Pan‐African eclogite facies metamorphism of ultramafic rocks in the Shackleton Range, Antarctica

Abstract In the Shackleton Range of East Antarctica, garnet‐bearing ultramafic rocks occur as lenses in supracrustal high‐grade gneisses. In the presence of olivine, garnet is an unmistakable indicator of eclogite facies metamorphic conditions. The eclogite facies assemblages are only present in ult...

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Bibliographic Details
Published in:Journal of Metamorphic Geology
Main Authors: ROMER, T., MEZGER, K., SCHMÄDICKE, E.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1525-1314.2009.00820.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.2009.00820.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.2009.00820.x