The Petrogenesis of the East Tasmania Terrane Devonian Granites. Appendix 5.5 WR δ18O calculated from δ18Ozir and δ18Oqz
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The estimation of late plutonic crustal assimilation was calculated by comparing estimated whole rock δ18O values from measured zircon and quartz mineral δ18O values. Calculations of whole rock δ18O at 650, 750, and 900 Celsius using measured zircon δ18O concentrations and at 470 Celsius using measured δ18O quartz concentrations are presented in this appendix.
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University of Tasmania, Australia
