dor_id: 4132554

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/1535/1656

100.1.#.a: Negendank, J.F.W.

524.#.#.a: Negendank, J.F.W. (1973). Geochemical aspects of volcanic rocks of the Valley of México. Geofísica Internacional; Vol. 13 Núm. 3: Julio 1, 1973; 267-278. Recuperado de https://repositorio.unam.mx/contenidos/4132554

245.1.0.a: Geochemical aspects of volcanic rocks of the Valley of México

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1973

264.#.1.c: 1973-07-01

653.#.#.a: Historia geológica; Actividad volcánica; Geoquímica; Rocas volcánicas; Valle de México; Geological history; Volcanic activity; Geochemistry; Volcanic rocks; Valley of 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/1535

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1535

041.#.7.h: spa

520.3.#.a: Three periods of volcanic activity connected with tectonic events form the geological history of the Valley of Mexico. An igneous rock suite from rhyodacites to andesites can be observed in each period, lacking real rhyolites and basalts. During the Tertiary -in the Oligo-Miocene and Upper Miocene-Pliocene periods- volcanism is more dacitic, and in the Quaternary epoch more andesitic. This result was verified by calculating the average of all available and stratigraphical datable chemical analyses. The average chemical composition of Oligo-Miocene, Upper Miocene-Pliocene and Quaternary products was computed in addition to the corresponding igneous rocks in the classification by the Rittmann norms in the Streckeisen double triangle with the following results:Quaternary: Quartz-la ti te-andesiteUpper Miocene-Pliocene: Leuco-quartz-latite-andesiteOligo-Miocene: Leuco-quartz-latite-andesiteThe similar average composition of Tertiary volcanic rocks seems to support the theory of a uniform primary andesite magma apart from the two possible theories of petrogenesis. The computed average trace element abundances show high Cr and Ni- values which speaks for an involvement of mantle material, if one considers the Tertiary products as partial melting products of the lower crust. A more elegant hypothesis seems to be the model of Gunn and Mooser (1971), who consider these volcanic rocks as partial melting products of oceanic tholeiites or their high pressure derivatives.

773.1.#.t: Geofísica Internacional; Vol. 13 Núm. 3: Julio 1, 1973; 267-278

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: 267-278

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

doi: https://doi.org/10.22201/igeof.00167169p.1973.13.3.958

handle: 6c6b3a46236c2004

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

856.#.0.q: application/pdf

file_creation_date: 2008-07-01 16:43:29.0

file_modification_date: 2023-02-07 06:51:32.0

file_creator: J.F W Negendank

file_name: fd132c2809c3db4d68af41bc7acb8b6110802d7a2d0d8b5c6d6fb8a58a915e6d.pdf

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245.1.0.b: Geochemical aspects of volcanic rocks of the Valley of México

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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Artículo

Geochemical aspects of volcanic rocks of the Valley of México

Negendank, J.F.W.

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

Negendank, J.F.W. (1973). Geochemical aspects of volcanic rocks of the Valley of México. Geofísica Internacional; Vol. 13 Núm. 3: Julio 1, 1973; 267-278. Recuperado de https://repositorio.unam.mx/contenidos/4132554

Descripción del recurso

Autor(es)
Negendank, J.F.W.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Geochemical aspects of volcanic rocks of the Valley of México
Fecha
1973-07-01
Resumen
Three periods of volcanic activity connected with tectonic events form the geological history of the Valley of Mexico. An igneous rock suite from rhyodacites to andesites can be observed in each period, lacking real rhyolites and basalts. During the Tertiary -in the Oligo-Miocene and Upper Miocene-Pliocene periods- volcanism is more dacitic, and in the Quaternary epoch more andesitic. This result was verified by calculating the average of all available and stratigraphical datable chemical analyses. The average chemical composition of Oligo-Miocene, Upper Miocene-Pliocene and Quaternary products was computed in addition to the corresponding igneous rocks in the classification by the Rittmann norms in the Streckeisen double triangle with the following results:Quaternary: Quartz-la ti te-andesiteUpper Miocene-Pliocene: Leuco-quartz-latite-andesiteOligo-Miocene: Leuco-quartz-latite-andesiteThe similar average composition of Tertiary volcanic rocks seems to support the theory of a uniform primary andesite magma apart from the two possible theories of petrogenesis. The computed average trace element abundances show high Cr and Ni- values which speaks for an involvement of mantle material, if one considers the Tertiary products as partial melting products of the lower crust. A more elegant hypothesis seems to be the model of Gunn and Mooser (1971), who consider these volcanic rocks as partial melting products of oceanic tholeiites or their high pressure derivatives.
Tema
Historia geológica; Actividad volcánica; Geoquímica; Rocas volcánicas; Valle de México; Geological history; Volcanic activity; Geochemistry; Volcanic rocks; Valley of Mexico
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces