Volcanic contribution to emergence of Central Panama in the Early Miocene View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2019-12

AUTHORS

David M. Buchs, Derek Irving, Henry Coombs, Roberto Miranda, Jian Wang, Maurylis Coronado, Rodrigo Arrocha, Mauricio Lacerda, Creed Goff, Eladio Almengor, Enier Portugal, Pastora Franceschi, Eric Chichaco, Stewart D. Redwood

ABSTRACT

Formation of the Panama Isthmus, that had global oceanographic and biotic effects in the Neogene, is generally associated with tectonic uplift during collision of the Panama volcanic arc with South America. However, new field, geochemical and geochronological data from the Culebra Cut of the Panama Canal suggest that volcanism also contributed to the Isthmus emergence in the Early Miocene. This volcanism is recorded in a newly-recognised Central Panama volcanic field that includes several phases of development. Early activity of this field along the Panama Canal was associated with proximal effusive to explosive felsic products during formation of subaerial stratovolcanoes and possible domes ca. 21 Ma. This was followed by a period of marine transgression ca. 21-18 Ma, with more distal volcanism documented by tuffs that deposited in marine to terrestrial environments. Finally, proximal mafic volcanism formed tephra cones in a monogenetic field ca. 18(-?) Ma. This was associated with phreatomagmatic processes in a coastal environment, with remarkable kilometre-wide subvolcanic peperitic intrusions. We propose based on these observations that formation of the Central Panama volcanic field was critical in shaping regional topography, and that this could have actively contributed to obstruction and closure of an interoceanic strait in Central Panama. More... »

PAGES

1417

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/s41598-018-37790-2

DOI

http://dx.doi.org/10.1038/s41598-018-37790-2

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1111911364

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/30723222


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