Iron isotopic evidence for convective resurfacing of recycled arc-front mantle beneath back-arc basins
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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|Source:||Geophysical Research Letters|
|01_Nebel_Iron_isotopic_evidence_for_2013.pdf||1.19 MB||Adobe PDF||Request a copy|
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