Laboratory observations of the hydraulic behavior of a permeable fracture from 3800 m depth in the KTB pilot hole
- 10 August 1997
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 102 (B8) , 18405-18416
- https://doi.org/10.1029/96jb02813
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Applicability of the Reynolds Equation for modeling fluid flow between rough surfacesGeophysical Research Letters, 1995
- Fluid flow along potentially active faults in crystalline rockGeology, 1995
- Self‐propping and fluid flow in slightly offset joints at high effective pressuresJournal of Geophysical Research, 1994
- Effects of lithology and depth on the permeability of core samples from the Kola and KTB drill holesJournal of Geophysical Research, 1994
- Evidence from borehole samples for the role of accessory minerals in lower-crustal conductivityNature, 1994
- PEAK: a new kind of surface microscopeInternational Journal of Rock Mechanics and Mining Sciences, 1993
- Fluid flow through rock joints: The effect of surface roughnessJournal of Geophysical Research, 1987
- The Effect of Tortuosity on Fluid Flow Through a Single FractureWater Resources Research, 1984
- Diffusional crack healing in quartzJournal of Geophysical Research, 1984
- Permeability of crystalline and argillaceous rocksInternational Journal of Rock Mechanics and Mining Sciences, 1980