The sanrafaelic remagnetization of precordillera in the permian: New evidence

A paleomagnetic study, carried out on 9 sites of the La Flecha Formation (facies Los Sapitos, Upper Cambrian, Marjuman-Steptoean) exposed along the la Angostura creek, Precordillera of La Rioja (29.5°S, 68.7°W), permitted to determine two magnetic components. One is postectonic and of low coerciviti...

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Autor principal: Rapalini, Augusto Ernesto
Publicado: 2005
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n2_p290_Rapalini
http://hdl.handle.net/20.500.12110/paper_00044822_v60_n2_p290_Rapalini
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spelling paper:paper_00044822_v60_n2_p290_Rapalini2023-06-08T14:25:53Z The sanrafaelic remagnetization of precordillera in the permian: New evidence Rapalini, Augusto Ernesto Cambrian Carbonates Paleomagnetism Precordillera San rafael Cambrian carbonate formation mechanism geographical distribution magnetite orogeny paleomagnetism Permian Permian-Triassic boundary remagnetization tectonic rotation Argentina La Rioja [Argentina] Mendoza Precordillera San Rafael Massif South America Angostura A paleomagnetic study, carried out on 9 sites of the La Flecha Formation (facies Los Sapitos, Upper Cambrian, Marjuman-Steptoean) exposed along the la Angostura creek, Precordillera of La Rioja (29.5°S, 68.7°W), permitted to determine two magnetic components. One is postectonic and of low coercivities and unblocking temperatures (A, Dec: 7.5°, Inc: -40.3°, a95: 10.1°, N: 6), being interpreted as a recent remanence of probable viscous origin. A second, pretectonic, component was isolated in seven sites with opposite polarities and is likely carried by magnetite (B, Dec: 206.9°, Inc: 63.3°, a95: 12.8°, N: 7). The paleomagnetic pole position for this component (Lat: 63.8°S, Long: 244.6°E, dp: 15.9°, dm: 20.2°) suggests that the remanence was acquired by the end of the Permian and it is interpreted as produced by the regional remagnetization associated with the San Rafael orogenic phase found in other units of the Precordillera. An analysis of pole positions, type of magnetizations, polarities and geographic distribution of the remagnetized units suggests a pattern of time-space migration of the remagnetization from west to east, between the Early Permian and the Permian-Triassic. This pattern is consistent with a model of remagnetization by migration of fluids expelled from the orogenic area that reached rocks not involved directly in the deformation. The pole position obtained for La Flecha Formation also suggests the lack of major tectonic rotations in the study area since the Permian. © 2005 Asociación Geológica Argentina. Fil:Rapalini, A.E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2005 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n2_p290_Rapalini http://hdl.handle.net/20.500.12110/paper_00044822_v60_n2_p290_Rapalini
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Cambrian
Carbonates
Paleomagnetism
Precordillera
San rafael
Cambrian
carbonate
formation mechanism
geographical distribution
magnetite
orogeny
paleomagnetism
Permian
Permian-Triassic boundary
remagnetization
tectonic rotation
Argentina
La Rioja [Argentina]
Mendoza
Precordillera
San Rafael Massif
South America
Angostura
spellingShingle Cambrian
Carbonates
Paleomagnetism
Precordillera
San rafael
Cambrian
carbonate
formation mechanism
geographical distribution
magnetite
orogeny
paleomagnetism
Permian
Permian-Triassic boundary
remagnetization
tectonic rotation
Argentina
La Rioja [Argentina]
Mendoza
Precordillera
San Rafael Massif
South America
Angostura
Rapalini, Augusto Ernesto
The sanrafaelic remagnetization of precordillera in the permian: New evidence
topic_facet Cambrian
Carbonates
Paleomagnetism
Precordillera
San rafael
Cambrian
carbonate
formation mechanism
geographical distribution
magnetite
orogeny
paleomagnetism
Permian
Permian-Triassic boundary
remagnetization
tectonic rotation
Argentina
La Rioja [Argentina]
Mendoza
Precordillera
San Rafael Massif
South America
Angostura
description A paleomagnetic study, carried out on 9 sites of the La Flecha Formation (facies Los Sapitos, Upper Cambrian, Marjuman-Steptoean) exposed along the la Angostura creek, Precordillera of La Rioja (29.5°S, 68.7°W), permitted to determine two magnetic components. One is postectonic and of low coercivities and unblocking temperatures (A, Dec: 7.5°, Inc: -40.3°, a95: 10.1°, N: 6), being interpreted as a recent remanence of probable viscous origin. A second, pretectonic, component was isolated in seven sites with opposite polarities and is likely carried by magnetite (B, Dec: 206.9°, Inc: 63.3°, a95: 12.8°, N: 7). The paleomagnetic pole position for this component (Lat: 63.8°S, Long: 244.6°E, dp: 15.9°, dm: 20.2°) suggests that the remanence was acquired by the end of the Permian and it is interpreted as produced by the regional remagnetization associated with the San Rafael orogenic phase found in other units of the Precordillera. An analysis of pole positions, type of magnetizations, polarities and geographic distribution of the remagnetized units suggests a pattern of time-space migration of the remagnetization from west to east, between the Early Permian and the Permian-Triassic. This pattern is consistent with a model of remagnetization by migration of fluids expelled from the orogenic area that reached rocks not involved directly in the deformation. The pole position obtained for La Flecha Formation also suggests the lack of major tectonic rotations in the study area since the Permian. © 2005 Asociación Geológica Argentina.
author Rapalini, Augusto Ernesto
author_facet Rapalini, Augusto Ernesto
author_sort Rapalini, Augusto Ernesto
title The sanrafaelic remagnetization of precordillera in the permian: New evidence
title_short The sanrafaelic remagnetization of precordillera in the permian: New evidence
title_full The sanrafaelic remagnetization of precordillera in the permian: New evidence
title_fullStr The sanrafaelic remagnetization of precordillera in the permian: New evidence
title_full_unstemmed The sanrafaelic remagnetization of precordillera in the permian: New evidence
title_sort sanrafaelic remagnetization of precordillera in the permian: new evidence
publishDate 2005
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n2_p290_Rapalini
http://hdl.handle.net/20.500.12110/paper_00044822_v60_n2_p290_Rapalini
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