The Southern Central Andes vertical axis tectonic rotations: Relations with the deformation pattern

Along the Central Andes a pattern of vertical axis tectonic rotations has been paleomagnetically identified. Such rotations are counterclockwise north of Arica Deflection (~19°S) and clockwise to the south. Different hypothesis and models have been proposed to explain the Central Andean Rotation Pat...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Prezzi, C., Llanos, M.P.I.
Formato: JOUR
Materias:
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_07187092_v39_n2_p279_Prezzi
Aporte de:
id todo:paper_07187092_v39_n2_p279_Prezzi
record_format dspace
spelling todo:paper_07187092_v39_n2_p279_Prezzi2023-10-03T15:36:39Z The Southern Central Andes vertical axis tectonic rotations: Relations with the deformation pattern Prezzi, C. Llanos, M.P.I. Cenozoic Deformation Paleomagnetic data Rotational domain Southern Central Andes Cenozoic deformation Paleogene paleomagnetism spatial distribution tectonic rotation temporal distribution Altiplano Andes Arica Arica and Parinacota Chile Cordillera Paraguay Puna Along the Central Andes a pattern of vertical axis tectonic rotations has been paleomagnetically identified. Such rotations are counterclockwise north of Arica Deflection (~19°S) and clockwise to the south. Different hypothesis and models have been proposed to explain the Central Andean Rotation Pattern (CARP). However, the CARP is a subject of ongoing debate. Recently, the quantity, quality, and geographic distribution of paleomagnetic data have expanded greatly. Such expansion has been accompanied by an increase in the knowledge of the deformation periods in the Andes, allowing a more detailed analysis of the temporal and spatial distribution of the detected rotations. We compiled and analyzed the available Cenozoic paleomagnetic data for the region extending between 19° and 27.5°S. The results suggest the possible existence of different rotational domains with distinct characteristics. We propose that in the Southern Central Andes, a close correlation would exist between the style and the temporal and spatial pattern of deformation and the amount of recorded vertical axis rotations. However, in order to further investigate such relationship, new paleomagnetic studies are necessary, particularly in the Eastern Cordillera domain, in Paleogene rocks cropping out in the Altiplano-Puna and in Neogene rocks of the forearc. Fil:Prezzi, C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Llanos, M.P.I. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_07187092_v39_n2_p279_Prezzi
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Cenozoic
Deformation
Paleomagnetic data
Rotational domain
Southern Central Andes
Cenozoic
deformation
Paleogene
paleomagnetism
spatial distribution
tectonic rotation
temporal distribution
Altiplano
Andes
Arica
Arica and Parinacota
Chile
Cordillera
Paraguay
Puna
spellingShingle Cenozoic
Deformation
Paleomagnetic data
Rotational domain
Southern Central Andes
Cenozoic
deformation
Paleogene
paleomagnetism
spatial distribution
tectonic rotation
temporal distribution
Altiplano
Andes
Arica
Arica and Parinacota
Chile
Cordillera
Paraguay
Puna
Prezzi, C.
Llanos, M.P.I.
The Southern Central Andes vertical axis tectonic rotations: Relations with the deformation pattern
topic_facet Cenozoic
Deformation
Paleomagnetic data
Rotational domain
Southern Central Andes
Cenozoic
deformation
Paleogene
paleomagnetism
spatial distribution
tectonic rotation
temporal distribution
Altiplano
Andes
Arica
Arica and Parinacota
Chile
Cordillera
Paraguay
Puna
description Along the Central Andes a pattern of vertical axis tectonic rotations has been paleomagnetically identified. Such rotations are counterclockwise north of Arica Deflection (~19°S) and clockwise to the south. Different hypothesis and models have been proposed to explain the Central Andean Rotation Pattern (CARP). However, the CARP is a subject of ongoing debate. Recently, the quantity, quality, and geographic distribution of paleomagnetic data have expanded greatly. Such expansion has been accompanied by an increase in the knowledge of the deformation periods in the Andes, allowing a more detailed analysis of the temporal and spatial distribution of the detected rotations. We compiled and analyzed the available Cenozoic paleomagnetic data for the region extending between 19° and 27.5°S. The results suggest the possible existence of different rotational domains with distinct characteristics. We propose that in the Southern Central Andes, a close correlation would exist between the style and the temporal and spatial pattern of deformation and the amount of recorded vertical axis rotations. However, in order to further investigate such relationship, new paleomagnetic studies are necessary, particularly in the Eastern Cordillera domain, in Paleogene rocks cropping out in the Altiplano-Puna and in Neogene rocks of the forearc.
format JOUR
author Prezzi, C.
Llanos, M.P.I.
author_facet Prezzi, C.
Llanos, M.P.I.
author_sort Prezzi, C.
title The Southern Central Andes vertical axis tectonic rotations: Relations with the deformation pattern
title_short The Southern Central Andes vertical axis tectonic rotations: Relations with the deformation pattern
title_full The Southern Central Andes vertical axis tectonic rotations: Relations with the deformation pattern
title_fullStr The Southern Central Andes vertical axis tectonic rotations: Relations with the deformation pattern
title_full_unstemmed The Southern Central Andes vertical axis tectonic rotations: Relations with the deformation pattern
title_sort southern central andes vertical axis tectonic rotations: relations with the deformation pattern
url http://hdl.handle.net/20.500.12110/paper_07187092_v39_n2_p279_Prezzi
work_keys_str_mv AT prezzic thesoutherncentralandesverticalaxistectonicrotationsrelationswiththedeformationpattern
AT llanosmpi thesoutherncentralandesverticalaxistectonicrotationsrelationswiththedeformationpattern
AT prezzic southerncentralandesverticalaxistectonicrotationsrelationswiththedeformationpattern
AT llanosmpi southerncentralandesverticalaxistectonicrotationsrelationswiththedeformationpattern
_version_ 1807318896943824896