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