Short Note: Earthquake families in the seismicity of Popocatépetl volcano

Analysis of the seismicity of Popocatepétl volcano (Central Mexico) over the period September 1 to December 31, 1995, shows the existence of three earthquake families, with correlation coefficients better than 0.5 in all components of three stations. For two families the events have similar magnitud...

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Main Authors: Z. Jiménez, A. Zamora-Camacho, J. M. Espíndola
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México, Instituto de Geofísica 2005-08-01
Series:Geofísica Internacional
Subjects:
Online Access:http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2005/02/Espindola.pdf
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author Z. Jiménez
A. Zamora-Camacho
J. M. Espíndola
author_facet Z. Jiménez
A. Zamora-Camacho
J. M. Espíndola
author_sort Z. Jiménez
collection DOAJ
description Analysis of the seismicity of Popocatepétl volcano (Central Mexico) over the period September 1 to December 31, 1995, shows the existence of three earthquake families, with correlation coefficients better than 0.5 in all components of three stations. For two families the events have similar magnitudes and occur over a relatively long period of time. This suggests that they are of the asperity type. They occur up to a depth of 4 km below sea level underneath the volcano, and may be generated by the passage of magma through the upper volcanic conduits.
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spelling doaj.art-243bcd3def1d4624b9149f60a83b6e9c2023-09-02T13:12:30ZengUniversidad Nacional Autónoma de México, Instituto de GeofísicaGeofísica Internacional0016-71692005-08-01442169176Short Note: Earthquake families in the seismicity of Popocatépetl volcanoZ. JiménezA. Zamora-CamachoJ. M. EspíndolaAnalysis of the seismicity of Popocatepétl volcano (Central Mexico) over the period September 1 to December 31, 1995, shows the existence of three earthquake families, with correlation coefficients better than 0.5 in all components of three stations. For two families the events have similar magnitudes and occur over a relatively long period of time. This suggests that they are of the asperity type. They occur up to a depth of 4 km below sea level underneath the volcano, and may be generated by the passage of magma through the upper volcanic conduits.http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2005/02/Espindola.pdfMexican volcanoesvolcano seismicityPopocatépetl volcanoearthquake families
spellingShingle Z. Jiménez
A. Zamora-Camacho
J. M. Espíndola
Short Note: Earthquake families in the seismicity of Popocatépetl volcano
Geofísica Internacional
Mexican volcanoes
volcano seismicity
Popocatépetl volcano
earthquake families
title Short Note: Earthquake families in the seismicity of Popocatépetl volcano
title_full Short Note: Earthquake families in the seismicity of Popocatépetl volcano
title_fullStr Short Note: Earthquake families in the seismicity of Popocatépetl volcano
title_full_unstemmed Short Note: Earthquake families in the seismicity of Popocatépetl volcano
title_short Short Note: Earthquake families in the seismicity of Popocatépetl volcano
title_sort short note earthquake families in the seismicity of popocatepetl volcano
topic Mexican volcanoes
volcano seismicity
Popocatépetl volcano
earthquake families
url http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2005/02/Espindola.pdf
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