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Fracturing of the Panamanian Isthmus during initial collision with: South America
ArticleAbstract: Tectonic collision between South America and Panama began at 23-25 Ma. The collision is signiflcantPalabras claves:Autores:Bayona G.A., Camilo Montes, Cardona A., Farris D.W., Glascock M., Jaramillo C.A., Mora A., Restrepo-Moreno S., Speakman R.J., Valencia V.A.Fuentes:scopusEvidence for middle Eocene and younger land emergence in central Panama: Implications for Isthmus closure
ArticleAbstract: The rise of the Isthmus of Panama, linked to a number of climatic, paleoceanographic, and biologicalPalabras claves:Autores:Bayona G.A., Bryan J., Camilo Montes, Cardona A., Farris D.W., Flores J.A., Hoyos N., Jaramillo C.A., McFadden R.R., Morón S.E., Ramírez D.A., Restrepo-Moreno S., Silva C.A., Valencia V.A., Wilson J.Fuentes:scopusMagmatic evolution of Panama Canal volcanic rocks: A record of arc processes and tectonic change
ArticleAbstract: Volcanic rocks along the Panama Canal present a world-class opportunity to examine the relationshipPalabras claves:Autores:Camilo Montes, Cardona A., Farris D.W., Foster D.A., Jaramillo C.A.Fuentes:scopus