Mantle flow through a tear in the Nazca slab inferred from shear wave splitting

A tear in the subducting Nazca slab is located between the end of the Pampean flat slab and normally subducting oceanic lithosphere. Tomographic studies suggest mantle material flows through this opening. The best way to probe this hypothesis is through observations of seismic anisotropy, such as sh...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Lynner, Colton, Anderson, Megan L., Portner, Daniel Evan, Beck, Susan, Gilbert, Hersh
Other Authors: Univ Arizona, Dept Geosci, Department of Geosciences; University of Arizona; Tucson Arizona USA, Department of Geology; Colorado College; Colorado Springs Colorado USA, Department of Geoscience; University of Calgary; Calgary Alberta Canada
Format: Article in Journal/Newspaper
Language:English
Published: AMER GEOPHYSICAL UNION 2017
Subjects:
Online Access:http://hdl.handle.net/10150/625357
https://doi.org/10.1002/2017GL074312
id ftunivarizona:oai:repository.arizona.edu:10150/625357
record_format openpolar
spelling ftunivarizona:oai:repository.arizona.edu:10150/625357 2023-05-15T18:19:10+02:00 Mantle flow through a tear in the Nazca slab inferred from shear wave splitting Lynner, Colton Anderson, Megan L. Portner, Daniel Evan Beck, Susan Gilbert, Hersh Univ Arizona, Dept Geosci Department of Geosciences; University of Arizona; Tucson Arizona USA Department of Geology; Colorado College; Colorado Springs Colorado USA Department of Geoscience; University of Calgary; Calgary Alberta Canada 2017-07-16 http://hdl.handle.net/10150/625357 https://doi.org/10.1002/2017GL074312 en eng AMER GEOPHYSICAL UNION http://doi.wiley.com/10.1002/2017GL074312 Mantle flow through a tear in the Nazca slab inferred from shear wave splitting 2017, 44 (13):6735 Geophysical Research Letters 00948276 doi:10.1002/2017GL074312 http://hdl.handle.net/10150/625357 Geophysical Research Letters ©2017. American Geophysical Union. All Rights Reserved. shear wave splitting flat slab slab tear mantle dynamics Article 2017 ftunivarizona https://doi.org/10.1002/2017GL074312 2020-06-14T08:15:49Z A tear in the subducting Nazca slab is located between the end of the Pampean flat slab and normally subducting oceanic lithosphere. Tomographic studies suggest mantle material flows through this opening. The best way to probe this hypothesis is through observations of seismic anisotropy, such as shear wave splitting. We examine patterns of shear wave splitting using data from two seismic deployments in Argentina that lay updip of the slab tear. We observe a simple pattern of plate-motion-parallel fast splitting directions, indicative of plate-motion-parallel mantle flow, beneath the majority of the stations. Our observed splitting contrasts previous observations to the north and south of the flat slab region. Since plate-motion-parallel splitting occurs only coincidentally with the slab tear, we propose mantle material flows through the opening resulting in Nazca plate-motion-parallel flow in both the subslab mantle and mantle wedge. NSF [EAR-0738935, EAR-0739001, EAR-1565475]; Colorado College Patricia Buster Scholarship Fund; National Science Foundation through the Seismological Facilities for the Advancement of Geoscience and EarthScope (SAGE) Proposal of the National Science Foundation [EAR-1261681] 6 month embargo; published online: 13 July 2017 This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. Article in Journal/Newspaper Seismological Facilities for the Advancement of Geoscience and EarthScope The University of Arizona: UA Campus Repository Argentina Geophysical Research Letters 44 13 6735 6742
institution Open Polar
collection The University of Arizona: UA Campus Repository
op_collection_id ftunivarizona
language English
topic shear wave splitting
flat slab
slab tear
mantle dynamics
spellingShingle shear wave splitting
flat slab
slab tear
mantle dynamics
Lynner, Colton
Anderson, Megan L.
Portner, Daniel Evan
Beck, Susan
Gilbert, Hersh
Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
topic_facet shear wave splitting
flat slab
slab tear
mantle dynamics
description A tear in the subducting Nazca slab is located between the end of the Pampean flat slab and normally subducting oceanic lithosphere. Tomographic studies suggest mantle material flows through this opening. The best way to probe this hypothesis is through observations of seismic anisotropy, such as shear wave splitting. We examine patterns of shear wave splitting using data from two seismic deployments in Argentina that lay updip of the slab tear. We observe a simple pattern of plate-motion-parallel fast splitting directions, indicative of plate-motion-parallel mantle flow, beneath the majority of the stations. Our observed splitting contrasts previous observations to the north and south of the flat slab region. Since plate-motion-parallel splitting occurs only coincidentally with the slab tear, we propose mantle material flows through the opening resulting in Nazca plate-motion-parallel flow in both the subslab mantle and mantle wedge. NSF [EAR-0738935, EAR-0739001, EAR-1565475]; Colorado College Patricia Buster Scholarship Fund; National Science Foundation through the Seismological Facilities for the Advancement of Geoscience and EarthScope (SAGE) Proposal of the National Science Foundation [EAR-1261681] 6 month embargo; published online: 13 July 2017 This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.
author2 Univ Arizona, Dept Geosci
Department of Geosciences; University of Arizona; Tucson Arizona USA
Department of Geology; Colorado College; Colorado Springs Colorado USA
Department of Geoscience; University of Calgary; Calgary Alberta Canada
format Article in Journal/Newspaper
author Lynner, Colton
Anderson, Megan L.
Portner, Daniel Evan
Beck, Susan
Gilbert, Hersh
author_facet Lynner, Colton
Anderson, Megan L.
Portner, Daniel Evan
Beck, Susan
Gilbert, Hersh
author_sort Lynner, Colton
title Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
title_short Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
title_full Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
title_fullStr Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
title_full_unstemmed Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
title_sort mantle flow through a tear in the nazca slab inferred from shear wave splitting
publisher AMER GEOPHYSICAL UNION
publishDate 2017
url http://hdl.handle.net/10150/625357
https://doi.org/10.1002/2017GL074312
geographic Argentina
geographic_facet Argentina
genre Seismological Facilities for the Advancement of Geoscience and EarthScope
genre_facet Seismological Facilities for the Advancement of Geoscience and EarthScope
op_relation http://doi.wiley.com/10.1002/2017GL074312
Mantle flow through a tear in the Nazca slab inferred from shear wave splitting 2017, 44 (13):6735 Geophysical Research Letters
00948276
doi:10.1002/2017GL074312
http://hdl.handle.net/10150/625357
Geophysical Research Letters
op_rights ©2017. American Geophysical Union. All Rights Reserved.
op_doi https://doi.org/10.1002/2017GL074312
container_title Geophysical Research Letters
container_volume 44
container_issue 13
container_start_page 6735
op_container_end_page 6742
_version_ 1766196123721007104