WebbI am a Senior Geologist with experience gained in a variety of roles and geological settings including exploration, development, production and operations in clastic and carbonate … Webb15 juli 2012 · Our model is based on field measurements of variations in healed microfracture damage (FIPs) around fault zones, where permeability cannot be …
Figure 6 from The where and how of faults, fluids and permeability ...
Webb9 feb. 2024 · Further shear displacement resulted in a slight increase in permeability. A fault compaction is observed after shear relaxation which is associated to a … WebbFig. 4. Comparison of along-strike (2k) versus across-strike (2s) separation between mineralised stepovers and examples from well-constrained strikeslip fault data (Aydin & Schultz 1990; Kim et al. 2004). (A) 2k versus 2s demonstrating that mineralised stepovers investigated were all underlapping (positive R) in contrast to the majority of data … earthdog trials
Figure 4 from The where and how of faults, fluids and permeability ...
Webb1 dec. 2001 · Examination of the fault permeability dataset provides several pointers to the ways in which faults may affect single-phase fluid flow in the subsurface that prove to … Webb18 sep. 2024 · Fault displacement has no obvious control over fault rock permeability. The results enable better predictions of fault rock permeability in similar lithotypes and … WebbFig. 9. Time-integrated fluid flux derived from initial coseismic permeabilities of 10 12 m2 decaying to 10 18 m2 over time periods of 2, 5, 10, 20 and 30 years (N). For comparison, the field in grey is the range of flux values if coseismic permeabilities were 10 13 m2, illustrating the sensitivity of time-integrated fluid flux to transient coseismic … earthdomwiki