Petrography, microprobe analyses and isotope composition of ultramafic rock from the northern Haskard Highlands, Shackleton Range, East Antarctica

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 ultramafic r...

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Bibliographic Details
Main Authors: Romer, T, Mezger, Klaus, Schmädicke, Esther
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.849763
https://doi.org/10.1594/PANGAEA.849763