dor_id: 4133511

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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

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270.#.#.d: MX

270.1.#.d: México

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590.#.#.a: Coordinación de Difusión Cultural

883.#.#.1: https://www.publicaciones.unam.mx/

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/445/459

100.1.#.a: Aguillón Robles, Alfredo; Tristán González, Margarito; López Doncel, Rubén Alfonso; García Arreola, María Elena; Almaguer Rodríguez., Joselin De Lourdes; Maury, René C.

524.#.#.a: Aguillón Robles, Alfredo, et al. (2012). Trace elements geochemistry and origin of volcanic units from the San Luis Potosí and Río Santa María volcanic fields, Mexico: The bearing of ICP-QMS data. Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 293-­308. Recuperado de https://repositorio.unam.mx/contenidos/4133511

245.1.0.a: Trace elements geochemistry and origin of volcanic units from the San Luis Potosí and Río Santa María volcanic fields, Mexico: The bearing of ICP-QMS data

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2012

264.#.1.c: 2012-07-01

653.#.#.a: campos volcánicos; elementos traza; ICP-QMS; San Luis Potosí; unidades volcánicas; volcanic fields; volcanic units; trace elements; ICP-QMS; San Luis Potosi

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/445

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/445

041.#.7.h: spa

520.3.#.a: Two main volcanic fields separated by a volcano-tectonic structure were emplaced in the southern part of San Luis Potosí state during the Cenozoic peak of continental extension in the SE portion of the Sierra Madre Occidental. The Eocene to Quaternary volcanic rocks associated to these structures range in composition either from subalkaline basalts to basanites or from basaltic andesite to rhyolites, and were emplaced during five magmatic events. New trace element analyses obtained by the ICP-QMS method show that the three oldest ones, ranging in age from middle Eocene to late Oligocene, emplaced potassic calc-alkaline intermediate to evolved lavas. These originated from subduction-related mafic magmas through open-system fractional cristallization coupled with assimilation and possibly melting of the continental crust. The two youngest volcanic phases (Miocene and Quaternary) emplaced intraplate subalkaline to alkaline basalt and basanites derived from variable melting degrees of enriched mantle.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1198

773.1.#.t: Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 293-­308

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: 293-­308

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

doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1198

handle: 304e34eb2f27e650

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-06 16:13:29.0

file_modification_date: 2022-07-06 16:13:29.0

file_creator: Alfredo Aguillón Robles

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245.1.0.b: Trace elements geochemistry and origin of volcanic units from the San Luis Potosí and Río Santa María volcanic fields, Mexico: The bearing of ICP-QMS data

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

Trace elements geochemistry and origin of volcanic units from the San Luis Potosí and Río Santa María volcanic fields, Mexico: The bearing of ICP-QMS data

Aguillón Robles, Alfredo; Tristán González, Margarito; López Doncel, Rubén Alfonso; García Arreola, María Elena; Almaguer Rodríguez., Joselin De Lourdes; Maury, René 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

Aguillón Robles, Alfredo, et al. (2012). Trace elements geochemistry and origin of volcanic units from the San Luis Potosí and Río Santa María volcanic fields, Mexico: The bearing of ICP-QMS data. Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 293-­308. Recuperado de https://repositorio.unam.mx/contenidos/4133511

Descripción del recurso

Autor(es)
Aguillón Robles, Alfredo; Tristán González, Margarito; López Doncel, Rubén Alfonso; García Arreola, María Elena; Almaguer Rodríguez., Joselin De Lourdes; Maury, René C.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Trace elements geochemistry and origin of volcanic units from the San Luis Potosí and Río Santa María volcanic fields, Mexico: The bearing of ICP-QMS data
Fecha
2012-07-01
Resumen
Two main volcanic fields separated by a volcano-tectonic structure were emplaced in the southern part of San Luis Potosí state during the Cenozoic peak of continental extension in the SE portion of the Sierra Madre Occidental. The Eocene to Quaternary volcanic rocks associated to these structures range in composition either from subalkaline basalts to basanites or from basaltic andesite to rhyolites, and were emplaced during five magmatic events. New trace element analyses obtained by the ICP-QMS method show that the three oldest ones, ranging in age from middle Eocene to late Oligocene, emplaced potassic calc-alkaline intermediate to evolved lavas. These originated from subduction-related mafic magmas through open-system fractional cristallization coupled with assimilation and possibly melting of the continental crust. The two youngest volcanic phases (Miocene and Quaternary) emplaced intraplate subalkaline to alkaline basalt and basanites derived from variable melting degrees of enriched mantle.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1198
Tema
campos volcánicos; elementos traza; ICP-QMS; San Luis Potosí; unidades volcánicas; volcanic fields; volcanic units; trace elements; ICP-QMS; San Luis Potosi
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces