Partitioning of Eu between augite and a highly spiked martian basalt composition as a function of oxygen fugacity (IW-1 to QFM): Determination of Eu2+/Eu3+ratios by XANES

American Mineralogist

Volumn 95, Issue 2-3, 2010, Pages 410-413

  Karner, J M ^a,e   Papike, J J ^a   Sutton, S R ^b,c   Burger, P V ^a   Shearer, C K ^a   Le, L ^d   Newville, M ^c   Choi, Y ^c  

^a UNIVERSITY OF NEW MEXICO   (United States)

^b UNIVERSITY OF CHICAGO   (United States)

^c UNIVERSITY OF CHICAGO   (United States)

^d JE23   (United States)

^e CASE WESTERN RESERVE UNIVERSITY   (United States)

Author keywords

Augite; Eu partitioning; XANES

Indexed keywords

BASALT; GLASS; OXYGEN;

AUGITE; D VALUES; DIRECT DETERMINATION; OXYGEN FUGACITY; VALENCE STATE; XANES;

SILICATE MINERALS;

AUGITE; BASALT; CRYSTALLIZATION; CRYSTALLOGRAPHY; FUGACITY; OXYGEN; PARTITIONING; PYROXENE; XANES SPECTROSCOPY;

EID: 77950204000     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2010.3394     Document Type: Article

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