The relation between monogenetic and polygenetic dacitic volcanism. Case study from Tapias dome (<95 ka) and Cerro Machín volcano (<50 ka), Colombia │ 2023 https://doi.org/10.18273/revbol.v45n1-2023001 Leer más artículos Entrada anteriorRatification of Neogene subseries as formal units in international chronostratigraphy │ 2022 Siguiente entradaLate Cretaceous calcareous nannofossil assemblages from Colombia: Biostratigraphic contributions to northwestern South American Basins │ 2023 También podría gustarte Morphological analysis of Serpocaulon (Polypodiaceae) spores from the Colombian Central Cordillera │ 2013 20 February, 2020 Tectonostratigraphy of the Cenozoic Tumaco forearc basin (Colombian Pacific) and its relationship with the northern Andes orogenic build up │ 2012 20 February, 2020 Transition From Collisional to Subduction-Related Regimes: An Example From Neogene Panama-Nazca-South America Interactions │ 2018 20 February, 2020
Morphological analysis of Serpocaulon (Polypodiaceae) spores from the Colombian Central Cordillera │ 2013 20 February, 2020
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Transition From Collisional to Subduction-Related Regimes: An Example From Neogene Panama-Nazca-South America Interactions │ 2018 20 February, 2020