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 Middle Miocene closure of the Central American Seaway │ 2015 20 February, 2020 Aquatic ecosystems in a newly formed ecospace: Early Pliocene lakes in the Central Andean Altiplano │ 2018 21 February, 2020 Increased megathrust shear force drives topographic uplift in the Colombian coastal forearc │ 2021 26 January, 2022
Aquatic ecosystems in a newly formed ecospace: Early Pliocene lakes in the Central Andean Altiplano │ 2018 21 February, 2020
Increased megathrust shear force drives topographic uplift in the Colombian coastal forearc │ 2021 26 January, 2022
