Second discussion by Hill (see also GeoScience Abstracts 2-311) of a paper by J.A. Chamberlain (GeoScience Abstracts 1-1377). Chamberlain has written a structural history [of this area of Saskatchewan] that omits consideration of certain faults showing movements on the order of 1,000 ft. as well as other features such as the concentric structures of Martin Lake, the Milliken Lake antiform, the intrusive(?) and nonintrusive (?) quartzites, etc.

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