Complex P-T-t-d history of supracrustal rocks of the Metamorphic Internal zone of the southern Wopmay Orogen, NT
An abundance of Paleoproterozoic orogenic belts are distributed globally, as peripheral terranes accreted against the margins of Archean cratons. The abundance of these terranes indicates a period of tectonic activity between 2.1 and 1.8 Ga. The study of such belts has offered insight into the natur...
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| Language: | English |
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University of British Columbia
2015
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| Online Access: | http://hdl.handle.net/2429/52715 |