Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melt: Substitution mechanisms and the effect of iron

Contributions to Mineralogy and Petrology

Volumn 159, Issue 4, 2010, Pages 459-473

  van Kan Parker, Mirjam ^a   Liebscher, Axel ^b,c   Frei, Dirk ^c,d   van Sijl, Jelle ^a   van Westrenen, Wim ^a   Blundy, Jon ^e   Franz, Gerhard ^b  

^a VU UNIVERSITY AMSTERDAM   (Netherlands)

^b TECHNISCHE UNIVERSITÄT BERLIN   (Germany)

^c GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^d GEOLOGICAL SURVEY OF DENMARK AND GREENLAND   (Denmark)

^e UNIVERSITY OF BRISTOL   (United Kingdom)

Author keywords

Computer simulations; Experimental determination; Orthopyroxene; Partition coefficient; Substitution mechanisms

Indexed keywords

AIR TEMPERATURE; ATMOSPHERIC PRESSURE; COMPUTER SIMULATION; ENSTATITE; EXPERIMENTAL STUDY; IRON; MAGMATIC DIFFERENTIATION; ORTHOPYROXENE; PARTITION COEFFICIENT; PARTITIONING; SILICATE MELT; TRACE ELEMENT; YOUNG MODULUS;

EID: 77952240740     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-009-0435-0     Document Type: Article

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