Experimentally-determined trace element characteristics of aqueous fluid from partially dehydrated mafic oceanic crust at 3.0 GPa, 650-700°C

By Green Trevor H.   Adam John  

European Journal of Mineralogy, Vol. 15, Iss. 5, 2003-10 ,pp. : 815-830

E. Schweizerbart'sche Verlagsbuchhandlung

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Decoupling of fluid and trace element release in subducting slab? Comment on “Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies; implications for deep subduction-zone processes” by C. Spandler et al. (Contrib Mineral Petrol 146:205–222, 2003)

By Liebscher Axel  

Contributions to Mineralogy and Petrology, Vol. 148, Iss. 4, 2004-12 ,pp. : 502-505

Springer Publishing Company

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Amphibole crystallization in the Etnean feeding system: mineral chemistry and trace element partitioning between Mg-hastingsite and alkali basaltic melt

By Viccaro Marco   Ferlito Carmelo   Cristofolini Renato  

European Journal of Mineralogy, Vol. 19, Iss. 4, 2007-08 ,pp. : 499-511

E. Schweizerbart'sche Verlagsbuchhandlung

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Experimental constraints on major and trace element partitioning during partial melting of eclogite

By Klemme S.   Blundy J.D.   Wood B.J.  

Geochimica et Cosmochimica Acta, Vol. 66, Iss. 17, 2002-09 ,pp. : 3109-3123

Elsevier

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Trace-element partitioning between garnet, clinopyroxene and Fe-rich picritic melts at 3 to 7 GPa

By Tuff J.   Gibson S.  

Contributions to Mineralogy and Petrology, Vol. 153, Iss. 4, 2007-04 ,pp. : 369-387

Springer Publishing Company

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