Campo Volcánico Monogenético Villamaría-Termales, Cordillera Central, Andes colombianos (Parte II): Características composicionales │ 2018 http://dx.doi.org/10.18273/revbol.v40n3-2018006 Leer más artículos Entrada anteriorOverview and plumbing system implications of monogenetic volcanism in the northernmost Andes’ volcanic province │ 2018 Siguiente entradaTransition From Collisional to Subduction-Related Regimes: An Example From Neogene Panama-Nazca-South America Interactions │ 2018 También podría gustarte Cretaceous Record from a Mariana– to an Andean–Type Margin in the Central Cordillera of the Colombian Andes │ 2020 24 January, 2022 Middle Miocene dinoflagellate cyst assemblages and changes in marine productivity in western Colombia │ 2021 27 January, 2022 Evidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 21 February, 2020
Cretaceous Record from a Mariana– to an Andean–Type Margin in the Central Cordillera of the Colombian Andes │ 2020 24 January, 2022
Middle Miocene dinoflagellate cyst assemblages and changes in marine productivity in western Colombia │ 2021 27 January, 2022
Evidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 21 February, 2020