Pages that link to "Item:Q54089"

The following pages link to David A Lockner (Q54089):

Displayed 50 items.

• Physical properties of sidewall cores from Decatur, Illinois (Q57935) ‎ (← links)
• Dependence of frictional strength on compositional variations of Hayward fault rock gouges (Q63695) ‎ (← links)
• Physical properties of two core samples from Well 34-9RD2 at the Coso geothermal field, California (Q67896) ‎ (← links)
• High-pressure rock-physics laboratories investigate earthquake processes (Q70203) ‎ (← links)
• Hayward Fault rocks: porosity, density, and strength measurements (Q73172) ‎ (← links)
• How brucite may affect the frictional properties of serpentinite (Q73239) ‎ (← links)
• Proceedings of the International workshop on the Nojima Fault core and borehole data analysis (Q74554) ‎ (← links)
• Sample characterizations and strength measurements of serpentinite gouges (Q80118) ‎ (← links)
• High-temperature permeability studies; 1, Permeability of granite and novaculite at 300 degrees to 500 degrees C (Q82285) ‎ (← links)
• Laboratory measurements of velocity-dependent frictional strength (Q95467) ‎ (← links)
• A laboratory control system using the PDP 1103 microprocessor (Q110276) ‎ (← 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)
• Rapid acceleration leads to rapid weakening in earthquake-like laboratory experiments (Q147416) ‎ (← links)
• Fault weakening and earthquake instability by powder lubrication (Q148741) ‎ (← links)
• Constraints on the stress state of the San Andreas fault with analysis based on core and cuttings from SAFOD drilling phases 1 and 2 (Q149077) ‎ (← links)
• Data Report: Permeability, porosity, and frictional strength of core samples from IODP Expedition 366 in the Mariana forearc (Q149606) ‎ (← links)
• Observations of quasistatic fault growth from acoustic emissions (Q151811) ‎ (← links)
• An earthquake mechanism based on rapid sealing of faults (Q151903) ‎ (← links)
• Fault growth and acoustic emissions in confined granite (Q152014) ‎ (← links)
• Fracture in Westerly granite under AE feedback and constant strain rate loading: Nucleation, quasi-static propagation, and the transition to unstable fracture propagation (Q152178) ‎ (← links)
• An earthquake instability model based on faults containing high fluid-pressure compartments (Q152447) ‎ (← links)
• Pseudotachylyte increases the post-slip strength of faults (Q152720) ‎ (← links)
• Calibrated acoustic emission system records M -3.5 to M -8 events generated on a saw-cut granite sample (Q153146) ‎ (← links)
• Hydrothermal frictional strengths of rock and mineral samples relevant to the creeping section of the San Andreas Fault (Q153281) ‎ (← links)
• Anisotropic changes in P-wave velocity and attenuation during deformation and fluid infiltration of granite (Q154152) ‎ (← links)
• Why earthquakes correlate weakly with the solid Earth tides: Effects of periodic stress on the rate and probability of earthquake occurrence (Q154277) ‎ (← links)
• Frictional properties of exhumed fault gouges in DFDP-1 cores, Alpine Fault, New Zealand (Q155069) ‎ (← links)
• COMPLEX RESISTIVITY OF FAULT GOUGE AND ITS SIGNIFICANCE FOR EARTHQUAKE LIGHTS AND INDUCED POLARIZATION. (Q155221) ‎ (← links)
• Preslip and cascade processes initiating laboratory stick slip (Q155811) ‎ (← links)
• Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study (Q155869) ‎ (← links)
• Low resistivity and permeability in actively deforming shear zones on the San Andreas Fault at SAFOD (Q155912) ‎ (← links)
• Frictional strength of wet and dry montmorillonite (Q156062) ‎ (← 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)
• Evolution of wear and friction along experimental faults (Q236202) ‎ (← links)
• Deep permeability of the San Andreas Fault from San Andreas Fault Observatory at Depth (SAFOD) core samples (Q236569) ‎ (← links)
• Laboratory generated M -6 earthquakes (Q237221) ‎ (← links)
• Buried shallow fault slip from the South Napa earthquake revealed by near-field geodesy (Q239630) ‎ (← links)
• Comparative deformation behavior of minerals in serpentinized ultramafic rock: Application to the slab-mantle interface in subduction zones (Q242462) ‎ (← links)
• San Andreas Fault Zone mineralogy, geochemistry, and physical properties from SAFOD cuttings and core (Q242466) ‎ (← links)
• Chemical controls on fault behavior: weakening of serpentinite sheared against quartz-bearing rocks and its significance for fault creep in the San Andreas system (Q243290) ‎ (← links)
• Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties (Q247508) ‎ (← links)
• Oscillating load-induced acoustic emission in laboratory experiment (Q247878) ‎ (← links)
• The coefficient of friction of chrysotile gouge at seismogenic depths (Q249079) ‎ (← links)
• Earthquake rupture at focal depth, part II: mechanics of the 2004 M2.2 earthquake along the Pretorius Fault, TauTona Mine, South Africa (Q251227) ‎ (← links)
• The role of adsorbed water on the friction of a layer of submicron particles (Q251271) ‎ (← links)
• Low strength of deep San Andreas fault gouge from SAFOD core (Q251870) ‎ (← links)
• Talc friction in the temperature range 25°–400 °C: relevance for fault-zone weakening (Q252737) ‎ (← links)