Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/561
AuthorsCivello, S.* 
Margheriti, L.* 
TitleToroidal mantle flow around the Calabrian slab (Italy) from SKS splitting
Issue Date2004
Series/Report no.31/10(2004)
DOI10.1029/2004GL019607
URIhttp://hdl.handle.net/2122/561
KeywordsSKS splitting
Calabrian
Subject Classification04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous 
AbstractSKS-wave birefringence is likely caused by ongoing and/or fossil mantle flow. Splitting parameters in the southern Tyrrhenian subduction zone define a quite complex pattern of fast directions with large delay times up to 2.7 s. Fast directions are prevalently trench parallel below the slab and rotate to trench normal at the western edge of the slab depicting a ring around it. We interpret these anisotropic patterns, also observed in laboratory experiment, as toroidal mantle flow induced by rollback subduction.
Appears in Collections:Papers Published / Papers in press
Papers Published / Papers in press

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