Site Response Evaluation in the Trans-Mexican Volcanic Belt Based on HVSR from Ambient Noise and Regional Seismicity

The Trans-Mexican Volcanic Belt (TMVB), located in central Mexico, is an area for which low to moderate seismic risk is considered. This is based on the limited instrumental data available, even though large historical earthquakes have damaged some urban centers in the past. However, site effects is...

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Main Authors: L. Francisco Pérez-Moreno, Quetzalcoatl Rodríguez-Pérez, F. Ramón Zúñiga, Jaime Horta-Rangel, M. de la Luz Pérez-Rea, Miguel A. Pérez-Lara
Format: Article
Language:English
Published: MDPI AG 2021-06-01
Series:Applied Sciences
Subjects:
Online Access:https://www.mdpi.com/2076-3417/11/13/6126
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spelling doaj-0795f749774c402fafeb4496b4d0bb822021-07-15T15:30:45ZengMDPI AGApplied Sciences2076-34172021-06-01116126612610.3390/app11136126Site Response Evaluation in the Trans-Mexican Volcanic Belt Based on HVSR from Ambient Noise and Regional SeismicityL. Francisco Pérez-Moreno0Quetzalcoatl Rodríguez-Pérez1F. Ramón Zúñiga2Jaime Horta-Rangel3M. de la Luz Pérez-Rea4Miguel A. Pérez-Lara5Facultad de Ingeniería, Universidad Autónoma de Querétaro, Querétaro 76010, MexicoConsejo Nacional de Ciencia y Tecnología, Dirección Adjunta de Desarrollo Científico, Ciudad de México 03940, MexicoCentro de Geociencias, Universidad Nacional Autónoma de México, Querétaro 76230, MexicoFacultad de Ingeniería, Universidad Autónoma de Querétaro, Querétaro 76010, MexicoFacultad de Ingeniería, Universidad Autónoma de Querétaro, Querétaro 76010, MexicoFacultad de Ingeniería, Universidad Autónoma de Querétaro, Querétaro 76010, MexicoThe Trans-Mexican Volcanic Belt (TMVB), located in central Mexico, is an area for which low to moderate seismic risk is considered. This is based on the limited instrumental data available, even though large historical earthquakes have damaged some urban centers in the past. However, site effects is an aspect that must be considered in estimating risk, because there are some instances of important amplifications that have been documented with serious effects. In this work, ambient noise and earthquake records from 90 seismic permanent and temporary stations are used to analyze site response in the TMVB. The results obtained show a heterogeneous range in the value of the fundamental frequency. When possible, a comparison was made of the results obtained from ambient noise and earthquake records. In almost all these comparisons, no significant differences were observed in terms of the fundamental frequency. However, there were some stations with a flat average HVSR ambient noise curve that contradicted earthquake data results, which showed peaks at some frequencies. Our results are a first step towards categorizing the different site responses in the TMVB but in order to provide finer details, it is necessary to improve the actual monitoring conditions.https://www.mdpi.com/2076-3417/11/13/6126site effectsspectral ratiotrans-mexican volcanic belt
collection DOAJ
language English
format Article
sources DOAJ
author L. Francisco Pérez-Moreno
Quetzalcoatl Rodríguez-Pérez
F. Ramón Zúñiga
Jaime Horta-Rangel
M. de la Luz Pérez-Rea
Miguel A. Pérez-Lara
spellingShingle L. Francisco Pérez-Moreno
Quetzalcoatl Rodríguez-Pérez
F. Ramón Zúñiga
Jaime Horta-Rangel
M. de la Luz Pérez-Rea
Miguel A. Pérez-Lara
Site Response Evaluation in the Trans-Mexican Volcanic Belt Based on HVSR from Ambient Noise and Regional Seismicity
Applied Sciences
site effects
spectral ratio
trans-mexican volcanic belt
author_facet L. Francisco Pérez-Moreno
Quetzalcoatl Rodríguez-Pérez
F. Ramón Zúñiga
Jaime Horta-Rangel
M. de la Luz Pérez-Rea
Miguel A. Pérez-Lara
author_sort L. Francisco Pérez-Moreno
title Site Response Evaluation in the Trans-Mexican Volcanic Belt Based on HVSR from Ambient Noise and Regional Seismicity
title_short Site Response Evaluation in the Trans-Mexican Volcanic Belt Based on HVSR from Ambient Noise and Regional Seismicity
title_full Site Response Evaluation in the Trans-Mexican Volcanic Belt Based on HVSR from Ambient Noise and Regional Seismicity
title_fullStr Site Response Evaluation in the Trans-Mexican Volcanic Belt Based on HVSR from Ambient Noise and Regional Seismicity
title_full_unstemmed Site Response Evaluation in the Trans-Mexican Volcanic Belt Based on HVSR from Ambient Noise and Regional Seismicity
title_sort site response evaluation in the trans-mexican volcanic belt based on hvsr from ambient noise and regional seismicity
publisher MDPI AG
series Applied Sciences
issn 2076-3417
publishDate 2021-06-01
description The Trans-Mexican Volcanic Belt (TMVB), located in central Mexico, is an area for which low to moderate seismic risk is considered. This is based on the limited instrumental data available, even though large historical earthquakes have damaged some urban centers in the past. However, site effects is an aspect that must be considered in estimating risk, because there are some instances of important amplifications that have been documented with serious effects. In this work, ambient noise and earthquake records from 90 seismic permanent and temporary stations are used to analyze site response in the TMVB. The results obtained show a heterogeneous range in the value of the fundamental frequency. When possible, a comparison was made of the results obtained from ambient noise and earthquake records. In almost all these comparisons, no significant differences were observed in terms of the fundamental frequency. However, there were some stations with a flat average HVSR ambient noise curve that contradicted earthquake data results, which showed peaks at some frequencies. Our results are a first step towards categorizing the different site responses in the TMVB but in order to provide finer details, it is necessary to improve the actual monitoring conditions.
topic site effects
spectral ratio
trans-mexican volcanic belt
url https://www.mdpi.com/2076-3417/11/13/6126
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