The impact of the Pan-African-aged tectonothermal event on high-grade rocks at Mount Brown, East Antarctica

• Published in: Antarctic Science
• Main Authors: Liu, Xiaochun, Fu, Bin, Li, Qiuli, Zhao, Yue, Liu, Jian, Chen, Hong
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2020
• Subjects: East Antarctica; Rayner; Mount Brown; Antarc*; Antarctic Science; Antarctica
• Online Access: http://dx.doi.org/10.1017/s0954102019000518; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102019000518

Abstract This study presents monazite and rutile U–Pb and hornblende and biotite 40 Ar/ 39 Ar geochronological data for high-grade rocks of the eastern Grenville-aged Rayner orogen at Mount Brown in order to analyse the extent and degree of Pan-African-aged reworking. Monazite from paragneiss yields U–Pb ages of 910 Ma for larger granular grains and 670–630 Ma for smaller globular beads around garnet porphyroblasts or hosted by symplectites. Rutile from leucogneiss yields U–Pb ages of 520–515 Ma. Hornblende and biotite from different rock types yield 40 Ar/ 39 Ar plateau ages of 744 and 520–505 Ma, respectively. Combining these results with published zircon U–Pb age data suggests that granulite facies metamorphism occurred at 910 Ma, with a local low-temperature fluid flow event at 670–630 Ma and thermal reworking at 520–505 Ma. The older age of 744 Ma may reflect cooling or partial resetting of the hornblende 40 Ar/ 39 Ar system, indicating that Pan-African-aged reworking did not exceed temperatures much higher than the hornblende Ar closure temperature. These data also suggest that the complete isotopic resetting of some minerals may occur without the growth of new mineral phases, providing an example of the style of reworking that is likely to occur in polymetamorphic terranes.