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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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2014-10-01
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| Series: | Geochemistry, Geophysics, Geosystems |
| Subjects: | |
| Online Access: | https://doi.org/10.1002/2014GC005441 |
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