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Dygert, Nick, Liang, Yan, Hess, Paul (2013) The importance of melt TiO2 in affecting major and trace element partitioning between Fe–Ti oxides and lunar picritic glass melts. Geochimica et Cosmochimica Acta, 106. 134-151 doi:10.1016/j.gca.2012.12.005

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Reference TypeJournal (article/letter/editorial)
TitleThe importance of melt TiO2 in affecting major and trace element partitioning between Fe–Ti oxides and lunar picritic glass melts
JournalGeochimica et Cosmochimica Acta
AuthorsDygert, NickAuthor
Liang, YanAuthor
Hess, PaulAuthor
Year2013 (April)Volume106
PublisherElsevier BV
DOIdoi:10.1016/j.gca.2012.12.005Search in ResearchGate
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Mindat Ref. ID355224Long-form Identifiermindat:1:5:355224:1
GUID0
Full ReferenceDygert, Nick, Liang, Yan, Hess, Paul (2013) The importance of melt TiO2 in affecting major and trace element partitioning between Fe–Ti oxides and lunar picritic glass melts. Geochimica et Cosmochimica Acta, 106. 134-151 doi:10.1016/j.gca.2012.12.005
Plain TextDygert, Nick, Liang, Yan, Hess, Paul (2013) The importance of melt TiO2 in affecting major and trace element partitioning between Fe–Ti oxides and lunar picritic glass melts. Geochimica et Cosmochimica Acta, 106. 134-151 doi:10.1016/j.gca.2012.12.005
In(2013) Geochimica et Cosmochimica Acta Vol. 106. Elsevier BV

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Dygert, Nick, Liang, Yan, Sun, Chenguang, Hess, Paul (2014) An experimental study of trace element partitioning between augite and Fe-rich basalts. Geochimica et Cosmochimica Acta, 132. 170-186 doi:10.1016/j.gca.2014.01.042
Dygert, Nick, Liang, Yan, Sun, Chenguang, Hess, Paul (2015) Corrigendum to ‘An experimental study of trace element partitioning between augite and Fe-rich basalts’ [Geochim. Cosmochim. Acta 132 (2014) 170–186]. Geochimica et Cosmochimica Acta, 149. 281-283 doi:10.1016/j.gca.2014.09.013
Ji, Dian, Dygert, Nicholas (2024) Trace element partitioning between apatite and silicate melts: Effects of major element composition, temperature, and oxygen fugacity, and implications for the volatile element budget of the lunar magma ocean. Geochimica et Cosmochimica Acta, 369. 141-159 doi:10.1016/j.gca.2023.11.004
Sun, Chenguang, Graff, Michelle, Liang, Yan (2017) Trace element partitioning between plagioclase and silicate melt: The importance of temperature and plagioclase composition, with implications for terrestrial and lunar magmatism. Geochimica et Cosmochimica Acta, 206. 273-295 doi:10.1016/j.gca.2017.03.003
Dygert, N., Draper, D.S., Rapp, J.F., Lapen, T.J., Fagan, A.L., Neal, C.R. (2020) Experimental determinations of trace element partitioning between plagioclase, pigeonite, olivine, and lunar basaltic melts and an fO2 dependent model for plagioclase-melt Eu partitioning. Geochimica et Cosmochimica Acta, 279. 258-280 doi:10.1016/j.gca.2020.03.037
Thacker, Carla, Liang, Yan, Peng, Qinglan, Hess, Paul (2009) The stability and major element partitioning of ilmenite and armalcolite during lunar cumulate mantle overturn. Geochimica et Cosmochimica Acta, 73 (3) 820-836 doi:10.1016/j.gca.2008.10.038
Sun, Chenguang, Liang, Yan (2013) Distribution of REE and HFSE between low-Ca pyroxene and lunar picritic melts around multiple saturation points. Geochimica et Cosmochimica Acta, 119. 340-358 doi:10.1016/j.gca.2013.05.036
Liu, Xingcheng, Xiong, Xiaolin, Audétat, Andreas, Li, Yuan (2015) Partitioning of Cu between mafic minerals, Fe–Ti oxides and intermediate to felsic melts. Geochimica et Cosmochimica Acta, 151. 86-102 doi:10.1016/j.gca.2014.12.010
van Kan Parker, Mirjam, Mason, Paul R.D., van Westrenen, Wim (2011) Trace element partitioning between ilmenite, armalcolite and anhydrous silicate melt: Implications for the formation of lunar high-Ti mare basalts. Geochimica et Cosmochimica Acta, 75 (15) 4179-4193 doi:10.1016/j.gca.2011.04.031
Morgan, Zachary, Liang, Yan, Hess, Paul (2006) An experimental study of anorthosite dissolution in lunar picritic magmas: Implications for crustal assimilation processes. Geochimica et Cosmochimica Acta, 70 (13) 3477-3491 doi:10.1016/j.gca.2006.04.027
Prowatke, Stefan, Klemme, Stephan (2006) Trace element partitioning between apatite and silicate melts. Geochimica et Cosmochimica Acta, 70 (17) 4513-4527 doi:10.1016/j.gca.2006.06.162
 
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