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 Emplacement conditions of the 1256 AD Al-Madinah lava flow field in Harrat Rahat, Kingdom of Saudi Arabia — Insights from surface morphology and lava flow simulations │ 2016 20 February, 2020 Depósitos volcaniclásticos: Términos y conceptos para una clasificación en español │ 2013 20 February, 2020 Appearance of an enigmatic Pb source in South America around 2000 BP: Anthropogenic vs natural origin │ 2020 24 January, 2022
Emplacement conditions of the 1256 AD Al-Madinah lava flow field in Harrat Rahat, Kingdom of Saudi Arabia — Insights from surface morphology and lava flow simulations │ 2016 20 February, 2020
Depósitos volcaniclásticos: Términos y conceptos para una clasificación en español │ 2013 20 February, 2020
Appearance of an enigmatic Pb source in South America around 2000 BP: Anthropogenic vs natural origin │ 2020 24 January, 2022