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

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Date

2013

Authors

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

Journal Title

Journal ISSN

Volume Title

Publisher

American Geophysical Union

Abstract

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

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Keywords

Citation

URI

http://hdl.handle.net/1885/75905

Collections

ANU Research Publications

Source

Geophysical Research Letters

Type

Journal article

Book Title

Entity type

Access Statement

Open Access

License Rights

DOI

10.1002/2013GL057976

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01_Nebel_Iron_isotopic_evidence_for_2013.pdf (1.16 MB)

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