Reply to comments on “Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies: implications for deep subduction zone processes”

By Spandler Carl   Hermann Jörg   Arculus Richard   Mavrogenes John  

Contributions to Mineralogy and Petrology, Vol. 148, Iss. 4, 2004-12 ,pp. : 506-509

Springer Publishing Company

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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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Coupling of oceanic and continental crust during Eocene eclogite-facies metamorphism: evidence from the Monte Rosa nappe, western Alps

By Lapen Thomas   Johnson Clark   Baumgartner Lukas   Piaz Giorgio   Skora Susanne   Beard Brian  

Contributions to Mineralogy and Petrology, Vol. 153, Iss. 2, 2007-02 ,pp. : 139-157

Springer Publishing Company

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Petrology and geochemistry of primitive lower oceanic crust from Pito Deep: implications for the accretion of the lower crust at the Southern East Pacific Rise

By Perk Neil   Coogan Laurence   Karson Jeffrey   Klein Emily   Hanna Heather  

Contributions to Mineralogy and Petrology, Vol. 154, Iss. 5, 2007-11 ,pp. : 575-590

Springer Publishing Company

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Fluids in a 2 Ga old subduction zone – deduced from eclogite-facies rocks of the Usagaran belt, Tanzania

By Herms Petra  

European Journal of Mineralogy, Vol. 14, Iss. 2, 2002-04 ,pp. : 361-373

E. Schweizerbart'sche Verlagsbuchhandlung

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