Three‐dimensional flow in the subslab mantle

Abstract Three‐dimensional models of mantle flow at subduction zones make it possible to explain the common occurrence of trench‐parallel subslab seismic anisotropy. Subslab flow becomes inherently three‐dimensional when slab‐driven flow interacts with a wide variety of ambient background mantle flo...

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Bibliographic Details
Main Authors: Karen Paczkowski, Laurent G. J. Montési, Maureen D. Long, Christopher J. Thissen
Format: Article
Language:English
Published: Wiley 2014-10-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1002/2014GC005441
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