Experimental Rock Deformation under Micro-CT - Two New Apparatuses for Rock Physics

References

1. Lakes, R. S.
   (2009), Viscoelastic materials, Cambridge University Press, Cambridge; New York.
2. Tatone, B. S. A., and G.Grasselli
   (2014), Characterization of the effect of normal load on the discontinuity morphology in direct shear specimens using X-ray micro-CT, Acta Geotechnica, 10(1), 31–54
   [Google Scholar]
3. Tisato, N., G.Di Toro, N.De Rossi, M.Quaresimin, and T.Candela
   (2012), Experimental investigation of flash weakening in limestone, Journal of Structural Geology, 38, 183–199.
4. Tisato, N., and C.Madonna
   (2012), Attenuation at low seismic frequencies in partially saturated rocks: Measurements and description of a new apparatus, Journal of Applied Geophysics, 86, 44–53.
   [Google Scholar]
5. Tisato, N., and B.Quintal
   (2013), Measurements of seismic attenuation and transient fluid pressure in partially saturated Berea sandstone: evidence of fluid flow on the mesoscopic scale, Geophysical Journal International, 195(1), 342–351.
   [Google Scholar]
6. Tisato, N., B.Quintal, G.Grasselli, and Y.Podladchikov
   (2014a), Seismic Wave Attenuation in Fluid-Saturated Rock as Result of Gas Dissolution, in SEG-2014–0926, Society of Exploration Geophysicists, SEG.
   [Google Scholar]
7. Tisato, N., B.Quintal, S.Chapman, C.Madonna, S.Subramaniyan, M.Frehner, E. H.Saenger, and G.Grasselli
   (2014b), Seismic attenuation in partially saturated rocks: Recent advances and future directions, The Leading Edge, 33(6), 640–646.
   [Google Scholar]