Trace-element partitioning in perovskite: Implications for the geochemistry of kimberlites and other mantle-derived undersaturated rocks

Chemical Geology

Volumn 353, Issue , 2013, Pages 112-131

  Chakhmouradian, Anton R ^a   Reguir, Ekaterina P ^a   Kamenetsky, Vadim S ^b   Sharygin, Victor V ^c   Golovin, Alexander V ^c  

^a UNIVERSITY OF MANITOBA   (Canada)

^b UNIVERSITY OF TASMANIA   (Australia)

^c SOBOLEV INSTITUTE OF GEOLOGY AND MINERALOGY   (Russian Federation)

Author keywords

Crystal fractionation; Element partitioning; Katungite; Kimberlite; Magma evolution; Perovskite

Indexed keywords

CRYSTAL FRACTIONATION; ELEMENT PARTITIONING; KATUNGITE; KIMBERLITE; MAGMA EVOLUTION;

HAFNIUM; LEAD; MINERALS; OLIVINE; PEROVSKITE; TITANIUM; TRACE ELEMENTS; URANIUM; ZONING;

VOLCANIC ROCKS;

EMPLACEMENT; FRACTIONATION; GEOCHEMISTRY; KIMBERLITE; MAGMA; MANTLE STRUCTURE; PARTITION COEFFICIENT; PEROVSKITE; PLUTONIC ROCK; RARE EARTH ELEMENT; TRACE ELEMENT;

CALIFORNIA; COLORADO; IRON MOUNTAIN; RUSSIAN FEDERATION; UGANDA; UNITED STATES; WYOMING;

EID: 84883653189     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2013.01.007     Document Type: Article

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