Abstract
Detailed methodology, and supplemental figures and tables.<br>
Highlights
Phlogopite mineral separates were prepared using ~10 g of rock fragments per sample
Oxygen isotopes were measured following the analytical protocol described in Bindeman et al (2014)
Taking the same amount of contamination from Harris et al (2005) and the Δ'17O values from Bindeman et al (2018), our calculation shows that it would produce magmatic Δ'17O maximizing at −0.063‰, which is lower than all but one of the Upper Group 2 (UG2) values
Summary
Phlogopite mineral separates were prepared using ~10 g of rock fragments per sample. Oxygen isotopes were measured following the analytical protocol described in Bindeman et al (2014).
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