The oxidation state of europium in silicate melts as a function of oxygen fugacity, composition and temperature

Chemical Geology

Volumn 411, Issue , 2015, Pages 248-259

  Burnham, A D ^a,b   Berry, A J ^a,b,c   Halse, H R ^a,c,d   Schofield, P F ^c   Cibin, G ^d   Mosselmans, J F W ^d  

^a IMPERIAL COLLEGE LONDON   (United Kingdom)

^b AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^c DEPARTMENT OF LIFE SCIENCES   (United Kingdom)

^d DIAMOND LIGHT SOURCE LTD   (United Kingdom)

Author keywords

Eu Eu; In situ; MORB; Rare earth element; Redox; Silicate glass; XANES

Indexed keywords

GLASS; MAGNETITE; OXYGEN; RARE EARTH ELEMENTS; RARE EARTHS; SILICATES; X RAY ABSORPTION; X RAY ABSORPTION NEAR EDGE STRUCTURE SPECTROSCOPY;

EMPIRICAL EQUATIONS; IN-SITU MEASUREMENT; LOGARITHMIC UNITS; MORB; REDOX; SILICATE GLASS; X-RAY ABSORPTION NEAR-EDGE STRUCTURE; XANES;

EUROPIUM COMPOUNDS;

CHEMICAL COMPOSITION; EUROPIUM; FUGACITY; HIGH TEMPERATURE; IN SITU MEASUREMENT; MID-OCEAN RIDGE BASALT; OXIDATION; OXYGEN; REDOX CONDITIONS; SILICATE MELT; XANES SPECTROSCOPY;

EID: 84937597520     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2015.07.002     Document Type: Article

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