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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

561.#.#.u: https://www.geofisica.unam.mx/

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

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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/

883.#.#.a: Revistas UNAM

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

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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/301/289

100.1.#.a: Bursik, M.

524.#.#.a: Bursik, M. (2009). A general model for tectonic control of magmatism: Examples from Long Valley Caldera (USA) and El Chichón (México). Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 171-183. Recuperado de https://repositorio.unam.mx/contenidos/4133057

245.1.0.a: A general model for tectonic control of magmatism: Examples from Long Valley Caldera (USA) and El Chichón (México)

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2009

264.#.1.c: 2009-01-01

653.#.#.a: Caldera Long Valley; arco volcánico chiapaneco; control tectónico del volcanismo; tectónica y magmatismo; fallamiento en ambientes volcánicos; Long Valley Caldera; Mono-Inyo Craters; El Chichón; California; Mexico; dike; releasing bend; pull apart; volcanotectonic; regional tectonics

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/301

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041.#.7.h: spa

520.3.#.a: The relationship of volcanoes to regional tectonic setting and earthquake dynamics is intimate. We know that eruptions are often triggered by earthquakes, and that volcanoes generally lie along or near major faults or within faulted provinces. It has been generally found that bimodal basaltic-rhyolitic volcanism is associated with extensional settings, presumably because of the creation of accommodating space. For intermediate arc volcanoes, tectonic settings are generally compressional or transpressional. The spatial pattern of faulting indicates that Long Valley was focussed by a releasing bend in the transtensional, Sierran range-front fault system. The temporal pattern of offset rates suggests that the zone of greatest activity has migrated to the NW through time, and is now focussed at the Mono-Inyo Craters. The southern Mexican volcanic arc presents an example of the coexistence of regional compressional and transpressional structures with volcanoes. On an event basis, slip on regional structures creates opportunities for magma movement and eruption, in a type of dynamic fault pumping of fl uids. Both kinematically and dynamically, volcanic activity may be completely dependent on tectonic factors for accumulation, storage and eruption of magma.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.106

773.1.#.t: Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 171-183

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: 171-183

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

doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.106

handle: 00d01813b98817e1

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

856.#.0.q: application/pdf

file_creation_date: 2009-01-21 15:59:28.0

file_modification_date: 2022-05-30 14:32:47.0

file_creator: Bursik M.

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245.1.0.b: A general model for tectonic control of magmatism: Examples from Long Valley Caldera (USA) and El Chichón (México)

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

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Artículo

A general model for tectonic control of magmatism: Examples from Long Valley Caldera (USA) and El Chichón (México)

Bursik, M.

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

Bursik, M. (2009). A general model for tectonic control of magmatism: Examples from Long Valley Caldera (USA) and El Chichón (México). Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 171-183. Recuperado de https://repositorio.unam.mx/contenidos/4133057

Descripción del recurso

Autor(es)
Bursik, M.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
A general model for tectonic control of magmatism: Examples from Long Valley Caldera (USA) and El Chichón (México)
Fecha
2009-01-01
Resumen
The relationship of volcanoes to regional tectonic setting and earthquake dynamics is intimate. We know that eruptions are often triggered by earthquakes, and that volcanoes generally lie along or near major faults or within faulted provinces. It has been generally found that bimodal basaltic-rhyolitic volcanism is associated with extensional settings, presumably because of the creation of accommodating space. For intermediate arc volcanoes, tectonic settings are generally compressional or transpressional. The spatial pattern of faulting indicates that Long Valley was focussed by a releasing bend in the transtensional, Sierran range-front fault system. The temporal pattern of offset rates suggests that the zone of greatest activity has migrated to the NW through time, and is now focussed at the Mono-Inyo Craters. The southern Mexican volcanic arc presents an example of the coexistence of regional compressional and transpressional structures with volcanoes. On an event basis, slip on regional structures creates opportunities for magma movement and eruption, in a type of dynamic fault pumping of fl uids. Both kinematically and dynamically, volcanic activity may be completely dependent on tectonic factors for accumulation, storage and eruption of magma.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.106
Tema
Caldera Long Valley; arco volcánico chiapaneco; control tectónico del volcanismo; tectónica y magmatismo; fallamiento en ambientes volcánicos; Long Valley Caldera; Mono-Inyo Craters; El Chichón; California; Mexico; dike; releasing bend; pull apart; volcanotectonic; regional tectonics
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces