El Escondido tuff cone (38 ka): a hidden history of monogenetic eruptions in the northernmost volcanic chain in the Colombian Andes │ 2019 https://doi.org/10.1007/s00445-019-1337-2 Leer más artículos Entrada anteriorCaracterización de las asociaciones de cocolitóforos en las cuencas offshore del Pacífico colombiano │ 2019 Siguiente entradaEvidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 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 Astrobiochronological calibration of an early Oligocene succession from the Colombian Caribe: Tectonostratigraphic implications │ 2023 8 May, 2023 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
Evidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 21 February, 2020
Astrobiochronological calibration of an early Oligocene succession from the Colombian Caribe: Tectonostratigraphic implications │ 2023 8 May, 2023
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