Geochemistry of the Santa Fé Batholith and Buriticá Tonalite in NW Colombia e Evidence of subduction initiation beneath the Colombian Caribbean Plateau │ 2015 http://dx.doi.org/10.1016/j.jsames.2015.04.002 Leer más artículos Entrada anteriorMiddle Miocene closure of the Central American Seaway │ 2015 Siguiente entradaPyroclastic deposits of San Diego maar, central Colombia: an example of a silicic magma-related monogenetic eruption in a hard substrate │ 2016 También podría gustarte Campo Volcánico Monogenético Villamaría-Termales, Cordillera Central, Andes colombianos (Parte II): Características composicionales │ 2018 20 February, 2020 Finding eruptive mechanisms through pyroclasts from the current eruption (1984–present) at Nevado del Ruiz Volcanic Complex, Colombia │ 2018 20 February, 2020 The relation between monogenetic and polygenetic dacitic volcanism. Case study from Tapias dome (<95 ka) and Cerro Machín volcano (<50 ka), Colombia │ 2023 14 March, 2023
Campo Volcánico Monogenético Villamaría-Termales, Cordillera Central, Andes colombianos (Parte II): Características composicionales │ 2018 20 February, 2020
Finding eruptive mechanisms through pyroclasts from the current eruption (1984–present) at Nevado del Ruiz Volcanic Complex, Colombia │ 2018 20 February, 2020
The relation between monogenetic and polygenetic dacitic volcanism. Case study from Tapias dome (<95 ka) and Cerro Machín volcano (<50 ka), Colombia │ 2023 14 March, 2023