Comparison of Fry strain ellipse and AMS ellipsoid trends to tectonic fabric trends in very low-strain sandstone of the Appalachian fold–thrust belt

Author:

Burmeister K.C.,Harrison M.J.,Marshak S.,Ferré E.C.,Bannister R.A.,Kodama K.P.

Publisher

Elsevier BV

Subject

Geology

Reference59 articles.

1. Subtle stretching lineation revealed by magnetic fabric of Callovian–Oxfordian black shales (French Alps);Aubourg;Tectonophysics,1991

2. Magnetic fabric as a structural indicator of the deformation path within a fold–thrust structure; a test case from the Corbieres (NE Pyrenees, France);Averbuch;Journal of Structural Geology,1992

3. Using JavaScript to standardize digital photomicrographs for Fry strain analysis: Binnewater Sandstone, central Hudson Valley, New York;Bannister;Geological Society of America,2004

4. Magnetic susceptibility, petrofabrics and strain;Borradaile;Tectonophysics,1988

5. Correlation of strain with anisotropy of magnetic susceptibility (AMS);Borradaile;Pure and Applied Geophysics,1991

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