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

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...

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Bibliographic Details
Published in:Journal of Metamorphic Geology
Main Authors: STÜWE, K., POWELL, R.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1989
Subjects:
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