Vertical-axis rotations and deformation along the active strike-slip El Tigre Fault (Precordillera of San Juan, Argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility

Palaeomagnetic data from poorly consolidated to non-consolidated late Cenozoic sediments along the central segment of the active El Tigre Fault (Central-Western Precordillera of the San Juan Province, Argentina) demonstrate broad cumulative deformation up to ~450 m from the fault trace and reveal cl...

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Autores principales: Fazzito, S.Y., Rapalini, A.E., Cortés, J.M., Terrizzano, C.M.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_14373254_v106_n2_p631_Fazzito
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spelling todo:paper_14373254_v106_n2_p631_Fazzito2023-10-03T16:16:00Z Vertical-axis rotations and deformation along the active strike-slip El Tigre Fault (Precordillera of San Juan, Argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility Fazzito, S.Y. Rapalini, A.E. Cortés, J.M. Terrizzano, C.M. Magnetic fabrics Neotectonics Palaeomagnetism applied to tectonics South America Vertical-axis rotations active fault Cenozoic deformation mechanism fault displacement kinematics magnetic anisotropy magnetic fabric magnetic susceptibility neotectonics paleomagnetism strike-slip fault tectonic setting Argentina Precordillera San Juan [Argentina] Palaeomagnetic data from poorly consolidated to non-consolidated late Cenozoic sediments along the central segment of the active El Tigre Fault (Central-Western Precordillera of the San Juan Province, Argentina) demonstrate broad cumulative deformation up to ~450 m from the fault trace and reveal clockwise and anticlockwise vertical-axis rotations of variable magnitude. This deformation has affected in different amounts Miocene to late Pleistocene samples and indicates a complex kinematic pattern. Several inherited linear structures in the shear zone that are oblique to the El Tigre Fault may have acted as block boundary faults. Displacement along these faults may have resulted in a complex pattern of rotations. The maximum magnitude of rotation is a function of the age of the sediments sampled, with largest values corresponding to middle Miocene–lower Pliocene deposits and minimum values obtained from late Pleistocene deposits. The kinematic study is complemented by low-field anisotropy of magnetic susceptibility data to show that the local strain regime suggests a N–S stretching direction, subparallel to the strike of the main fault. © 2016, Springer-Verlag Berlin Heidelberg. Fil:Fazzito, S.Y. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Rapalini, A.E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Cortés, J.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Terrizzano, C.M. 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_14373254_v106_n2_p631_Fazzito
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Magnetic fabrics
Neotectonics
Palaeomagnetism applied to tectonics
South America
Vertical-axis rotations
active fault
Cenozoic
deformation mechanism
fault displacement
kinematics
magnetic anisotropy
magnetic fabric
magnetic susceptibility
neotectonics
paleomagnetism
strike-slip fault
tectonic setting
Argentina
Precordillera
San Juan [Argentina]
spellingShingle Magnetic fabrics
Neotectonics
Palaeomagnetism applied to tectonics
South America
Vertical-axis rotations
active fault
Cenozoic
deformation mechanism
fault displacement
kinematics
magnetic anisotropy
magnetic fabric
magnetic susceptibility
neotectonics
paleomagnetism
strike-slip fault
tectonic setting
Argentina
Precordillera
San Juan [Argentina]
Fazzito, S.Y.
Rapalini, A.E.
Cortés, J.M.
Terrizzano, C.M.
Vertical-axis rotations and deformation along the active strike-slip El Tigre Fault (Precordillera of San Juan, Argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility
topic_facet Magnetic fabrics
Neotectonics
Palaeomagnetism applied to tectonics
South America
Vertical-axis rotations
active fault
Cenozoic
deformation mechanism
fault displacement
kinematics
magnetic anisotropy
magnetic fabric
magnetic susceptibility
neotectonics
paleomagnetism
strike-slip fault
tectonic setting
Argentina
Precordillera
San Juan [Argentina]
description Palaeomagnetic data from poorly consolidated to non-consolidated late Cenozoic sediments along the central segment of the active El Tigre Fault (Central-Western Precordillera of the San Juan Province, Argentina) demonstrate broad cumulative deformation up to ~450 m from the fault trace and reveal clockwise and anticlockwise vertical-axis rotations of variable magnitude. This deformation has affected in different amounts Miocene to late Pleistocene samples and indicates a complex kinematic pattern. Several inherited linear structures in the shear zone that are oblique to the El Tigre Fault may have acted as block boundary faults. Displacement along these faults may have resulted in a complex pattern of rotations. The maximum magnitude of rotation is a function of the age of the sediments sampled, with largest values corresponding to middle Miocene–lower Pliocene deposits and minimum values obtained from late Pleistocene deposits. The kinematic study is complemented by low-field anisotropy of magnetic susceptibility data to show that the local strain regime suggests a N–S stretching direction, subparallel to the strike of the main fault. © 2016, Springer-Verlag Berlin Heidelberg.
format JOUR
author Fazzito, S.Y.
Rapalini, A.E.
Cortés, J.M.
Terrizzano, C.M.
author_facet Fazzito, S.Y.
Rapalini, A.E.
Cortés, J.M.
Terrizzano, C.M.
author_sort Fazzito, S.Y.
title Vertical-axis rotations and deformation along the active strike-slip El Tigre Fault (Precordillera of San Juan, Argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility
title_short Vertical-axis rotations and deformation along the active strike-slip El Tigre Fault (Precordillera of San Juan, Argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility
title_full Vertical-axis rotations and deformation along the active strike-slip El Tigre Fault (Precordillera of San Juan, Argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility
title_fullStr Vertical-axis rotations and deformation along the active strike-slip El Tigre Fault (Precordillera of San Juan, Argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility
title_full_unstemmed Vertical-axis rotations and deformation along the active strike-slip El Tigre Fault (Precordillera of San Juan, Argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility
title_sort vertical-axis rotations and deformation along the active strike-slip el tigre fault (precordillera of san juan, argentina) assessed through palaeomagnetism and anisotropy of magnetic susceptibility
url http://hdl.handle.net/20.500.12110/paper_14373254_v106_n2_p631_Fazzito
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