Thermo-tectonic history of the Kisseynew Domain near Sandy Narrows, Saskatchewan
The Sandy Narrows study area is comprised of mainly 1.86-1.84 Ga Kisseynew Domain marine metaturbidite rocks which represent the uppermost stratigraphic level in the Reindeer Zone. Based on mineralogical changes from west to east, isograds delineating metamorphic and compositional zones are recogniz...
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| Format: | Others |
| Language: | en |
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University of Saskatchewan
2010
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| Online Access: | http://library.usask.ca/theses/available/etd-06292010-093018/ |