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 Late-Holocene pollen-based paleoenvironmental reconstruction of the El Triunfo wetland, Los Nevados National Park (Central Cordillera of Colombia) │ 2017 20 February, 2020 Andesitic (SiO2: ~60 wt%) monogenetic volcanism in the northern Colombian Andes: Crystallisation history of three Quaternary volcanoes │ 2021 24 January, 2022 Emplacement conditions of the 1256 AD Al-Madinah lava flow field in Harrat Rahat, Kingdom of Saudi Arabia — Insights from surface morphology and lava flow simulations │ 2016 20 February, 2020
Late-Holocene pollen-based paleoenvironmental reconstruction of the El Triunfo wetland, Los Nevados National Park (Central Cordillera of Colombia) │ 2017 20 February, 2020
Andesitic (SiO2: ~60 wt%) monogenetic volcanism in the northern Colombian Andes: Crystallisation history of three Quaternary volcanoes │ 2021 24 January, 2022
Emplacement conditions of the 1256 AD Al-Madinah lava flow field in Harrat Rahat, Kingdom of Saudi Arabia — Insights from surface morphology and lava flow simulations │ 2016 20 February, 2020