Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
Abstract
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....
Paper Details
Title
Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
Published Date
Jul 13, 2017
Journal
Volume
44
Issue
13
Pages
6735 - 6742
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