Geología y geoquímica de elementos mayores de la Caldera de Huichapan, Hidalgo, México

La Caldera de Huichapan cuya estructura aproximadamente subcircular es de -8.5 km de diámetro, se localiza en la parte central del Cinturón Volcánico Mexicano. Esta caldera se formó por la erupción de varios flujos de ignimbritas (San Francisco y Don Guinyó), hace aproximadamente 4.2 Ma. Litológicam...

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Bibliographic Details
Published in:	Geofísica Internacional
Main Authors:	M. Mitlán, C. Yañez, I. Navarro L., S. P. Verma
Format:	Article
Language:	English
Published:	Universidad Nacional Autónoma de México, Instituto de Geofísica 1993-04-01
Subjects:	calderas cinturón volcánico mexicano ignimbrita huichapan méxico
Online Access:	http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1386

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