Zr-in-rutile resetting in aluminosilicate bearing ultra-high temperature granulites: Refining the record of cooling and hydration in the Napier Complex, Antarctica
Peak ultra-high temperatures (UHT) > 1100 °C at 11–14 kbar in the Napier Complex. Post-peak evolution dominated by cooling and minor decompression to 850 °C, 11 kbar. Petrographic record of hydrous fluid–rock interaction during cooling below ~ 820 °C. Widespread Zr-in-rutile resetting throughout post-peak Napier Complex cooling. Valid Zr-in-rutile records of UHT conditions require zircon reintegration.