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

336.#.#.b: article

336.#.#.3: Artículo de Investigación

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351.#.#.b: Geofísica Internacional

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

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

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

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1235/1214

100.1.#.a: Krishna Singh, Shri; Arroyo, Danny; Pérez-campos, Xyoli; Iglesias, Arturo; Espíndola, Víctor Hugo; Ramírez, Leonardo; Pérez, Citlalli; Sandoval, Héctor

524.#.#.a: Krishna Singh, Shri, et al. (2017). Guadalajara, Mexico, Earthquake Sequence of December. Geofísica Internacional; Vol. 56 Núm. 2: Abril 1, 2017; 173-186. Recuperado de https://repositorio.unam.mx/contenidos/4132362

245.1.0.a: Guadalajara, Mexico, Earthquake Sequence of December

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2017

264.#.1.c: 2017-04-01

653.#.#.a: secuencia de sismos de Guadalajara; valores pico de movimiento del terreno; peligro sísmico en Guadalajara; Guadalajara earthquake sequence; peak ground motion; Seismic hazard in Guadalajara

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/1235

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1235

041.#.7.h: spa

520.3.#.a: We analyze an earthquake sequence which occurred 24 km NNW from Guadalajara Cathedral. The activity began on 15 December, 2015 with an Mw4.1 earthquake and resumed, again, on 11 May, 2016 when the largest earthquake of the sequence, Mw4.8, occurred. The earthquakes were recorded in the city by two accelerographs and at larger distances by broadband seismographs. The source region of the sequence is located in the north of the broad junction formed by NW-SE trending Tepic-Zacoalco rift, N-S trending Colima rift, and E-W trending Chapala rift. The focal mechanism of the largest event is characterized by: strike ϕ= 21º, dip = 49º, and rake = -86º, with horizontal tensional axis trending 110º. This mechanism is not consistent with NE-SW direction of motion measured on fault strike by Barrier et al. (1990) ~ 35 km WNW of Guadalajara. It also differs from the mechanism reported in a previous study for a seismic sequence in the Zacoalco rift about 60 km south of Guadalajara. Similarities among recorded waveforms at the accelerographic stations suggest that the mechanism of other events in the sequence were similar and the events were located in a small volume, probably 1 to 2 km in radius. From the análisis of the recordings of the 11 May shock along the Trans-Mexican Volcanic Belt, from Ceboruco volcano to the west and Popocatepetl volcano to the east, the attenuation parameter Q as 141f 0.63 was estimated. The earthquake on 11 May was felt very strongly in the city and produced peak ground acceleration (PGA) reaching 80 cm/s2. Relatively large earthquakes have been reported in the region; e.g., on 11 February, 1875 near the town of San Cristobal de la Barranca, about 40 km NNW of Guadalajara, therefore, the interest on using recordings from accelerographic stations to estimate peak ground motion parameters for scenario earthquakes of Mw ≤ 6.0 using random vibration theory (RVT) and empirical Green’s function (EGF) techniques. From RVT simulations, the expected PGA, peak ground velocity (PGV), and peak ground displacement (PGD) at the accelerographic stations from an Mw6.0 earthquake in the source region of the sequence are 195 cm/s2, 10 cm/s, and 3 cm, respectively. The predictions from the EGF technique are somewhat higher but still within a factor of two of the RVT predictions.doi: https://doi.org/10.22201/igeof.00167169p.2017.56.2.1764

773.1.#.t: Geofísica Internacional; Vol. 56 Núm. 2: Abril 1, 2017; 173-186

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: 173-186

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

doi: https://doi.org/10.22201/igeof.00167169p.2017.56.2.1764

handle: 5c6028eada0c3dea

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

856.#.0.q: application/pdf

file_creation_date: 2017-06-21 23:14:22.0

file_modification_date: 2022-04-07 21:15:02.0

file_creator: Shri Krishna Singh

file_name: 9b2afa4bbdb9d973f2fbc554500ed875611fdc0959e21972fc24c837bfff3110.pdf

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file_size: 11371062

245.1.0.b: Guadalajara, Mexico, Earthquake Sequence of December 2015 and May 2016: Source, Q, and Ground Motions

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

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Artículo

Guadalajara, Mexico, Earthquake Sequence of December

Krishna Singh, Shri; Arroyo, Danny; Pérez-campos, Xyoli; Iglesias, Arturo; Espíndola, Víctor Hugo; Ramírez, Leonardo; Pérez, Citlalli; Sandoval, Héctor

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

Krishna Singh, Shri, et al. (2017). Guadalajara, Mexico, Earthquake Sequence of December. Geofísica Internacional; Vol. 56 Núm. 2: Abril 1, 2017; 173-186. Recuperado de https://repositorio.unam.mx/contenidos/4132362

Descripción del recurso

Autor(es)
Krishna Singh, Shri; Arroyo, Danny; Pérez-campos, Xyoli; Iglesias, Arturo; Espíndola, Víctor Hugo; Ramírez, Leonardo; Pérez, Citlalli; Sandoval, Héctor
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Guadalajara, Mexico, Earthquake Sequence of December
Fecha
2017-04-01
Resumen
We analyze an earthquake sequence which occurred 24 km NNW from Guadalajara Cathedral. The activity began on 15 December, 2015 with an Mw4.1 earthquake and resumed, again, on 11 May, 2016 when the largest earthquake of the sequence, Mw4.8, occurred. The earthquakes were recorded in the city by two accelerographs and at larger distances by broadband seismographs. The source region of the sequence is located in the north of the broad junction formed by NW-SE trending Tepic-Zacoalco rift, N-S trending Colima rift, and E-W trending Chapala rift. The focal mechanism of the largest event is characterized by: strike ϕ= 21º, dip = 49º, and rake = -86º, with horizontal tensional axis trending 110º. This mechanism is not consistent with NE-SW direction of motion measured on fault strike by Barrier et al. (1990) ~ 35 km WNW of Guadalajara. It also differs from the mechanism reported in a previous study for a seismic sequence in the Zacoalco rift about 60 km south of Guadalajara. Similarities among recorded waveforms at the accelerographic stations suggest that the mechanism of other events in the sequence were similar and the events were located in a small volume, probably 1 to 2 km in radius. From the análisis of the recordings of the 11 May shock along the Trans-Mexican Volcanic Belt, from Ceboruco volcano to the west and Popocatepetl volcano to the east, the attenuation parameter Q as 141f 0.63 was estimated. The earthquake on 11 May was felt very strongly in the city and produced peak ground acceleration (PGA) reaching 80 cm/s2. Relatively large earthquakes have been reported in the region; e.g., on 11 February, 1875 near the town of San Cristobal de la Barranca, about 40 km NNW of Guadalajara, therefore, the interest on using recordings from accelerographic stations to estimate peak ground motion parameters for scenario earthquakes of Mw ≤ 6.0 using random vibration theory (RVT) and empirical Green’s function (EGF) techniques. From RVT simulations, the expected PGA, peak ground velocity (PGV), and peak ground displacement (PGD) at the accelerographic stations from an Mw6.0 earthquake in the source region of the sequence are 195 cm/s2, 10 cm/s, and 3 cm, respectively. The predictions from the EGF technique are somewhat higher but still within a factor of two of the RVT predictions.doi: https://doi.org/10.22201/igeof.00167169p.2017.56.2.1764
Tema
secuencia de sismos de Guadalajara; valores pico de movimiento del terreno; peligro sísmico en Guadalajara; Guadalajara earthquake sequence; peak ground motion; Seismic hazard in Guadalajara
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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