Inelastic compaction, dilation and hysteresis of sandstones under hydrostatic conditions
Author:
Affiliation:
1. Geological Survey of Israel, 30 Malkhe Israel Street, Jerusalem 95501, Israel. E-mail: eyal@gsi.gov.il
2. Department of Geology, University of Maryland, 237 Regents Drive, College Park, MD 20742, USA
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/197/2/920/27641046/ggu052.pdf
Reference33 articles.
1. Density, porosity, and compaction of sedimentary rocks;Athy;Am. Assoc. Pet. Geol. Bull.,1930
2. Compaction curves;Baldwin;Am. Assoc. Petrol. Geol. Bull.,1985
3. Fundamental observations concerning hysteresis in the deformation of rock with applications to nonlinear attenuation in the near source region;Boitnott,1993
4. Experimental characterization of the nonlinear rheology of rock;Boitnott;Int. J. Rock Mech. & Min. Sci.,1997
5. Linear and nonlinear modulus surfaces in stress space, from stress-strain measurements on Berea sandstone;Boudjema;Nonlinear Process. Geophys.,2003
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