Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina
- Autores
- Vizan, Haroldo; Ixer, Robert; Turner, Peter; Cortes, Jose Maria; Cladera, Gerardo
- Año de publicación
- 2004
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Different authors have highlighted a systematic disagreement between Late Carboniferous-Triassic paleomagnetic poles (PPs) for Gondwanaland and Laurasia when they are repositioned in a classical reconstruction prior to the breakup of Pangea A. This disagreement has been interpreted in geodynamic terms or as an evidence of non-dipole components of the geomagnetic field. Such analyses have been made using data on South American PPs published approximately 25 years ago and obtained using outdated methodologies. In this article, the authors present new Late Triassic paleomagnetic data from rocks that crop out in the Pre-Andean ranges (Precordillera) of Mendoza province (Argentina). Samples of different lithologies were taken from two limbs of a doubly plunging syncline, and several field tests of paleomagnetic stability were applied. The results indicate primary site mean directions that yield a PP with geographic coordinates and statistical parameters as follows: Lat.=76°S, Lon.=280°E, N=12, R=11.63, α95=8°, K=30.2. This PP agrees with mean PPs of Laurasia of similar ages in different models of Pangea A, indicating that the hypothesis of a dipolar paleomagnetic field could be valid for the Late Triassic.
Fil: Vizan, Haroldo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas; Argentina
Fil: Ixer, Robert. The University of Birmingham; Estados Unidos
Fil: Turner, Peter. The University of Birmingham; Estados Unidos
Fil: Cortes, Jose Maria. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas; Argentina
Fil: Cladera, Gerardo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Museo Paleontológico Egidio Feruglio; Argentina - Materia
-
Argentina
Late Triassic
Paleomagnetism
Pangea
Precordillera - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/83508
Ver los metadatos del registro completo
id |
CONICETDig_6958e271e392ed731b90a25177d4106b |
---|---|
oai_identifier_str |
oai:ri.conicet.gov.ar:11336/83508 |
network_acronym_str |
CONICETDig |
repository_id_str |
3498 |
network_name_str |
CONICET Digital (CONICET) |
spelling |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, ArgentinaVizan, HaroldoIxer, RobertTurner, PeterCortes, Jose MariaCladera, GerardoArgentinaLate TriassicPaleomagnetismPangeaPrecordillerahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Different authors have highlighted a systematic disagreement between Late Carboniferous-Triassic paleomagnetic poles (PPs) for Gondwanaland and Laurasia when they are repositioned in a classical reconstruction prior to the breakup of Pangea A. This disagreement has been interpreted in geodynamic terms or as an evidence of non-dipole components of the geomagnetic field. Such analyses have been made using data on South American PPs published approximately 25 years ago and obtained using outdated methodologies. In this article, the authors present new Late Triassic paleomagnetic data from rocks that crop out in the Pre-Andean ranges (Precordillera) of Mendoza province (Argentina). Samples of different lithologies were taken from two limbs of a doubly plunging syncline, and several field tests of paleomagnetic stability were applied. The results indicate primary site mean directions that yield a PP with geographic coordinates and statistical parameters as follows: Lat.=76°S, Lon.=280°E, N=12, R=11.63, α95=8°, K=30.2. This PP agrees with mean PPs of Laurasia of similar ages in different models of Pangea A, indicating that the hypothesis of a dipolar paleomagnetic field could be valid for the Late Triassic.Fil: Vizan, Haroldo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas; ArgentinaFil: Ixer, Robert. The University of Birmingham; Estados UnidosFil: Turner, Peter. The University of Birmingham; Estados UnidosFil: Cortes, Jose Maria. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas; ArgentinaFil: Cladera, Gerardo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Museo Paleontológico Egidio Feruglio; ArgentinaPergamon-Elsevier Science Ltd2004-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/83508Vizan, Haroldo; Ixer, Robert; Turner, Peter; Cortes, Jose Maria; Cladera, Gerardo; Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 18; 1; 12-2004; 41-590895-9811CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0895981104000756info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2004.08.008info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:31:43Zoai:ri.conicet.gov.ar:11336/83508instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:31:43.779CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina |
title |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina |
