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The document discusses the tectonic evolution of the Santander Massif in Colombia, highlighting the impact of the convergence between the Santander Massif and the Pamplona Wedge, which has led to the formation of transpressional structures and oblique faults. It presents a compilation of thermochronological data that supports the interpretation of episodic exhumation and deformation from the Eocene to recent times, driven by tectonic forces and the collision of the Panamá Indenter. The study emphasizes the

Author

alejandrapt430

Language

EN