Partitioning of Fe and Mn between ilmenite and olivine at 1100 °C: constraints on the thermodynamic mixing properties of (Fe, Mn)TiO 3 ilmenite solid solutions
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s004100050452.pdf
Cited by 7 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. The responses of the four main substitution mechanisms of H in olivine to H2O activity at 1050 °C and 3 GPa;Progress in Earth and Planetary Science;2017-05-09
2. The effect of Mn on mineral stability in metapelites revisited: new a -x relations for manganese-bearing minerals;Journal of Metamorphic Geology;2014-07-25
3. The effect of sulfur on the partitioning of Ni and other first-row transition elements between olivine and silicate melt;Geochimica et Cosmochimica Acta;2010-11
4. The partitioning of trace elements between ilmenite, ulvospinel, armalcolite and silicate melts with implications for the early differentiation of the moon;Chemical Geology;2006-11
5. Critical thermodynamic evaluation and optimization of the MnO–SiO2–“ TiO2 ”–“ Ti2O3 ” system;Calphad;2006-09
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