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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

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

270.1.#.d: México

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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/477/491

100.1.#.a: Maillol, J. M.; Bandy, W. L.

524.#.#.a: Maillol, J. M., et al. (1994). Paleomagnetism of the Talpa de Allende and Mascota grabens, western Mexico: A preliminary report. Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 153-160. Recuperado de https://repositorio.unam.mx/contenidos/4133231

245.1.0.a: Paleomagnetism of the Talpa de Allende and Mascota grabens, western Mexico: A preliminary report

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1994

264.#.1.c: 1994-01-01

653.#.#.a: Paleomagnetismo; tectónica; Jalisco; México; Paleomagnetism; tectonics; Jalisco; 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

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/477

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041.#.7.h: spa

520.3.#.a: The Jalisco Block of Western Mexico is thought to be undergoing internal deformation associated with its proposed NW translation relative to the North America plate. This deformation has resulted in the formation of several graben structures within the northern portion of the Jalisco Block; two of which are the Talpa de Allende and Mascota grabens.An analysis of paleomagnetic data collected at six distinct, recent, lava flows within the Talpa de Allende and Mascota grabens fail to indicated any statically significant (95% confidence level) motions in this area. Specifically, the expected direction of the geocentric axial dipole field at the site location (D=0°, I=37°)lies within the 95% confidence cone associated with the mean direction calculated for these six sites (D=352.2°, I=24.0°, α95=16.8°).However, the flattening parameter associated with the mean direction of these six sites (12.8±13.1), along with the close proximity of both the North American reference pole and the expected field direction at the side to the corresponding 95% confidence cones of the paleomagnetic results, indicates that additional data may allow for the resolution of the proposed northward movement of the Jalisco Block or of local tiling associated with faulting.doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.546

773.1.#.t: Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 153-160

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: 153-160

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

doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.546

handle: 56a3928e544f58d6

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

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file_creation_date: 2008-02-22 16:51:43.0

file_modification_date: 2022-07-05 18:17:28.0

file_creator: J. M. Maillol and W. L. Bandy

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245.1.0.b: Paleomagnetism of the Talpa de Allende and Mascota grabens, western Mexico: A preliminary report

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Artículo

Paleomagnetism of the Talpa de Allende and Mascota grabens, western Mexico: A preliminary report

Maillol, J. M.; Bandy, W. L.

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

Maillol, J. M., et al. (1994). Paleomagnetism of the Talpa de Allende and Mascota grabens, western Mexico: A preliminary report. Geofísica Internacional; Vol. 33 Núm. 1: Enero 1, 1994; 153-160. Recuperado de https://repositorio.unam.mx/contenidos/4133231

Descripción del recurso

Autor(es)
Maillol, J. M.; Bandy, W. L.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Paleomagnetism of the Talpa de Allende and Mascota grabens, western Mexico: A preliminary report
Fecha
1994-01-01
Resumen
The Jalisco Block of Western Mexico is thought to be undergoing internal deformation associated with its proposed NW translation relative to the North America plate. This deformation has resulted in the formation of several graben structures within the northern portion of the Jalisco Block; two of which are the Talpa de Allende and Mascota grabens.An analysis of paleomagnetic data collected at six distinct, recent, lava flows within the Talpa de Allende and Mascota grabens fail to indicated any statically significant (95% confidence level) motions in this area. Specifically, the expected direction of the geocentric axial dipole field at the site location (D=0°, I=37°)lies within the 95% confidence cone associated with the mean direction calculated for these six sites (D=352.2°, I=24.0°, α95=16.8°).However, the flattening parameter associated with the mean direction of these six sites (12.8±13.1), along with the close proximity of both the North American reference pole and the expected field direction at the side to the corresponding 95% confidence cones of the paleomagnetic results, indicates that additional data may allow for the resolution of the proposed northward movement of the Jalisco Block or of local tiling associated with faulting.doi: https://doi.org/10.22201/igeof.00167169p.1994.33.1.546
Tema
Paleomagnetismo; tectónica; Jalisco; México; Paleomagnetism; tectonics; Jalisco; Mexico
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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