dor_id: 4133024

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

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

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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/1083/1014

100.1.#.a: Pasquare, G.; Vezzoli, L.; Zanchi, A.

524.#.#.a: Pasquare, G., et al. (1987). Morphological and structural model of Mexican Volcanic Belt. Geofísica Internacional; Vol. 26 Núm. 2: Abril 1, 1987; 159-175. Recuperado de https://repositorio.unam.mx/contenidos/4133024

245.1.0.a: Morphological and structural model of Mexican Volcanic Belt

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1987

264.#.1.c: 1987-04-01

653.#.#.a: Morfología; unidades estructurales; cinturón volcánico mexicano; Morphology; structural units; 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

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1083

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1083

041.#.7.h: spa

520.3.#.a: On the basis of geological, geomorphological and structural data, the main structural units forming the Mexican Volcanic Belt (MVB) were recognized. They have been generated during several tensional phases since Oligocene. Many of the structures connected with these units are still active. Three main sectors were recognized inside the MVB. The western sector, activated during Pliocene times, shows a NW-SE trending graben system, associated to the opening of the Gulf of California. The central sector is represented by a block-faulted and tilted WSW-ENE trending graben system, surrounding a central depression. In the oriental sector the disjunctive structures are represented by N-S fault systems affecting the rigid basement of Sierra Madre Oriental, and controlling the development of the largest strato-volcanoes of the MVB. The MVB intersects older N-S and NNE-SW block-faulted structures, belonging to the Basin and Range province. Reactivated tensional lineaments belonging to the same province were recognized inside the western and the central sector, and probably in the eastern one too. Along the southern margin of the same volcanic belt all the described distensive structures are interrupted, and huge E-W collapsed structures coincident with the Rio Balsas valley develop. doi: https://doi.org/10.22201/igeof.00167169p.1987.26.2.1107

773.1.#.t: Geofísica Internacional; Vol. 26 Núm. 2: Abril 1, 1987; 159-175

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: 159-175

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

doi: https://doi.org/10.22201/igeof.00167169p.1987.26.2.1107

handle: 00ac564efedf61f7

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

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245.1.0.b: Morphological and structural model of Mexican Volcanic Belt

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Artículo

Morphological and structural model of Mexican Volcanic Belt

Pasquare, G.; Vezzoli, L.; Zanchi, A.

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

Pasquare, G., et al. (1987). Morphological and structural model of Mexican Volcanic Belt. Geofísica Internacional; Vol. 26 Núm. 2: Abril 1, 1987; 159-175. Recuperado de https://repositorio.unam.mx/contenidos/4133024

Descripción del recurso

Autor(es)
Pasquare, G.; Vezzoli, L.; Zanchi, A.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Morphological and structural model of Mexican Volcanic Belt
Fecha
1987-04-01
Resumen
On the basis of geological, geomorphological and structural data, the main structural units forming the Mexican Volcanic Belt (MVB) were recognized. They have been generated during several tensional phases since Oligocene. Many of the structures connected with these units are still active. Three main sectors were recognized inside the MVB. The western sector, activated during Pliocene times, shows a NW-SE trending graben system, associated to the opening of the Gulf of California. The central sector is represented by a block-faulted and tilted WSW-ENE trending graben system, surrounding a central depression. In the oriental sector the disjunctive structures are represented by N-S fault systems affecting the rigid basement of Sierra Madre Oriental, and controlling the development of the largest strato-volcanoes of the MVB. The MVB intersects older N-S and NNE-SW block-faulted structures, belonging to the Basin and Range province. Reactivated tensional lineaments belonging to the same province were recognized inside the western and the central sector, and probably in the eastern one too. Along the southern margin of the same volcanic belt all the described distensive structures are interrupted, and huge E-W collapsed structures coincident with the Rio Balsas valley develop. doi: https://doi.org/10.22201/igeof.00167169p.1987.26.2.1107
Tema
Morfología; unidades estructurales; cinturón volcánico mexicano; Morphology; structural units; mexican volcanic belt
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces