dor_id: 4132901

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

561.#.#.u: https://www.geofisica.unam.mx/

650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

270.1.#.d: México

590.#.#.b: Concentrador

883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/892/846

100.1.#.a: Montalvo-arrieta, J. C.; Reinoso Angulo, E.; Sánchez-sesma, F. J.

524.#.#.a: Montalvo-arrieta, J. C., et al. (2003). Observations of strong ground motion at hill sites in Mexico City from recent earthquakes. Geofísica Internacional; Vol. 42 Núm. 2: Abril 1, 2003; 205-217. Recuperado de https://repositorio.unam.mx/contenidos/4132901

245.1.0.a: Observations of strong ground motion at hill sites in Mexico City from recent earthquakes

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2003

264.#.1.c: 2003-04-01

653.#.#.a: Ciudad de México; zona de lomas; cocientes espectrales; efectos de sitio; amplificación y trayectoria; Mexico City; hill zone; spectral ratio; site effects; amplification and wave path

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/892

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/892

041.#.7.h: spa

520.3.#.a: Results of seismic response of the stations of the Acelerometric Network of Mexico City located in the hill zone are pre- sented. Seven earthquakes from different seismic sources were analyzed, with magnitudes between 5.9 and 7.3. There is a depen- dence of the seismic response at hill sites on earthquake magnitude, azimuth, epicentral distance and depth. Subduction earth- quakes concentrate their energy at low frequencies (<1 Hz), while intraplate earthquakes have frequencies higher than 1 Hz. We find two significant types of amplification: regional, for sites located to the southwest hill zone over sites located to the north of the city, and local. Stations located in the southwest area show higher amplification with respect to the reference station. The spectral ratios of stations located in the central and southwest part of the hill zone show relative amplifications up to four times higher than stations located in the north area of the city for frequencies between 1 and 3 Hz. These local amplifications may be due to the presence of soft material under the lava flows where the stations are located.doi: https://doi.org/10.22201/igeof.00167169p.2003.42.2.265

773.1.#.t: Geofísica Internacional; Vol. 42 Núm. 2: Abril 1, 2003; 205-217

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 205-217

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.2003.42.2.265

handle: 00fc0c369d2cb7f4

harvesting_date: 2023-06-20 16:00:00.0

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file_creation_date: 2022-07-18 18:51:58.0

file_modification_date: 2022-07-18 18:51:58.0

file_creator: J. C. Montalvo-Arrieta

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245.1.0.b: Observations of strong ground motion at hill sites in Mexico City from recent earthquakes

last_modified: 2023-06-20 16:00:00

license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

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Artículo

Observations of strong ground motion at hill sites in Mexico City from recent earthquakes

Montalvo-arrieta, J. C.; Reinoso Angulo, E.; Sánchez-sesma, F. J.

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Montalvo-arrieta, J. C., et al. (2003). Observations of strong ground motion at hill sites in Mexico City from recent earthquakes. Geofísica Internacional; Vol. 42 Núm. 2: Abril 1, 2003; 205-217. Recuperado de https://repositorio.unam.mx/contenidos/4132901

Descripción del recurso

Autor(es)
Montalvo-arrieta, J. C.; Reinoso Angulo, E.; Sánchez-sesma, F. J.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Observations of strong ground motion at hill sites in Mexico City from recent earthquakes
Fecha
2003-04-01
Resumen
Results of seismic response of the stations of the Acelerometric Network of Mexico City located in the hill zone are pre- sented. Seven earthquakes from different seismic sources were analyzed, with magnitudes between 5.9 and 7.3. There is a depen- dence of the seismic response at hill sites on earthquake magnitude, azimuth, epicentral distance and depth. Subduction earth- quakes concentrate their energy at low frequencies (<1 Hz), while intraplate earthquakes have frequencies higher than 1 Hz. We find two significant types of amplification: regional, for sites located to the southwest hill zone over sites located to the north of the city, and local. Stations located in the southwest area show higher amplification with respect to the reference station. The spectral ratios of stations located in the central and southwest part of the hill zone show relative amplifications up to four times higher than stations located in the north area of the city for frequencies between 1 and 3 Hz. These local amplifications may be due to the presence of soft material under the lava flows where the stations are located.doi: https://doi.org/10.22201/igeof.00167169p.2003.42.2.265
Tema
Ciudad de México; zona de lomas; cocientes espectrales; efectos de sitio; amplificación y trayectoria; Mexico City; hill zone; spectral ratio; site effects; amplification and wave path
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces