Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones
A set of fracture zones left by transform faults segmenting the active Chile Ridge that separates the Nazca and Antarctica Plates has been subducting beneath western Patagonia in the last 18 Myr. The subduction direction of these fractures zones has remained almost unaltered during this time lapse s...
Published in: | Journal of Geodynamics |
---|---|
Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Pergamon-Elsevier Science Ltd
|
Subjects: | |
Online Access: | http://hdl.handle.net/11336/147021 |
id |
ftconicet:oai:ri.conicet.gov.ar:11336/147021 |
---|---|
record_format |
openpolar |
spelling |
ftconicet:oai:ri.conicet.gov.ar:11336/147021 2023-10-09T21:44:45+02:00 Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones Orts, Darío Leandro Alvarez Pontoriero, Orlando Zaffarana, Claudia Beatriz Gimenez, Mario Ernesto Ruiz, Francisco Folguera Telichevsky, Andres application/pdf http://hdl.handle.net/11336/147021 eng eng Pergamon-Elsevier Science Ltd info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jog.2020.101806 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0264370720301484?via%3Dihub http://hdl.handle.net/11336/147021 Orts, Darío Leandro; Alvarez Pontoriero, Orlando; Zaffarana, Claudia Beatriz; Gimenez, Mario Ernesto; Ruiz, Francisco; et al.; Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones; Pergamon-Elsevier Science Ltd; Journal of Geodynamics; 143; 101806; 12-2020; 1-49 0264-3707 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ FRACTURE ZONES PATAGONIA ANDEAN DEFORMATION ANDES 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.jog.2020.101806 2023-09-24T19:13:35Z A set of fracture zones left by transform faults segmenting the active Chile Ridge that separates the Nazca and Antarctica Plates has been subducting beneath western Patagonia in the last 18 Myr. The subduction direction of these fractures zones has remained almost unaltered during this time lapse since these intersected the Chilean trench. In this context, the analyzed Patagonian sector is associated with the subduction of a highly buoyant oceanic floor due to its relatively young age that contrasts with the ocean floor bathymetry to the north where oceanic crust gets progressively older up to the Eocene and consequently isostatically subsides. Short-term elastic deformational patterns associated with the earthquake cycle have been linked to this segmentation imposed by subducting fracture zones in previous works. Similarly, this work explores the relationship between long-term topography, seismicity, gravity, and magnetic anomalies as a proxy for upper crustal structure, deformation, exhumation, and consequently surface geology segmented nature associated with this pattern of oceanic fracture zones. Through these analyses, we have identified a series of ENE structural trends or lineaments across the continental crust that could be directly related to the segmented mechanical behavior of the plate interface and enhanced by particular climatic and tectonic history of the Patagonian region. These evidences could contribute to the understanding of how fracture zones can control, to a certain extent, the segmented nature of the upper plate in a subduction setting. Fil: Orts, Darío Leandro. Universidad Nacional de Río Negro. Sede Alto Valle. Instituto de Investigaciones en Paleobiología y Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina Fil: Alvarez Pontoriero, Orlando. Universidad Nacional ... Article in Journal/Newspaper Antarc* Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Patagonia Argentina Alvarez ENVELOPE(-64.483,-64.483,-65.633,-65.633) Journal of Geodynamics 143 101806 |
institution |
Open Polar |
collection |
CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
op_collection_id |
ftconicet |
language |
English |
topic |
FRACTURE ZONES PATAGONIA ANDEAN DEFORMATION ANDES https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
spellingShingle |
FRACTURE ZONES PATAGONIA ANDEAN DEFORMATION ANDES https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Orts, Darío Leandro Alvarez Pontoriero, Orlando Zaffarana, Claudia Beatriz Gimenez, Mario Ernesto Ruiz, Francisco Folguera Telichevsky, Andres Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones |
topic_facet |
FRACTURE ZONES PATAGONIA ANDEAN DEFORMATION ANDES https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
description |
A set of fracture zones left by transform faults segmenting the active Chile Ridge that separates the Nazca and Antarctica Plates has been subducting beneath western Patagonia in the last 18 Myr. The subduction direction of these fractures zones has remained almost unaltered during this time lapse since these intersected the Chilean trench. In this context, the analyzed Patagonian sector is associated with the subduction of a highly buoyant oceanic floor due to its relatively young age that contrasts with the ocean floor bathymetry to the north where oceanic crust gets progressively older up to the Eocene and consequently isostatically subsides. Short-term elastic deformational patterns associated with the earthquake cycle have been linked to this segmentation imposed by subducting fracture zones in previous works. Similarly, this work explores the relationship between long-term topography, seismicity, gravity, and magnetic anomalies as a proxy for upper crustal structure, deformation, exhumation, and consequently surface geology segmented nature associated with this pattern of oceanic fracture zones. Through these analyses, we have identified a series of ENE structural trends or lineaments across the continental crust that could be directly related to the segmented mechanical behavior of the plate interface and enhanced by particular climatic and tectonic history of the Patagonian region. These evidences could contribute to the understanding of how fracture zones can control, to a certain extent, the segmented nature of the upper plate in a subduction setting. Fil: Orts, Darío Leandro. Universidad Nacional de Río Negro. Sede Alto Valle. Instituto de Investigaciones en Paleobiología y Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina Fil: Alvarez Pontoriero, Orlando. Universidad Nacional ... |
format |
Article in Journal/Newspaper |
author |
Orts, Darío Leandro Alvarez Pontoriero, Orlando Zaffarana, Claudia Beatriz Gimenez, Mario Ernesto Ruiz, Francisco Folguera Telichevsky, Andres |
author_facet |
Orts, Darío Leandro Alvarez Pontoriero, Orlando Zaffarana, Claudia Beatriz Gimenez, Mario Ernesto Ruiz, Francisco Folguera Telichevsky, Andres |
author_sort |
Orts, Darío Leandro |
title |
Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones |
title_short |
Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones |
title_full |
Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones |
title_fullStr |
Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones |
title_full_unstemmed |
Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones |
title_sort |
tectonic segmentation across patagonia controlled by the subduction of oceanic fracture zones |
publisher |
Pergamon-Elsevier Science Ltd |
url |
http://hdl.handle.net/11336/147021 |
long_lat |
ENVELOPE(-64.483,-64.483,-65.633,-65.633) |
geographic |
Patagonia Argentina Alvarez |
geographic_facet |
Patagonia Argentina Alvarez |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jog.2020.101806 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0264370720301484?via%3Dihub http://hdl.handle.net/11336/147021 Orts, Darío Leandro; Alvarez Pontoriero, Orlando; Zaffarana, Claudia Beatriz; Gimenez, Mario Ernesto; Ruiz, Francisco; et al.; Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones; Pergamon-Elsevier Science Ltd; Journal of Geodynamics; 143; 101806; 12-2020; 1-49 0264-3707 CONICET Digital CONICET |
op_rights |
info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
op_doi |
https://doi.org/10.1016/j.jog.2020.101806 |
container_title |
Journal of Geodynamics |
container_volume |
143 |
container_start_page |
101806 |
_version_ |
1779313443782787072 |