Effects of induced stress on seismic forward modelling and inversion
Author:
Affiliation:
1. Department of Geosciences and Program in Applied & Computational Mathematics, Princeton University, Princeton, NJ, USA
2. Department of Earth Sciences, Utrecht University, P.O. Box 80115, 8305 TC Utrecht, The Netherlands
Funder
Seventh Framework Programme
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/213/2/851/24178480/ggy020.pdf
Reference34 articles.
1. On the parametrisation of equilibrium stress fields in the Earth;Al-Attar;Geophys. J. Int.,2010
2. The velocity of compressional waves in rocks to 10 kilobars: 2;Birch;J. geophys. Res.,1961
3. Comment on ‘Seismic velocities in dry and saturated cracked solids’ by Richard J. O’Connell and Bernard Budiansky;Bruner;J. geophys. Res.,1976
4. Elastic dislocation theory for a self-gravitating elastic configuration with an initial static stress field;Dahlen;Geophys. J. R. astr. Soc.,1972
5. Elastic velocity anisotropy in the presence of an anisotropic initial stress;Dahlen;Bull. seism. Soc. Am.,1972
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