Osmium abundance and isotope variations in mafic Mexican volcanic rocks: Evidence for crustal contamination and constraints on the geochemical behavior of osmium during partial melting and fractional crystallization

Geochemistry, Geophysics, Geosystems

Volumn 2, Issue 3, 2001, Pages

  Lassiter, John C ^a,b   Luhr, James F ^c  

^a GEOPHYSICAL LABORATORY   (United States)

^b DEPARTMENT OF PALEOBIOLOGY   (United States)

^c MAX PLANCK INSTITUTE FOR CHEMISTRY   (Germany)

Author keywords

bulk partition coefficient; crustal contamination; Os isotopes; oxygen fugacity; sulfides

Indexed keywords

BASALT; ISOTOPES; SILICATE MINERALS; SILICATES; STRUCTURAL GEOLOGY; SULFUR COMPOUNDS; VOLCANIC ROCKS; VOLCANOES;

CRUSTAL CONTAMINATION; OS ISOTOPES; OXYGEN FUGACITY; PARTITION COEFFICIENT; SULFIDES;

OSMIUM;

EID: 82355179844     PISSN: None     EISSN: 15252027     Source Type: Journal    
DOI: 10.1029/2000GC000116     Document Type: Article

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