Earthquake families in the seismicity of Popocatépetl volcano

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Auteur principal: A. Zamora-Camacho
Format: Artículo científico
Langue:en
Publié: Universidad Nacional Autónoma de México 2005
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author A. Zamora-Camacho
author_facet A. Zamora-Camacho
contents Earthquake families in the seismicity of Popocatépetl volcano A. Zamora-Camacho Z. Jiménez J. M. Espíndola Ciencias de la Tierra Mexican volcanoes volcano seismicity earthquake families 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 magnitudes and occur over a relatively long period of time. This suggests that they are ofthe asperity type. They occur up to a depth of 4 km below sea level underneath the volcano, and may be generated by the passageof magma through the upper volcanic conduits. 2005 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56844204 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.2 Vol.44
format Artículo científico
id redalyc_56844204
institution Redalyc
language en
publishDate 2005
publisher Universidad Nacional Autónoma de México
spellingShingle Earthquake families in the seismicity of Popocatépetl volcano
A. Zamora-Camacho
Ciencias de la Tierra
Mexican volcanoes
volcano seismicity
earthquake families
Popocatépetl volcano
Earthquake families in the seismicity of Popocatépetl volcano A. Zamora-Camacho Z. Jiménez J. M. Espíndola Ciencias de la Tierra Mexican volcanoes volcano seismicity earthquake families 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 magnitudes and occur over a relatively long period of time. This suggests that they are ofthe asperity type. They occur up to a depth of 4 km below sea level underneath the volcano, and may be generated by the passageof magma through the upper volcanic conduits. 2005 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56844204 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.2 Vol.44
title Earthquake families in the seismicity of Popocatépetl volcano
topic Ciencias de la Tierra
Mexican volcanoes
volcano seismicity
earthquake families
Popocatépetl volcano
url https://www.redalyc.org/articulo.oa?id=56844204