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 Increased megathrust shear force drives topographic uplift in the Colombian coastal forearc │ 2021 26 January, 2022 Lower to Middle Miocene multiproxy biostratigraphy of the P-18 core-stratigraphic well in Sinú-San Jacinto Basin, Caribbean region of Colombia. │ 2023 8 May, 2023 Sedimentary record of the Cretaceous–Paleocene arc–continent collision in the northwestern Colombian Andes: Insights from stratigraphic and provenance constraints │ 2020 24 January, 2022
Increased megathrust shear force drives topographic uplift in the Colombian coastal forearc │ 2021 26 January, 2022
Lower to Middle Miocene multiproxy biostratigraphy of the P-18 core-stratigraphic well in Sinú-San Jacinto Basin, Caribbean region of Colombia. │ 2023 8 May, 2023
Sedimentary record of the Cretaceous–Paleocene arc–continent collision in the northwestern Colombian Andes: Insights from stratigraphic and provenance constraints │ 2020 24 January, 2022