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 Regional provenance from southwestern Colombia fore-arc and intra-arc basins: implications for Middle to Late Miocene orogeny in the Northern Andes │ 2015 20 February, 2020 Transition From Collisional to Subduction-Related Regimes: An Example From Neogene Panama-Nazca-South America Interactions │ 2018 20 February, 2020 Evolution of a fluvial-dominated delta during the Oligocene of the Colombian Caribbean: Sedimentological and ichnological signatures in well-cores │ 2021 27 January, 2022
Regional provenance from southwestern Colombia fore-arc and intra-arc basins: implications for Middle to Late Miocene orogeny in the Northern Andes │ 2015 20 February, 2020
Transition From Collisional to Subduction-Related Regimes: An Example From Neogene Panama-Nazca-South America Interactions │ 2018 20 February, 2020
Evolution of a fluvial-dominated delta during the Oligocene of the Colombian Caribbean: Sedimentological and ichnological signatures in well-cores │ 2021 27 January, 2022