Microstructural control of physical properties during deformation of porous limestone
We performed triaxial deformation experiments in Purbeck limestone (13.8% average porosity) across the brittle‐ductile transition and monitored the evolution of permeability and wave velocities as a function of strain. In the brittle regime, the rock yields in dilation. In the ductile regime, the ro...
| Päätekijät: | , , , |
|---|---|
| Aineistotyyppi: | Journal article |
| Julkaistu: |
Wiley-Blackwell Publishing, Inc.
2018
|