Concentration of incompatible elements in oceanic mantle: Effect of melt/wall interaction in stagnant or failed melt conduits within peridotite

Primary hydrous and other minerals enriched with incompatible components were found in ocean-floor ultramafic-mafic plutonic rock suites recovered from two contrasting ridge systems, i.e., the East Pacific Rise (Hess Deep, equatorial Pacific), a typical fast-spreading system, and Mid-Cayman Trough,...

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Veröffentlicht in:	Geochimica et cosmochimica acta 1997-02, Vol.61 (3), p.671-675
Hauptverfasser:	Arai, Shoji, Matsukage, Kyoko, Isobe, Eiichi, Vysotskiy, Sergei
Format:	Artikel
Sprache:	eng
Schlagworte:	Marine
Online-Zugang:	Volltext
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