Partitioning of elements between peridotite and H2O at 2.0-3.0 GPa and 900-1100°C, and application to models of subduction zone processes

Earth and Planetary Science Letters

Volumn 150, Issue 3-4, 1997, Pages 381-398

  Ayers, John C ^a   Dittmer, Sondra K ^a,c   Layne, Graham D ^b,d  

^a VANDERBILT UNIVERSITY   (United States)

^b UNIVERSITY OF NEW MEXICO   (United States)

^c Summit Risk Services Inc   (United States)

^d WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

Author keywords

Experimental studies; Fluid phase; Geochemistry; Partition coefficients; Peridotites; Subduction zones; Trace elements

Indexed keywords

IGNEOUS GEOCHEMISTRY; PARTITIONING; PERIDOTITE; SUBDUCTION; TRACE ELEMENT;

EID: 0031411443     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/s0012-821x(97)00096-4     Document Type: Article

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