dor_id: 4132310

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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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850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1077/1008

100.1.#.a: Cebull, S. E.; Shurbet, D. H.

524.#.#.a: Cebull, S. E., et al. (1987). Mexican Volcanic Belt: an intraplate transform?. Geofísica Internacional; Vol. 26 Núm. 1: Enero 1, 1987; 1-13. Recuperado de https://repositorio.unam.mx/contenidos/4132310

245.1.0.a: Mexican Volcanic Belt: an intraplate transform?

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1987

264.#.1.c: 1987-01-01

653.#.#.a: Tectónica; volcanismo; cinturón volcánico mexicano; Tectonics; volcanism; mexican volcanic belt

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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001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1077

041.#.7.h: spa

520.3.#.a: Temporal and "geometric" evidence suggests that several regional tectonic events were especially important contributors during the evolution of the Mexican Volcanic Belt (MVB). These include (1) development of a tectonic zone of weakness in the area of the present MVB, followed in Cenozoic time by (2) tectonic activity in the Caribbean region that includes sea-floor spreading in the Cayman Trough, (3) progressive southward cessation of subduction along the west coast of North and Central America, and (4) development of the proto-Gulf, Gulf of California, and basin-and-range (extensional) faulting north of the MVB. The zone of weakness fixed the location and orientation of the MVB. Subsequently, in response to cessation of subduction along the coast of North America, extensional tectonics developed to the north of the zone. To the south, where subduction of Chilean-type prevailed, extensional tectonism was inhibited. Thus, the zone of weakness became a belt of tectonic accomodation, perhaps associated with internal extension, between regions of contrasting structural kinematics. In short, it became an (leaky) intraplate tr-ansform (in the sense of Davis, 1980) along which the volcanism was both permitted and localized. Paradoxically, this interpretation implies that volcanism along the MVB is more closely allied to the cessation of subduction north of the MVB than to ongoing subduction to the south. It further implies that the MVB is fundamentally unlike the typical volcanic arcs of the Pacific rim.doi: https://doi.org/10.22201/igeof.00167169p.1987.26.1.1187

773.1.#.t: Geofísica Internacional; Vol. 26 Núm. 1: Enero 1, 1987; 1-13

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: 1-13

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doi: https://doi.org/10.22201/igeof.00167169p.1987.26.1.1187

handle: 6fbe8dfd0b627745

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

856.#.0.q: application/pdf

file_creation_date: 2008-06-25 22:11:21.0

file_modification_date: 2022-07-14 03:12:35.0

file_creator: S.E. Cebull

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245.1.0.b: Mexican Volcanic Belt: an intraplate transform?

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Artículo

Mexican Volcanic Belt: an intraplate transform?

Cebull, S. E.; Shurbet, D. H.

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

Cebull, S. E., et al. (1987). Mexican Volcanic Belt: an intraplate transform?. Geofísica Internacional; Vol. 26 Núm. 1: Enero 1, 1987; 1-13. Recuperado de https://repositorio.unam.mx/contenidos/4132310

Descripción del recurso

Autor(es)
Cebull, S. E.; Shurbet, D. H.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Mexican Volcanic Belt: an intraplate transform?
Fecha
1987-01-01
Resumen
Temporal and "geometric" evidence suggests that several regional tectonic events were especially important contributors during the evolution of the Mexican Volcanic Belt (MVB). These include (1) development of a tectonic zone of weakness in the area of the present MVB, followed in Cenozoic time by (2) tectonic activity in the Caribbean region that includes sea-floor spreading in the Cayman Trough, (3) progressive southward cessation of subduction along the west coast of North and Central America, and (4) development of the proto-Gulf, Gulf of California, and basin-and-range (extensional) faulting north of the MVB. The zone of weakness fixed the location and orientation of the MVB. Subsequently, in response to cessation of subduction along the coast of North America, extensional tectonics developed to the north of the zone. To the south, where subduction of Chilean-type prevailed, extensional tectonism was inhibited. Thus, the zone of weakness became a belt of tectonic accomodation, perhaps associated with internal extension, between regions of contrasting structural kinematics. In short, it became an (leaky) intraplate tr-ansform (in the sense of Davis, 1980) along which the volcanism was both permitted and localized. Paradoxically, this interpretation implies that volcanism along the MVB is more closely allied to the cessation of subduction north of the MVB than to ongoing subduction to the south. It further implies that the MVB is fundamentally unlike the typical volcanic arcs of the Pacific rim.doi: https://doi.org/10.22201/igeof.00167169p.1987.26.1.1187
Tema
Tectónica; volcanismo; cinturón volcánico mexicano; Tectonics; volcanism; mexican volcanic belt
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces