Evidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 https://doi.org/10.1007/s00445-019-1334-5 Leer más artículos Entrada anteriorEl Escondido tuff cone (38 ka): a hidden history of monogenetic eruptions in the northernmost volcanic chain in the Colombian Andes │ 2019 Siguiente entradaCaracterización petrofísica como potencial reservorio de las sucesiones siliciclásticas paleógenas del pozo ANHTIERRALTA- 2-X-P en la Cuenca Sinú-San Jacinto, caribe colombiano │ 2020 También podría gustarte Uncommon mafic rocks (MgO >10 wt.%) in the northernmost Andean volcanic chain (4◦ 25′′ N): Implications for magma source and evolution │ 2021 24 January, 2022 Miocene biostratigraphy and paleoecology from dinoflagellates, benthic foraminifera and calcareous nannofossils on the Colombian Pacific coast │ 2018 20 February, 2020 The relation between monogenetic and polygenetic dacitic volcanism. Case study from Tapias dome (<95 ka) and Cerro Machín volcano (<50 ka), Colombia │ 2023 14 March, 2023
Uncommon mafic rocks (MgO >10 wt.%) in the northernmost Andean volcanic chain (4◦ 25′′ N): Implications for magma source and evolution │ 2021 24 January, 2022
Miocene biostratigraphy and paleoecology from dinoflagellates, benthic foraminifera and calcareous nannofossils on the Colombian Pacific coast │ 2018 20 February, 2020
The relation between monogenetic and polygenetic dacitic volcanism. Case study from Tapias dome (<95 ka) and Cerro Machín volcano (<50 ka), Colombia │ 2023 14 March, 2023