Almandine garnet-bearing rhyolites associated to bimodal volcanism in the Mesa Central of Mexico: Geochemical, petrological and geochronological evolution

Author:

Sieck Pascal,López-Doncel Rubén,Dávila-Harris PabloORCID,Aguillón-Robles AlfredoORCID,Wemmer Klaus,Maury René C.ORCID

Funder

National Council of Science and Technology, MexicoNational Council of Science and Technology, Mexico (CONACYT)

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference112 articles.

1. Syn-extensional intra-plate trachydacite-rhyolitic dome volcanism of the Mesa Central, southern Sierra Madre Occidental Volcanic Province, Mexico;Aguillón-Robles;J. Volcanol. Geotherm. Res.,2009

2. 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;Geofis. Int.,2012

3. Eocene to Quaternary mafic-intermediate volcanism in San Luis Potosí, central Mexico: the transition from Farallon plate subduction to intra-plate continental magmatism;Aguillón-Robles;J. Volcanol. Geotherm. Res.,2014

4. The volcanic section at Nazas, Durango, Mexico, and the possibility of widespread Eocene volcanism within the Sierra Madre Occidental;Aguirre-Díaz;J. Geophys. Res.: Solid Earth,1991

5. Nature and timing of faulting and synextensional magmatism in the southern Basin and Range, central-eastern Durango, Mexico;Aguirre-Díaz;Geol. Soc. Am. Bull.,1993

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