Seawater-derived rare earth element addition to abyssal peridotites during serpentinization

Serpentinized abyssal peridotites are evidence for active communication between the Earth's hydrosphere and the upper mantle, where exchange and retention of both major and trace elements occur. Bulk rock Nd isotopes in serpentinized abyssal peridotites imply interaction of seawater with the pe...

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Veröffentlicht in:	Lithos 2016-04, Vol.248-251, p.432-454
Hauptverfasser:	Frisby, Carl, Bizimis, Michael, Mallick, Soumen
Format:	Artikel
Sprache:	eng
Schlagworte:	Marine Nd-isotopes Negative Ce anomaly Rare earth elements Sequential leaching Serpentinization Sr-isotopes
Online-Zugang:	Volltext
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