Inelastic compaction, dilation and hysteresis of sandstones under hydrostatic conditions

Author:

Shalev Eyal1,Lyakhovsky Vladimir1,Ougier-Simonin Audrey2,Hamiel Yariv1,Zhu Wenlu2

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

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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