Ratification of Neogene subseries as formal units in international chronostratigraphy │ 2022 https://doi.org/10.18814/epiiugs/2022/022008 Leer más artículos Entrada anteriorPaleoenvironmental conditions over the Caribbean Large Igneous Province during the Late Cretaceous in NWof South American Margin: A sedimentological and ichnological approach │ 2022 Siguiente entradaThe relation between monogenetic and polygenetic dacitic volcanism. Case study from Tapias dome (<95 ka) and Cerro Machín volcano (<50 ka), Colombia │ 2023 También podría gustarte Evidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 21 February, 2020 Middle Miocene dinoflagellate cyst assemblages and changes in marine productivity in western Colombia │ 2021 27 January, 2022 Granulitic rocks at the Western Cordillera of Colombia: Evidence of metamorphism in the Colombian Caribbean Oceanic Plateau │ 2020 24 January, 2022
Evidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 21 February, 2020
Middle Miocene dinoflagellate cyst assemblages and changes in marine productivity in western Colombia │ 2021 27 January, 2022
Granulitic rocks at the Western Cordillera of Colombia: Evidence of metamorphism in the Colombian Caribbean Oceanic Plateau │ 2020 24 January, 2022