Experimental study of trace element distribution between calcite, fluorite and carbonatitic melt in the system CaCO3 + CaF2 + Na2CO3 ± Ca3(PO4)2 at 100 MPa
Author:
Funder
Institute of geology and mineralogy SB RAS
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s00410-018-1530-x/fulltext.html
Reference52 articles.
1. Blundy J, Dalton J (2000) Experimental comparison of trace element partitioning between clinopyroxene and melt in carbonate and silicate systems, and implications for mantle metasomatism. Contrib Mineral Petrol 139:356–371
2. Brey GP, Bulatov VK, Girnis AV, Lahaye Y (2008) Experimental melting of carbonated peridotite at 6–10 GPa. J Petrol 49:797–821
3. Brey GP, Bulatov VK, Girnis AV (2011) Melting of K-rich carbonated peridotite at 6–10 GPa and the stability of K-phases in the upper mantle. Chem Geol 281:333–342. https://doi.org/10.1016/j.chemgeo.2010.12.019
4. Broom-Fendley S, Brady AE, Wall F, Gunn G, Dawes W (2017) REE minerals at the Songwe Hill carbonatite, Malawi: HREE-enrichment in late-stage apatite. Ore Geol Rev 81:23–41
5. Chakhmouradian AR, Reguir EP, Couëslan C et al (2016) Calcite and dolomite in intrusive carbonatites. II. Trace-element variations. Minerol Petrol 110:361–377. https://doi.org/10.1007/s00710-015-0392-4
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