Minor and trace element partitioning between pyroxene and melt in rapidly cooled chondrules

American Mineralogist

Volumn 82, Issue 5-6, 1997, Pages 534-545

  Jones, Rhian H ^a   Layne, Graham D ^a,b  

^a UNIVERSITY OF NEW MEXICO   (United States)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ALUMINA; ALUMINUM OXIDE; COOLING; CRYSTAL STRUCTURE; POSITIVE IONS; SILICATE MINERALS;

AL2O3 CONTENTS; APPARENT PARTITION COEFFICIENTS; CHARGE-BALANCED SUBSTITUTIONS; EQUILIBRIUM DATA; MINOR AND TRACE ELEMENTS; ORDINARY CHONDRITES; ORTHOENSTATITE; PARTITION COEFFICIENT;

TRACE ELEMENTS;

CHONDRITE; CHONDRULE; PYROXENE; SEMARKONA; TRACE ELEMENT PARTITIONING;

EID: 0030773695     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am-1997-5-613     Document Type: Article

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