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. 2018 Oct 1;376(2132):20180103. doi: 10.1098/rsta.2018.0103

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© 2018 The Authors.

Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.

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Figure 4. — Ba/Yb in igneous rocks, divided according to intrusion episodes, of the Yalgoo Dome illustrating the increase in LILE in transitional (tr) TTG. The increase is only visible for this rock suite, and is proposed to reflect the role of partial melting of plagioclase and/or mica. (Online version in colour.)