Non-steady-state subduction and trench-parallel flow induced by overriding plate structure
The direction of plate tectonic motion and the direction of mantle flow, as inferred from observations of seismic anisotropy measurements, show a good global correlation far from subduction zones. However, this correlation is poor near subduction zones, where below the slab seismic anisotropy is ali...
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Published in | Earth and planetary science letters Vol. 401; pp. 227 - 235 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.09.2014
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Subjects | |
Online Access | Get full text |
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