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 POLLEN MORPHOLOGY OF Ombrophytum villamariensis (BALANOPHORACEAE) │ 2020 24 January, 2022 Uncommon mafic rocks (MgO >10 wt.%) in the northernmost Andean volcanic chain (4◦ 25′′ N): Implications for magma source and evolution │ 2021 24 January, 2022 Appearance of an enigmatic Pb source in South America around 2000 BP: Anthropogenic vs natural origin │ 2020 24 January, 2022
Uncommon mafic rocks (MgO >10 wt.%) in the northernmost Andean volcanic chain (4◦ 25′′ N): Implications for magma source and evolution │ 2021 24 January, 2022
Appearance of an enigmatic Pb source in South America around 2000 BP: Anthropogenic vs natural origin │ 2020 24 January, 2022