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This study utilizes U-Pb ages and Hf isotopes from zircons to analyze geological units in the Central Cordillera of Colombia, revealing distinct sources and ages for the Cajamarca Complex and Tierradentro unit. The results indicate that the Tierradentro gneisses and amphibolites are not Grenvillian rocks as previously thought, and suggest a more complex tectonic history involving Jurassic metasedimentary rocks. These findings challenge existing models of terrane boundaries and highlight the need for a reeva

Author
Jesus
Language
EN