Forekomster av tillitt på nordsiden av Atnsjøvinduet, Syd-Norge.
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A previously reported tillite-like conglomerate occurring on the northern side of the Atnsjø Window rests with an erosional contact on Precambrian granite and gabbro and is overthrust by fieldspathic metasandstones of the Rondane Nappe. The conglomerate is matrix-supported and shows lateral variation in stone size and composition. It is analagous to the tillites occurring on the southeastern side of the Atnsjø Window and in the Snødøla, Spekedal and Tufsingdal Windows, and is correlative with the Late Precambrian Moelv Tillite of the Lake Mjøsa district.