Late Cenozoic To Modern- Day Volcanism in The Northern Andes: A Geochronological
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2019-01-01
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The Northern Andean Block is the result of complex tectonic interaction between the Farallon-Nazca, South American, and Caribbean Plates. Abundant late Cenozoic volcanism (and associated hypabyssal porphyritic plutonism), beginning in the mid- to late Mio