dor_id: 4133244

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

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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

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

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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/231/225

100.1.#.a: Rodríguez-lozoya, H. E.; Quintanar Robles, Luis; Huerta López, C. I.; Bojórquez Mora, E.; León Monzón, I.

524.#.#.a: Rodríguez-lozoya, H. E., et al. (2010). Source parameters of the July 30,. Geofísica Internacional; Vol. 49 Núm. 3: Julio 1, 2010; 119-129. Recuperado de https://repositorio.unam.mx/contenidos/4133244

245.1.0.a: Source parameters of the July 30,

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2010

264.#.1.c: 2010-06-01

653.#.#.a: Análisis espectral; mecanismo de falla lateral derecho; ejes principales de esfuerzos; Spectral analysis; right lateral strike slip fault mechanism; Principal axes of the stress

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/231

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041.#.7.h: spa

520.3.#.a: On July 30, 2006 at 01:20:52.28 (UTC) an earthquake of Mw 5.5, occurred in central Gulf of California (GoC), 226 km from Topolobampo and north-west of the transform fault between Guaymas and El Carmen basins.The earthquake was recorded on six broadband stations of the NARS-Baja seismic network (NE75, NE76, NE77, NE79, NE81 and NE82), and one broadband station of the RESBAN seismic network (TOPB). All stations were located within of epicentral distances of 70 to 220 km. From spectral analysis of SH-waveforms, the source dimensions, seismic moment, stress drop, source time and average displacement of this earthquake were obtained. The fault mechanism estimated by inversion of the seismic moment tensor yields a right lateral strike slip fault mechanism in agreement well with regional tectonics. Principal axes of the stress field (average azimuth 160º) matches the regional trend of the stress field of GoC (about 168º). We propose that the great majority of moderate magnitude earthquakes in this region, have right lateral strike-slip mechanism with principal stress oriented NW-SE. From the seismic history, the motion between plates can be described; moreover, plate motions along the Northwest-Southeast plate boundary between the Pacific and the North-America plates agree well with the regional seismic activity as obtained from the principal stress axes of moderate earthquakes in the region.doi: https://doi.org/10.22201/igeof.00167169p.2010.49.3.108

773.1.#.t: Geofísica Internacional; Vol. 49 Núm. 3: Julio 1, 2010; 119-129

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: 119-129

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

doi: https://doi.org/10.22201/igeof.00167169p.2010.49.3.108

handle: 0098314c1cc5a515

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

856.#.0.q: application/pdf

file_creation_date: 2010-08-25 17:50:05.0

file_modification_date: 2022-05-31 18:49:29.0

file_creator: H. E. Rodríguez-Lozoya

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245.1.0.b: Source parameters of the July 30, 2006 (Mw 5.5) Gulf of California earthquake and a comparison with other moderate earthquakes in the region

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

Source parameters of the July 30,

Rodríguez-lozoya, H. E.; Quintanar Robles, Luis; Huerta López, C. I.; Bojórquez Mora, E.; León Monzón, I.

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

Rodríguez-lozoya, H. E., et al. (2010). Source parameters of the July 30,. Geofísica Internacional; Vol. 49 Núm. 3: Julio 1, 2010; 119-129. Recuperado de https://repositorio.unam.mx/contenidos/4133244

Descripción del recurso

Autor(es)
Rodríguez-lozoya, H. E.; Quintanar Robles, Luis; Huerta López, C. I.; Bojórquez Mora, E.; León Monzón, I.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Source parameters of the July 30,
Fecha
2010-06-01
Resumen
On July 30, 2006 at 01:20:52.28 (UTC) an earthquake of Mw 5.5, occurred in central Gulf of California (GoC), 226 km from Topolobampo and north-west of the transform fault between Guaymas and El Carmen basins.The earthquake was recorded on six broadband stations of the NARS-Baja seismic network (NE75, NE76, NE77, NE79, NE81 and NE82), and one broadband station of the RESBAN seismic network (TOPB). All stations were located within of epicentral distances of 70 to 220 km. From spectral analysis of SH-waveforms, the source dimensions, seismic moment, stress drop, source time and average displacement of this earthquake were obtained. The fault mechanism estimated by inversion of the seismic moment tensor yields a right lateral strike slip fault mechanism in agreement well with regional tectonics. Principal axes of the stress field (average azimuth 160º) matches the regional trend of the stress field of GoC (about 168º). We propose that the great majority of moderate magnitude earthquakes in this region, have right lateral strike-slip mechanism with principal stress oriented NW-SE. From the seismic history, the motion between plates can be described; moreover, plate motions along the Northwest-Southeast plate boundary between the Pacific and the North-America plates agree well with the regional seismic activity as obtained from the principal stress axes of moderate earthquakes in the region.doi: https://doi.org/10.22201/igeof.00167169p.2010.49.3.108
Tema
Análisis espectral; mecanismo de falla lateral derecho; ejes principales de esfuerzos; Spectral analysis; right lateral strike slip fault mechanism; Principal axes of the stress
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces