Tectonic uplift of the Costa Rica - Panamá arc in the Paleocene time as a consequence of the collision between the Cuban arc and the Bahamas Bank

Abstract

The article resumes the sedimentary record in southern Central America from tectonic uplift of the Costa Rica - Panamá arc in the Paleocene time as a consequence of the collision between the Cuban arc and the Bahamas Bank

Description

Keywords

Citation

Endorsement

Review

Supplemented By

Referenced By