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The relationship between foliation and strain: an experimental investigation: reply
Authors:B.E. Hobbs  W.D. Means  P.F. Williams
Affiliation:Department of Earth Sciences, Monash University, Clayton, Victoria 3168, Australia;Department of Geological Sciences, State University of New York at Albany, 1400 Washington Avenue, Albany, New York 12222, U.S.A.;Department of Geology, University of New Brunswick, Fredericton, New Brunswick E3B 5A3, Canada
Abstract:Contrary to the criticisms of our ideas by Treagus, we still believe that our experiments show that a secondary preferred orientation of micas or of small kink-like folds, closely resembling similar features in some cleaved rocks, can form at large angles to the λ1λ2 plane of strain, where the strain referred to is the strain coeval with development of these features.
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