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 The Morales Formation (New Unit): Record of Fluvial–Lacustrine Environments and the Beginning of the Miocene Explosive Volcanism in the Patía Sub–basin (SW Colombia) │ 2020 24 January, 2022 Mid to late holocene dry events in Colombia’s super humid Western Cordillera reveal changes in regional atmospheric circulation │ 2021 24 January, 2022 Paleoenvironmental conditions over the Caribbean Large Igneous Province during the Late Cretaceous in NWof South American Margin: A sedimentological and ichnological approach │ 2022 17 November, 2022
The Morales Formation (New Unit): Record of Fluvial–Lacustrine Environments and the Beginning of the Miocene Explosive Volcanism in the Patía Sub–basin (SW Colombia) │ 2020 24 January, 2022
Mid to late holocene dry events in Colombia’s super humid Western Cordillera reveal changes in regional atmospheric circulation │ 2021 24 January, 2022
Paleoenvironmental conditions over the Caribbean Large Igneous Province during the Late Cretaceous in NWof South American Margin: A sedimentological and ichnological approach │ 2022 17 November, 2022