Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/6055
DC Field | Value | Language |
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dc.contributor.authorall | Palo, M.; Universit´a degli Studio di Salerno, Dipartimento di Matematica e Informatica, Italy | en |
dc.contributor.authorall | Ibanez, J. M.; Instituto Andaluz de Geofısica, Universidad de Granada, Spain. 3Departamento de F´ısica Te´orica y del Cosmos, Universidad de Granada. | en |
dc.contributor.authorall | Cisneros, M.; Observatorio Vulcanologico, Universidad de Colima, Colima, Mexico | en |
dc.contributor.authorall | Breton, M.; Observatorio Vulcanologico, Universidad de Colima, Colima, Mexico | en |
dc.contributor.authorall | Del Pezzo, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.authorall | Ocana, E.; Instituto Andaluz de Geof´ısica, Universidad de Granada, Spain. | en |
dc.contributor.authorall | Orozco-Rojas, J.; Observatorio Vulcanol´ogico, Universidad de Colima, Colima, Mexico | en |
dc.contributor.authorall | Posadas, A. M.; Departamento de Fısica Aplicada, Universidad de Almerıa, Spain | en |
dc.date.accessioned | 2010-06-30T07:10:48Z | en |
dc.date.available | 2010-06-30T07:10:48Z | en |
dc.date.issued | 2009 | en |
dc.identifier.uri | http://hdl.handle.net/2122/6055 | en |
dc.description.abstract | We have investigated thewavefield properties of the seismic signals generated by the explosions of Volc´an de Colima (M´exico). We have analysed these properties to understand the initial mechanism that triggered the explosive events. Our study is focused on the direct waves coming from the crater area. Thus, we have analysed a set of moderate volcanic explosions at Volc´an de Colima that was recorded by a small aperture seismic array over two periods: October 2005 and April 2006. We can distinguish two types of explosions, Vulcanian and ash-free events. Both types of explosions share the same characteristics, that is a long-period signal (not related to any type of emission) before the arrival of high frequency phases, and a later high frequency signal directly related to ash or gas emission. We have applied the Zero Lag Cross Correlation technique to obtain backazimuth and apparent slowness of the incoming waves. We have also applied polarization analysis to the record of every detected volcanic explosion. By comparing the results of both of these analyses, we have been able to identify the dominant wave types that comprise the seismic wavefield and infer in time and space a possible primary source mechanism that would trigger the volcanic explosions. We have observed an apparent slowness variation of the first onset of the long-period (LP) signal with a possible upward migration of the source; the depth of the source has been identified at a range between 2.6 and 3.3 km below the crater, associated with the range of measured apparent velocities relative to the first onset of the LP signal. | en |
dc.language.iso | English | en |
dc.publisher.name | Blackwell Publishing | en |
dc.relation.ispartof | Geophys. J. Int. | en |
dc.relation.ispartofseries | /177(2009) | en |
dc.subject | Explosive volcanism; | en |
dc.subject | Volcano monitoring. | en |
dc.title | Analysis of the seismic wavefield properties of volcanic explosions at Volc ´an de Colima,Mexico: insights into the source mechanism | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 1383–1398 | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology | en |
dc.identifier.doi | 10.1111/j.1365-246X.2009.04134.x | en |
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Hawaiian and Strombolian eruptions, in Encyclopedia of Volcanoes, pp. 447–461, ed. Sigurdsson, H., Academic Press, San Diego, CA. Zobin, V.M.et al;, 2002. Overview of the 1997–2000 activity of Volc´an de Colima, M´exico, J. Volcanol. Geotherm. Res., 117, 1–19. Zobin, V.M., Orozco-Rojas, J, Reyes-D´avila, G. & Navarro, C., 2005. Seismicity of an andesitic volcano during block-lava effusion: Volc´an de Colima, M´exico, November 1998–January 1999, Bull. Volcanol., 67, 679– 688. Zobin, V.M., Navarro, C., Reyes-D´avil, G., Orozco, J., Bret´on, M., T´ellez, A., Reyes-Alfaro, G. & V´azquez, H., 2006. The methodology of quantification of volcanic explosions from broad-band seismic signals and its application to the 2004–2005 explosions at Volc´an de Colima, Mexico, Geophys. J. Int., 167, 467–478. | en |
dc.description.obiettivoSpecifico | 3.1. Fisica dei terremoti | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Palo, M. | en |
dc.contributor.author | Ibanez, J. M. | en |
dc.contributor.author | Cisneros, M. | en |
dc.contributor.author | Breton, M. | en |
dc.contributor.author | Del Pezzo, E. | en |
dc.contributor.author | Ocana, E. | en |
dc.contributor.author | Orozco-Rojas, J. | en |
dc.contributor.author | Posadas, A. M. | en |
dc.contributor.department | Universit´a degli Studio di Salerno, Dipartimento di Matematica e Informatica, Italy | en |
dc.contributor.department | Instituto Andaluz de Geofısica, Universidad de Granada, Spain. 3Departamento de F´ısica Te´orica y del Cosmos, Universidad de Granada. | en |
dc.contributor.department | Observatorio Vulcanologico, Universidad de Colima, Colima, Mexico | en |
dc.contributor.department | Observatorio Vulcanologico, Universidad de Colima, Colima, Mexico | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.department | Instituto Andaluz de Geof´ısica, Universidad de Granada, Spain. | en |
dc.contributor.department | Observatorio Vulcanol´ogico, Universidad de Colima, Colima, Mexico | en |
dc.contributor.department | Departamento de Fısica Aplicada, Universidad de Almerıa, Spain | 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 | University of Salerno | - |
crisitem.author.dept | Instituto Andaluz de Geofísica, University of Granada, Granada, Spain, | - |
crisitem.author.dept | Observatorio Vulcanologico, Universidad de Colima, Colima, Mexico | - |
crisitem.author.dept | Universidad de Colima, Observatorio Volcanológico, Colima, Mexico | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
crisitem.author.dept | Instituto Andaluz de Geof´ısica, Universidad de Granada, Spain. | - |
crisitem.author.dept | Observatorio Vulcanol´ogico, Universidad de Colima, Colima, Mexico | - |
crisitem.author.dept | Departamento De Quımica y Fısica, Canana de San Urbano, University of Almerıa, E-04071 Almerıa, Spain | - |
crisitem.author.orcid | 0000-0002-9846-8781 | - |
crisitem.author.orcid | 0000-0002-6981-5967 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
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