Continental stretching preceding the opening of the Drake Passage: Evidence from Tierra del Fuego
Age estimates for the onset of a seaway through the Drake Passage range from middle Eocene to early Miocene, complicating interpretations of the relation between ocean circulation and Cenozoic global cooling. Here we present evidence for the presence of a latest Paleocene-early Eocene extensional ba...
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Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00917613_v36_n8_p643_Ghiglione http://hdl.handle.net/20.500.12110/paper_00917613_v36_n8_p643_Ghiglione |
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paper:paper_00917613_v36_n8_p643_Ghiglione2023-06-08T15:08:11Z Continental stretching preceding the opening of the Drake Passage: Evidence from Tierra del Fuego Airborne magnetic data Continental stretching Scotia Sea Tierra del Fuego Airborne magnetic data Continental stretching Drake passage Scotia Sea Tierra del Fuego Concentration (process) Isomers Oceanography Structural geology basin evolution Cenozoic Eocene extensional tectonics faulting lithospheric structure Miocene oceanic circulation Paleocene Atlantic Ocean Drake Passage Scotia Sea South America Tierra del Fuego [(ARC) South America] Age estimates for the onset of a seaway through the Drake Passage range from middle Eocene to early Miocene, complicating interpretations of the relation between ocean circulation and Cenozoic global cooling. Here we present evidence for the presence of a latest Paleocene-early Eocene extensional basin (i.e., lateral rift) in Tierra del Fuego. An accurately dated postrift unconformity indicates that extensional faulting ended in the studied area ca. 49 Ma, in concurrence with a previously reported eightfold increase in South America-Antarctica separation rate, and the proposed onset of oceanic basins in the incipient Drake Passage. The coincidence of these facts indicates progressive strain concentration on the zone of future crustal separation (i.e., Drake Passage) after abandonment of lateral rifts ca. 49 Ma. Although the described extensional depocenters did not allow the exchange of water between the Pacific and Atlantic Oceans, they represent a direct indication of continental lithospheric stretching preceding the recently proposed Eocene opening of embryonic basins in the West Scotia Sea. © 2008 The Geological Society of America. 2008 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00917613_v36_n8_p643_Ghiglione http://hdl.handle.net/20.500.12110/paper_00917613_v36_n8_p643_Ghiglione |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Airborne magnetic data Continental stretching Scotia Sea Tierra del Fuego Airborne magnetic data Continental stretching Drake passage Scotia Sea Tierra del Fuego Concentration (process) Isomers Oceanography Structural geology basin evolution Cenozoic Eocene extensional tectonics faulting lithospheric structure Miocene oceanic circulation Paleocene Atlantic Ocean Drake Passage Scotia Sea South America Tierra del Fuego [(ARC) South America] |
spellingShingle |
Airborne magnetic data Continental stretching Scotia Sea Tierra del Fuego Airborne magnetic data Continental stretching Drake passage Scotia Sea Tierra del Fuego Concentration (process) Isomers Oceanography Structural geology basin evolution Cenozoic Eocene extensional tectonics faulting lithospheric structure Miocene oceanic circulation Paleocene Atlantic Ocean Drake Passage Scotia Sea South America Tierra del Fuego [(ARC) South America] Continental stretching preceding the opening of the Drake Passage: Evidence from Tierra del Fuego |
topic_facet |
Airborne magnetic data Continental stretching Scotia Sea Tierra del Fuego Airborne magnetic data Continental stretching Drake passage Scotia Sea Tierra del Fuego Concentration (process) Isomers Oceanography Structural geology basin evolution Cenozoic Eocene extensional tectonics faulting lithospheric structure Miocene oceanic circulation Paleocene Atlantic Ocean Drake Passage Scotia Sea South America Tierra del Fuego [(ARC) South America] |
description |
Age estimates for the onset of a seaway through the Drake Passage range from middle Eocene to early Miocene, complicating interpretations of the relation between ocean circulation and Cenozoic global cooling. Here we present evidence for the presence of a latest Paleocene-early Eocene extensional basin (i.e., lateral rift) in Tierra del Fuego. An accurately dated postrift unconformity indicates that extensional faulting ended in the studied area ca. 49 Ma, in concurrence with a previously reported eightfold increase in South America-Antarctica separation rate, and the proposed onset of oceanic basins in the incipient Drake Passage. The coincidence of these facts indicates progressive strain concentration on the zone of future crustal separation (i.e., Drake Passage) after abandonment of lateral rifts ca. 49 Ma. Although the described extensional depocenters did not allow the exchange of water between the Pacific and Atlantic Oceans, they represent a direct indication of continental lithospheric stretching preceding the recently proposed Eocene opening of embryonic basins in the West Scotia Sea. © 2008 The Geological Society of America. |
title |
Continental stretching preceding the opening of the Drake Passage: Evidence from Tierra del Fuego |
title_short |
Continental stretching preceding the opening of the Drake Passage: Evidence from Tierra del Fuego |
title_full |
Continental stretching preceding the opening of the Drake Passage: Evidence from Tierra del Fuego |
title_fullStr |
Continental stretching preceding the opening of the Drake Passage: Evidence from Tierra del Fuego |
title_full_unstemmed |
Continental stretching preceding the opening of the Drake Passage: Evidence from Tierra del Fuego |
title_sort |
continental stretching preceding the opening of the drake passage: evidence from tierra del fuego |
publishDate |
2008 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00917613_v36_n8_p643_Ghiglione http://hdl.handle.net/20.500.12110/paper_00917613_v36_n8_p643_Ghiglione |
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1768542829310640128 |