Transition From Collisional to Subduction-Related Regimes: An Example From Neogene Panama-Nazca-South America Interactions │ 2018 https://doi.org/10.1002/2017TC004785 Leer más artículos Entrada anteriorCampo Volcánico Monogenético Villamaría-Termales, Cordillera Central, Andes colombianos (Parte II): Características composicionales │ 2018 Siguiente entradaFirst record of middle Miocene marine diatoms from the Colombian Pacific (NW South America) and their paleoceanographic significance │ 2018 También podría gustarte Cenozoic Geologic Evolution of the Southern Tumaco Forearc Basin (SW Colombian Pacific) │ 2020 24 January, 2022 Ichnological analysis of the Upper Miocene in the ANH-Tumaco-1-ST-P well: assessing paleoenvironmental conditions at the Tumaco Basin, in the Colombian Pacific │ 2016 20 February, 2020 Granulitic rocks at the Western Cordillera of Colombia: Evidence of metamorphism in the Colombian Caribbean Oceanic Plateau │ 2020 24 January, 2022
Cenozoic Geologic Evolution of the Southern Tumaco Forearc Basin (SW Colombian Pacific) │ 2020 24 January, 2022
Ichnological analysis of the Upper Miocene in the ANH-Tumaco-1-ST-P well: assessing paleoenvironmental conditions at the Tumaco Basin, in the Colombian Pacific │ 2016 20 February, 2020
Granulitic rocks at the Western Cordillera of Colombia: Evidence of metamorphism in the Colombian Caribbean Oceanic Plateau │ 2020 24 January, 2022