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...
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Online Access: | http://hdl.handle.net/10150/625357 https://doi.org/10.1002/2017GL074312 |
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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 |