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 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 Cenozoic Geologic Evolution of the Southern Tumaco Forearc Basin (SW Colombian Pacific) │ 2020 24 January, 2022 El Escondido tuff cone (38 ka): a hidden history of monogenetic eruptions in the northernmost volcanic chain in the Colombian Andes │ 2019 21 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
Cenozoic Geologic Evolution of the Southern Tumaco Forearc Basin (SW Colombian Pacific) │ 2020 24 January, 2022
El Escondido tuff cone (38 ka): a hidden history of monogenetic eruptions in the northernmost volcanic chain in the Colombian Andes │ 2019 21 February, 2020