Element partitioning during carbonated pelite melting at 8, 13 and 22GPa and the sediment signature in the EM mantle components

Earth and Planetary Science Letters

Volumn 327-328, Issue , 2012, Pages 84-96

  Grassi, Daniele ^a   Schmidt, Max W ^a   Günther, Detlef ^a  

^a ETH ZURICH   (Switzerland)

Author keywords

Carbonate melts; Carbonated pelites; Mantle metasomatism; Partitioning coefficients; Trace elements; Ultrapotassic magmatism

Indexed keywords

ABSOLUTE VALUES; CARBONATED PELITES; CARBONATED SEDIMENTS; CLINOPYROXENES; ELEMENT FRACTIONATION; ELEMENT PARTITIONING; INCOMPATIBLE ELEMENT; MAGMATISMS; MANTLE COMPONENT; MANTLE CONCENTRATIONS; MANTLE GEOTHERM; MANTLE METASOMATISM; OCEANIC CRUST; PARTITION COEFFICIENT; PARTITIONING COEFFICIENTS; SOURCE REGION; SUB-ARC; TRACE ELEMENT COMPOSITION; TRANSITION ZONES;

ANOXIC SEDIMENTS; BARIUM; GADOLINIUM; HAFNIUM; ISOTOPES; LANTHANUM; LEAD; LITHOLOGY; MELTING; MINERALOGY; MINERALS; PEROVSKITE; RUBIDIUM; SEDIMENTARY ROCKS; SEDIMENTOLOGY; STRONTIUM; STRUCTURAL GEOLOGY; TECTONICS; TRACE ELEMENTS; ZIRCONIUM;

CARBONATION;

CARBONATE; CLINOPYROXENE; ECLOGITE; FRACTIONATION; ISOTOPIC COMPOSITION; MAGMATISM; MELTING; METASOMATISM; OCEAN ISLAND BASALT; P-T CONDITIONS; PARTITION COEFFICIENT; PARTITIONING; PELITE; PRESSURE EFFECT; RARE EARTH ELEMENT;

EID: 84857673401     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.01.023     Document Type: Article

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