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Iron isotopic evidence for convective resurfacing of recycled arc-front mantle beneath back-arc basins

Nebel, Oliver; Arculus, Richard; Sossi, Paolo; Jenner, Frances; Whan, Tarun

Description

Geophysical observations suggest sub-arc convective flow transports melt-exhausted and metasomatized wedge mantle into deeper mantle regions. Reciprocally, asthenospheric, fertile mantle may supply back-arc ridges distal to the trench by shallow, lateral

CollectionsANU Research Publications
Date published: 2013
Type: Journal article
URI: http://hdl.handle.net/1885/75905
Source: Geophysical Research Letters
DOI: 10.1002/2013GL057976

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