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En 1918 el geólogo Emile Grosse recibió el encargo de realizar estudios geológicos en la cuenca de Amagá, Colombia. En 1923 Grosse terminó un trabajo cartográfico exhaustivo que se convirtió en la piedra angular para la geología del noroccidente de los Andes colombianos. Hoy, 100 años después, las unidades volcanoclásticas preservadas en la cuenca de Amagá son cruciales para entender los principales eventos tectónicos que ocurrieron en el margen noroccidental suramericano entre el Oligoceno y el Plioceno, incluyendo la fragmentación de la Placa de Nazca, la colisión del Bloque Panamá-Chocó y la subducción plana. El presente trabajo incluye nuevos datos de química mineral y petrocronología en circón del complejo volcánico de Combia e integra datos publicados para proporcionar una revisión de los patrones de deformación, sedimentación y magmatismo del Oligoceno al Plioceno en la cuenca de Amagá y sus implicaciones para la evolución tectónica del noroccidente suramericano. La cuenca de Amagá fue el resultado del levantamiento del Eoceno al Oligoceno de la cordillera occidental, seguido por el levantamiento del Mioceno Medio al Plioceno de las cordilleras central y occidental. Estas fases de levantamiento modificaron la red de drenaje del Mioceno en los Andes del norte. Coincidiendo con las fases finales de deformación del Mioceno en la cuenca de Amagá, el magmatismo del complejo de Combia fue el resultado de magmas de subducción emplazados en una corteza continental afectada por la tectónica de rumbo.
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