Pages that link to "Item:Q44745"
From geokb
The following pages link to Nicholas (Nick) M Beeler (Q44745):
Displayed 50 items.
- Characterizing fault roughness—Are faults rougher at long or short wavelengths? (Q56287) (← links)
- Premonitory slip and tidal triggering of earthquakes (Q144859) (← links)
- Conversion of wet glass to melt at lower seismogenic zone conditions: Implications for pseudotachylyte creep (Q145662) (← links)
- Evolution of fluid transmissivity and strength recovery of shear fractures under hydrothermal conditions (Q146368) (← links)
- The instantaneous rate dependence in low temperature laboratory rock friction and rock deformation experiments (Q147049) (← links)
- Attempting to bridge the gap between laboratory and seismic estimates of fracture energy (Q148560) (← links)
- Earthquake source properties from pseudotachylite (Q153021) (← links)
- On the expected relationships among apparent stress, static stress drop, effective shear fracture energy, and efficiency (Q154153) (← links)
- Why earthquakes correlate weakly with the solid Earth tides: Effects of periodic stress on the rate and probability of earthquake occurrence (Q154277) (← links)
- Inferring fault rheology from low-frequency earthquakes on the San Andreas (Q155722) (← links)
- High-frequency imaging of elastic contrast and contact area with implications for naturally observed changes in fault properties (Q155806) (← links)
- Laboratory constraints on models of earthquake recurrence (Q155810) (← links)
- Direct measurement of asperity contact growth in quartz at hydrothermal conditions (Q155822) (← links)
- Slip-pulse rupture behavior on a 2 meter granite fault (Q155887) (← links)
- Effective stress, friction and deep crustal faulting (Q155909) (← links)
- Rock friction under variable normal stress (Q156188) (← links)
- Earthquake source properties from instrumented laboratory stick-slip (Q156321) (← links)
- A robust calibration technique for acoustic emission systems based on momentum transfer from a ball drop (Q234368) (← links)
- A simple stick-slip and creep-slip model for repeating earthquakes and its implication for microearthquakes at Parkfield (Q235410) (← links)
- Laboratory generated M -6 earthquakes (Q237221) (← links)
- Re‐estimated effects of deep episodic slip on the occurrence and probability of great earthquakes in Cascadia (Q244933) (← links)
- Laboratory observations of fault strength in response to changes in normal stress (Q245522) (← links)
- Observed source parameters for dynamic rupture with non-uniform initial stressand relatively high fracture energy (Q246063) (← links)
- The roles of time and displacement in velocity-dependent volumetric strain of fault zones (Q253796) (← links)
- On the depth extent of co-seismic rupture (Q255428) (← links)
- Strength recovery in quartzite is controlled by changes in friction in experiments at hydrothermal conditions up to 200°C (Q256890) (← links)
- The transition from frictional sliding to shear melting in laboratory stick-slip experiments (Q257423) (← links)
- Near-fault velocity spectra from laboratory failures and their relation to natural ground motion (Q263865) (← links)
- 32 - Rock failure and earthquakes (Q263929) (← links)
- Constitutive relationships and physical basis of fault strength due to flash heating (Q264420) (← links)
- On the scale-dependence of fault surface roughness (Q264956) (← links)
- Frictional behavior of large displacement experimental faults (Q265331) (← links)
- Stress drop with constant, scale independent seismic efficiency and overshoot (Q266698) (← links)
- Effect of thermal and mechanical processes on hydraulic transmissivity evolution (Q269749) (← links)
- Stress-induced, time-dependent fracture closure at hydrothermal conditions (Q273515) (← links)
- The evolution of rock friction is more sensitive to slip than elapsed time, even at near-zero slip rates (Q276667) (← links)
- Teleseismic waves reveal anisotropic poroelastic response of wastewater disposal reservoir (Q280975) (← links)
- Strength recovery and sealing under hydrothermal conditions (Q282877) (← links)
- Tidal triggering of low frequency earthquakes near Parkfield, California: Implications for fault mechanics within the brittle-ductile transition (Q285276) (← links)
- Direct evidence for fluid pressure, dilatancy, and compaction affecting slip in isolated faults (Q286920) (← links)
- Transient triggering of near and distant earthquakes (Q290766) (← links)
- Earthquake triggering by transient and static deformations (Q291804) (← links)
- Self-healing slip pulses in dynamic rupture models due to velocity-dependent strength (Q292001) (← links)
- Laboratory triggering of stick-slip events by oscillatory loading in the presence of pore fluid with implications for physics of tectonic tremor (Q292299) (← links)
- Implications of Coulomb plasticity for the velocity dependence of experimental faults (Q294064) (← links)
- Inferring earthquake source properties from laboratory observations and the scope of lab contributions to source physics (Q294441) (← links)
- Time-dependent weakening of granite at hydrothermal conditions (Q294600) (← links)
- Faulting within the Mount St. Helens conduit and implications for volcanic earthquakes (Q295118) (← links)
- The role of fluid pressure on frictional behavior at the base of the seismogenic zone (Q295573) (← links)
- Constructing constitutive relationships for seismic and aseismic fault slip (Q296173) (← links)