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Li, Yuan, Audétat, Andreas (2012) Partitioning of V, Mn, Co, Ni, Cu, Zn, As, Mo, Ag, Sn, Sb, W, Au, Pb, and Bi between sulfide phases and hydrous basanite melt at upper mantle conditions. Earth and Planetary Science Letters, 355. 327-340 doi:10.1016/j.epsl.2012.08.008

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Reference TypeJournal (article/letter/editorial)
TitlePartitioning of V, Mn, Co, Ni, Cu, Zn, As, Mo, Ag, Sn, Sb, W, Au, Pb, and Bi between sulfide phases and hydrous basanite melt at upper mantle conditions
JournalEarth and Planetary Science Letters
AuthorsLi, YuanAuthor
Audétat, AndreasAuthor
Year2012 (November)Volume355
PublisherElsevier BV
DOIdoi:10.1016/j.epsl.2012.08.008Search in ResearchGate
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Mindat Ref. ID388228Long-form Identifiermindat:1:5:388228:7
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Full ReferenceLi, Yuan, Audétat, Andreas (2012) Partitioning of V, Mn, Co, Ni, Cu, Zn, As, Mo, Ag, Sn, Sb, W, Au, Pb, and Bi between sulfide phases and hydrous basanite melt at upper mantle conditions. Earth and Planetary Science Letters, 355. 327-340 doi:10.1016/j.epsl.2012.08.008
Plain TextLi, Yuan, Audétat, Andreas (2012) Partitioning of V, Mn, Co, Ni, Cu, Zn, As, Mo, Ag, Sn, Sb, W, Au, Pb, and Bi between sulfide phases and hydrous basanite melt at upper mantle conditions. Earth and Planetary Science Letters, 355. 327-340 doi:10.1016/j.epsl.2012.08.008
In(2012) Earth and Planetary Science Letters Vol. 355. Elsevier BV

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Li, Yuan, Audétat, Andreas (2015) Effects of temperature, silicate melt composition, and oxygen fugacity on the partitioning of V, Mn, Co, Ni, Cu, Zn, As, Mo, Ag, Sn, Sb, W, Au, Pb, and Bi between sulfide phases and silicate melt. Geochimica et Cosmochimica Acta, 162. 25-45 doi:10.1016/j.gca.2015.04.036
Righter, K., Pando, K.M., Danielson, L., Lee, Cin-Ty (2010) Partitioning of Mo, P and other siderophile elements (Cu, Ga, Sn, Ni, Co, Cr, Mn, V, and W) between metal and silicate melt as a function of temperature and silicate melt composition. Earth and Planetary Science Letters, 291 (1) 1-9 doi:10.1016/j.epsl.2009.12.018
Feng, Lu, Li, Yuan (2019) Comparative partitioning of Re and Mo between sulfide phases and silicate melt and implications for the behavior of Re during magmatic processes. Earth and Planetary Science Letters, 517. 14-25 doi:10.1016/j.epsl.2019.04.010
Li, Yuan, Audétat, Andreas (2013) Gold solubility and partitioning between sulfide liquid, monosulfide solid solution and hydrous mantle melts: Implications for the formation of Au-rich magmas and crust–mantle differentiation. Geochimica et Cosmochimica Acta, 118. 247-262 doi:10.1016/j.gca.2013.05.014
Li, Yuan (2014) Chalcophile element partitioning between sulfide phases and hydrous mantle melt: Applications to mantle melting and the formation of ore deposits. Journal of Asian Earth Sciences, 94. 77-93 doi:10.1016/j.jseaes.2014.08.009
Liu, Zhiwei, Li, Yuan (2025) The partitioning of selenium and tellurium between sulfide liquid and silicate melt and their abundances in the silicate Earth. Earth and Planetary Science Letters, 656. doi:10.1016/j.epsl.2025.119277
Li, Yuan, Audétat, Andreas, Liu, Zhiwei, Wang, Fangyue (2021) Chalcophile element partitioning between Cu-rich sulfide phases and silicate melt and implications for the formation of Earth’s continental crust. Geochimica et Cosmochimica Acta, 302. 61-82 doi:10.1016/j.gca.2021.03.020
Le Roux, V., Dasgupta, R., Lee, C.-T.A. (2011) Mineralogical heterogeneities in the Earth's mantle: Constraints from Mn, Co, Ni and Zn partitioning during partial melting. Earth and Planetary Science Letters, 307 (3) 395-408 doi:10.1016/j.epsl.2011.05.014
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Okamoto, Hiroaki (2018) Supplemental Literature Review of Binary Phase Diagrams: Ag-Ni, Ag-Zr, Au-Bi, B-Ni, Co-Sb, Cu-Mn, Cu-Si, Cu-Zn, Fe-Zr, Li-Sb, Mg-Pu, and Si-Zr. Journal of Phase Equilibria and Diffusion, 39 (1) 87-100 doi:10.1007/s11669-017-0610-3
Yakob, Jessica L., Feineman, Maureen D., Deane, James A., Eggler, David H., Penniston-Dorland, Sarah C. (2012) Lithium partitioning between olivine and diopside at upper mantle conditions: An experimental study. Earth and Planetary Science Letters, 329. 11-21 doi:10.1016/j.epsl.2012.01.035
 
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