Glacitectonites in till stratigraphy
- 1 June 1977
- Vol. 6 (2) , 101-105
- https://doi.org/10.1111/j.1502-3885.1977.tb00339.x
Abstract
By analogy with hard rock myloniles it is suggested that the base of a glacial, litho‐structural, stratigraphical unit should he taken at the lower limit of penetrative structures in (soft) bedrock. Reference is made to mylonites in the NW Basal Gneiss Complex of South Norway and to the Marly Drift of Norfolk, England.Keywords
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