info:eu-repo/semantics/article
Structure and tectonic evolution of the Fuegian Andes (southernmost South America) in the framework of the Scotia Arc development
Fecha
2014-12Registro en:
Torres Carbonell, Pablo Juan; Dimieri, Luis Vicente; Olivero, Eduardo Bernardo; Bohoyo, Fernando; Galindo Zaldívar, Jesús; Structure and tectonic evolution of the Fuegian Andes (southernmost South America) in the framework of the Scotia Arc development; Elsevier Science; Global and Planetary Change; 123; Part B; 12-2014; 174-188
0921-8181
Autor
Torres Carbonell, Pablo Juan
Dimieri, Luis Vicente
Olivero, Eduardo Bernardo
Bohoyo, Fernando
Galindo Zaldívar, Jesús
Resumen
The major structural and tectonic features of the Fuegian Andes provide an outstanding onshore geological framework that aids in the understanding of the tectonic evolution of the Scotia Arc, mainly known from offshore studies. The orogenic history of the Fuegian Andes (Late Cretaceous-Miocene) is thus compared and integrated with the tectonic history of the Scotia Sea. Late Cretaceous-Paleocene structures in the Fuegian Andes suggest a N-directed contraction consistent with an oroclinal bending of the southernmost South America-Antarctic Peninsula continental bridge. This N-directed contraction in the Fuegian Andes continued during the spreading of the West Scotia Ridge, between 40-50 and 10. Ma ago. The onset of major strike-slip faulting in Tierra del Fuego is considered here to be not older than the late Miocene, consistent with the recent history of the North Scotia Ridge thus forming part of a tectonic regime superposed to the prior contraction in the Fuegian Andes.