Nunavut Tunngavik Inc., Nunavut

The Bathurst, Back River and Regan Lake areas are host to a number of Au in iron formation and VHMS showings.  I spent a summer in this area of Nunavut gathering data for a B.Sc. thesis in conjunction with Nunavut Tunngavik Incorporated.

The area at which I spent most of my time was in the Crazy Bear Metamorphic Complex.  Most of the rocks are sillimanite-grade metamorphosed wackes, argillites and iron formation intruded by late pegmatites and granitoids.  Au is located in silicate-facies iron formation overprinted by garnet, grunerite, pyrrhotite and chalcopyrite.

Bathurst Inlet area

Highly deformed iron formation in turbidites, Bathurst Inlet area

Geology of the Bathurst Inlet area, Thompson (1978)

Geological Consultant

Ronnie Therriault.  #32 Hwy. 595. Kakabeka Falls, ON. P.O. Box 256. P0T-1W0 Phone: (807) 766-9764; E-mail: rtherriault@geologistforhire.com

R. Therriault, M.Sc., P.Geo

Ronnie Therriault, M.Sc., P.Geo

#32 Hwy. 595 Kakabeka Falls, ON. P.O. Box 256. P0T-1W0

P: (807) 766-9764; E-mail: rtherriault@geologistforhire.com

 

 

 

 

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Pyrrhotite core showing liesegang banding, Bathurst Inlet area

F2/F3 fold nose in silicate facies iron formation, Bathurst Inlet area