Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks
This contribution addresses new structural data from Upper Cretaceous-Danian sedimentary rocks of the Fuegian Andes orogenic front in Argentina. The structures studied, called D0 , were formed during the early foreland deformation of the orogen, in the Late Cretaceous-Danian, in times when South Ame...
Published in: | Journal of Structural Geology |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
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Online Access: | http://hdl.handle.net/11336/26392 |
_version_ | 1821772065096597504 |
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author | Torres Carbonell, Pablo Juan Dimieri, Luis Vicente Martinioni, Daniel Roberto |
author_facet | Torres Carbonell, Pablo Juan Dimieri, Luis Vicente Martinioni, Daniel Roberto |
author_sort | Torres Carbonell, Pablo Juan |
collection | CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
container_start_page | 14 |
container_title | Journal of Structural Geology |
container_volume | 48 |
description | This contribution addresses new structural data from Upper Cretaceous-Danian sedimentary rocks of the Fuegian Andes orogenic front in Argentina. The structures studied, called D0 , were formed during the early foreland deformation of the orogen, in the Late Cretaceous-Danian, in times when South America and Antarctica were still connected. The strain analysis of these structures indicates that deformation occurred at upper-crustal depths, and was characterized by flexural folding accompanied by formation of pressure-solution tectonic foliations in zones of higher strain. Deformation intensities increase toward the hinterland and with depth. The history of deformation involved progression from layer-parallel shortening to folding above a detachment, and further formation of a forward-propagating thrust wedge. Layer-parallel shortening and incipient folding recorded in Maastrichtian-Danian rocks indicate the leading edge of D0 deformation. Non-coaxial finite strain orientations were involved during formation of D0 structures along the Fuegian Andes front. These finite strain orientations cannot be explained with the SW-NE regional contraction usually assumed to have driven Andean deformation in this region; alternatively, we consider that N-S contraction combined with buttressing against the cratonic foreland comprise a more suitable interpretation for D0 and younger deformation. Fil: Torres Carbonell, Pablo Juan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Dimieri, Luis Vicente. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina Fil: Martinioni, Daniel Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctica |
genre_facet | Antarc* Antarctica |
geographic | Austral Argentina Pablo Carbonell |
geographic_facet | Austral Argentina Pablo Carbonell |
id | ftconicet:oai:ri.conicet.gov.ar:11336/26392 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-63.717,-63.717,-64.283,-64.283) ENVELOPE(-56.983,-56.983,-63.533,-63.533) |
op_collection_id | ftconicet |
op_container_end_page | 32 |
op_doi | https://doi.org/10.1016/j.jsg.2012.12.010 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsg.2012.12.010 info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0191814112002817 http://hdl.handle.net/11336/26392 Torres Carbonell, Pablo Juan; Dimieri, Luis Vicente; Martinioni, Daniel Roberto; Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks; Elsevier; Journal Of Structural Geology; 48; 1-2013; 14-32 0191-8141 |
op_rights | info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
publisher | Elsevier |
record_format | openpolar |
spelling | ftconicet:oai:ri.conicet.gov.ar:11336/26392 2025-01-16T19:38:47+00:00 Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks Torres Carbonell, Pablo Juan Dimieri, Luis Vicente Martinioni, Daniel Roberto application/pdf http://hdl.handle.net/11336/26392 eng eng Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsg.2012.12.010 info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0191814112002817 http://hdl.handle.net/11336/26392 Torres Carbonell, Pablo Juan; Dimieri, Luis Vicente; Martinioni, Daniel Roberto; Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks; Elsevier; Journal Of Structural Geology; 48; 1-2013; 14-32 0191-8141 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ Strain Analysis Orogenic Front Fuegian Andes Deformation History https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.jsg.2012.12.010 2023-09-24T19:38:42Z This contribution addresses new structural data from Upper Cretaceous-Danian sedimentary rocks of the Fuegian Andes orogenic front in Argentina. The structures studied, called D0 , were formed during the early foreland deformation of the orogen, in the Late Cretaceous-Danian, in times when South America and Antarctica were still connected. The strain analysis of these structures indicates that deformation occurred at upper-crustal depths, and was characterized by flexural folding accompanied by formation of pressure-solution tectonic foliations in zones of higher strain. Deformation intensities increase toward the hinterland and with depth. The history of deformation involved progression from layer-parallel shortening to folding above a detachment, and further formation of a forward-propagating thrust wedge. Layer-parallel shortening and incipient folding recorded in Maastrichtian-Danian rocks indicate the leading edge of D0 deformation. Non-coaxial finite strain orientations were involved during formation of D0 structures along the Fuegian Andes front. These finite strain orientations cannot be explained with the SW-NE regional contraction usually assumed to have driven Andean deformation in this region; alternatively, we consider that N-S contraction combined with buttressing against the cratonic foreland comprise a more suitable interpretation for D0 and younger deformation. Fil: Torres Carbonell, Pablo Juan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Dimieri, Luis Vicente. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina Fil: Martinioni, Daniel Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Article in Journal/Newspaper Antarc* Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Austral Argentina Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Carbonell ENVELOPE(-56.983,-56.983,-63.533,-63.533) Journal of Structural Geology 48 14 32 |
spellingShingle | Strain Analysis Orogenic Front Fuegian Andes Deformation History https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Torres Carbonell, Pablo Juan Dimieri, Luis Vicente Martinioni, Daniel Roberto Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks |
title | Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks |
title_full | Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks |
title_fullStr | Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks |
title_full_unstemmed | Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks |
title_short | Early foreland deformation of the Fuegian Andes (Argentina): Constraints from the strain analysis of Upper Cretaceous-Danian sedimentary rocks |
title_sort | early foreland deformation of the fuegian andes (argentina): constraints from the strain analysis of upper cretaceous-danian sedimentary rocks |
topic | Strain Analysis Orogenic Front Fuegian Andes Deformation History https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
topic_facet | Strain Analysis Orogenic Front Fuegian Andes Deformation History https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
url | http://hdl.handle.net/11336/26392 |