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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Bibliographic Details
Published inEarth and planetary science letters Vol. 401; pp. 227 - 235
Main Authors Rodríguez-González, Juan, Billen, Magali I., Negredo, Ana M.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.09.2014
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