The influence of melt composition on the partitioning of trace elements between anorthite and silicate melt
Author:
Funder
Australian Government
Australian Research Council
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s00410-019-1548-8/fulltext.html
Reference37 articles.
1. Aigner-Torres M, Blundy J, Ulmer P, Pettke T (2007) Laser ablation ICPMS study of trace element partitioning between plagioclase and basaltic melts: an experimental approach. Contrib Mineral Petrol 153:647–667. https://doi.org/10.1007/s00410-006-0168-2
2. Bédard JH (2006) Trace element partitioning in plagioclase feldspar. Geochimica et Cosmochimica Acta 70:3717–3742. https://doi.org/10.1016/j.gca.2006.05.003
3. Berman RG (1983) A thermodynamic model for multicomponent melts, with application to the system CaO–MgO–Al2O3–SiO2. University of British Columbia
4. Berman RG, Brown TH (1984) A thermodynamic model for multicomponent melts, with application to the system CaO–Al2O3–SiO2. Geochimica et Cosmochimica Acta 48:661–678. https://doi.org/10.1016/0016-7037(84)90094-2
5. Bindeman IN, Davis AM (2000) Trace element partitioning between plagioclase and melt: investigation of dopant influence on partition behavior. Geochimica et Cosmochimica Acta 64:2863–2878
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