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 Late Neogene chronostratigraphy and integrated paleoecological trends in the southwestern Caribbean Sea │ 2022 24 February, 2022 The Northernmost Volcanoes in South America (Colombia, 5–6°N): The Potentially Active Samaná Monogenetic Volcanic Field │ 2022 7 July, 2022 I.A. Petrinovic, and L D’Elia: Rocas Volcaniclásticas, Depósitos, Procesos y Modelos de Facies: desde el origen hasta las zonas finales de depositación │ 2020 21 February, 2020
Late Neogene chronostratigraphy and integrated paleoecological trends in the southwestern Caribbean Sea │ 2022 24 February, 2022
The Northernmost Volcanoes in South America (Colombia, 5–6°N): The Potentially Active Samaná Monogenetic Volcanic Field │ 2022 7 July, 2022
I.A. Petrinovic, and L D’Elia: Rocas Volcaniclásticas, Depósitos, Procesos y Modelos de Facies: desde el origen hasta las zonas finales de depositación │ 2020 21 February, 2020