Granulites and garnet–cordierite gneisses from Dronning Maud Land, Antarctica

• Published in: Journal of Metamorphic Geology
• Main Authors: BUCHER‐NURMINEN, K., OHTA, Y.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1993
• Subjects: Antarc*; Antarctic; Antarctica; Dronning Maud Land
• Online Access: http://dx.doi.org/10.1111/j.1525-1314.1993.tb00181.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1993.tb00181.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1993.tb00181.x

Abstract The central sector of Mühlig‐Hofmannfjellet (3°E/71°S) in western Dronning Maud Land (East Antarctic shield) is dominated by large intrusive bodies of predominantly orthopyroxene‐bearing quartz syenites (charnockites). Metasedimentary rocks are rare; however, two distinct areas with banded gneiss–marble–quartzite sequences of sedimentary origin were found during the Norwegian Antarctic Research Expedition NARE 1989/90. Cordierite‐bearing metapelitic gneisses from two different localities contain the characteristic mineral assemblage: cordierite + garnet + biotite + K‐feldspar + plagioclase + quartz ± sillimanite ± spinel. Thermobarometry indicates equilibration conditions of about 650°C and 4 kbar. Associated orthopyroxene–garnet granulites, on the other hand, revealed pressures of about 8 kbar and temperatures of 750°C. The earlier granulite facies metamorphism is not well preserved in the cordierite gneisses as a result of excess K‐feldspar combined with interaction with an H 2 O‐rich fluid phase, probably released by the cooling intrusives. These two features allowed the original high‐grade K‐feldspar + garnet assemblages to recrystallize as cordierite–biotite–sillimanite gneisses, completely re‐equilibrating them. Phase relationships indicate that the younger metamorphic event occurred in the presence of a fluid phase that varied in composition between the lithologies.