Metamorphic evolution of the Bunger Hills, East Antarctica: evidence for substantial post‐metamorphic peak compression with minimal cooling in a Proterozoic orogenic event

ABSTRACT The Bunger Hills, East Antarctica, experienced a low‐pressure granulite facies orogenic event during the Proterozoic. The stable coexistence of the S1 foliation‐parallel M1 assemblages, garnet‐cordierite‐spinel‐ilmenite and garnet‐sillimanite‐spinel‐ilmenite‐rutile, in quartz‐bearing peliti...

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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.tb00608.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1989.tb00608.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1989.tb00608.x