dor_id: 4132328

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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

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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

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

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

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/757/1190

100.1.#.a: González-pomposo, G. J.; Valdés-gonzález, Carlos

524.#.#.a: González-pomposo, G. J., et al. (1995). Seismicity of the State of Puebla, Mexico, 1986-1989. Geofísica Internacional; Vol. 34 Núm. 2: Abril 1, 1995; 221-231. Recuperado de https://repositorio.unam.mx/contenidos/4132328

245.1.0.a: Seismicity of the State of Puebla, Mexico, 1986-1989

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1995

264.#.1.c: 1995-04-01

653.#.#.a: Sismicidad; hipocentro; magnitud; estado de Puebla; Seismicity; hypocenter; magnitud; Puebla State

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

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041.#.7.h: spa

520.3.#.a: The seismic activity in the State of Puebla, Mexico and its surroundings, between January 1986 and August 1989, is discussed using data from the seismic network of the University of Puebla. The hypocentral locations were obtained using the programs HYP071PC and HYPOCENT. The calculated theoretical errors using the program HYPOERR coincide with the estimated errors from the location procedure. A total of 350 earthquakes were located with rms less to 2. Most of the hypocenters are at depths less than 50 km, with the exception of the southern region, where events deeper than 50 km are found. These deeper events are probably associated with the contact between the oceanic and continental lithospheres, which correspond to the Cocos and North American plates. 92% of the events have coda magnitude between 2 and 4, although events with magnitudes greater than 7 have occurred in this region.

773.1.#.t: Geofísica Internacional; Vol. 34 Núm. 2: Abril 1, 1995; 221-231

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: 221-231

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

doi: https://doi.org/10.22201/igeof.00167169p.1995.34.2.757

handle: 00ee1504d8c0a5c1

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

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file_creator: G. J. González-Pomposo

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245.1.0.b: Seismicity of the State of Puebla, Mexico, 1986-1989

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Artículo

Seismicity of the State of Puebla, Mexico, 1986-1989

González-pomposo, G. J.; Valdés-gonzález, Carlos

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

González-pomposo, G. J., et al. (1995). Seismicity of the State of Puebla, Mexico, 1986-1989. Geofísica Internacional; Vol. 34 Núm. 2: Abril 1, 1995; 221-231. Recuperado de https://repositorio.unam.mx/contenidos/4132328

Descripción del recurso

Autor(es)
González-pomposo, G. J.; Valdés-gonzález, Carlos
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Seismicity of the State of Puebla, Mexico, 1986-1989
Fecha
1995-04-01
Resumen
The seismic activity in the State of Puebla, Mexico and its surroundings, between January 1986 and August 1989, is discussed using data from the seismic network of the University of Puebla. The hypocentral locations were obtained using the programs HYP071PC and HYPOCENT. The calculated theoretical errors using the program HYPOERR coincide with the estimated errors from the location procedure. A total of 350 earthquakes were located with rms less to 2. Most of the hypocenters are at depths less than 50 km, with the exception of the southern region, where events deeper than 50 km are found. These deeper events are probably associated with the contact between the oceanic and continental lithospheres, which correspond to the Cocos and North American plates. 92% of the events have coda magnitude between 2 and 4, although events with magnitudes greater than 7 have occurred in this region.
Tema
Sismicidad; hipocentro; magnitud; estado de Puebla; Seismicity; hypocenter; magnitud; Puebla State
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces