Effect of melt composition on the partitioning of trace elements between titanite and silicate melt

By Stefan Prowatke, S. Klemme. 2003

267 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

GRENVILLE SKARN TITANITE: POTENTIAL REFERENCE MATERIAL FOR SIMS U–Th–Pb ANALYSIS (2010, background): “These levels of the REE are typical of what is observed for titanite from granites (Marks et al. 2008), and LREE/HREE > 1 would be predicted from partitioning studies of titanite (Prowatke & Klemme 2005).”
The key role of mica during igneous concentration of tantalum (2014, background): “…anatexis occurs at higher temperature at which micas are completely consumed, then the main hosts for Nb and Ta become Ti-bearing oxides (titanite, rutile and ilmenite), which all partition Ta relative to Nb (Nash and Crecraft 1985; Prowatke and Klemme 2005; Xiong et al. 2011; Olin and Wolff 2012).”
The partitioning of trace elements between ilmenite, ulvospinel, armalcolite and silicate melts with implications for the early differentiation of the moon (2006, result): “This is in good agreement with previous experimental results on HFSE partitioning between titanium-rich phases (rutile and titanite) and melts (Green and Pearson, 1987; Horng and Hess, 2000; Schmidt et al., 2004; Klemme et al., 2005; Prowatke and Klemme, 2005; Xiong et al., 2005), only Linnen and Ke”