAKE CATALOGUE 
690 1 0 |a EARTHQUAKE SWARM 
690 1 0 |a NOISE 
690 1 0 |a SEISMIC SURVEY 
690 1 0 |a SEISMICITY 
690 1 0 |a TECTONIC SETTING 
690 1 0 |a VOLCANIC EARTHQUAKE 
690 1 0 |a VOLCANIC ERUPTION 
690 1 0 |a COPAHUE 
651 4 |a ARGENTINA 
651 4 |a ARGENTINA 
651 4 |a NEUQUEN 
651 4 |a SOUTH AMERICA 
700 1 |a Del Pezzo, E. 
700 1 |a Bengoa, C. 
700 1 |a Caselli, A. 
700 1 |a Badi, G. 
700 1 |a Almendros, J. 
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