A study of the P-T-t-fluid evolution of the Glennie domain, Trans-Hudson Orogen
The Glennie domain of the Trans-Hudson Orogen (THO) is characterized by arcuate belts of Paleoproterozoic supracrustal rocks, including island arc volcanogenic assemblages, among variably deformed and metamorphosed granitoid rocks. Four discrete deformation events, termed D1 through D4, have been re...
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| Format: | Others |
| Language: | en |
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University of Saskatchewan
1997
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| Online Access: | http://library.usask.ca/theses/available/etd-10212004-000525 |