Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordillera

A paleomagnetic study on mid-Cretaceous rocks from the San Bernardo foldbelt (Patagonia) yields high unblocking temperature and high-coercivity magnetizations. The results indicate absence of relative vertical-axis rotations during development of the foldbelt, with the associated pole position being...

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Autores principales: Somoza, Ruben, Zaffarana, Claudia Beatriz
Publicado: 2008
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_0012821X_v271_n1-4_p267_Somoza
http://hdl.handle.net/20.500.12110/paper_0012821X_v271_n1-4_p267_Somoza
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spelling paper:paper_0012821X_v271_n1-4_p267_Somoza2025-07-30T17:18:23Z Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordillera Somoza, Ruben Zaffarana, Claudia Beatriz Andes Hotspots Mid-Cretaceous Paleomagnetism South America Atlantic coercivity Continental (CO) Early stages Elsevier (CO) Evolution (CO) Extensional tectonics Hot spotting Hot-spots Late Cretaceous Mid Cretaceous Patagonia (CO) Reference frames South America Time intervals Calcium Coercive force Ferromagnetism Magnetic properties Magnetism Tectonics Poles Cretaceous fold belt hot spot magnetization paleolatitude paleomagnetism polar wandering temperature Andes Brazil Patagonia South America A paleomagnetic study on mid-Cretaceous rocks from the San Bernardo foldbelt (Patagonia) yields high unblocking temperature and high-coercivity magnetizations. The results indicate absence of relative vertical-axis rotations during development of the foldbelt, with the associated pole position being highly concordant with coeval poles from Brazil and Patagonia. Taken together, mid-Cretaceous poles derived from studies in widely distributed localities provide supportive evidence that South America was essentially motionless with respect to the paleomagnetic axis from ca 125 to at least 100 Ma. The paleolatitudes of South America are not consistent with the occurrence of mid-Cretaceous true polar wander, suggesting that the previously observed discrepancy between the paleomagnetic and the fixed Indo-Atlantic hotspot reference frames be related to motion of the Atlantic hotspots. In agreement with this, the discrepancy is diminished by half when the Cretaceous poles of the Americas are observed in a moving-hotpots reference frame, with the residual offset being comparable to that seen for younger time intervals. The South American paleopoles and the moving-hotspot framework provide a kinematic scenario that allows relating the extensional tectonics in the early stages of Andean evolution with episodic divergence between the trench and the continental interior. Likewise, the beginning of contractional events correlates with model-predicted westward acceleration of South America in the Late Cretaceous, suggesting that the continent episodically overrode the Andean trench by those times. We argue that this change in Andean tectonic regime is associated to major plate reorganization at ca 95 Ma. © 2008 Elsevier B.V. All rights reserved. Fil:Somoza, R. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Zaffarana, C.B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2008 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_0012821X_v271_n1-4_p267_Somoza http://hdl.handle.net/20.500.12110/paper_0012821X_v271_n1-4_p267_Somoza
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Andes
Hotspots
Mid-Cretaceous
Paleomagnetism
South America
Atlantic
coercivity
Continental (CO)
Early stages
Elsevier (CO)
Evolution (CO)
Extensional tectonics
Hot spotting
Hot-spots
Late Cretaceous
Mid Cretaceous
Patagonia (CO)
Reference frames
South America
Time intervals
Calcium
Coercive force
Ferromagnetism
Magnetic properties
Magnetism
Tectonics
Poles
Cretaceous
fold belt
hot spot
magnetization
paleolatitude
paleomagnetism
polar wandering
temperature
Andes
Brazil
Patagonia
South America
spellingShingle Andes
Hotspots
Mid-Cretaceous
Paleomagnetism
South America
Atlantic
coercivity
Continental (CO)
Early stages
Elsevier (CO)
Evolution (CO)
Extensional tectonics
Hot spotting
Hot-spots
Late Cretaceous
Mid Cretaceous
Patagonia (CO)
Reference frames
South America
Time intervals
Calcium
Coercive force
Ferromagnetism
Magnetic properties
Magnetism
Tectonics
Poles
Cretaceous
fold belt
hot spot
magnetization
paleolatitude
paleomagnetism
polar wandering
temperature
Andes
Brazil
Patagonia
South America
Somoza, Ruben
Zaffarana, Claudia Beatriz
Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordillera
topic_facet Andes
Hotspots
Mid-Cretaceous
Paleomagnetism
South America
Atlantic
coercivity
Continental (CO)
Early stages
Elsevier (CO)
Evolution (CO)
Extensional tectonics
Hot spotting
Hot-spots
Late Cretaceous
Mid Cretaceous
Patagonia (CO)
Reference frames
South America
Time intervals
Calcium
Coercive force
Ferromagnetism
Magnetic properties
Magnetism
Tectonics
Poles
Cretaceous
fold belt
hot spot
magnetization
paleolatitude
paleomagnetism
polar wandering
temperature
Andes
Brazil
Patagonia
South America
description A paleomagnetic study on mid-Cretaceous rocks from the San Bernardo foldbelt (Patagonia) yields high unblocking temperature and high-coercivity magnetizations. The results indicate absence of relative vertical-axis rotations during development of the foldbelt, with the associated pole position being highly concordant with coeval poles from Brazil and Patagonia. Taken together, mid-Cretaceous poles derived from studies in widely distributed localities provide supportive evidence that South America was essentially motionless with respect to the paleomagnetic axis from ca 125 to at least 100 Ma. The paleolatitudes of South America are not consistent with the occurrence of mid-Cretaceous true polar wander, suggesting that the previously observed discrepancy between the paleomagnetic and the fixed Indo-Atlantic hotspot reference frames be related to motion of the Atlantic hotspots. In agreement with this, the discrepancy is diminished by half when the Cretaceous poles of the Americas are observed in a moving-hotpots reference frame, with the residual offset being comparable to that seen for younger time intervals. The South American paleopoles and the moving-hotspot framework provide a kinematic scenario that allows relating the extensional tectonics in the early stages of Andean evolution with episodic divergence between the trench and the continental interior. Likewise, the beginning of contractional events correlates with model-predicted westward acceleration of South America in the Late Cretaceous, suggesting that the continent episodically overrode the Andean trench by those times. We argue that this change in Andean tectonic regime is associated to major plate reorganization at ca 95 Ma. © 2008 Elsevier B.V. All rights reserved.
author Somoza, Ruben
Zaffarana, Claudia Beatriz
author_facet Somoza, Ruben
Zaffarana, Claudia Beatriz
author_sort Somoza, Ruben
title Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordillera
title_short Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordillera
title_full Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordillera
title_fullStr Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordillera
title_full_unstemmed Mid-Cretaceous polar standstill of South America, motion of the Atlantic hotspots and the birth of the Andean cordillera
title_sort mid-cretaceous polar standstill of south america, motion of the atlantic hotspots and the birth of the andean cordillera
publishDate 2008
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_0012821X_v271_n1-4_p267_Somoza
http://hdl.handle.net/20.500.12110/paper_0012821X_v271_n1-4_p267_Somoza
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