dor_id: 4132624

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

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

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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/1084/1015

100.1.#.a: Pasquare, G.; Ferrari, L.; Perazzoli, V.; Tiberi, M.; Turchetti, F.

524.#.#.a: Pasquare, G., et al. (1987). Morphological and structural analysis of the central sector of the Transmexican Volcanic Belt. Geofísica Internacional; Vol. 26 Núm. 2: Abril 1, 1987; 177-193. Recuperado de https://repositorio.unam.mx/contenidos/4132624

245.1.0.a: Morphological and structural analysis of the central sector of the Transmexican 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; geología; evolución post laramídica; Morphology; geology; post laramidic evolution; cinturón volcánico mexicano

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/1084

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1084

041.#.7.h: spa

520.3.#.a: In this paper the post-orogenic evolution of a central sector of the Mexican Volcanic Belt (MVB) in the states of Guanajuato and Michoacan is analyzed. The main structural units are recognized on the basis of a morphological analysis and geological data. Four categories of morphological units were established. These are: 1. Reliefs belonging to geological formations older than MVB and characterized by Laramide orogenic deformation. 2. Pre-MVB planar structural surfaces. 3. Depositional surfaces belonging to sedimentary orvolcanoclastic infilling of post-orogenic tectonic depressions. 4. Surfaces of MVB volcanoes. In this analysis the main morphogenetic stages were recognized ;these were related to tensional tectonic phases and to the main volcanic events. An early tensional tectonic phase is associated with the volcanic activity which formed the pre-Miocene deposits of the Sierra Madre Occidental. A NNW-SSE trending system is dominant during the late Miocene and is related to the "Basin and Range" province of western U. S. A. NW-SE faulting during Pliocene along Californian trends is responsible for the initial volcanic activity of the MVB. Late Pliocene trends are WSW-ENE. The last tensional phase causes N-S and NNE-SSW grabens, as a possible reactivation of "Basin and Range" structures.doi: https://doi.org/10.22201/igeof.00167169p.1987.26.2.1108

773.1.#.t: Geofísica Internacional; Vol. 26 Núm. 2: Abril 1, 1987; 177-193

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: 177-193

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

doi: https://doi.org/10.22201/igeof.00167169p.1987.26.2.1108

handle: 00ad3c027288405b

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

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file_modification_date: 2022-07-15 01:57:53.0

file_creator: G. Pasquare

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245.1.0.b: Morphological and structural analysis of the central sector of the Transmexican Volcanic Belt

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

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Artículo

Morphological and structural analysis of the central sector of the Transmexican Volcanic Belt

Pasquare, G.; Ferrari, L.; Perazzoli, V.; Tiberi, M.; Turchetti, F.

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 analysis of the central sector of the Transmexican Volcanic Belt. Geofísica Internacional; Vol. 26 Núm. 2: Abril 1, 1987; 177-193. Recuperado de https://repositorio.unam.mx/contenidos/4132624

Descripción del recurso

Autor(es)
Pasquare, G.; Ferrari, L.; Perazzoli, V.; Tiberi, M.; Turchetti, F.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Morphological and structural analysis of the central sector of the Transmexican Volcanic Belt
Fecha
1987-04-01
Resumen
In this paper the post-orogenic evolution of a central sector of the Mexican Volcanic Belt (MVB) in the states of Guanajuato and Michoacan is analyzed. The main structural units are recognized on the basis of a morphological analysis and geological data. Four categories of morphological units were established. These are: 1. Reliefs belonging to geological formations older than MVB and characterized by Laramide orogenic deformation. 2. Pre-MVB planar structural surfaces. 3. Depositional surfaces belonging to sedimentary orvolcanoclastic infilling of post-orogenic tectonic depressions. 4. Surfaces of MVB volcanoes. In this analysis the main morphogenetic stages were recognized ;these were related to tensional tectonic phases and to the main volcanic events. An early tensional tectonic phase is associated with the volcanic activity which formed the pre-Miocene deposits of the Sierra Madre Occidental. A NNW-SSE trending system is dominant during the late Miocene and is related to the "Basin and Range" province of western U. S. A. NW-SE faulting during Pliocene along Californian trends is responsible for the initial volcanic activity of the MVB. Late Pliocene trends are WSW-ENE. The last tensional phase causes N-S and NNE-SSW grabens, as a possible reactivation of "Basin and Range" structures.doi: https://doi.org/10.22201/igeof.00167169p.1987.26.2.1108
Tema
Morfología; geología; evolución post laramídica; Morphology; geology; post laramidic evolution; cinturón volcánico mexicano
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces