The Taxco–San Miguel de Allende fault system and the Trans-Mexican Volcanic Belt: Two tectonic boundaries in central México active during the Cenozoic-Reference-Cited by-同舟云学术

The Taxco–San Miguel de Allende fault system and the Trans-Mexican Volcanic Belt: Two tectonic boundaries in central México active during the Cenozoic

Published:2007 Issue: Volume: Page:
ISSN:
Container-title:Geology of Me´xico: Celebrating the Centenary of the Geological Society of Me´xico
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Author:

Alaniz-Álvarez Susana A.,Nieto-Samaniego Ángel Francisco

Publisher

Geological Society of America

Reference67 articles.

1. Effect of strain rate in the distribution of monogenetic and polygenetic volcanism in the Transmexican volcanic belt

2. El sistema de fallas Taxco-San Miguel de Allende: Implicaciones en la deformación post-eocénica del centro de México

3. Rhyolitic volcanism in extension zone associated with strike-slip tectonics in the Taxco region, southern Mexico

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