The Record of the Transition From an Oceanic Arc to a Young Continent in the Talamanca Cordillera

Author:

Gazel Esteban1ORCID,Hayes Jorden L.2,Ulloa Andres3,Alfaro Aristides1,Coleman Drew S.4ORCID,Carr Michael J.5ORCID

Affiliation:

1. Department of Earth and Atmospheric SciencesCornell University Ithaca NY USA

2. Department of Earth SciencesDickinson College Carlisle PA USA

3. Centro de Investigación en Ciencias GeológicasUniversidad de Costa Rica San José Costa Rica

4. Department of Geological SciencesUniversity of North Carolina at Chapel Hill Chapel Hill NC USA

5. Department of Earth and Planetary SciencesRutgers University New Brunswick NJ USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference156 articles.

1. Abratis M.(1998).Geochemical variations in magmatic rocks from southern Costa Rica as a consequence of Cocos Ridge subduction and uplift of the Cordillera de Talamanca Universität Göttingen Göttingen.

2. Ridge collision, slab-window formation, and the flux of Pacific asthenosphere into the Caribbean realm

3. Geochronological synthesis of magmatism, metamorphism and metallogeny of Costa Rica, Central America;Alvarado G.;Revista Geológica de América Central,2012

4. Resumen cronoestratigráfico de las rocas ígneas de Costa Rica basado en dataciones radiométricas

5. Formation and Evolution of the Continental Crust

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