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Erratum: Vesuvianite in high-pressure-metamorphosed oceanic lithosphere (Raspas Complex, Ecuador) and its role for transport of water and trace elements in subduction zones (European Journal of Mineralogy (2013) 25 (193-219) DOI: 10.1127/0935-1221/2013/0025-2281)
OtherAbstract:Palabras claves:Autores:Garbe-Schönberg D., Halama R., Savov I.P., Schenk V., Theofilos ToulkeridisFuentes:scopusPetrology of mafic lavas within the Onega plateau, central Karelia: evidence for 2.0 Ga plume-related continental crustal growth in the Baltic Shield
ArticleAbstract: The Onega plateau consistitues part of a vast continental flood basalt province in the SE Baltic ShiPalabras claves:Autores:Alfred Kron̈er, Arndt N.T., Garbe-Schönberg D., Haase K.M., Hofmann A.W., Kulikov V.S., Kulikova V.V., Nemchin A.A., Puchtel I.S.Fuentes:scopusVesuvianite in high-pressure-metamorphosed oceanic lithosphere (Raspas Complex, Ecuador) and its role for transport of water and trace elements in subduction zones
ArticleAbstract: Metamorphosed, vesuvianite-bearing dykes occur in serpentinised peridotites of the Raspas Complex (EPalabras claves:fluid-rock interaction, geochemistry, Oceanic lithosphere, Raspas complex, Serpentinite, Subduction, Trace elements, VesuvianiteAutores:Garbe-Schönberg D., Halama R., Savov I.P., Schenk V., Theofilos ToulkeridisFuentes:googlescopus