UPPER CENOZOIC MAGMATIC EVOLUTION OF THE ARGENTINE PUNA—A MODEL FOR CHANGING SUBDUCTION GEOMETRY-Reference-Cited by-同舟云学术

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UPPER CENOZOIC MAGMATIC EVOLUTION OF THE ARGENTINE PUNA—A MODEL FOR CHANGING SUBDUCTION GEOMETRY

Published:1993-08 Issue:8 Volume:35 Page:677-720
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Coira B.¹,Kay S. Mahlburg²,Viramonte J.³

Affiliation:

1. a Universidad Nacional de Jujuy , Casilla de Correo 258, S.S. de Jujuy, 4600, Argentina

2. b Department of Geological Sciences and Institute for the Study of the Continents (INSTOC) , Cornell University , Ithaca, NY 14853, USA

3. c Universidad Nacional de Salta , Buenos Aires 177, Salta, 4000, Argentina

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206819309465552

Reference124 articles.

1. Tectonic development, southeastern border of the Puna Plateau, northwestern Argentine Andes

2. Neotectonic deformation of the southern Puna Plateau, northwestern Argentina

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5. Generation of Neogene adakitic-like magmas in the Argentine Puna-Eastern Cordillera transition: the Huachichocana Subvolcanic Complex;International Journal of Earth Sciences;2023-03-28

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