Comparison of the natural deformation of the State-Line Serpentinite U.S.A., with experimental studies
Author:
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geophysics
Reference18 articles.
1. Orthogneiss, mylonite and non-coaxial deformation of granites: the example of the South Armorican shear zone;Berthe;J. Struct. Geol.,1979
2. Implications of the mechanical and frictional behavior of serpentinite to seismogenic faulting;Dengo;J. Geophys. Res.,1981
3. A model for the development of crenulations in shear zones with applications from the Southern Appalachian Piedmont;Dennis;J. Struct. Geol.,1987
4. Stability of chrysotile and antigorite in the serpentine multisystem;Evans;Schweiz. Mineral. Petrogr. Mitt.,1976
5. The serpentinite mass in Glen Urquhart, Inverness-Shire;Francis;Scotland. Am. J. Sci.,1956
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