Low‐pressure granulite facies metamorphism in the Larsemann Hills area, East Antarctica; petrology and tectonic implications for the evolution of the Prydz Bay area

• Published in: Journal of Metamorphic Geology
• Main Authors: STÜWE, K., POWELL, R.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1989
• Subjects: Collerson; East Antarctica; Kerr; Landing Bluff; Larsemann Hills; Munro Kerr Mountains; Prydz Bay; Rauer Group; Vestfold; Vestfold Hills; Antarc*; Antarctica
• Online Access: http://dx.doi.org/10.1111/j.1525-1314.1989.tb00609.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1989.tb00609.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1989.tb00609.x

ABSTRACT Thermobarometric studies on various granulite facies areas along the Prydz Bay coast, East Antarctica (73°‐79°E, 68°‐70°S), show that, at around 1100 Ma, during a late Proterozoic orogeny, the rocks of the Larsemann Hills suffered a lower pressure metamorphic peak than the surrounding areas. Along the Prydz Bay coast, the rocks affected by this event include parts of the Vestfold Hills block plus all of the Rauer Group, the Larsemann Hills and the Munro Kerr Mountains. The dykes in the south‐west corner of the Vestfold Hills were recrystallized during this event with little deformation at temperatures not quite as high as in the areas further south‐west (650°C, 6.5 kbar) (Collerson et al. , 1983), the Rauer Group was metamorphosed at 800°C and 7.5 kbar (Harley, 1987a), the Larsemann Hills at 750°C and 4.5 kbar, and the Munro Kerr Mountains probably at around 850°C and 5 kbar. Retrograde equilibration in the different areas occurred during decompression to about 10 km depth in all areas, followed by isobaric cooling at this depth. This paper shows that the peak metamorphism in the Larsemann Hills occurred at a pressure which is too low to have been the consequence of thermal relaxation of overthickened crust with normal mantle heat flow. Although other areas in Prydz Bay were metamorphosed at sufficiently high pressures so that their decompression paths are not inconsistent with a continental collision model, the inferred pre‐metamorphic peak histories and the requirement of consistency with the Larsemann Hills, make it unlikely that collision followed by erosion‐driven decompression is an appropriate model. We suggest that the thermal regime of the crust in the Larsemann Hills region was controlled by a perturbation in the asthenosphere, with magma invasion of the crust. We suggest that the 500 Ma event, represented in Prydz Bay by granitic outcrops at Landing Bluff and by several K/Ar ages from the Larsemann Hills area, was responsible for the final excavation of the terrane.