dor_id: 4132397

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

270.1.#.d: México

590.#.#.b: Concentrador

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/990/932

100.1.#.a: Ferriz, H.; Mahood, G.A.

524.#.#.a: Ferriz, H., et al. (1986). Volcanismo riolitico en el Eje Neo volcanico Mexicano. Geofísica Internacional; Vol. 25 Núm. 1: Enero 1, 1986; 117-156. Recuperado de https://repositorio.unam.mx/contenidos/4132397

245.1.0.a: Volcanismo riolitico en el Eje Neo volcanico Mexicano

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1986

264.#.1.c: 1986-01-01

653.#.#.a: Volcanismo; Volcanismo riolitico; Volcanismo silícico; Volcanism; Rhyolitic volcanism; Silicic volcanism; Eje Neovolcánico 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/990

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/990

041.#.7.h: spa

520.3.#.a: The Mexican Neovolcanic Belt is a plio-quaternary volcanic belt, of east-west orientation, that bisects central Mexico. It is formed by large andesitic stratovolcanoes, silicic volcanic centers, and extensive basaltic and an: desitic cinder cone fields. Five silicic volcanic centers have been recognized to date in the Neovolcanic Belt: La Primavera, Jal., Los Azufres, Mich., Amealco, Qro., Huichapan, Hgo., and Los Humeros, Pue .. These centers are located along the northern portion of the Belt, "behind" the front of the active andesitic stratovolcanoes. Toe volumes of rhyolitic and rhyodacitic magmas erupted in each one of these centers range from 10 to 150 km 3. In most of these centers sorne of the individual eruptive units are strongly zoned in composition, and in sorne instances span the range rhyolite to andesite. An exception is La Primavera, where only high-silica rhyolitic magma was erupted. In addition to these five centers, there are numerous other occurrences of rhyolitic volcanism throughout the Neovolcanic Belt; sorne of them might be related to large but as yet unrecognized volcanic centers, but others seem to represent isolated events. Toe silicic volcanism of the Neovolcanic Belt has two important economic implications: volcanic risk and geothermal energy. Among the known silicic centers, La Primavera represents the major potential hazard on account of its youth and proximity to the city of Guadalajara. With respect to geothermal energy, Los Azufres is a geothermal field currently under production, and La Primavera and Los Humeros are prospects currently under exploration. In ali three cases the reservoirs are located in zones of secondary permeability within the local volcanic basement.doi: https://doi.org/10.22201/igeof.00167169p.1986.25.1.803

773.1.#.t: Geofísica Internacional; Vol. 25 Núm. 1: Enero 1, 1986; 117-156

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: 117-156

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

doi: https://doi.org/10.22201/igeof.00167169p.1986.25.1.803

handle: 0fc745afc0f99ee0

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

856.#.0.q: application/pdf

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file_modification_date: 2022-07-11 19:07:54.0

file_creator: H. Ferriz

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245.1.0.b: Volcanismo riolitico en el Eje Neo volcanico Mexicano

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

license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

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