New constraints on the tectonometamorphic evolution of the Fisher Terrane, central Prince Charles Mountains, eastern Antarctica

This item is only available electronically. The Fisher Terrane, located in the central region of the Prince Charles Mountains, east Antarctica, evolved during the Mesoproterozoic as a magmatic arc system. Metapelitic schists from the Fisher Massif were deposited after 1206 ± 49 Ma and yield metamorp...

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Bibliographic Details
Main Author: Van Leeuwin, A. T. dV.
Other Authors: School of Physical Sciences
Format: Thesis
Language:English
Published: 2017
Subjects:
Online Access:http://hdl.handle.net/2440/128283