Evidence of Nonlinear Elasticity of the Crust from the Mw7.6 Manyi (Tibet) Earthquake
Author:
Affiliation:
1. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
2. Institut de Physique du Globe de Paris, France.
Abstract
Publisher
American Association for the Advancement of Science (AAAS)
Subject
Multidisciplinary
Reference56 articles.
1. Surface deformation due to shear and tensile faults in a half-space
2. See for example
3. Hudnut K. W. et al. 84 625 (1994);
4. ; J. Freymuller N. E. King P. Segall ibid. p. 646.
5. Many crustal rocks exhibit nonlinear elastic properties with a Young's modulus dependent on the confining pressure. Tests on laboratory samples showed that rocks such as sandstone marble limestone quartzite and granite have a Young's modulus in tension smaller than the Young's modulus in compression in a ratio ranging from 1/2 to 1/10 [J. C. Jaeger and N. G. Cook Fundamentals of Rocks Mechanics (Chapman & Hall London ed. 3 1979) chaps. 10 and 12;
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