dor_id: 4133026

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

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270.#.#.d: MX

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883.#.#.u: https://revistas.unam.mx/catalogo/

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

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/575/594

100.1.#.a: Campillo, M.; Singh, S. K.; Shapiro, N.; Pacheco, J.; Hemnann, R. B.

524.#.#.a: Campillo, M., et al. (1996). Crustal structure south of the Mexican volcanic belt, base don group velocity dispersion. Geofísica Internacional; Vol. 35 Núm. 4: Octubre 1, 1996; 361-370. Recuperado de https://repositorio.unam.mx/contenidos/4133026

245.1.0.a: Crustal structure south of the Mexican volcanic belt, base don group velocity dispersion

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1996

264.#.1.c: 1996-10-01

653.#.#.a: Estructura cortical; corteza Mexicana; dispersión de ondas superficiales; Crustal structure; Mexican crust; surface-wave dispersion

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/575

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/575

041.#.7.h: spa

520.3.#.a: An average shear-wave velocity structure of the crust has been estimated for paths between the Guerrero-Michoacan coast, along the Mexican subduction zone, and Mexico City. This structure is obtained from inversion of group velocity dispersion data, estimated from broadband seismograms of regional events recorded in the city. For a better defmition of the dispersion curve we have used a new stacking technique of the period-group velocity amplitude distributions of individual records. The mid-crustal structure (5 to 30 km depth) is well defmed but both the shallow and the deep structures are not well resolved due to limited period range of the dispersion data. A clear boundary between the upper and lower crust is found between 15 and 20 km. Synthetic seismograms computed for the model compare well with the observed ones, giving us confidence in the results and in the possible use of this model in routine determination of moment tensor solutions. The thick low-velocity superficial layer found in the Oaxaca region is not present beneath the region studied here.doi: https://doi.org/10.22201/igeof.00167169p.1996.35.4.529

773.1.#.t: Geofísica Internacional; Vol. 35 Núm. 4: Octubre 1, 1996; 361-370

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: 361-370

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

doi: https://doi.org/10.22201/igeof.00167169p.1996.35.4.529

handle: 00c9da79c7390a9a

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

856.#.0.q: application/pdf

file_creation_date: 2008-02-14 20:11:49.0

file_modification_date: 2022-07-11 17:22:00.0

file_creator: M. Campillo

file_name: e29e80c6450d4d0a6cb12994933e4681b68d673786a7f5bf52d246494e6184d2.pdf

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245.1.0.b: Crustal structure south of the Mexican volcanic belt, base don group velocity dispersion

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

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

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Artículo

Crustal structure south of the Mexican volcanic belt, base don group velocity dispersion

Campillo, M.; Singh, S. K.; Shapiro, N.; Pacheco, J.; Hemnann, R. B.

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

Campillo, M., et al. (1996). Crustal structure south of the Mexican volcanic belt, base don group velocity dispersion. Geofísica Internacional; Vol. 35 Núm. 4: Octubre 1, 1996; 361-370. Recuperado de https://repositorio.unam.mx/contenidos/4133026

Descripción del recurso

Autor(es)
Campillo, M.; Singh, S. K.; Shapiro, N.; Pacheco, J.; Hemnann, R. B.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Crustal structure south of the Mexican volcanic belt, base don group velocity dispersion
Fecha
1996-10-01
Resumen
An average shear-wave velocity structure of the crust has been estimated for paths between the Guerrero-Michoacan coast, along the Mexican subduction zone, and Mexico City. This structure is obtained from inversion of group velocity dispersion data, estimated from broadband seismograms of regional events recorded in the city. For a better defmition of the dispersion curve we have used a new stacking technique of the period-group velocity amplitude distributions of individual records. The mid-crustal structure (5 to 30 km depth) is well defmed but both the shallow and the deep structures are not well resolved due to limited period range of the dispersion data. A clear boundary between the upper and lower crust is found between 15 and 20 km. Synthetic seismograms computed for the model compare well with the observed ones, giving us confidence in the results and in the possible use of this model in routine determination of moment tensor solutions. The thick low-velocity superficial layer found in the Oaxaca region is not present beneath the region studied here.doi: https://doi.org/10.22201/igeof.00167169p.1996.35.4.529
Tema
Estructura cortical; corteza Mexicana; dispersión de ondas superficiales; Crustal structure; Mexican crust; surface-wave dispersion
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces