Anhydrite cementation and compaction in geothermal reservoirs: Interaction of pore-space structure with flow, transport, P–T conditions, and chemical reactions
- 27 June 2005
- journal article
- Published by Elsevier BV in International Journal of Rock Mechanics and Mining Sciences
- Vol. 42 (7-8), 1056-1069
- https://doi.org/10.1016/j.ijrmms.2005.05.007
Abstract
No abstract availableThis publication has 13 references indexed in Scilit:
- Fractal Geometry of Surface Areas of Sand Grains Probed by Pulsed Field Gradient NMRPhysical Review Letters, 2002
- Variation of Permeability with Porosity in Sandstone Diagenesis Interpreted with a Fractal Pore Space ModelPure and Applied Geophysics, 2000
- Permeability prediction based on fractal pore‐space geometryGeophysics, 1999
- Laboratory measurement of compaction-induced permeability change in porous rocks: Implications for the generation and maintenance of pore pressure excess in the crustPure and Applied Geophysics, 1994
- Diffusion propagator as a probe of the structure of porous mediaPhysical Review Letters, 1992
- Interlayer conductivity of rocks — a fractal model of interface irregularities for calculating interlayer conductivity of natural porous mineral systemsColloids and Surfaces, 1987
- Theory of self‐similar network structures in sedimentary and igneous rocks and their investigation with microscopical and physical methodsJournal of Microscopy, 1987
- Hydraulic and acoustic properties as a function of porosity in Fontainebleau SandstoneJournal of Geophysical Research, 1985
- EXPERIMENTELLE METHODEN UND EINE APPARATUR ZUR UNTERSUCHUNG DER BEZIEHUNGEN ZWISCHEN HYDRAU-LISCHEN UND ELEKTRISCHEN EIGENSCHAFTEN LOSER UND KUNSTLICH VERFESTIGTER POROSER MEDIEN *Geophysical Prospecting, 1967
- Some physical aspects of water flow in porous mediaDiscussions of the Faraday Society, 1948