dor_id: 4132307

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

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100.1.#.a: Rodríguez-lozoya, Héctor E.; Domínguez R., Tonatiuh; Quintanar Robles, Luis; Aguilar Meléndez, Armando; Rodríguez-leyva, Héctor E.; Plata Rocha, Wenseslao; García Páez, Fernando

524.#.#.a: Rodríguez-lozoya, Héctor E., et al. (2017). Attenuation of Coda Waves in the Central Region of the Gulf of California, México. Geofísica Internacional; Vol. 56 Núm. 2: Abril 1, 2017; 137-145. Recuperado de https://repositorio.unam.mx/contenidos/4132307

245.1.0.a: Attenuation of Coda Waves in the Central Region of the Gulf of California, México

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: Atenuación de coda; atenuación-frecuencia; Golfo de California; Mexico; Coda attenuation; attenuationfrequency; Gulf of California; Mexico

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: Coda waves were analyzed from events recorded by NARS seismic network deployed along both margins of the Gulf of California, Mexico, to estimate coda attenuation Qc. Sato’s (1977) single scattering model was used for a coda window of 20 to 25 s beginning at twice the S-wave travel time. Events recorded from 2003 to 2007 located in the central region of the Gulf of California were analyzed. Source-to-receiver distances are between 40 and 500 km. Assuming a power law of the form QC (f) = QO f a, QC values were averaged and a value of QO = 83±3 and a frequency-dependence α value of 1.06±0.03 in the frequency range from 1 to 7 Hz was obtained. QO value and the high frequency dependency agree with the values of other regions characterized by a high tectonic activity. Based on source-station distribution two subregions (north and south) were defined. QC values were calculated and correlated with tectonics and morphology of each area. The observed higher attenuation in the south region can be attributed to the fact that south region is more fractured since the greater earthquakes occur in central to south Gulf of California and the oceanic crust is reported to be thinner in the southern region.doi: https://doi.org/10.22201/igeof.00167169p.2017.56.2.1761

773.1.#.t: Geofísica Internacional; Vol. 56 Núm. 2: Abril 1, 2017; 137-145

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

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

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300.#.#.a: Páginas: 137-145

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doi: https://doi.org/10.22201/igeof.00167169p.2017.56.2.1761

handle: 00a66da6d2ea1c45

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

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file_modification_date: 2022-04-04 16:59:12.0

file_creator: Héctor E. Rodríguez-Lozoya

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245.1.0.b: Attenuation of Coda Waves in the Central Region of the Gulf of California, México

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Artículo

Attenuation of Coda Waves in the Central Region of the Gulf of California, México

Rodríguez-lozoya, Héctor E.; Domínguez R., Tonatiuh; Quintanar Robles, Luis; Aguilar Meléndez, Armando; Rodríguez-leyva, Héctor E.; Plata Rocha, Wenseslao; García Páez, Fernando

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, Héctor E., et al. (2017). Attenuation of Coda Waves in the Central Region of the Gulf of California, México. Geofísica Internacional; Vol. 56 Núm. 2: Abril 1, 2017; 137-145. Recuperado de https://repositorio.unam.mx/contenidos/4132307

Descripción del recurso

Autor(es)
Rodríguez-lozoya, Héctor E.; Domínguez R., Tonatiuh; Quintanar Robles, Luis; Aguilar Meléndez, Armando; Rodríguez-leyva, Héctor E.; Plata Rocha, Wenseslao; García Páez, Fernando
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Attenuation of Coda Waves in the Central Region of the Gulf of California, México
Fecha
2017-04-01
Resumen
Coda waves were analyzed from events recorded by NARS seismic network deployed along both margins of the Gulf of California, Mexico, to estimate coda attenuation Qc. Sato’s (1977) single scattering model was used for a coda window of 20 to 25 s beginning at twice the S-wave travel time. Events recorded from 2003 to 2007 located in the central region of the Gulf of California were analyzed. Source-to-receiver distances are between 40 and 500 km. Assuming a power law of the form QC (f) = QO f a, QC values were averaged and a value of QO = 83±3 and a frequency-dependence α value of 1.06±0.03 in the frequency range from 1 to 7 Hz was obtained. QO value and the high frequency dependency agree with the values of other regions characterized by a high tectonic activity. Based on source-station distribution two subregions (north and south) were defined. QC values were calculated and correlated with tectonics and morphology of each area. The observed higher attenuation in the south region can be attributed to the fact that south region is more fractured since the greater earthquakes occur in central to south Gulf of California and the oceanic crust is reported to be thinner in the southern region.doi: https://doi.org/10.22201/igeof.00167169p.2017.56.2.1761
Tema
Atenuación de coda; atenuación-frecuencia; Golfo de California; Mexico; Coda attenuation; attenuationfrequency; Gulf of California; Mexico
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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