Petrology of two contrasting Mexican volcanoes, the Chiapanecan (El Chichón) and Central American (Tacaná) volcanic belts: the result of rift- versus subduction-related volcanism
Author:
Affiliation:
1. Instituto de Geología, UNAM, Cd. Universitaria Coyoacan, México, DF, Mexico
2. Department of Geology and Environmental Geosciences, Northern Illinois University, DeKalb, IL, USA
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206814.2013.879375
Reference68 articles.
1. The Neogene Veracruz fault: evidences for left-lateral slip along the southern Mexico block
2. Repeated recharge, assimilation, and hybridization in magmas erupted from El Chichón as recorded by plagioclase and amphibole phenocrysts
3. Reconstruction of the Sibinal Pumice, an andesitic Plinian eruption at Tacaná Volcanic Complex, Mexico–Guatemala
4. The Caribbean-North America-Cocos Triple Junction and the dynamics of the Polochic-Motagua fault systems: Pull-up and zipper models
5. Evolution of pull-apart basins and their scale independence
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