Trace element partitioning between clinopyroxene, magnetite, ilmenite and ferrobasaltic to dacitic magmas: an experimental study on the role of oxygen fugacity and melt composition
Author:
Funder
FWO
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00410-022-01957-y.pdf
Reference125 articles.
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2. Andersen DJ, Lindsley DH (1988) Internally consistent solution models for Fe-Mg-Mn-Ti oxides: Fe-Ti oxides. Am Min 73:714–726
3. Andersen DJ, Lindsley DH, Davidson PM (1993) QUILF: A pascal program to assess equilibria among FeMgMnTi oxides, pyroxenes, olivine, and quartz. Comput Geosci 19:1333–1350. https://doi.org/10.1016/0098-3004(93)90033-2
4. Anovitz LM, Treiman AH, Essene EJ et al (1985) The heat-capacity of ilmenite and phase equilibria in the system Fe-T-O. Geochim Cosmochim Acta 49:2027–2040. https://doi.org/10.1016/0016-7037(85)90061-4
5. Arató R, Audétat A (2017a) FeTiMM—a new oxybarometer for mafic to felsic magmas. Geochemical Perspect Lett 5:19–23. https://doi.org/10.7185/geochemlet.1740
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