Dimensional Fabric and Ice Flow, Precambrian (Huronian) Glaciation
- 9 February 1962
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 135 (3502) , 442
- https://doi.org/10.1126/science.135.3502.442
Abstract
The Huronian Cobalt tillite (Gowganda formation) exhibits a preferred dimensional orientation of embedded elongate rock fragments. The orientation is believed to be due to ice motion. Data from four localities show an alignment in about a north-south direction. Data are inadequate to locate center of ice dispersal.Keywords
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