We investigated the frictional strength recovery (healing) and subsequent reactivation and slip-weakening behaviour of simulated fault gouges derived from key stratigraphic units in the seismogenic Groningen gas field (N.E. Netherlands). Direct-shear, Slide-Hold-Slide (SHS) experiments were performed at in-situ conditions of 100 °C, 40 MPa effective normal stress and 10-15 MPa pore fluid pressure (synthetic formation brine). Sheared gouges were allowed to heal for periods up to 100 days before subsequent re-shearing. The initial coefficient of (steady) sliding friction μ was highest in the Basal Zechstein caprock (μ=0.65±0.02) and Slochteren sandstone reservoir (μ=0.61±0.02) gouges, and the lowest in the Ten Boer claystone at the reservoir ...
We investigated the effects of long-term CO2-brine-rock interactions on the frictional and transport...
[1] We study the mechanisms of frictional strength recovery for tectonic faults with particular focu...
This paper experimentally explores the frictional sliding behavior of two simulated gouges: one, a s...
We investigated the frictional strength recovery (healing) and subsequent reactivation and slip-weak...
We investigated the frictional properties of simulated fault gouges derived from the main lithologie...
Since the 1990’s, Europe’s largest gas field, the Groningen field, N.E. Netherlands, has exhibited n...
Rock materials show dramatic dynamic weakening in large-displacement (m), high-velocity (~1 m/s) fri...
Despite the importance of hydromechanical effects in fault processes, not much is known about the in...
Rock materials show dramatic dynamic weakening in large-displacement (m), high-velocity (∼1 m/s) fri...
AbstractFault strength recovery (healing) following an earthquake is a key process in controlling th...
We investigated the rate-and-state frictional properties of simulated anhydrite-carbonate fault goug...
We report 21 frictional sliding experiments performed on simulated fault gouges prepared from shale-...
We report 21 frictional sliding experiments performed on simulated fault gouges prepared from shale-...
Slide-hold-slide friction experiments are reported on fault gouges of salt and salt-muscovite mixtur...
We investigated the effects of long-term CO2-brine-rock interactions on the frictional and transport...
[1] We study the mechanisms of frictional strength recovery for tectonic faults with particular focu...
This paper experimentally explores the frictional sliding behavior of two simulated gouges: one, a s...
We investigated the frictional strength recovery (healing) and subsequent reactivation and slip-weak...
We investigated the frictional properties of simulated fault gouges derived from the main lithologie...
Since the 1990’s, Europe’s largest gas field, the Groningen field, N.E. Netherlands, has exhibited n...
Rock materials show dramatic dynamic weakening in large-displacement (m), high-velocity (~1 m/s) fri...
Despite the importance of hydromechanical effects in fault processes, not much is known about the in...
Rock materials show dramatic dynamic weakening in large-displacement (m), high-velocity (∼1 m/s) fri...
AbstractFault strength recovery (healing) following an earthquake is a key process in controlling th...
We investigated the rate-and-state frictional properties of simulated anhydrite-carbonate fault goug...
We report 21 frictional sliding experiments performed on simulated fault gouges prepared from shale-...
We report 21 frictional sliding experiments performed on simulated fault gouges prepared from shale-...
Slide-hold-slide friction experiments are reported on fault gouges of salt and salt-muscovite mixtur...
We investigated the effects of long-term CO2-brine-rock interactions on the frictional and transport...
[1] We study the mechanisms of frictional strength recovery for tectonic faults with particular focu...
This paper experimentally explores the frictional sliding behavior of two simulated gouges: one, a s...