dor_id: 4133476

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/628/1167

100.1.#.a: Wong, V.; Frez, J.; Suarez, F.

524.#.#.a: Wong, V., et al. (1997). The Victoria, Mexico, Earthquake of June 9, 1980. Geofísica Internacional; Vol. 36 Núm. 3: Julio 1, 1997; 139-159. Recuperado de https://repositorio.unam.mx/contenidos/4133476

245.1.0.a: The Victoria, Mexico, Earthquake of June 9, 1980

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1997

264.#.1.c: 1997-07-01

653.#.#.a: Sismo de Victoria; actividad de replicas; efectos por el sismo; Valle de Mexicali; Victoria Earthquake; aftershock activity; earthquake effects; Mexicali Valley

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/628

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/628

041.#.7.h: spa

520.3.#.a: The Victoria earthquake of June 9, 1980 (ML = 6.1 ), occurred in the Mexicali Valley near the trace of the Cerro Prieto fault with a focal mechanism consisting of a dextral strike-slip motion on a vertical fault. We present results from an analysis of local data concerning ground surface effects, epicenter locations, and focal mechanisms of the main shock and its aftershock activity. A field reconnaissance showed no clear ground surface displacement related to the main shock. The aftershocks occurred northwest of the main shock epicenter, in a few clusters at or near the northwest end of the Cerro Prieto fault. There was some aftershock activity north of the Cerro Prieto fault tip and towards the southeast end of the Imperial fault. Only a few aftershocks were located near the main shock; they occurred during the first few hours after the main event. The aftershock activity was mainly located between 3 and 8 km in depth, beneath the thick overlying sediments. The average depth of the aftershocks generally decreases to the northwest, away from the main epicenter which is at a depth of about 9 km. Composite focal mechanisms of the aftershocks show a right-lateral strike-slip motion on a vertical plane striking N45°W for the cluster near the main shock epicenter, and normal faulting for the cluster at the northwest end of the Cerro Prieto fault. Two small tightly clustered earthquake swarms occurred a few hours before the main shock.

773.1.#.t: Geofísica Internacional; Vol. 36 Núm. 3: Julio 1, 1997; 139-159

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: 139-159

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

doi: https://doi.org/10.22201/igeof.00167169p.1997.36.3.628

handle: 555aaf0ad361f4f4

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-07 12:00:36.0

file_modification_date: 2022-07-12 18:27:52.0

file_creator: V.Wong

file_name: e4eda88973e34e4251534c92825d912d7cd1307ffa599a52b4a7ad29418b42c6.pdf

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245.1.0.b: The Victoria, Mexico, Earthquake of June 9, 1980

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

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

license_type: by-nc-sa

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Artículo

The Victoria, Mexico, Earthquake of June 9, 1980

Wong, V.; Frez, J.; Suarez, F.

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

Wong, V., et al. (1997). The Victoria, Mexico, Earthquake of June 9, 1980. Geofísica Internacional; Vol. 36 Núm. 3: Julio 1, 1997; 139-159. Recuperado de https://repositorio.unam.mx/contenidos/4133476

Descripción del recurso

Autor(es)
Wong, V.; Frez, J.; Suarez, F.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
The Victoria, Mexico, Earthquake of June 9, 1980
Fecha
1997-07-01
Resumen
The Victoria earthquake of June 9, 1980 (ML = 6.1 ), occurred in the Mexicali Valley near the trace of the Cerro Prieto fault with a focal mechanism consisting of a dextral strike-slip motion on a vertical fault. We present results from an analysis of local data concerning ground surface effects, epicenter locations, and focal mechanisms of the main shock and its aftershock activity. A field reconnaissance showed no clear ground surface displacement related to the main shock. The aftershocks occurred northwest of the main shock epicenter, in a few clusters at or near the northwest end of the Cerro Prieto fault. There was some aftershock activity north of the Cerro Prieto fault tip and towards the southeast end of the Imperial fault. Only a few aftershocks were located near the main shock; they occurred during the first few hours after the main event. The aftershock activity was mainly located between 3 and 8 km in depth, beneath the thick overlying sediments. The average depth of the aftershocks generally decreases to the northwest, away from the main epicenter which is at a depth of about 9 km. Composite focal mechanisms of the aftershocks show a right-lateral strike-slip motion on a vertical plane striking N45°W for the cluster near the main shock epicenter, and normal faulting for the cluster at the northwest end of the Cerro Prieto fault. Two small tightly clustered earthquake swarms occurred a few hours before the main shock.
Tema
Sismo de Victoria; actividad de replicas; efectos por el sismo; Valle de Mexicali; Victoria Earthquake; aftershock activity; earthquake effects; Mexicali Valley
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces