Late Cenozoic To Modern- Day Volcanism in The Northern Andes: A Geochronological

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dc.creatorMARIN, MARIA ISABEL
dc.creatorLeal, Hildebrandon
dc.creatorBernet, Matthias
dc.creatorMesa-García J.
dc.date.accessioned2021-03-26T21:28:27Z
dc.date.available2021-03-26T21:28:27Z
dc.date.issued2019-01-01
dc.description.abstractThe 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
dc.identifierhttps://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=8930
dc.identifierhttps://www.researchgate.net/publication/326978394_Late_Cenozoic_to_Modern-Day_Volcanism_in_the_Northern_Andes_A_Geochronological_Petrographical_and_Geochemical_Review_The_Pacific-Caribbean-Andean_Junction
dc.identifier.urihttp://hdl.handle.net/10784/27313
dc.languageeng
dc.relationDOI;10.1007/978-3-319-76132-9_8
dc.sourceLate Cenozoic To Modern-Day Volcanism In The Northern Andes: A Geochronological, Petrographical, And Geochemical Review
dc.sourceISBN: 9783319761329
dc.titleLate Cenozoic To Modern- Day Volcanism in The Northern Andes: A Geochronological
dc.typeinfo:eu-repo/semantics/bookPart
dc.typeCapítulo de un Libro
dc.typeinfo:eu-repo/semantics/publishedVersion

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