Transition From Collisional to Subduction-Related Regimes: An Example From Neogene Panama-Nazca-South America Interactions │ 2018 https://doi.org/10.1002/2017TC004785 Leer más artículos Entrada anteriorCampo Volcánico Monogenético Villamaría-Termales, Cordillera Central, Andes colombianos (Parte II): Características composicionales │ 2018 Siguiente entradaFirst record of middle Miocene marine diatoms from the Colombian Pacific (NW South America) and their paleoceanographic significance │ 2018 También podría gustarte Geochemistry of the Santa Fé Batholith and Buriticá Tonalite in NW Colombia e Evidence of subduction initiation beneath the Colombian Caribbean Plateau │ 2015 20 February, 2020 Detrital zircon typology and U/Pb geochronology for the Miocene Ladrilleros-Juanchaco sedimentary sequence, Equatorial Pacific (Colombia): New constraints on provenance and paleogeography in northwestern South America │ 2017 20 February, 2020 Contemporaneous Paleogene arc-magmatism within continental and accreted oceanic arc complexes in the northwestern Andes and Panama │ 2019 21 February, 2020
Geochemistry of the Santa Fé Batholith and Buriticá Tonalite in NW Colombia e Evidence of subduction initiation beneath the Colombian Caribbean Plateau │ 2015 20 February, 2020
Detrital zircon typology and U/Pb geochronology for the Miocene Ladrilleros-Juanchaco sedimentary sequence, Equatorial Pacific (Colombia): New constraints on provenance and paleogeography in northwestern South America │ 2017 20 February, 2020
Contemporaneous Paleogene arc-magmatism within continental and accreted oceanic arc complexes in the northwestern Andes and Panama │ 2019 21 February, 2020