dor_id: 4133451

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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

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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/764/736

100.1.#.a: García-palomo, A.; Macías, J. L.; Tolson, G.; Valdez, G.; Mora, J. C.

524.#.#.a: García-palomo, A., et al. (2002). Volcanic stratigraphy and geological evolution of the Apan region, east-central sector of the Trans-Mexican Volcanic Belt. Geofísica Internacional; Vol. 41 Núm. 2: Abril 1, 2002; 133-150. Recuperado de https://repositorio.unam.mx/contenidos/4133451

245.1.0.a: Volcanic stratigraphy and geological evolution of the Apan region, east-central sector of the Trans-Mexican Volcanic Belt

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2002

264.#.1.c: 2002-04-01

653.#.#.a: Geología; estratigrafía; geología estructural; Apan; México Central; Geology; stratigraphy; structural geology; Apan; Central 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/764

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041.#.7.h: spa

520.3.#.a: The Apan region, which straddles the central and eastern sectors of the Trans-Mexican Volcanic Belt (TMVB), was geologically shaped by interrelated, intermittent tectonism and volcanism. The oldest volcanic rocks in the area were erupted about 13.5 Ma ago, followed by a nearly 10-million year volcanic hiatus. Volcanism in the area then resumed ~3.0-1.5 Ma; the most recent volcanic activity occurred in the late Pleistocene (~42-31 ka). The volcanic rocks in the Apan region range in composition from basalt to rhyolite (50-75 wt.% SiO2) and exhibit calc-alkaline affinity; their geochemical characteristics suggest that they are subduction-zone eruptive products. Detailed geologic and stratigraphic studies using a new digital 1:100 000 scale base map for compilation of new and previous data, coupled with new K-Ar age determinations, demonstrate that the loci of volcanic centers in the region were controlled largely by a system of NE-SW-trending normal faults and associated horst-and- graben structures, resulting from a stress field with a least principal stress (ó3) oriented to the NW. Moreover, the results of this study, combined with a reexamination of geologic and age data from other investigations of the TMVB, make possible a refined correlation of the volcanic stratigraphy of the Apan region with the stratigraphic sequences of volcanic rocks in other areas of the TMVB. An important conclusion of our study is that volcanic activity in the TMVB was initiated during the Middle Miocene.doi: https://doi.org/10.22201/igeof.00167169p.2002.41.2.282

773.1.#.t: Geofísica Internacional; Vol. 41 Núm. 2: Abril 1, 2002; 133-150

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: 133-150

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

doi: https://doi.org/10.22201/igeof.00167169p.2002.41.2.282

handle: 009e4b64aa92538b

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

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file_creator: A. García-Palomo

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245.1.0.b: Volcanic stratigraphy and geological evolution of the Apan region, east-central sector of the Trans-Mexican Volcanic Belt

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Artículo

Volcanic stratigraphy and geological evolution of the Apan region, east-central sector of the Trans-Mexican Volcanic Belt

García-palomo, A.; Macías, J. L.; Tolson, G.; Valdez, G.; Mora, J. C.

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

García-palomo, A., et al. (2002). Volcanic stratigraphy and geological evolution of the Apan region, east-central sector of the Trans-Mexican Volcanic Belt. Geofísica Internacional; Vol. 41 Núm. 2: Abril 1, 2002; 133-150. Recuperado de https://repositorio.unam.mx/contenidos/4133451

Descripción del recurso

Autor(es)
García-palomo, A.; Macías, J. L.; Tolson, G.; Valdez, G.; Mora, J. C.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Volcanic stratigraphy and geological evolution of the Apan region, east-central sector of the Trans-Mexican Volcanic Belt
Fecha
2002-04-01
Resumen
The Apan region, which straddles the central and eastern sectors of the Trans-Mexican Volcanic Belt (TMVB), was geologically shaped by interrelated, intermittent tectonism and volcanism. The oldest volcanic rocks in the area were erupted about 13.5 Ma ago, followed by a nearly 10-million year volcanic hiatus. Volcanism in the area then resumed ~3.0-1.5 Ma; the most recent volcanic activity occurred in the late Pleistocene (~42-31 ka). The volcanic rocks in the Apan region range in composition from basalt to rhyolite (50-75 wt.% SiO2) and exhibit calc-alkaline affinity; their geochemical characteristics suggest that they are subduction-zone eruptive products. Detailed geologic and stratigraphic studies using a new digital 1:100 000 scale base map for compilation of new and previous data, coupled with new K-Ar age determinations, demonstrate that the loci of volcanic centers in the region were controlled largely by a system of NE-SW-trending normal faults and associated horst-and- graben structures, resulting from a stress field with a least principal stress (ó3) oriented to the NW. Moreover, the results of this study, combined with a reexamination of geologic and age data from other investigations of the TMVB, make possible a refined correlation of the volcanic stratigraphy of the Apan region with the stratigraphic sequences of volcanic rocks in other areas of the TMVB. An important conclusion of our study is that volcanic activity in the TMVB was initiated during the Middle Miocene.doi: https://doi.org/10.22201/igeof.00167169p.2002.41.2.282
Tema
Geología; estratigrafía; geología estructural; Apan; México Central; Geology; stratigraphy; structural geology; Apan; Central Mexico
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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