spellingShingle |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina Vizan, Haroldo Argentina Late Triassic Paleomagnetism Pangea Precordillera |
title_short |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina |
title_full |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina |
title_fullStr |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina |
title_full_unstemmed |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina |
title_sort |
Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina |
dc.creator.none.fl_str_mv |
Vizan, Haroldo Ixer, Robert Turner, Peter Cortes, Jose Maria Cladera, Gerardo |
author |
Vizan, Haroldo |
author_facet |
Vizan, Haroldo Ixer, Robert Turner, Peter Cortes, Jose Maria Cladera, Gerardo |
author_role |
author |
author2 |
Ixer, Robert Turner, Peter Cortes, Jose Maria Cladera, Gerardo |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
Argentina Late Triassic Paleomagnetism Pangea Precordillera |
topic |
Argentina Late Triassic Paleomagnetism Pangea Precordillera |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Different authors have highlighted a systematic disagreement between Late Carboniferous-Triassic paleomagnetic poles (PPs) for Gondwanaland and Laurasia when they are repositioned in a classical reconstruction prior to the breakup of Pangea A. This disagreement has been interpreted in geodynamic terms or as an evidence of non-dipole components of the geomagnetic field. Such analyses have been made using data on South American PPs published approximately 25 years ago and obtained using outdated methodologies. In this article, the authors present new Late Triassic paleomagnetic data from rocks that crop out in the Pre-Andean ranges (Precordillera) of Mendoza province (Argentina). Samples of different lithologies were taken from two limbs of a doubly plunging syncline, and several field tests of paleomagnetic stability were applied. The results indicate primary site mean directions that yield a PP with geographic coordinates and statistical parameters as follows: Lat.=76°S, Lon.=280°E, N=12, R=11.63, α95=8°, K=30.2. This PP agrees with mean PPs of Laurasia of similar ages in different models of Pangea A, indicating that the hypothesis of a dipolar paleomagnetic field could be valid for the Late Triassic. Fil: Vizan, Haroldo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas; Argentina Fil: Ixer, Robert. The University of Birmingham; Estados Unidos Fil: Turner, Peter. The University of Birmingham; Estados Unidos Fil: Cortes, Jose Maria. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas; Argentina Fil: Cladera, Gerardo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Museo Paleontológico Egidio Feruglio; Argentina |
description |
Different authors have highlighted a systematic disagreement between Late Carboniferous-Triassic paleomagnetic poles (PPs) for Gondwanaland and Laurasia when they are repositioned in a classical reconstruction prior to the breakup of Pangea A. This disagreement has been interpreted in geodynamic terms or as an evidence of non-dipole components of the geomagnetic field. Such analyses have been made using data on South American PPs published approximately 25 years ago and obtained using outdated methodologies. In this article, the authors present new Late Triassic paleomagnetic data from rocks that crop out in the Pre-Andean ranges (Precordillera) of Mendoza province (Argentina). Samples of different lithologies were taken from two limbs of a doubly plunging syncline, and several field tests of paleomagnetic stability were applied. The results indicate primary site mean directions that yield a PP with geographic coordinates and statistical parameters as follows: Lat.=76°S, Lon.=280°E, N=12, R=11.63, α95=8°, K=30.2. This PP agrees with mean PPs of Laurasia of similar ages in different models of Pangea A, indicating that the hypothesis of a dipolar paleomagnetic field could be valid for the Late Triassic. |
publishDate |
2004 |
dc.date.none.fl_str_mv |
2004-12 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/83508 Vizan, Haroldo; Ixer, Robert; Turner, Peter; Cortes, Jose Maria; Cladera, Gerardo; Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 18; 1; 12-2004; 41-59 0895-9811 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/83508 |
identifier_str_mv |
Vizan, Haroldo; Ixer, Robert; Turner, Peter; Cortes, Jose Maria; Cladera, Gerardo; Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 18; 1; 12-2004; 41-59 0895-9811 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0895981104000756 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2004.08.008 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Pergamon-Elsevier Science Ltd |
publisher.none.fl_str_mv |
Pergamon-Elsevier Science Ltd |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
_version_ |
1844614328574017536 |
score |
13.070432 |