Evidence for middle Cretaceous accretion at Santa Elena Peninsula (Santa Rosa Accretionary Complex), Costa Rica

Evidence for middle Cretaceous accretion at Santa Elena Peninsula (Santa Rosa Accretionary Complex), Costa Rica

An oceanic assemblage of alkaline basalts, radiolarites and polymictic breccias forms the tectonic substratum of the Santa Elena Nappe, which is constituted by extensive outcrops of ultramafic and mafic rocks of the Santa Elena Peninsula (NW Costa Rica). The undulating basal contact of this nappe de...

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Bibliographic Details
Main Authors: P. O. BAUMGARTNER, P. DENYER
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2006-01-01
Series:Geologica Acta
Subjects:
Santa Elena Peninsula
Accretion
Costa Rica
Radiolarites
Megabreccias
Middle Cretaceous
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/2016

Internet

https://revistes.ub.edu/index.php/GEOACTA/article/view/2016

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