Roughness and mismatch of fracture surfaces (walls) are key hydromechanical rock properties that influence (or control) how the rock masses slide and the ways in which fluids permeate the structure. Fracture roughness has been studied for decades from outcrop fractures and experimental analogues because it is difficult to detect and describe roughness of reservoir rock fractures in the deep subsurface. Here, we present new insights about roughness and wall mismatch of opening-mode fractures (hereinafter fractures) in deep carbonate reservoir rocks using a combination of new measuring techniques. The fractures are described from core and modern electrical borehole imaging data that were obtained from extended-reach drilling into the Arab oil...
Fluid flow through a single fracture is traditionally described by the cubic law, which is derived f...
Fluid flow in carbonate reservoirs is largely controlled by multiscale fracture networks. Significan...
The work tackles the control exerted by a sub-seismic fracture network on both secondary porosity an...
Roughness and mismatch of fracture surfaces (walls) are key hydromechanical rock properties that inf...
Several methods exist for collecting data about opening-mode fractures (hereinafter fractures) in su...
Fractures can profoundly affect the capacity of carbonate reservoirs to store and permeate fluids, d...
textOpen and connected fractures, where present, control fluid flow and dominate solute transport. ...
A large scientific interest has risen in the last decade on the characterization of carbonates’ mech...
Fluid flow through natural rock fractures is an important - and often dominant - factor in many aqui...
Heterogeneous fracture aperture distribution, dictated by surface roughness, mechanical rock and fra...
Low-permeability geological seals may be compromised by the occurrence of fluid-conductive fault and...
Fractures are ubiquitous in geological sequences, and play an important role in the movement of flui...
This thesis investigates the impact of low permeability faults on fluid flow in carbonate reservoirs...
Heterogeneous fracture aperture distribution, dictated by surface roughness, mechanical rock and fra...
Reservoir quality in tight fractured carbonate rocks is controlled by the fracture properties, the t...
Fluid flow through a single fracture is traditionally described by the cubic law, which is derived f...
Fluid flow in carbonate reservoirs is largely controlled by multiscale fracture networks. Significan...
The work tackles the control exerted by a sub-seismic fracture network on both secondary porosity an...
Roughness and mismatch of fracture surfaces (walls) are key hydromechanical rock properties that inf...
Several methods exist for collecting data about opening-mode fractures (hereinafter fractures) in su...
Fractures can profoundly affect the capacity of carbonate reservoirs to store and permeate fluids, d...
textOpen and connected fractures, where present, control fluid flow and dominate solute transport. ...
A large scientific interest has risen in the last decade on the characterization of carbonates’ mech...
Fluid flow through natural rock fractures is an important - and often dominant - factor in many aqui...
Heterogeneous fracture aperture distribution, dictated by surface roughness, mechanical rock and fra...
Low-permeability geological seals may be compromised by the occurrence of fluid-conductive fault and...
Fractures are ubiquitous in geological sequences, and play an important role in the movement of flui...
This thesis investigates the impact of low permeability faults on fluid flow in carbonate reservoirs...
Heterogeneous fracture aperture distribution, dictated by surface roughness, mechanical rock and fra...
Reservoir quality in tight fractured carbonate rocks is controlled by the fracture properties, the t...
Fluid flow through a single fracture is traditionally described by the cubic law, which is derived f...
Fluid flow in carbonate reservoirs is largely controlled by multiscale fracture networks. Significan...
The work tackles the control exerted by a sub-seismic fracture network on both secondary porosity an...