An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc

The backbone of this book is the analysis of the relation between the tectonic evolution of the Southernmost Andes and its southern neighbors: Antarctica and the Scotia Sea. The Southernmost Andes comprise the southern bent of the Andean mountains, where they progressively change their strike from t...

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Main Author: Ghiglione, Matias
Format: Book Part
Language:English
Published: Springer
Subjects:
Online Access:http://hdl.handle.net/11336/99074
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author Ghiglione, Matias
author2 Ghiglione, Matias
author_facet Ghiglione, Matias
author_sort Ghiglione, Matias
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
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description The backbone of this book is the analysis of the relation between the tectonic evolution of the Southernmost Andes and its southern neighbors: Antarctica and the Scotia Sea. The Southernmost Andes comprise the southern bent of the Andean mountains, where they progressively change their strike from the N-S?oriented Southern Patagonian Andes to the E-W?trending Fuegian Andes (Fig. 1). These Andean segments and their corresponding basement, sedimentary basins, magmatic rocks and batholithic belts are linked, even if sometimes elusively, to the evolution of the Antarctic Peninsula and of the islands spread in the southern ocean. The Scotia Sea separating South America and the Antarctic Pe-ninsula (Fig. 1) is only ~30 Myr old, very young, considering a joint geological history of the Southernmost Andes, Patagonia and Antarctica than can be traced back to late Paleozoic times (i.e. 300 Myr or more). Analysis of marine geophysical data in the Scotia Sea (cf. Eagles et al. 2006) and geological data from Tierra del Fuego (Ghiglione et al. 2008) demonstrate that the disconnection of South America and Antarctica started at about 50 Ma. However, oceanic spreading producing the final opening of the Drake Passage, and the consequent strike-slip movements along the North and South Scotia ridges (Fig. 1), occurred just since the Oligocene. Therefore, there is a joint history of Antarctica and South America that was shattered by the opening of the Scotia Sea; the remaining pieces of the puzzle, how can they fit together, and how were they separated from each other are the subjects of this book. Fil: Ghiglione, Matias. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
format Book Part
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Drake Passage
Scotia Sea
Southern Ocean
Tierra del Fuego
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Drake Passage
Scotia Sea
Southern Ocean
Tierra del Fuego
geographic Antarctic
Southern Ocean
The Antarctic
Antarctic Peninsula
Patagonia
Drake Passage
Scotia Sea
Argentina
Pablo
geographic_facet Antarctic
Southern Ocean
The Antarctic
Antarctic Peninsula
Patagonia
Drake Passage
Scotia Sea
Argentina
Pablo
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http://hdl.handle.net/11336/99074
Ghiglione, Matias; An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc; Springer; 2016; 1-6
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/99074 2025-01-16T19:11:10+00:00 An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc Ghiglione, Matias Ghiglione, Matias application/pdf http://hdl.handle.net/11336/99074 eng eng Springer info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-39727-6_1 info:eu-repo/semantics/altIdentifier/doi/10.1007/978-3-319-39727-6_1 http://hdl.handle.net/11336/99074 Ghiglione, Matias; An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc; Springer; 2016; 1-6 978-3-319-39725-2 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Southernmost Andes Scotia Arc Antarctic Peninsula Malvinas Basin https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/bookPart info:ar-repo/semantics/parte de libro ftconicet https://doi.org/10.1007/978-3-319-39727-6_1 2023-09-24T20:03:43Z The backbone of this book is the analysis of the relation between the tectonic evolution of the Southernmost Andes and its southern neighbors: Antarctica and the Scotia Sea. The Southernmost Andes comprise the southern bent of the Andean mountains, where they progressively change their strike from the N-S?oriented Southern Patagonian Andes to the E-W?trending Fuegian Andes (Fig. 1). These Andean segments and their corresponding basement, sedimentary basins, magmatic rocks and batholithic belts are linked, even if sometimes elusively, to the evolution of the Antarctic Peninsula and of the islands spread in the southern ocean. The Scotia Sea separating South America and the Antarctic Pe-ninsula (Fig. 1) is only ~30 Myr old, very young, considering a joint geological history of the Southernmost Andes, Patagonia and Antarctica than can be traced back to late Paleozoic times (i.e. 300 Myr or more). Analysis of marine geophysical data in the Scotia Sea (cf. Eagles et al. 2006) and geological data from Tierra del Fuego (Ghiglione et al. 2008) demonstrate that the disconnection of South America and Antarctica started at about 50 Ma. However, oceanic spreading producing the final opening of the Drake Passage, and the consequent strike-slip movements along the North and South Scotia ridges (Fig. 1), occurred just since the Oligocene. Therefore, there is a joint history of Antarctica and South America that was shattered by the opening of the Scotia Sea; the remaining pieces of the puzzle, how can they fit together, and how were they separated from each other are the subjects of this book. Fil: Ghiglione, Matias. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Book Part Antarc* Antarctic Antarctic Peninsula Antarctica Drake Passage Scotia Sea Southern Ocean Tierra del Fuego CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Southern Ocean The Antarctic Antarctic Peninsula Patagonia Drake Passage Scotia Sea Argentina Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) 1 6
spellingShingle Southernmost Andes
Scotia Arc
Antarctic Peninsula
Malvinas Basin
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Ghiglione, Matias
An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc
title An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc
title_full An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc
title_fullStr An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc
title_full_unstemmed An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc
title_short An introduction to the Geodynamic Evolution of the Southernmost Andes: Connections with the Scotia Arc
title_sort introduction to the geodynamic evolution of the southernmost andes: connections with the scotia arc
topic Southernmost Andes
Scotia Arc
Antarctic Peninsula
Malvinas Basin
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Southernmost Andes
Scotia Arc
Antarctic Peninsula
Malvinas Basin
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/99074