Granitoid plutons in the Iskwasum Lake area, Manitoba: Part of the Flin Flon domain, Trans-Hudson orogen.
Granites of the Iskwasum Lake area, Manitoba occupy greater than 60% of the exposed precambrian bedrock, and include seven different intrusive bodies. They are important indicators of the processes occurring during 1.88-1.83 Ga, a period in the formation of the Flin Flon domain of the Trans-Hudson o...
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University of Ottawa (Canada)
2009
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| Online Access: | http://hdl.handle.net/10393/9899 http://dx.doi.org/10.20381/ruor-16561 |